Integrated Evaluation of Indoor Particulate Exposure: The VIEPI Project

: Despite the progress made in recent years, reliable modeling of indoor air quality is still far from being obtained. This requires better chemical characterization of the pollutants and airﬂow physics included in forecasting tools, for which ﬁeld observations conducted simultaneously indoors and outdoors are essential. The project “Integrated Evaluation of Indoor Particulate Exposure” (VIEPI) aimed at evaluating indoor air quality and exposure to particulate matter (PM) of humans in workplaces. VIEPI ran from February 2016 to December 2019 and included both numerical simulations and ﬁeld campaigns carried out in universities and research environments located in urban and non-urban sites in the metropolitan area of Rome (Italy). VIEPI focused on the role played by micrometeorology and indoor airﬂow characteristics in determining indoor PM concentration. Short- and long-term study periods captured diurnal, weekly, and seasonal variability of airﬂow and PM concentration. Chemical characterization of PM 10 , including the determination of elements, ions, elemental carbon, organic carbon, and bioaerosol, was also carried out. Large di ﬀ erences in the composition of PM 10 were detected between inside and outside as well as between di ﬀ erent periods of the day and year. Indoor PM composition was related to the presence of people, to the season, and to the ventilation regime.


1.
Micrometeorological and indoor airflow characterization by field experiments and CFD modeling; 2.
Study of the spatio-temporal variability of outdoor ultra-fine particles (UFPs) by means of a land use regression (LUR) model;  3. Measurement and CFD simulation of indoor and outdoor particle number concentration at high time resolution; 4.
Chemical and biological characterization of PM 10 and evaluation of the main PM 10 macro-sources.
In particular, VIEPI was focused on the description of the chemical and biological features of indoor suspended particles in several rooms of a building where many people gather. Great attention has been paid in the literature to school buildings because of the particular vulnerability of children to air pollution [45][46][47], as well as domestic environments [23,[48][49][50]. In contrast, our attention has been paid to universities and research centers, considered as work environments that gather a very large number of students and teachers with seasonal and time slot variability.
The project took place in the Roman area from November 2016 to November 2019. Two sites were considered for the experimental campaigns: the Physics Department of the University of Rome "La Sapienza", and one of the buildings of the Italian Workers' Compensation Authority (INAIL) Research Center, located at Monte Porzio Catone, a small city about 10 km south of Rome. A further goal of VIEPI is to suggest recommendations on the best way to plan indoor field campaigns and to use CFD in indoor environments for air pollution assessment. Specifically, the project has the target of giving useful indications concerning (a) the optimal position of the monitoring stations (meteorological and PM) according to the geometric characteristics of the site and sampling times, (b) optimum data resolution (e.g., acquisition frequency, average period, and time slots), and (c) indications on indoor data analysis.
The objectives of this paper are (i) to give the basic rationale for the project, (ii) to describe the field campaigns, including the instrumentation and problems encountered during the experiments, (iii) to provide a description of the meteorological field that characterized the Roman area during the project, and (iv) to give a few examples of the results achieved so far, which will be further analyzed and discussed in subsequent papers of this special issue.

Sampling Sites and Periods
Experimental field activity within the VIEPI project took place in the greater Rome area (Italy). Two sites were considered: the Physics Department of the Sapienza University of Rome (building Enrico Fermi, Google coordinates: 41 •  The PD, a five-story building covered by a terrace, was chosen because it had a number of features that made it attractive for the main goals of this project. Sapienza University is located in the center of Rome, in a morphologically heterogeneous area with buildings of different heights and shapes. Figure 1 (left picture) shows the University area and the location of the PD building (24 m high) in the southern area of the Campus. There are a number of narrow street canyons on the four sides of the building, including a main road at the south border, characterized by high traffic volumes and vehicular emission. Thermally driven sea-and land-breeze circulations typically develop in the Roman area during periods of weak synoptic forcing [51]. The mountain chains surrounding Rome contribute to the formation of anabatic (daytime) and katabatic (nighttime) winds that normally merge with the breezes for large parts of the year (see, e.g., [52,53]). These factors are conducive to the formation of a well-defined daily wind direction cycle, which deeply affects the outdoor-indoor pressure gradient in correspondence with the PD building. Inside the building, there are a number of classrooms, laboratories, and rooms of different sizes, ranging from a wide lecture hall (about 300 seats) to small offices, which were suitable for investigating the role played by the people in determining indoor air quality and airflow circulation. The sites where the experimental campaigns of the project were carried out are reported in Table 1; the map of the indoor sites is shown in the Supplementary Material ( Figure S1). The lecture hall (LH), located on the ground floor, overlooks both the south and north sides of the PD building and has a double volume compared to classrooms A3, A4, and A7. Classrooms A3 and A4 and the computer room (CR) are located on the same floor. Classroom A3 faces north and looks towards the center of the University Campus. Classroom A4 faces south, over the internal courtyard, and looks towards the border of the Campus and a traffic street, about 50 m away. Both classrooms have identical volume, geometry, and capacity; they have access to an emergency staircase with an outward opening on the east side. During the winter, this door is normally closed and only occasionally opened during breaks; it remains almost systematically opened in the late spring/summer period. The CR faces east over the same courtyard as A4, and is equipped with air conditioners. Classroom A7, located on the fourth floor of the building, is identical to classroom A4. The two laboratories (SL and AL) face the internal courtyard and are also air-conditioned.
At the MPC (Figure 1, right picture), the measurements were carried out inside and outside a meeting room, which was 135 m 3 in volume, and in three smaller offices of 45, 48, and 52 m 3 .
The VIEPI project started on February 2016 and had the duration of 33 months (until November 2019). During this period, a number of experimental studies were carried out at both the PD and MPC sites in order to build a robust database supporting the activities.
Sampling periods within Activity 1 (micrometeorological and indoor airflow characterization by field experiments and CFD modeling) covered the whole duration of the project, with preliminary field studies carried out at the MPC during 2016 and many intensive observation periods run at the PD during the following two years (in the AL during the winter 2017-2018 and in the CR from March 2018 to June 2019). Inside the building, there are a number of classrooms, laboratories, and rooms of different sizes, ranging from a wide lecture hall (about 300 seats) to small offices, which were suitable for investigating the role played by the people in determining indoor air quality and airflow circulation. The sites where the experimental campaigns of the project were carried out are reported in Table 1; the map of the indoor sites is shown in the Supplementary Materials ( Figure S1). The lecture hall (LH), located on the ground floor, overlooks both the south and north sides of the PD building and has a double volume compared to classrooms A3, A4, and A7. Classrooms A3 and A4 and the computer room (CR) are located on the same floor. Classroom A3 faces north and looks towards the center of the University Campus. Classroom A4 faces south, over the internal courtyard, and looks towards the border of the Campus and a traffic street, about 50 m away. Both classrooms have identical volume, geometry, and capacity; they have access to an emergency staircase with an outward opening on the east side. During the winter, this door is normally closed and only occasionally opened during breaks; it remains almost systematically opened in the late spring/summer period. The CR faces east over the same courtyard as A4, and is equipped with air conditioners. Classroom A7, located on the fourth floor of the building, is identical to classroom A4. The two laboratories (SL and AL) face the internal courtyard and are also air-conditioned.
At the MPC (Figure 1, right picture), the measurements were carried out inside and outside a meeting room, which was 135 m 3 in volume, and in three smaller offices of 45, 48, and 52 m 3 .
The VIEPI project started on February 2016 and had the duration of 33 months (until November 2019). During this period, a number of experimental studies were carried out at both the PD and MPC sites in order to build a robust database supporting the activities.
Sampling periods within Activity 1 (micrometeorological and indoor airflow characterization by field experiments and CFD modeling) covered the whole duration of the project, with preliminary field studies carried out at the MPC during 2016 and many intensive observation periods run at the PD Experimental campaigns within Activity 2 (spatio-temporal variability of outdoor UFPs) were carried out for seven consecutive days in November 2017 and in June 2018 in a 1 km × 1 km area surrounding the University Campus and centered on the PD (21 points in the study domain).
Field observations within Activity 3 (indoor and outdoor particle number concentration) consisted of four intensive periods during both winter and summer in order to capture different weather conditions and conditions of use of indoor environments typical of the cold and warm seasons (November-December 2017, June 2018, November-December 2018, June 2019). They were carried out in LH, CR, A3, A4, and A7. Activity 4 (aerobiological particles) was carried out at the MPC with some preliminary monitoring periods during the period June 2016-July 2017 and, continuously, at the PD from November 2017 to November 2018.
In the framework of Activity 5 (chemical and biological characterization of PM 10 ), two types of field studies were conducted. The first one (short-term intensive campaigns) was carried out during three periods: November-December 2017, June 2018, and November-December, 2018. PM 10 samples were simultaneously collected at five indoor sites (LH, CR, A4, SL, and A7) and outdoors (on the ground floor). The sampling schedule was designed to obtain five samples a week: two during lesson times (from 09:00 to 18:00 local standard time, LST), two during the evening/night, when the rooms were empty (from 18:00 to 09:00 LST of the following day), and one during the weekend. The second type of study (long-term campaign) was continuously carried out from November 2017 to October 2018, with 12 sampling periods of the duration of one month. Indoor sampling sites were in LH, CR, A3, A4, SL, and A7. Each sampling was simultaneously performed indoors and outdoors, out of the window and at the same height from the ground. Measurements of both PM 10 and PM 2.5 were carried out. Two additional outdoor sampling points were set on the roof of the PD building and the roof of another building that was about 50 m away.

Activity 1: Micrometeorological and Indoor Airflow Characterization by Field Experiments and CFD Modeling
Wind velocity and air temperature were measured both inside and outside the PD building. In particular, one sonic anemometer/thermometer (Gill Instruments Limited, Lymington, UK, acquisition frequency of 32 Hz) was mounted on a 3.5 m mast located on the terrace (i.e., z = 1.14H, where z is the height), while two sonic anemometers (Gill Instruments Limited, 4 Hz) were mounted on a metallic brace 80 cm outside one of the windows on the second and fifth floor, in correspondence with the CR and AR (Figure 2). Two sensors of differential pressure (Delta Ohm, Caselle di Salvazzano, Italy, 1 Hz) were installed on the same windows to collect outdoor-indoor pressure differences. The pressure differences between the two rooms and the corresponding hallways were measured by means of two other differential pressure sensors. Indoor measurements of velocity and temperature were collected in the CR and AL by means of two sonic thermometer/anemometers (Gill Instruments Limited, 20 Hz). In addition, a triaxial monostatic Doppler SODAR (Sonic Detection and Ranging) system (APM-301) located on the terrace permitted investigations of the three components of the wind velocity up to an altitude of about 200 m with approximately 7.5 m vertical resolution (see [54,55] for details). The SODAR belongs to the BAQUNIN (Boundary-layer Air Quality analysis Using a Network of Instruments, https://www.baqunin.eu/) super-site urban location. BAQUNIN also hosts an elastic LIDAR (Light Detection and Ranging) through which it is possible to retrieve vertical aerosol profiles for a large part of the troposphere (spatial and temporal resolution: 7.5 m and 10 s, respectively) and the planetary boundary layer (PBL) height [56,57].
The CFD software ANSYS Fluent 18.2 [58] was employed to simulate airflow and PM dispersion for several case studies.

Activity 2: Spatio-Temporal Variability of Outdoor UFPs
Spatio-temporal generalized additive models (GAMs) were developed to describe the spatiotemporal variability of the ultrafine particles (UFPs) at the microscale level and to identify the main descriptors of such variability. The total monitored particle number concentration (PNC, as a proxy of the UFPs) data were used as response variable. The 21 points of the study domain were chosen so as to obtain measurements representative of the maximum spatial gradient of detectable concentration in the area, assuming the road traffic to be the main source of UFPs in the urban context.
The PNC measurements were made using portable condensation particle counters (3007 TSI) for one week (10 min for each site, three times a day), following paths characterizing the area of study ( Figure 3): route A (blue) University Campus; route B (red) external perimeter of the University Campus; route C (green): San Lorenzo district.
Due to the large number of measurement sites along with the limited number of available devices (four), a rounding measurement strategy was adopted, sharing devices among monitoring sites. Geographic information system (GIS) analyses were conducted to derive the spatial variables at each monitoring site. The set of spatial predictors included the traffic intensity, distance to the nearest local and major roads and their various combinations, total length of major and local roads, land cover variables (high-density residential land, low-density residential land, commercial and public urban areas, urban green), and population density, all calculated in several small circular buffers.
To represent the height and the continuity of street canyons, four variables for buildings and/or street configurations were designed. In addition, a triaxial monostatic Doppler SODAR (Sonic Detection and Ranging) system (APM-301) located on the terrace permitted investigations of the three components of the wind velocity up to an altitude of about 200 m with approximately 7.5 m vertical resolution (see [54,55] for details). The SODAR belongs to the BAQUNIN (Boundary-layer Air Quality analysis Using a Network of Instruments, https://www.baqunin.eu/) super-site urban location. BAQUNIN also hosts an elastic LIDAR (Light Detection and Ranging) through which it is possible to retrieve vertical aerosol profiles for a large part of the troposphere (spatial and temporal resolution: 7.5 m and 10 s, respectively) and the planetary boundary layer (PBL) height [56,57].
The CFD software ANSYS Fluent 18.2 [58] was employed to simulate airflow and PM dispersion for several case studies.

Activity 2: Spatio-Temporal Variability of Outdoor UFPs
Spatio-temporal generalized additive models (GAMs) were developed to describe the spatio-temporal variability of the ultrafine particles (UFPs) at the microscale level and to identify the main descriptors of such variability. The total monitored particle number concentration (PNC, as a proxy of the UFPs) data were used as response variable. The 21 points of the study domain were chosen so as to obtain measurements representative of the maximum spatial gradient of detectable concentration in the area, assuming the road traffic to be the main source of UFPs in the urban context.
The PNC measurements were made using portable condensation particle counters (3007 TSI) for one week (10 min for each site, three times a day), following paths characterizing the area of study ( Figure 3  The temporal variables acquired for use as potential predictors were meteorological parameters (wind speed and direction, air temperature, relative humidity, pressure, precipitation, global solar radiation) and micrometeorological parameters (standard deviation of the horizontal and vertical wind speed module, turbulent kinetic energy, z/L stability parameter (L is the Obukhov length), and atmospheric stability classes) (Pasquill-Gifford). Moreover, only during the summer period, the PBL height was calculated by vertical aerosol profiles measured using LIDAR combined with SODAR data.

Activity 3: Indoor and Outdoor Particle Number Concentration
Total particle number concentration (TPNC) was simultaneously measured indoors and outdoors by using co-located condensation particle counters (CPC3007, TSI Inc., Shoreview, MN, USA, min detectable particle (D50): 10 nm, time resolution: 1 s). In the CR and LH, at the same time as the aforementioned measurements, size-resolved PNC measurements were carried out to study the temporal variability of the dimensional distribution in number of particles from 10 nm to 10 µm using a scanning mobility particle sizer and optical particle sizer (SMPS 3910, Fast Mobility Particle Sizes (FMPS) mod. 3091, OPS 3330 TSI Inc., Shoreview, MN, USA). Moreover, measurements of the average and cumulative lung-deposited surface area (LDSA, in µm 2 /cm 3 ) of particles from 10 nm to 1 µm, corresponding to the tracheobronchial or alveolar pulmonary fractions, were carried out by using a nanoparticle surface area monitor (NSAM mod. 3550, TSI Inc., Shoreview, MN, USA; 1 s time resolution). Additional measurements also included: PNC (#/cm 3 ), average diameter (nm), and LDSA (µm 2 /cm 3 ) with a time resolution of 1 s by a mini diffusion size classifier (DM-UF5, mod. TESTO), size distribution (dN/dLogDp) and TPNC (#/cm 3 ) in the size range of 6 nm-10 µm, with 1 s time resolution using an electric low-pressure impactor (ELPI+, mod. Dekati), and polycyclic aromatic hydrocarbons (PAHs) surface-adsorbed on carbon aerosol in the size range 10 nm-1.5 µm using a photoelectric aerosol sensor (PAS2000, EcoChem Analytics, League City, TX, USA).

Activity 4: Aerobiological Particles
Aerobiological particles 10-100 µm in diameter were collected in compliance with the UNI 11108/2004 [59] and following UNI CEN/TS 16868:2015 [60] using a seven-day volumetric Hirst type sampler (Lanzoni VPPS ® 2000, Bologna, Italy). The sampling method is based on the impact of particles on a surface consisting of a transparent plastic Melinex ® (TEKRA LLC., New Berlin, WI, USA) tape coated with a 2% silicon solution. The tape moves with a speed of 2 mm per hour on a cylindrical drum that makes a complete round in a week. Air sucking is provided by a vacuum pump operating at the flowrate of 10 L/min, matching the human breathing rate. The system is tailed directionally, allowing it to be continually oriented against the wind. The outdoor sampler is placed at a standard height of about 15-20 m from the ground; in these conditions, it is able to monitor an Due to the large number of measurement sites along with the limited number of available devices (four), a rounding measurement strategy was adopted, sharing devices among monitoring sites. Geographic information system (GIS) analyses were conducted to derive the spatial variables at each monitoring site. The set of spatial predictors included the traffic intensity, distance to the nearest local and major roads and their various combinations, total length of major and local roads, land cover variables (high-density residential land, low-density residential land, commercial and public urban areas, urban green), and population density, all calculated in several small circular buffers.
To represent the height and the continuity of street canyons, four variables for buildings and/or street configurations were designed.
The temporal variables acquired for use as potential predictors were meteorological parameters (wind speed and direction, air temperature, relative humidity, pressure, precipitation, global solar radiation) and micrometeorological parameters (standard deviation of the horizontal and vertical wind speed module, turbulent kinetic energy, z/L stability parameter (L is the Obukhov length), and atmospheric stability classes) (Pasquill-Gifford). Moreover, only during the summer period, the PBL height was calculated by vertical aerosol profiles measured using LIDAR combined with SODAR data.

Activity 3: Indoor and Outdoor Particle Number Concentration
Total particle number concentration (TPNC) was simultaneously measured indoors and outdoors by using co-located condensation particle counters (CPC3007, TSI Inc., Shoreview, MN, USA, min detectable particle (D50): 10 nm, time resolution: 1 s). In the CR and LH, at the same time as the aforementioned measurements, size-resolved PNC measurements were carried out to study the temporal variability of the dimensional distribution in number of particles from 10 nm to 10 µm using a scanning mobility particle sizer and optical particle sizer (SMPS 3910, Fast Mobility Particle Sizes (FMPS) mod. 3091, OPS 3330 TSI Inc., Shoreview, MN, USA). Moreover, measurements of the average and cumulative lung-deposited surface area (LDSA, in µm 2 /cm 3 ) of particles from 10 nm to 1 µm, corresponding to the tracheobronchial or alveolar pulmonary fractions, were carried out by using a nanoparticle surface area monitor (NSAM mod. 3550, TSI Inc., Shoreview, MN, USA; 1 s time resolution). Additional measurements also included: PNC (#/cm 3 ), average diameter (nm), and LDSA (µm 2 /cm 3 ) with a time resolution of 1 s by a mini diffusion size classifier (DM-UF5, mod. TESTO), size distribution (dN/dLogDp) and TPNC (#/cm 3 ) in the size range of 6 nm-10 µm, with 1 s time resolution using an electric low-pressure impactor (ELPI+, mod. Dekati), and polycyclic aromatic hydrocarbons (PAHs) surface-adsorbed on carbon aerosol in the size range 10 nm-1.5 µm using a photoelectric aerosol sensor (PAS2000, EcoChem Analytics, League City, TX, USA). . The sampling method is based on the impact of particles on a surface consisting of a transparent plastic Melinex ® (TEKRA LLC., New Berlin, WI, USA) tape coated with a 2% silicon solution. The tape moves with a speed of 2 mm per hour on a cylindrical drum that makes a complete round in a week. Air sucking is provided by a vacuum pump operating at the flowrate of 10 L/min, matching the human breathing rate. The system is tailed directionally, allowing it to be continually oriented against the wind. The outdoor sampler is placed at a standard height of about 15-20 m from the ground; in these conditions, it is able to monitor an area of about 15 km radius. The Hirst sampler is designed to detect the atmospheric concentration of biocontaminants, such as pollen and fungal spores, using morphological recognition. Following a weekly air monitoring, the stripes are cut into daily segments, placed on single glass slides, stained using glycerine jelly with fuchsine, and then observed with an optical microscope (magnification: 40×) for the count and characterization of pollen and fungal spores [61].

Short-Term Intensive Campaigns
In each room and at the outdoor site, we set three PM 10 samplers. Given the necessity to avoid any inconvenience to teaching and research, we used very quiet samplers (<35 dB) specifically designed for use in indoor environments (Silent Sequential Sampler, FAI Instruments, Fonte Nuova, Rome, Italy) operating at the flow rate of 10 L min −1 . Each sampler was equipped with a sequential system able to run four sampling lines without attendance. Outdoors, each sampling line was provided with a cap to protect the inlet from wind and rain.
Teflon filters were used for the determination of PM 10 mass concentration by gravimetry, using an automated microbalance (mod. ME5, 1 µg sensitivity; Sartorius AG, Goettingen, Germany), after conditioning at 50% Relative Humidity and 20 • C for 48 h. Then they were analyzed using energy-dispersion X-ray fluorescence (X-Lab 2000 and XEPOS, Spectro Analytical Instruments, Kleve, Germany) for the contents of Si, Al, Fe, Na, K, Mg, Ca, and minor elements. Then, the filters were extracted in deionized water and analyzed for ions (chloride, nitrate, sulfate, sodium, potassium, ammonium, magnesium, and calcium) by ion chromatography (ICS1000, Dionex Co., Sunnyvale, CA, USA). Finally, the soluble and residual fractions of 23 elements were analyzed by sequential extraction and inductively coupled plasma mass spectrometry (ICP-MS, Bruker 820 MS, Billerica, MA, USA). This overall procedure, which allows a high number of analytical determinations on the same filter, is described in detail in [23,62,63].
The determination of the organic and elemental carbon was carried out on quartz filters using thermo-optical analysis (OCEC Carbon Aerosol Analyzer, Sunset Laboratory, Tigard, OR, USA) and the NIOSH-QUARTZ thermal protocol. Samples collected in the A4, CR, and outdoors were also analyzed for the content of eight carcinogenic and mutagenic congeners of polycyclic aromatic hydrocarbons (PAHs) included in the Environmental Protection Agency priority list: benzo(a)anthracene (BaA), benzo(b)fluoranthene, benzo(j)fluoranthene, benzo(k)fluoranthene (BbjkF), benzo(a)pyrene (BaP), indeno(1,2,3-cd)pyrene (IP), dibenzo(a,h)anthracene (DBahA), and benzo(g,h,i)perylene (BPE). They were extracted from the quartz membrane using sonication with dichloromethane/acetone sequence and concentrated. The obtained low-volume samples were analyzed by using a gas chromatograph (6890N Agilent Technologies, Santa Clara, CA, USA) equipped with a mass-selective detector (5973N Sustainability 2020, 12, 9758 9 of 25 Agilent Technologies). The validation of the analytical method was carried out according to the guidelines given by the EURACHEM (1998) by using the certified urban dust (SRM 1649a), which was purchased from the National Institute of Standards and Technology (NIST) (Gaithersburg, MD, USA).
Polycarbonate filters were used for the evaluation of the bio-aerosol content by a method involving propidium-iodide staining, optical microscopy observation, image processing, and calculation of the mass concentration. Details of the procedure are described in [64].
Outdoors, we also added a dual-channel beta attenuation monitor (and sampler) operating at the flow rate of 2.3 m 3 /h, compliant with the requirements of the regulations about outdoor PM measurement (SWAM 5a Dual Channel Monitor, FAI Instruments, Fonte Nuova, Rome, Italy). The monitor was equipped with Teflon and quartz filters and was operated on a 24 h basis. The samples were analyzed for the same species and by following the same analytical methods described above.

Long-Term Campaign
In this case, we used very low flow-rate samplers (Smart Sampler, FAI Instruments-Roma, Italy) operating at the flow rate of 0.5 L/min. Four samplers were placed in each indoor and outdoor site. Three of them were devoted to PM 10 measurement and equipped with Teflon, quartz, and polycarbonate filters, respectively. The fourth one was fitted with a Teflon filter and a PM 2.5 impactor to obtain more information about the size distribution of PM components and the dependence of infiltration on particle size.

Quality Control
The particle counters and particle sizers were calibrated in the factory before each one of the two sampling campaigns using monodisperse artificial aerosol. Moreover, in the cases of both particle counters and meteorological instruments, during the project, we adopted a Quality Control procedure consisting of devoting one day before the start of each experimental campaign to the inter-calibration of the instruments and comparison of the obtained experimental results.
The flow rate of the indoor PM 10 samplers was checked once a week by using an external mass flow meter. The dual-channel monitor used for outdoor PM 10 sampling was subjected to an internal span check and leak test procedure that was run daily before the start of each sampling period.
The overall analytical method applied to the chemical characterization of PM 10 has been widely validated in previous studies. A detailed discussion of the applied Quality Assurance/Quality Control procedure is reported in [62].

Activity 1: Main Characteristics of the Outdoor Airflow
The near-surface wind field observed during VIEPI activities was in line with what was found in previous studies concerning meteorological analysis conducted in the Roman urban area (e.g., [65,66]). During the spring, summer, and autumn, the wind was mostly oriented along the southwest-northeast axis as a result of the diurnal wind cycle caused by the sea-land-breeze regime characterizing the region (see Figure S2 in the Supplementary Materials). Figure 4 shows the scatter plot of the wind direction as a function of the time of day in which the measurement took place during April 2018 by the SODAR and by the three anemometers installed outside the PD building. The diurnal behavior of the wind direction shows a marked day-to-night variation both above the building (z = 1.4H and z = 1.14H) and within the canyon (z = 0.8H), even though in the latter case, the wind speed is considerably lower. At all three locations, it is possible to recognize two distinct clusters in the wind direction pattern. One is concentrated between south and west from 12:00 to 20:00 LST, and the second between north and east from 20:00 LST to 12:00 LST. Note that the nocturnal regime at z = 0.8H appears more concentrated in the north-northeast sector. This is reasonable in that the façade where the sonic anemometers are installed is oriented nearly 20 • from north (see Figures 1 and 2). Even more pronounced effects of the façade's orientation on the wind direction are observed on the second floor (z = 0.4H), where two much narrower clusters (southwest and north-northwest), are present irrespective of the time of day. The wind, therefore, is parallel to the façade regardless of the wind direction above the terrace. However, it is worthwhile to remember that wind speed and direction over building walls change considerably with height and approaching wind direction, even for building arrangements much simpler than the one considered in the present case (e.g., [67,68]).
Additional information on the flow field with respect to the PD building was also inferred from CFD. This tool has become attractive at the microscale because of its ability to simulate airflows for real building arrangements, complex scenarios, and different research fields (e.g., [69][70][71]). ANSYS Fluent 18.2 was used, adopting the standard k-ε turbulence closure based on the 3D Reynoldsaveraged Navier-Stokes (RANS) equations. The computational domain and grid (see Figure S3 in the Supplementary Materials) were set according to the guidelines [72,73].
The numerical simulation refers to 16:00 LST on 21 April 2018. The idea behind this is that in the area of interest, in case of clear skies and weak synoptic forcing, the wind direction in the afternoon is fairly constant for several hours due to the breeze regime (nearly from southwest). This simplifies the analysis and facilitates the comparison between numerical and experimental results. A logarithmic wind-speed profile based on data taken from the meteorological station located at G.B. Pastine Airport in Ciampino, about 10 km southeast of Rome, was imposed at the inlet. Figure 5 (left panel) shows the contour map of the wind speed simulated on the horizontal plane at z = 0.4H (second floor). The flow pattern shows high complexity and inhomogeneities. The wind comes from southwest and is deflected by the features located upstream of the PD building. The velocity is higher in the streets corresponding with the west and south façades, whereas it is considerably lower (about 0.7 ms −1 ) in the canyon on the east side (i.e., between the PD building and the adjacent Chemistry Department). The corresponding pressure field ( Figure 5, right panel) shows that between the PD façades, the maximum differential pressure is about 0.75 Pa. This value is large enough to generate an indoor airflow from the west to the east façade. It is worthwhile to mention that the indoor/outdoor differential pressure measured at z = 0.4H is nearly approximately 0.7 Pa. However, note that the pressure distribution over building walls is expected to change considerably with the approaching wind direction (e.g., [74]). Consequently, the use of wind-speed data measured Even more pronounced effects of the façade's orientation on the wind direction are observed on the second floor (z = 0.4H), where two much narrower clusters (southwest and north-northwest), are present irrespective of the time of day. The wind, therefore, is parallel to the façade regardless of the wind direction above the terrace. However, it is worthwhile to remember that wind speed and direction over building walls change considerably with height and approaching wind direction, even for building arrangements much simpler than the one considered in the present case (e.g., [67,68]).
Additional information on the flow field with respect to the PD building was also inferred from CFD. This tool has become attractive at the microscale because of its ability to simulate airflows for real building arrangements, complex scenarios, and different research fields (e.g., [69][70][71]). ANSYS Fluent 18.2 was used, adopting the standard k-ε turbulence closure based on the 3D Reynolds-averaged Navier-Stokes (RANS) equations. The computational domain and grid (see Figure S3 in the Supplementary Materials) were set according to the guidelines [72,73].
The numerical simulation refers to 16:00 LST on 21 April 2018. The idea behind this is that in the area of interest, in case of clear skies and weak synoptic forcing, the wind direction in the afternoon is fairly constant for several hours due to the breeze regime (nearly from southwest). This simplifies the analysis and facilitates the comparison between numerical and experimental results. A logarithmic wind-speed profile based on data taken from the meteorological station located at G.B. Pastine Airport in Ciampino, about 10 km southeast of Rome, was imposed at the inlet. Figure 5 (left panel) shows the contour map of the wind speed simulated on the horizontal plane at z = 0.4H (second floor). The flow pattern shows high complexity and inhomogeneities. The wind comes from southwest and is deflected by the features located upstream of the PD building. The velocity is higher in the streets corresponding with the west and south façades, whereas it is considerably lower (about 0.7 ms −1 ) in the canyon on the east side (i.e., between the PD building and the adjacent Chemistry Department). The corresponding pressure field ( Figure 5, right panel) shows that between the PD façades, the maximum differential pressure is about 0.75 Pa. This value is large enough to generate an indoor airflow from the west to the east façade. It is worthwhile to mention that the indoor/outdoor differential pressure measured at z = 0.4H is nearly approximately 0.7 Pa. However, note that the pressure distribution over building walls is expected to change considerably with the approaching wind direction (e.g., [74]). Consequently, the use of wind-speed data measured on the terrace is often useless for the purpose of calculating the pressure acting on the walls of buildings.
Sustainability 2020, 12, x FOR PEER REVIEW 11 of 25 on the terrace is often useless for the purpose of calculating the pressure acting on the walls of buildings. The vector field of the wind speed over the vertical plane perpendicular to the east façade (passing through the point where the sonic anemometer on the second floor is located) shows the well-defined vortical structure typically observed in canyon flows (e.g., [75,76]), i.e., a current descending in the portion close to the Chemistry Department and ascending near PD ( Figure S4 in the Supplementary Materials). That kind of structure is usually responsible for the transport and dispersion of pollutants emitted at street level, which can thus reach the highest floors of the building [77].
The agreement between modeled and observed horizontal velocity is rather good above the building (z = 1.4H and z = 1.14H) and reasonable at z = 0.4H, whereas the error is larger at z = 0.8H (Table S1 in the Supplementary Materials). Therefore, the model does not reproduce the turbulence structures within the canyon very well, even if the mesh has been refined near the walls. We should also consider the fact that the shape, size, and direction of rotation of vortical structures within canyons depend considerably on the angle between the approaching flow and canyon axis (e.g., [78][79][80]). Moreover, non-stationarities intrinsic of the real approaching flow make the agreement between observation and simulation very challenging within the canyon.

Activity 2: Spatio-Temporal Variability of Outdoor UFPs
The PNC was the response variable used to assess the spatio-temporal variability of outdoor UFPs using GAM models. Here, we show the results of the monitoring campaigns, while the calculation of the main parameters for urban morphology description and the development and validation of a land use regression (LUR) model for PNC estimation will be reported elsewhere.
The chosen sites were characterized with respect to the main local source (i.e., road traffic) using both distance from the nearest road and traffic flow therein. They potentially allowed us to catch a large portion of microscale spatial variability, since the median of the ratios of traffic flow by distance ranged between 0.2 and 280 vehicle h −1 m −1 . Figure 6 shows average PNC values at the measurement points selected in the study area. The PNC recorded in the university area (A1-A6, cars allowed for restricted personnel only) were significantly lower than those observed in the two external routes (PNCA1-A6 = 13,724 part/cm 3 and PNCA1-A6 = 19,645 part/cm 3 , respectively). The points close to roads with high traffic flows were points B1, B2, B3, B4, B5 (quadrilateral outside the university), C1, C3, and C7 (on Via Tiburtina, the main busy road). The average concentrations in points B6, C2, and C6, relatively far from the busiest roads, are comparable in both seasons with those of the sites within the University Campus (PNCB6-C1-C6 = 12,959 part/cm 3 and PNCA1-A6 = 13,724 part/cm 3 , respectively). The vector field of the wind speed over the vertical plane perpendicular to the east façade (passing through the point where the sonic anemometer on the second floor is located) shows the well-defined vortical structure typically observed in canyon flows (e.g., [75,76]), i.e., a current descending in the portion close to the Chemistry Department and ascending near PD ( Figure S4 in the Supplementary Materials). That kind of structure is usually responsible for the transport and dispersion of pollutants emitted at street level, which can thus reach the highest floors of the building [77].
The agreement between modeled and observed horizontal velocity is rather good above the building (z = 1.4H and z = 1.14H) and reasonable at z = 0.4H, whereas the error is larger at z = 0.8H (Table S1 in the Supplementary Materials). Therefore, the model does not reproduce the turbulence structures within the canyon very well, even if the mesh has been refined near the walls. We should also consider the fact that the shape, size, and direction of rotation of vortical structures within canyons depend considerably on the angle between the approaching flow and canyon axis (e.g., [78][79][80]). Moreover, non-stationarities intrinsic of the real approaching flow make the agreement between observation and simulation very challenging within the canyon.

Activity 2: Spatio-Temporal Variability of Outdoor UFPs
The PNC was the response variable used to assess the spatio-temporal variability of outdoor UFPs using GAM models. Here, we show the results of the monitoring campaigns, while the calculation of the main parameters for urban morphology description and the development and validation of a land use regression (LUR) model for PNC estimation will be reported elsewhere.
The chosen sites were characterized with respect to the main local source (i.e., road traffic) using both distance from the nearest road and traffic flow therein. They potentially allowed us to catch a large portion of microscale spatial variability, since the median of the ratios of traffic flow by distance ranged between 0.2 and 280 vehicle h −1 m −1 . Figure 6 shows average PNC values at the measurement points selected in the study area. The PNC recorded in the university area (A1-A6, cars allowed for restricted personnel only) were significantly lower than those observed in the two external routes (PNC A1-A6 = 13,724 part/cm 3 and PNC A1-A6 = 19,645 part/cm 3 , respectively). The points close to roads with high traffic flows were points B1, B2, B3, B4, B5 (quadrilateral outside the university), C1, C3, and C7 (on Via Tiburtina, the main busy road). The average concentrations in points B6, C2, and C6, relatively far from the busiest roads, are comparable in both seasons with those of the sites within the University Campus (PNC B6-C1-C6 = 12,959 part/cm 3 and PNC A1-A6 = 13,724 part/cm 3 , respectively).
While several studies attempted to assess the spatial variability of PNC and other pollutants at the local/urban scale through statistical modeling based on dense monitoring in a wide spatial domain (e.g., [81][82][83][84]), only a few studies have addressed whether the spatial variation of particle number concentration (PNC) within a microscale environment can have an effect on exposure estimation results (e.g., [85]).
Vehicle emissions clearly increase background particle concentrations. In particular, UFPs are characterized by a sharp spatial decline from the emission sources, since they are removed through coagulation processes. Thus, it is expected that nearby traffic load and distance from major roads could be relevant explanatory variables for UFPs' spatial pattern, together with land use variables (e.g., population density, urban green). The monitoring results allow us to confirm the large spatial variability of PNC still existing on the microscale (here, 1 km × 1 km), likely leading to significant differences in exposure pattern. This should be taken into account when assessment of indoor to outdoor ratios is carried out using a single or a few fixed outdoor sites in the study area. Moreover, the spatial variability needs to be further investigated, since, other than the relative distance to traffic, the urban morphology can be a relevant factor explaining such variability.
The excellent linear correlation between the average PNC recorded at each site during winter vs. PNC during summer (R 2 = 0.86) accounts for the fact that the spatial gradient in the domain under examination is comparable in the two seasons. Moreover, a clear daily pattern was found: maxima were found during winter rush hours (early morning and mid/late afternoon) that are often coincident with the lowest mixing height observed during the daylight hours.
During winter, the morning and evening PNC peaks at rush hours can be considered the result of the motor vehicle emissions combined with a lower diurnal mixing layer height and lower ambient temperature, which favors nucleation mechanisms, at least for particles with dimensions up to some tenths of a nanometer (e.g., [88]).
The morning peak still present in summer months might be related predominantly to particles directly emitted by road traffic. The more favorable diurnal conditions for atmospheric dispersion during the warm season lead to lower absolute values of PNC.

Activity 3: Indoor and Outdoor Particle Number Concentration
To assess the possible observable differences between classrooms located on the same floor, but with different orientation of the windows with respect to the outside, three classrooms were selected: While several studies attempted to assess the spatial variability of PNC and other pollutants at the local/urban scale through statistical modeling based on dense monitoring in a wide spatial domain (e.g., [81][82][83][84]), only a few studies have addressed whether the spatial variation of particle number concentration (PNC) within a microscale environment can have an effect on exposure estimation results (e.g., [85]).
Vehicle emissions clearly increase background particle concentrations. In particular, UFPs are characterized by a sharp spatial decline from the emission sources, since they are removed through coagulation processes. Thus, it is expected that nearby traffic load and distance from major roads could be relevant explanatory variables for UFPs' spatial pattern, together with land use variables (e.g., population density, urban green).
The monitoring results allow us to confirm the large spatial variability of PNC still existing on the microscale (here, 1 km × 1 km), likely leading to significant differences in exposure pattern. This should be taken into account when assessment of indoor to outdoor ratios is carried out using a single or a few fixed outdoor sites in the study area. Moreover, the spatial variability needs to be further investigated, since, other than the relative distance to traffic, the urban morphology can be a relevant factor explaining such variability.
The excellent linear correlation between the average PNC recorded at each site during winter vs. PNC during summer (R 2 = 0.86) accounts for the fact that the spatial gradient in the domain under examination is comparable in the two seasons. Moreover, a clear daily pattern was found: maxima were found during winter rush hours (early morning and mid/late afternoon) that are often coincident with the lowest mixing height observed during the daylight hours.
During winter, the morning and evening PNC peaks at rush hours can be considered the result of the motor vehicle emissions combined with a lower diurnal mixing layer height and lower ambient temperature, which favors nucleation mechanisms, at least for particles with dimensions up to some tenths of a nanometer (e.g., [88]).
The morning peak still present in summer months might be related predominantly to particles directly emitted by road traffic. The more favorable diurnal conditions for atmospheric dispersion during the warm season lead to lower absolute values of PNC.

Activity 3: Indoor and Outdoor Particle Number Concentration
To assess the possible observable differences between classrooms located on the same floor, but with different orientation of the windows with respect to the outside, three classrooms were selected: A3, A4, and CR, all located on floor 2 (Supplementary Materials, Figure S1). To evaluate the possible observable differences between classrooms located at different heights from the ground, two classrooms were selected: LH and A7. The measurement campaigns were carried out in different seasonal periods in order to capture different weather conditions and conditions of use of indoor environments typical of cold and warm seasons.
Descriptive statistics (Tables 2 and 3) are reported for both the horizontal and vertical gradient assessments.  A clear seasonal pattern was found linked both to different ways of classroom use and meteorological conditions. In June, classrooms were occupied rather discontinuously, with alternating periods of zero or very limited occupation and periods of greater crowding. The prevailing ventilation conditions were those typical of the summer period (natural ventilation with open doors and windows; air conditioners turned on in LH and CR). During winter, the scenario was radically different: systematic occupation of the classrooms with a succession of teaching activities without interruption from 08:00 to 18:00 LST on most days. However, since particularly cold days did not occur, it was often observed that the upper doors directly opening to the outside were open.
Concerning indoor measurements, the horizontal gradient showed very similar PNC values between the two sides, with the same modulation in summer and slightly higher concentrations in the classroom on the street side. As regards the indoor vertical gradient, the PNC values were higher in the classroom on the fourth floor than in the LH on the ground floor, but this difference is influenced by the different geometries and uses of the considered classrooms rather than by the altitude relative to the ground.
As for external measurements, in the comparison between the two measurement points on the north and south sides of the same floor, the PNC levels were very similar and with the same modulation, with slightly higher concentrations on the road side. The comparison between the outdoor measurements on the ground floor and on the fourth floor shows higher PNC values at the lowest level, with excellent correlation between the two time series.
The preliminary results related to the autumn-winter campaign have been reported in Boccuni et al. [89]. Data of PNC and particle size distribution (PSD) measured by FMPS for airborne UFPs in the size range 5.6-560 nm were collected during a working week at three different heights. Nighttime measurements were also performed to include non-working activities.
In general, the average daily trends (Figure 7) suggested that multiple factors influenced UFPs' PNC levels, probably related to both outdoor and indoor contributions. In particular, at the beginning of the day, in the transition hours (from 05:00 to 07:00 LST), we noted an increase in outdoor UFPs' PNC, probably due to the starting of anthropic activities; the indoor values reflect the same structure with a certain delay time. During the daylight hours (from 07:00 to 16:00 LST), the outside component outnumbers the influences from other internal sources of PNC. In the transition from daylight hours to the night (from 16:00to 18:00 LST), a general increase of PNC in indoor sampling points was mainly recognized. The outdoor average daily trends of UFPs' PNC confirm the daily profiles of population mobility indicators already proposed by [90] for the city of Rome in their study on urban population mobility using mobile phone traffic data. Concerning indoor measurements, the horizontal gradient showed very similar PNC values between the two sides, with the same modulation in summer and slightly higher concentrations in the classroom on the street side. As regards the indoor vertical gradient, the PNC values were higher in the classroom on the fourth floor than in the LH on the ground floor, but this difference is influenced by the different geometries and uses of the considered classrooms rather than by the altitude relative to the ground.
As for external measurements, in the comparison between the two measurement points on the north and south sides of the same floor, the PNC levels were very similar and with the same modulation, with slightly higher concentrations on the road side. The comparison between the outdoor measurements on the ground floor and on the fourth floor shows higher PNC values at the lowest level, with excellent correlation between the two time series.
The preliminary results related to the autumn-winter campaign have been reported in Boccuni et al. [89]. Data of PNC and particle size distribution (PSD) measured by FMPS for airborne UFPs in the size range 5.6-560 nm were collected during a working week at three different heights. Nighttime measurements were also performed to include non-working activities.
In general, the average daily trends (Figure 7) suggested that multiple factors influenced UFPs' PNC levels, probably related to both outdoor and indoor contributions. In particular, at the beginning of the day, in the transition hours (from 05:00 to 07:00 LST), we noted an increase in outdoor UFPs' PNC, probably due to the starting of anthropic activities; the indoor values reflect the same structure with a certain delay time. During the daylight hours (from 07:00 to 16:00 LST), the outside component outnumbers the influences from other internal sources of PNC. In the transition from daylight hours to the night (from 16:00to 18:00 LST), a general increase of PNC in indoor sampling points was mainly recognized. The outdoor average daily trends of UFPs' PNC confirm the daily profiles of population mobility indicators already proposed by [90] for the city of Rome in their study on urban population mobility using mobile phone traffic data. The study in the spring on 19-21 June 2018 confirmed that FMPS and DM-UF5 at z/H = 1.1 are linearly correlated. They are also sensitive in monitoring different particle-size distributions. The best correlation between the two instruments was achieved at nighttime, when a steady state can be assumed for the contributions of meteorological conditions and sources, which are suitable for proper measurement either by FMPS or DM ( Figure S5   The study in the spring on 19-21 June 2018 confirmed that FMPS and DM-UF5 at z/H = 1.1 are linearly correlated. They are also sensitive in monitoring different particle-size distributions. The best correlation between the two instruments was achieved at nighttime, when a steady state can be assumed for the contributions of meteorological conditions and sources, which are suitable for proper measurement either by FMPS or DM ( Figure S5 in the Supplementary Materials). During this period, the daily PNC vertical gradient was positive, equal to about 170 (#/cm 3 )/m.

Activity 4: Aerobiological Particles
The results of the preliminary campaigns seem to indicate an increase of aerobiological particle concentrations during working hours in relation to workers' presence and behavior. Workers interact continuously with the indoor environment to realize their thermal and physiological comfort (window and door opening/closing or turning off ventilation), as shown in Table 4. The preliminary results were obtained through aerobiological monitoring in the MPC, that is, an area characterized by the Holm oak range, which consists of mixed oak woods with Quercus ilex and deciduous trees, with prevalence of cultivated species such as Olea europaea and Vitis vinifera. The Research Center of the MPC is surrounded by herbaceous plants, hedges, coniferous trees, olive groves, and vineyards.
During the non-working days (from Saturday to Sunday) or in absence of occupants, the biocontaminant values decreased. Figure 8 shows pollen trends in relation to the occupants observed in the summer campaigns. By looking these trends, the relationship between occupants and biocontaminants is mostly evident with respect to the non-working days. These results suggest that the presence of the occupants is an important factor contributing to the indoor concentrations of biocontaminants, such as pollen.

Activity 4: Aerobiological Particles
The results of the preliminary campaigns seem to indicate an increase of aerobiological particle concentrations during working hours in relation to workers' presence and behavior. Workers interact continuously with the indoor environment to realize their thermal and physiological comfort (window and door opening/closing or turning off ventilation), as shown in Table 4. The preliminary results were obtained through aerobiological monitoring in the MPC, that is, an area characterized by the Holm oak range, which consists of mixed oak woods with Quercus ilex and deciduous trees, with prevalence of cultivated species such as Olea europaea and Vitis vinifera. The Research Center of the MPC is surrounded by herbaceous plants, hedges, coniferous trees, olive groves, and vineyards.
During the non-working days (from Saturday to Sunday) or in absence of occupants, the biocontaminant values decreased. Figure 8 shows pollen trends in relation to the occupants observed in the summer campaigns. By looking these trends, the relationship between occupants and biocontaminants is mostly evident with respect to the non-working days. These results suggest that the presence of the occupants is an important factor contributing to the indoor concentrations of biocontaminants, such as pollen. Occupants' presence and behavior may affect diffusion and concentration of aerobiological particles as well as microclimatic parameters, which, in turn, may themselves affect pollens and fungal spores. In fact, during the summer, the microclimatic monitoring showed that the mean air temperature is higher (25.9 °C), while in the non-working days, it is lower (24.5 °C); mean relative humidity is higher (50.1%) in the non-working days with respect to the working days (49.7%). Our data do not seem to indicate a relationship between the aerobiological particles and the Tair and Occupants' presence and behavior may affect diffusion and concentration of aerobiological particles as well as microclimatic parameters, which, in turn, may themselves affect pollens and fungal spores. In fact, during the summer, the microclimatic monitoring showed that the mean air temperature is higher (25.9 • C), while in the non-working days, it is lower (24.5 • C); mean relative humidity is higher (50.1%) in the non-working days with respect to the working days (49.7%). Our data do not seem to indicate a relationship between the aerobiological particles and the T air and relative humidity, while the W S trend decreases in non-working days, as do the pollen and fungal spores' trends ( Figure S6 in the Supplementary Materials).
It is worth noting that occupants' actions, such as opening of doors and windows, affect biocontaminant values during working and non-working periods, as shown in Figure 9 for pollen. Sustainability 2020, 12, x FOR PEER REVIEW 16 of 25 relative humidity, while the WS trend decreases in non-working days, as do the pollen and fungal spores' trends ( Figure S6 in the Supplementary Materials). It is worth noting that occupants' actions, such as opening of doors and windows, affect biocontaminant values during working and non-working periods, as shown in Figure 9 for pollen.

Activity 5: Chemical and Biological Characterization of PM10
In this paragraph, we discuss the chemical and biological characterization of PM10 obtained during the short-term intensive campaign carried out during the winter of 2018 (for the description of the campaign schedule, see Section 2.1, activity 5).
The first step in the evaluation of the results was a check of the mass closure, that is, the correspondence between the mass concentration determined by gravimetry and the sum of the individual chemical determinations (reconstructed mass) obtained by applying appropriate conversion factors for non-measured elements (typically H or O). Very satisfactory results were obtained, with the sum of the chemical measurements accounting for 93%-115% of the gravimetric mass, and a Pearson's coefficient of the scatter plot (R 2 ) in the range of 0.91-0.97 (winter campaign 2018). The results of the chemical characterization were then elaborated to obtain a robust evaluation of the strength of the primary sources of PM: soil, sea-spray, secondary inorganics (ammonium nitrate and ammonium sulphate), organics, and traffic. The algorithms used for calculating the macro-sources are widely described in [62,63,92] and are briefly reported in Appendix A. Figure 10 shows the mass closure for PM10 samples collected outdoors and in one of the two classrooms located on the third or fourth floor during the period 26 November-9 December 2018 (left panels). In the same figure, we report the day-by-day variation in the strength of the PM10 macrosources at the same sites (right panels). We chose classroom A4 because it was the more crowded one during classes and it showed the widest day-night variations. The mass closure was very satisfactory, as the reconstructed mass constituted 97% ± 7% of the gravimetric mass outdoors and 102% ± 8% indoors. The data show that indoor concentrations widely exceeded outdoor values during the daytime, while they were closer to each other during the other periods. On average, the indoor increase in concentration recorded during the daytime samplings was as high as 16.5 µg/m 3 , while it was only 5.1 µg/m 3 during the night periods. During the weekends, outdoor values exceeded indoor concentrations by 5.3 µg/m 3 .

Activity 5: Chemical and Biological Characterization of PM 10
In this paragraph, we discuss the chemical and biological characterization of PM 10 obtained during the short-term intensive campaign carried out during the winter of 2018 (for the description of the campaign schedule, see Section 2.1, activity 5).
The first step in the evaluation of the results was a check of the mass closure, that is, the correspondence between the mass concentration determined by gravimetry and the sum of the individual chemical determinations (reconstructed mass) obtained by applying appropriate conversion factors for non-measured elements (typically H or O). Very satisfactory results were obtained, with the sum of the chemical measurements accounting for 93-115% of the gravimetric mass, and a Pearson's coefficient of the scatter plot (R 2 ) in the range of 0.91-0.97 (winter campaign 2018). The results of the chemical characterization were then elaborated to obtain a robust evaluation of the strength of the primary sources of PM: soil, sea-spray, secondary inorganics (ammonium nitrate and ammonium sulphate), organics, and traffic. The algorithms used for calculating the macro-sources are widely described in [62,63,92] and are briefly reported in Appendix A. Figure 10 shows the mass closure for PM 10 samples collected outdoors and in one of the two classrooms located on the third or fourth floor during the period 26 November-9 December 2018 (left panels). In the same figure, we report the day-by-day variation in the strength of the PM 10 macro-sources at the same sites (right panels). We chose classroom A4 because it was the more crowded one during classes and it showed the widest day-night variations. The mass closure was very satisfactory, as the reconstructed mass constituted 97% ± 7% of the gravimetric mass outdoors and 102% ± 8% indoors. The data show that indoor concentrations widely exceeded outdoor values during the daytime, while they were closer to each other during the other periods. On average, the indoor increase in concentration recorded during the daytime samplings was as high as 16.5 µg/m 3 , while it was only 5.1 µg/m 3 during the night periods. During the weekends, outdoor values exceeded indoor concentrations by 5.3 µg/m 3 . The study of the macro-sources shows that the indoor increase in the mass concentration of PM10 during weekdays was mainly due to an increase in soil components. This contribution was mostly due to the presence and movements of the students and to the use of chalk; it was found to be related to both the occupancy rate in the classroom and the duration of the lessons. Soil components are brought inside attached to the shoes and clothes of the students; moreover, particles already deposited on the floor and other surfaces are re-suspended when people walk and move. On average, the indoor increase in the concentration of this component recorded during daytime was 20.3 µg/m 3 . The indoor-to-outdoor ratio (I/O) ranged between 4.8-recorded during the second daytime period (28-30 November)-and 0.9-recorded during the second weekend (8)(9). These results indicate that the indoor source of soil components prevails on the infiltration from outdoors and that some particles remain suspended in the indoor atmosphere for a long period.
Sea-salt and secondary inorganics, instead, showed lower values indoors in all cases. In the case of sea-salt, this is due to the dimensions of these particles, which are mainly in the coarse range, and their consequent low infiltration rate. Outdoor concentration exceeded indoor concentration by 0.1-1.5 µg/m 3 , and the I/O values were, on average, between 0.5 and 0.6, with small differences between day, night, and weekend periods. This result indicates that there are no indoor sources for this component.
For ammonium nitrate, which constitutes most of the secondary inorganics during the cold season, indoor concentration was lower than outdoors because of the higher indoor temperatures, which caused a shift in the equilibrium of the ammonium nitrate formation reaction towards the precursors in the gaseous phase (nitric acid and ammonia). As a consequence, the indoor-outdoor difference was higher during daytime (on average, 2.3 µg/m 3 ), when the indoor temperature was higher, than during the night periods (0.9 µg/m 3 ). Accordingly, I/O values were, on average, 0.3 during daytime and 0.6 during the night periods.
Indoor and outdoor concentrations of particles from traffic emissions were comparable because their small size range (below 1 µm) favors the penetration from the outdoors. In this case, I/O values were close to 1.
In the case of organics, the reduced infiltration of larger particles is counterbalanced by the primary emission of biogenic particles (human skin debris) and natural fibers, which occurs indoors. Accordingly, a significant indoor increase was observed during day periods, with an average value of 3.7 µg/m 3 . During the night and the weekends, when the classrooms were empty, the penetration The study of the macro-sources shows that the indoor increase in the mass concentration of PM 10 during weekdays was mainly due to an increase in soil components. This contribution was mostly due to the presence and movements of the students and to the use of chalk; it was found to be related to both the occupancy rate in the classroom and the duration of the lessons. Soil components are brought inside attached to the shoes and clothes of the students; moreover, particles already deposited on the floor and other surfaces are re-suspended when people walk and move. On average, the indoor increase in the concentration of this component recorded during daytime was 20.3 µg/m 3 . The indoor-to-outdoor ratio (I/O) ranged between 4.8-recorded during the second daytime period (28-30 November)-and 0.9-recorded during the second weekend (8)(9). These results indicate that the indoor source of soil components prevails on the infiltration from outdoors and that some particles remain suspended in the indoor atmosphere for a long period.
Sea-salt and secondary inorganics, instead, showed lower values indoors in all cases. In the case of sea-salt, this is due to the dimensions of these particles, which are mainly in the coarse range, and their consequent low infiltration rate. Outdoor concentration exceeded indoor concentration by 0.1-1.5 µg/m 3 , and the I/O values were, on average, between 0.5 and 0.6, with small differences between day, night, and weekend periods. This result indicates that there are no indoor sources for this component.
For ammonium nitrate, which constitutes most of the secondary inorganics during the cold season, indoor concentration was lower than outdoors because of the higher indoor temperatures, which caused a shift in the equilibrium of the ammonium nitrate formation reaction towards the precursors in the gaseous phase (nitric acid and ammonia). As a consequence, the indoor-outdoor difference was higher during daytime (on average, 2.3 µg/m 3 ), when the indoor temperature was higher, than during the night periods (0.9 µg/m 3 ). Accordingly, I/O values were, on average, 0.3 during daytime and 0.6 during the night periods.
Indoor and outdoor concentrations of particles from traffic emissions were comparable because their small size range (below 1 µm) favors the penetration from the outdoors. In this case, I/O values were close to 1.
In the case of organics, the reduced infiltration of larger particles is counterbalanced by the primary emission of biogenic particles (human skin debris) and natural fibers, which occurs indoors. Accordingly, a significant indoor increase was observed during day periods, with an average value of 3.7 µg/m 3 . During the night and the weekends, when the classrooms were empty, the penetration from outdoors was the only mechanism contributing to indoor concentration, with an average outdoor-indoor difference of 2.3 µg/m 3 (night) and 4.0 µg/m 3 . On average, I/O values were 1.3 during the day periods, 0.9 during the nights, and 0.8 during the weekends.
Optical microscopy observations confirmed the presence of bioaerosol in the considered indoor environments. During the day hours of weekdays, bioaerosol concentration increased about twice with respect to night hours and about four times with respect to the weekend. A typical photo of a bioaerosol sample collected in the classroom during daytime hours is shown in Figure 11. It is possible to recognize some skin flakes (the widest particles, partially unfolded), some fibers, some fungal spores, and bacteria. These results are in line with the findings of the aerobiological studies (Section 3.4). Optical microscopy observations confirmed the presence of bioaerosol in the considered indoor environments. During the day hours of weekdays, bioaerosol concentration increased about twice with respect to night hours and about four times with respect to the weekend. A typical photo of a bioaerosol sample collected in the classroom during daytime hours is shown in Figure 11. It is possible to recognize some skin flakes (the widest particles, partially unfolded), some fibers, some fungal spores, and bacteria. These results are in line with the findings of the aerobiological studies (Section 3.4). Figure 11. Image of indoor bioaerosol through an optical microscope (montage of ten fields).
The overall results obtained in the chemical characterization of PM10 are well in agreement with previous studies carried out in schools in the same geographical area [47]. Similarly, in the recent study of [93], which was carried out in seven primary schools in Spain, the values of I/O in occupied classrooms were found to be higher than those recorded when the children were not inside, and this finding was mainly attributed to particle generation and re-suspension by the occupants. Instead, when finer particles were addressed (PM2.5 instead of PM10), indoor concentrations of inorganics were found by [94] to be lower than outdoors, and the major PM sources were identified as secondary pollution and traffic. For PM2.5, in fact, the contribution of soil components, which are mainly in the coarse dimensional range, is much smaller. When also considering the organic fraction [95], I/O ratios higher than one were also detected for PM2.5, showing the existence of an indoor source of organics, in agreement with our findings.
Samples collected in A4 and CR during the winter campaign 2017 were also analyzed for eight carcinogenic congeners of PM10-bound PAH (cPAH). The congeners' concentrations were used to calculate source profiles and carcinogenic potency factors relative to BaP (relative potency factors-RFPs). For this purpose, two schemes of toxicity equivalence factors (TEFs) were used, contributing to the potency of the mixture, with individual values also differing by an order of magnitude: factors from [96] and from one of the first published studies, [97]: A and B, respectively.
Averaging cPAH values over all the periods gave the highest concentration indoors (in the CR), whereas during the daytime and weekends, the highest values were measured outdoors. The CR had cPAH values higher than those of A4 in each single time range, as far as indoor results are concerned.
For the outdoor source profile based on cPAHs, the results centered on BbkF by day, night, and weekend; the two indoor ones were both still centered on BbkF on weekends and on BghiP on working days (either by day or by night).
The mean values of the total relative potency factors over all three periods analyzed (weekend, day, and night) are reported in Table 5. The RFPs from TEFs-A were about two and a half times those from TEFs-B. The indoor RPFs from either TEFs-A or -B were always lower than those from outdoors, where maximum RFPs were 4.93 in daytime for TEFs-A and 1.59 during weekends for TEFs-B. Looking inside the building, A4 presented higher daytime RFPs than those of the CR, independently from the TEFs used, and lower ones at night, differently from what was observed for cPAH concentrations, which were always higher for CR than for A4. Figure 11. Image of indoor bioaerosol through an optical microscope (montage of ten fields).
The overall results obtained in the chemical characterization of PM 10 are well in agreement with previous studies carried out in schools in the same geographical area [47]. Similarly, in the recent study of [93], which was carried out in seven primary schools in Spain, the values of I/O in occupied classrooms were found to be higher than those recorded when the children were not inside, and this finding was mainly attributed to particle generation and re-suspension by the occupants. Instead, when finer particles were addressed (PM 2.5 instead of PM 10 ), indoor concentrations of inorganics were found by [94] to be lower than outdoors, and the major PM sources were identified as secondary pollution and traffic. For PM 2.5 , in fact, the contribution of soil components, which are mainly in the coarse dimensional range, is much smaller. When also considering the organic fraction [95], I/O ratios higher than one were also detected for PM 2.5 , showing the existence of an indoor source of organics, in agreement with our findings.
Samples collected in A4 and CR during the winter campaign 2017 were also analyzed for eight carcinogenic congeners of PM 10 -bound PAH (cPAH). The congeners' concentrations were used to calculate source profiles and carcinogenic potency factors relative to BaP (relative potency factors-RFPs). For this purpose, two schemes of toxicity equivalence factors (TEFs) were used, contributing to the potency of the mixture, with individual values also differing by an order of magnitude: factors from [96] and from one of the first published studies, [97]: A and B, respectively.
Averaging cPAH values over all the periods gave the highest concentration indoors (in the CR), whereas during the daytime and weekends, the highest values were measured outdoors. The CR had cPAH values higher than those of A4 in each single time range, as far as indoor results are concerned.
For the outdoor source profile based on cPAHs, the results centered on BbkF by day, night, and weekend; the two indoor ones were both still centered on BbkF on weekends and on BghiP on working days (either by day or by night).
The mean values of the total relative potency factors over all three periods analyzed (weekend, day, and night) are reported in Table 5. The RFPs from TEFs-A were about two and a half times those from TEFs-B. The indoor RPFs from either TEFs-A or -B were always lower than those from outdoors, where maximum RFPs were 4.93 in daytime for TEFs-A and 1.59 during weekends for TEFs-B. Looking inside the building, A4 presented higher daytime RFPs than those of the CR, independently from the TEFs used, and lower ones at night, differently from what was observed for cPAH concentrations, which were always higher for CR than for A4. On working days, in both daytime and nighttime, indoor environments presented source profiles similar to each other, but different from that found outdoors, even if no internal direct sources of combustion were expected. Even though higher levels of PM 10 -bound PAHs were sometimes presented indoors than outdoors, the RFPs were always lower. The latter changed over the investigated periods, and was not in accordance with the corresponding trends of airborne cPAH concentrations.

Final Discussion and Conclusions
The VIEPI project, which is based on experimental activities and numerical simulations by computational fluid dynamics, was aimed at studying how atmospheric particles penetrate into indoor environments as a function of the physicochemical characteristics of the particles and the micrometeorological parameters. More specifically, the project intends to highlight the problems related to indoor PM evaluation linked to the characteristics of both buildings and surrounding urban areas.
To this end, the choice of research and academic environments allowed a reduction of the number of the indoor sources responsible for the build-up of particles, which were mainly combustion sources, as well as the clarification of the link with outdoor PM particles of different size ranges.
By performing fixed and travelling outdoor measurements at high time resolution, it was possible to describe the space-time variability of the number concentration of PM at a microscale level and to identify the primary descriptors of this variability.
The chemical composition of PM samples collected in different indoor environments (classrooms, laboratories) and during different periods (day, night, and weekend) made it possible to quantify the contributions of the main PM sources and to the highlight the role of people in crowded environments (release of biological materials and re-suspension of deposited particles). The selection of the sample locations also seems be a challenging task for assessing the indoor carcinogenic risk PM 10 -bound PAH.
In particular, the main conclusions of this study can be summarized as follows: • The CFD simulations and experimental data highlight the profound difference between the airflow above the building and that within the urban canyon. The horizontal wind speed within the canyon was always lower than that above the terrace (on April 2018, 0.35 ms −1 , 0.67 ms −1 , and 1.83 ms −1 at z = 0.8H, z = 0.4H, and z = 1.14H, respectively). The correlation between the wind speed measured by the two anemometers placed inside the canyon was weak (R 2 = 0.58), although it was higher than the correlation between the canyon and the terrace (R 2 = 0.16).

•
The vertical gradient of the outdoor UFPs observed in the canyon depended considerably on the season and was about −550 parts/cm 3 /m in winter, while it was nearly negligible in summer. This is probably due to the larger vertical mixing occurring in summer associated with the convective activity that characterizes the hottest periods. • Conversely, the vertical gradients of the indoor PM and UFPs measured indoors were dependent on both external and indoor sources.

•
The pollen concentrations measured in the suburban environment show a strict relation with occupants' habits.
Ultimately, these results confirm that indoor particulate matter concentration depends not only on outdoor and indoor sources, but also on the indoor airflow and outdoor microclimate near the considered building.
The results of this project made it possible to make significant steps forward in understanding the mechanisms that regulate air quality in indoor sites, where people spend most of their time, to highlight the peculiar features of crowded environments and to provide a set of data that are essential for assessing the exposure of students and workers in the university and research sectors.
Supplementary Materials: The following are available online at http://www.mdpi.com/2071-1050/12/22/9758/s1: Figure S1: Maps of the Physics Department and of the sites chosen for the experimental activity, Figure S2: Wind roses, Figure S3: Numerical setup, Figure S4: Wind velocity vector field, Figure S5: Daily trends of UFPs' PNC, Figure S6: Trends of pollens and fungal spores, Table S1: Comparison between CFD and observations.

Conflicts of Interest:
The authors declare no conflict of interest.

Calculation of Macro-Sources
The contribution of soil was calculated by summing the concentration of elements (as metal oxides) generally associated with mineral dust: aluminum, silicon, iron, and the insoluble fractions of potassium, magnesium, and calcium (calculated as the difference between the X-Ray Fluorescence and the Ion Cromatography), as well as calcium and magnesium carbonate.
The contribution of sea-salt was calculated from the concentration of soluble sodium and chloride, determined by IC and multiplied by 1.176 in order to take into account minor seawater components (sulphate, magnesium, calcium, and potassium).
The fraction due to secondary inorganics was calculated as the sum of non-sea-salt sulphate, nitrate, and ammonium.
The traffic source was calculated as the amount of elemental carbon (EC) plus the same amount multiplied by 1.1 to take into account organic species that condense from the exhaust gases and coat the surfaces of elemental carbon particles.
The remaining amount of organic carbon (OC), multiplied by an OC-to-OM (organic matter) conversion to account for non-C atoms in the organic molecules, constituted the organics. The conversion factors were set at 1.8 and 1.3 for outdoor and indoor samples, respectively.