Thermal Performance Analysis of Heat Collection Wall in High-Rise Building Based on the Measurement of Near-Wall Microclimate

: Near-wall microenvironment of a building refers to parameters such as wind speed, temperature, relative humidity, solar radiation near the building’s façade, etc. The distribution of these parameters on the building façade shows a certain variation based on changes in height. As a technology of passive heating and ventilation, the effectiveness of this application on heat collection wall is signiﬁcantly affected by the near-wall microclimate, which is manifested by the differences, and rules of the thermal process of the components present at different elevations. To explore the feasibility and speciﬁcity of this application of heat collection wall in high-rise buildings, this study uses three typical high-rise buildings from Zhengzhou, China, as research buildings. Periodic measurements of the near-wall microclimate during winter and summer were carried out, and the changing rules of vertical and horizontal microclimate were discussed in detail. Later, by combining these measured data with numerical method, thermal process and performance of heat collection wall based on increasing altitude were quantitatively analyzed through numerical calculations, and the optimum scheme for heat collection wall components was summarized to provide a theoretical basis for the structural design of heat-collecting wall in high-rise buildings.


Introduction
Since the 20th century, global population growth, energy consumption, and environmental pollution have gradually gained an increased focus worldwide. These urgent problems bring out new needs to the pattern of energy supply and demand. According to the latest world energy outlook British Petroleum (2020 edition) [1], estimates show that by 2050, the percentage of oil, gas, and coal in global energy total would drop from 85% in 2018 to a 20-65% range, while renewable energy proportion would rise from 20-60%, respectively. Buildings are one of the essential parts of energy consumption, which accounts for 39% of the total consumption. According to data from the International Refrigeration Association, the power consumption of the refrigeration and air conditioning industry accounts for about 15% of total power consumption in the world [2].
Since 1950, the world urbanization rate has increased from 29.2 to 57.4%, and the urban population has increased from 734 million to 4488 million. Urbanization in China has been developing rapidly for nearly twenty years. According to statistics, by the end of 2019, the total population occupied by the mainland was about 1.4 billion, of which 60.60% belonged to permanent urban residents (the urbanization rate of permanent residents), and 44.38% of them were registered as permanent residents. Urban area and population density in cities have increased rapidly, and the increase of high-rise buildings has brought huge pressure on heating and cooling energy requirements. The heating demand during sales. At the same time, China's floating population had reached 247 million, of which 70% live in rented houses. This provided a good market demand for the studio industry. It can be seen that studios and apartment buildings take up a large proportion of the current urban high-rise buildings, which is of great representativeness and research significance. The main objectives of this study were to clarify the regular of near-wall microclimate change of urban high-rise residential buildings and evaluated the thermal performance of the heat collection wall on this basis. The relationships between the indoor thermal environment, microclimate of near-wall south-facing and outdoor climate were examined.

Research Area and Climate
This study conducted a field measurement of three buildings in Zhengzhou which is located in the south of the warm temperate zone and experiences the continental monsoon humid climate. According to the regulations of Thermal Climate Area Zone of Chinese Architecture, Zhengzhou belongs to a primarily cold region and the third-level area of solar energy resources in China (the annual sunshine duration is 2200-3000 h). The urbanization rate of Zhengzhou city is 74.6%, and its permanent resident population is 10.352 million with commercial housing sales area of 35.93 million m 2 . In Figure 1, it can be seen the monthly average temperature, relative humidity and monthly total solar radiation, which are from the annual report of typical meteorology in Zhengzhou (the unit of monthly total solar radiation is MJ/m 2 ).

Test Buildings
A studio-building and two apartment buildings from Zhengzhou were taken as the test buildings. The building envelope wall is composed of cement mortar, external insulation layer, and aerated concrete blocks. None of the three buildings has external sunshade systems. More details of the three buildings are listed in Tables 1 and 2, the locations, photographs, and shapes of buildings are shown in Figure 2.

Test Buildings
A studio-building and two apartment buildings from Zhengzhou were taken as the test buildings. The building envelope wall is composed of cement mortar, external insulation layer, and aerated concrete blocks. None of the three buildings has external sunshade systems. More details of the three buildings are listed in Tables 1 and 2, the locations, photographs, and shapes of buildings are shown in Figure 2.  2. Locations, photographs, and shapes of three buildings.

Measurement Campaign
According to the aforementioned studies, it can be seen that near-wall microclimate will affect surrounding temperature, concentration of CO2, surface heat transfer coefficient and other thermal performance of ordinary single buildings. As for the application of heat collection wall on high-rise buildings, it will affect the heat transfer process and thermal efficiency of heat-collecting wall components. Thus near-wall microclimate measurement campaigns of different buildings were carried out to find out how microclimate parameters change on buildings' façade. As for the selection of measurement time, we conducted tests in December and August of China's typical meteorological year and conducted outdoor near-wall microclimate tests in winter and summer, respectively. According to previous studies, Lin et al.
[3738] conducted a 20-day test of microclimate parameters outside a five-story building. And Pan [3941] carried out a measurement in a short period and analyzed the near-wall parameters of a super high-rise building in one day. It was found that the test results were consistent with those of Lin, which proved the validity of the short-term test data. Zhang et al. [41,4242,43] also used three-day observation data to analyze the outdoor microenvironment in Kunming and Beijing, China. Moreover, Ana Sa [50] designed several test cycles ranging from one day to three weeks to measure the thermal performance of the heat-collecting wall under different working conditions. Moreover, to reduce instrument errors, the instruments used have been calibrated, and in data processing, the average values of 50 min, 55 min, 0 min, 5 min and 10 min are selected as data at 0 min. This method refers to the previous literature [41,42].

Measurement Campaign
According to the aforementioned studies, it can be seen that near-wall microclimate will affect surrounding temperature, concentration of CO 2 , surface heat transfer coefficient and other thermal performance of ordinary single buildings. As for the application of heat collection wall on high-rise buildings, it will affect the heat transfer process and thermal efficiency of heat-collecting wall components. Thus near-wall microclimate measurement campaigns of different buildings were carried out to find out how microclimate parameters change on buildings' façade. As for the selection of measurement time, we conducted tests in December and August of China's typical meteorological year and conducted outdoor near-wall microclimate tests in winter and summer, respectively. According to previous studies, Lin et al. [38] conducted a 20-day test of microclimate parameters outside a fivestory building. And Pan [41] carried out a measurement in a short period and analyzed the near-wall parameters of a super high-rise building in one day. It was found that the test results were consistent with those of Lin, which proved the validity of the short-term test data. Zhang et al. [42,43] also used three-day observation data to analyze the outdoor microenvironment in Kunming and Beijing, China. Moreover, Sa [50] designed several test cycles ranging from one day to three weeks to measure the thermal performance of the heat-collecting wall under different working conditions. Moreover, to reduce instrument errors, the instruments used have been calibrated, and in data processing, the average values of 50 min, 55 min, 0 min, 5 min and 10 min are selected as data at 0 min. This method refers to the previous literature [41,42].

. Measurement Campaign in Winter
To explore the vertical and horizontal distribution rules of the near-wall microclimate of a high-rise building and to quantitatively evaluate the influence of the near-wall microclimate specificity on the thermal performance of the heat collection walls, in this paper, three buildings in Zhengzhou were measured in December 2019. A small weather station was set up on the roof to measure the wind speed, solar radiation intensity, outdoor temperature, humidity, and other measurement schemes as follows. The indoor temperature and the relative humidity measuring points were arranged in the center of the room, and the other measuring points were located on the southern wall. The detailed layout is shown in Figure 3 (The height of three measured buildings is different, so Building 1 was taken as an example.) three buildings in Zhengzhou were measured in December 2019. A small weather station was set up on the roof to measure the wind speed, solar radiation intensity, outdoor temperature, humidity, and other measurement schemes as follows. The indoor temperature and the relative humidity measuring points were arranged in the center of the room, and the other measuring points were located on the southern wall. The detailed layout is shown in Figure 3 (The height of three measured buildings is different, so Building 1 was taken as an example.) 1. West of Building 1 (B1) measurement in winter: Measuring points were arranged in the south-facing rooms on the west side on the 2nd, 6th, 14th, 18th, and 22nd floors of the 22-story building. Presuming that the skirt house would affect the test results, the measuring points were not arranged on the 10th floor. The solar radiation meters were arranged in the south-facing rooms on the 2nd and 22nd floors, respectively, to measure the vertical solar radiation of the same building. 2. Middle of Building 1 (B1) measurement in winter: Measuring points were arranged in the south-facing rooms in the middle of the 2nd, 6th, 14th, 18th and 22nd floors of this 22-story studios building in contrast to the west side. 3. Building 2 (B2) measurement in winter: Measuring points were arranged on the 3rd, 5th, 8th, 12th, and 15th floors of the southern wall of the 15-story apartment building. 4. Building 3 (B3) measurement in winter: Measuring points were arranged on the 3rd, 5th, 7th, 9th, and 11th floors of the southern wall of the 11-story apartment building.

Measurement Campaign in Summer
To contrast with the winter test results, the 11-story apartment building was selected for the measurement in summer. Moreover, the vertical and horizontal measurements were designed to explore the changing law of the microclimate near the facade of residential buildings as shown in Figure 4 which were carried out in August 2020. The measuring equipment and arrangement of measuring points were consistent with the aforementioned winter experiment. The measurement scheme is as follows.
1. B3 vertical measurement in summer: Measurement points were arranged in the middle room of the southern wall on the 3rd, 5th, 7th, 9th, and 11th floors. 2. B3 horizontal measurements in summer: Measurement points are arranged in the three rooms on the 3rd and 11th floors, respectively.

1.
West of Building 1 (B1) measurement in winter: Measuring points were arranged in the south-facing rooms on the west side on the 2nd, 6th, 14th, 18th, and 22nd floors of the 22-story building. Presuming that the skirt house would affect the test results, the measuring points were not arranged on the 10th floor. The solar radiation meters were arranged in the south-facing rooms on the 2nd and 22nd floors, respectively, to measure the vertical solar radiation of the same building.

2.
Middle of Building 1 (B1) measurement in winter: Measuring points were arranged in the south-facing rooms in the middle of the 2nd, 6th, 14th, 18th and 22nd floors of this 22-story studios building in contrast to the west side.

3.
Building 2 (B2) measurement in winter: Measuring points were arranged on the 3rd, 5th, 8th, 12th, and 15th floors of the southern wall of the 15-story apartment building.

4.
Building 3 (B3) measurement in winter: Measuring points were arranged on the 3rd, 5th, 7th, 9th, and 11th floors of the southern wall of the 11-story apartment building.

Measurement Campaign in Summer
To contrast with the winter test results, the 11-story apartment building was selected for the measurement in summer. Moreover, the vertical and horizontal measurements were designed to explore the changing law of the microclimate near the facade of residential buildings as shown in Figure 4 which were carried out in August 2020. The measuring equipment and arrangement of measuring points were consistent with the aforementioned winter experiment. The measurement scheme is as follows.

1.
B3 vertical measurement in summer: Measurement points were arranged in the middle room of the southern wall on the 3rd, 5th, 7th, 9th, and 11th floors.

2.
B3 horizontal measurements in summer: Measurement points are arranged in the three rooms on the 3rd and 11th floors, respectively.

Equipment
The following measurement parameters were determined as per the definition and literature of the near-wall microclimate; namely, air temperature and relative humidity, wind speed near the southern wall of the building, temperature, and relative humidity indoors and of the wall, furthermore the intensity of solar radiation. The measuring equipment is shown in Table 3.

Equipment
The following measurement parameters were determined as per the definition and literature of the near-wall microclimate; namely, air temperature and relative humidity, wind speed near the southern wall of the building, temperature, and relative humidity indoors and of the wall, furthermore the intensity of solar radiation. The measuring equipment is shown in Table 3.

Equipment
The following measurement parameters were determined as per the definition and literature of the near-wall microclimate; namely, air temperature and relative humidity, wind speed near the southern wall of the building, temperature, and relative humidity indoors and of the wall, furthermore the intensity of solar radiation. The measuring equipment is shown in Table 3.

Equipment
The following measurement parameters were determined as per the definition and literature of the near-wall microclimate; namely, air temperature and relative humidity, wind speed near the southern wall of the building, temperature, and relative humidity indoors and of the wall, furthermore the intensity of solar radiation. The measuring equipment is shown in Table 3.

Equipment
The following measurement parameters were determined as per the definition and literature of the near-wall microclimate; namely, air temperature and relative humidity, wind speed near the southern wall of the building, temperature, and relative humidity indoors and of the wall, furthermore the intensity of solar radiation. The measuring equipment is shown in Table 3.

Uncertainty Analysis
Uncertainty refers to the degree of uncertainty of the measured value due to the existence of measurement error. In order to evaluate the reliability of the data in this study and enhance the comparability between the measured results, uncertainty analysis was performed. Take the wall temperature data at 19:00 on December 7, 2019 as an example to calculate the uncertainty: the data at 18:50, 18:55, 19:00, 19:05, 19:10 are 3.5, 3.3, 3.2, 3.2, 3.1, respectively. The instrument is a RC-4 temperature and humidity recorder with an accuracy of ±0.6 °C. The calculation process is as follows.
In the direct measurement, type A evaluation of uncertainty is calculated by Bessel

Uncertainty Analysis
Uncertainty refers to the degree of uncertainty of the measured value due to the existence of measurement error. In order to evaluate the reliability of the data in this study and enhance the comparability between the measured results, uncertainty analysis was performed. Take the wall temperature data at 19:00 on December 7, 2019 as an example to calculate the uncertainty: the data at 18:50, 18:55, 19:00, 19:05, 19:10 are 3.5, 3.3, 3.2, 3.2, 3.1, respectively. The instrument is a RC-4 temperature and humidity recorder with an accuracy of ±0.6 • C. The calculation process is as follows.
In the direct measurement, type A evaluation of uncertainty is calculated by Bessel Q gsun = α g I A g -Amount of solar radiation absorbed by the glass cover; -Radiation exchange glass cover and heatcollecting wall; Q ga = h ga A g t g − t a -Heat transfer by convection between the glass cover and the outdoor air; Q gc = h gc A g t g − t m -Heat transfer by convection between the glass cover and the air layer.

2.
Heat balance equation of the air layer -Heat exchange by convection between the heat-collecting wall and the air layer; The amount of heat absorbed as the air temperature rises in the interlayer.

3.
Heat balance equation of heat-collecting wall Q wsun = α w βI A w -The amount of solar radiation absorbed by the heat-collecting wall; l -Heat conduction through the heat collecting wall; Heat transfer by convection between the wall and the indoor air.

4.
Thermal balance equation of the room (the rest of the envelope is insulated surface) Q s -Heat source in the room;

Parameter calculation
When calculating the above equations of heat balance, some parameters are calculated as follows [51,52]: h ga is the convective heat transfer coefficient between the glass cover plate and the outdoor air, and the calculation formula is: where V is the outdoor wind speed, which is obtained from the experimental data; m is the air mass flow rate through the air interlayer of the heat collecting wall, and its formula is: where is the air mass flow rate through the air interlayer of the heat collecting wall; A g is the cross-sectional area of the air sandwich in the hot wall; ρ is the air density when the temperature is t m ; h v is the vertical distance of the center of the lower tuyere on the heat collecting wall. h gc is a variable that depends on the airflow state in the interlayer of the heat-collecting wall. Its calculation formula is as follows: Re > 2000, h gc = 0.0158Re 0.8 λ l where Pr is Prandtl number; Re is Reynolds number; λ is the thermal conductivity of air; l is the thickness of the air cavity; Dh is the equivalent diameter of the air cavity. In the mathematical model of the heat collecting wall, t a , t i , I, V can be obtained through experimental data. The mathematical calculation model of the heat collection wall is established, and unknown quantities t g , t o , t m , t w , v are obtained through iteration to calculate the heat transfer performance of this heat collecting wall.

Natural Ventilation under the Action of Hot and Wind Pressure
In summer, the airflow in the heat collecting wall is affected by thermal pressure and wind pressure. The thermal pressure effect refers to the change in air buoyancy caused by changes in air density due to the temperature difference between the indoors and outdoors in certain areas. Wind pressure effect is the difference in wind pressure caused by obstacles encountered by wind, which forms a negative pressure zone on the leeward side of the building and positive pressure on the windward side of the building.
The calculation of natural ventilation under hot pressing is as follows: where α is the air expansion coefficient; C d is the flow coefficient; A is the tuyere area. The calculation of natural ventilation under wind pressure is as follows: where ε is the local resistance coefficient of the tuyere; v is the velocity of air.

Solar Radiation in Winter
As shown in Figure 5, no significant delay was found in the duration of sunshine and no significant difference in the intensity of solar radiation at different heights. The maximum solar radiation during the day can be more than 600 W/m 2 , which satisfies the requirement of the solar energy collecting wall; thus, proves the feasibility and tremendous potential of the application of solar energy collecting wall in Zhengzhou.
where is the air expansion coefficient; is the flow coefficient; is the tuyere area. The calculation of natural ventilation under wind pressure is as follows: where is the local resistance coefficient of the tuyere; is the velocity of air.

Solar Radiation in Winter
As shown in Figure 5, no significant delay was found in the duration of sunshine and no significant difference in the intensity of solar radiation at different heights. The maximum solar radiation during the day can be more than 600 W/m 2 , which satisfies the requirement of the solar energy collecting wall; thus, proves the feasibility and tremendous potential of the application of solar energy collecting wall in Zhengzhou.

Horizontal Analysis of Near-Wall
Temperature of B1 Figure 6 shows the indoor and near-wall temperature changes of B1. t out-ave represents the average near-wall temperature of the five measuring points, T out represents the outdoor temperature measured by the weather station, and t in-ave represents the average indoor temperature of the five measuring points. It can be seen that the temperature trend was t out-ave > T out > t in-ave . It can be seen that the range of temperature change of the measuring points in the west is larger than that of the middle ones.
3.1.2. Horizontal Analysis of Near-Wall Temperature of B1 Figure 6 shows the indoor and near-wall temperature changes of B1. tout-ave represents the average near-wall temperature of the five measuring points, Tout represents the outdoor temperature measured by the weather station, and tin-ave represents the average indoor temperature of the five measuring points. It can be seen that the temperature trend was tout-ave > Tout > tin-ave. It can be seen that the range of temperature change of the measuring points in the west is larger than that of the middle ones.  Figure 7 shows the variation of the vertical temperature difference of B1, which is the difference between the near-wall temperature present at the top and the bottom temperatures. The comparison shows that the average value and variance of the vertical temperature difference on the central wall are smaller than that in the west, indicating that the temperature fluctuation on the western wall is greater than that of the middle, which is greatly affected by the outdoor environment.   Figure 7 shows the variation of the vertical temperature difference of B1, which is the difference between the near-wall temperature present at the top and the bottom temperatures. The comparison shows that the average value and variance of the vertical temperature difference on the central wall are smaller than that in the west, indicating that the temperature fluctuation on the western wall is greater than that of the middle, which is greatly affected by the outdoor environment.
3.1.2. Horizontal Analysis of Near-Wall Temperature of B1 Figure 6 shows the indoor and near-wall temperature changes of B1. tout-ave represents the average near-wall temperature of the five measuring points, Tout represents the outdoor temperature measured by the weather station, and tin-ave represents the average indoor temperature of the five measuring points. It can be seen that the temperature trend was tout-ave > Tout > tin-ave. It can be seen that the range of temperature change of the measuring points in the west is larger than that of the middle ones.  Figure 7 shows the variation of the vertical temperature difference of B1, which is the difference between the near-wall temperature present at the top and the bottom temperatures. The comparison shows that the average value and variance of the vertical temperature difference on the central wall are smaller than that in the west, indicating that the temperature fluctuation on the western wall is greater than that of the middle, which is greatly affected by the outdoor environment.

Vertical Analysis of Near-Wall Temperature of Three Buildings
To clearly describe the temperature distribution in the vertical direction, Figure 8 below shows the changes in the near-wall temperature and the adjacent temperature with height in the four test cycles. The solid line represents the near-wall temperature, and the dashed line represents the surrounding temperature (50 mm from the wall), which are obtained by the WFWZY-1 universal wind speed and wind temperature recorder. According to the test data, we find that the temperature fluctuated significantly with height from 11:00 to 15:00. Due to a large number of measured data, Figure 8 only shows the temperature at 12:00 every day which can best display the temperature change. For the 22-story studios B1, the outer wall temperature and surrounding temperature are presented as highly increased s-shaped fluctuations. Firstly, they increase as the height increases at the surface layer until it reaches a maximum of 23 m, and then reaches a minimum at 60 m, and then finally rises again. This process reflects the s-shaped change of temperature in the vertical direction, and the average amplitude of the two tests is 1.37 • C and 0.43 • C, respectively, which indicates that the western measuring point is more susceptible to airflow. For the 15-story and 11-story apartment buildings (B2 and B3), the temperature also presents S-shaped changes in the vertical direction, with a wave average amplitude of 0.39 • C and 0.27 • C, respectively. At the same time, the surrounding temperature is lower than the wall temperature, which is due to the heating effect after the wall absorbs the solar radiation is greater than the convective heat transfer effect between the wall and surrounding air.
To clearly describe the temperature distribution in the vertical direction, Figure 8 below shows the changes in the near-wall temperature and the adjacent temperature with height in the four test cycles. The solid line represents the near-wall temperature, and the dashed line represents the surrounding temperature (50 mm from the wall), which are obtained by the WFWZY-1 universal wind speed and wind temperature recorder. According to the test data, we find that the temperature fluctuated significantly with height from 11:00 to 15:00. Due to a large number of measured data, Figure 8 only shows the temperature at 12:00 every day which can best display the temperature change. For the 22-story studios B1, the outer wall temperature and surrounding temperature are presented as highly increased s-shaped fluctuations. Firstly, they increase as the height increases at the surface layer until it reaches a maximum of 23 m, and then reaches a minimum at 60 m, and then finally rises again. This process reflects the s-shaped change of temperature in the vertical direction, and the average amplitude of the two tests is 1.37 °C and 0.43 °C, respectively, which indicates that the western measuring point is more susceptible to airflow. For the 15-story and 11-story apartment buildings (B2 and B3), the temperature also presents S-shaped changes in the vertical direction, with a wave average amplitude of 0.39 °C and 0.27 °C, respectively. At the same time, the surrounding temperature is lower than the wall temperature, which is due to the heating effect after the wall absorbs the solar radiation is greater than the convective heat transfer effect between the wall and surrounding air. To sum up, the outdoor temperature of the building presented an S-shaped fluctuation with the increase of height, which rises as the height increases in the surface layer and then gets fluctuated. This variation trend is related to the horizontal position and height of the building. The amplitude of the side of the building is larger than that of the middle, and the greater the height of the building, the larger the amplitude. To sum up, the outdoor temperature of the building presented an S-shaped fluctuation with the increase of height, which rises as the height increases in the surface layer and then gets fluctuated. This variation trend is related to the horizontal position and height of the building. The amplitude of the side of the building is larger than that of the middle, and the greater the height of the building, the larger the amplitude. Figure 9 shows the comparison of wind speed of B1, in which v-i is the attached airflow velocity at the measurement point i. It can be seen that the attached air velocity fluctuates under ambient wind speed. While ambient wind speed remains the same, the average airflow velocity of the west-side reaches up to 2.146 times that of the middle, which indicates that horizontally, the side of the building is more susceptible to the influence of ambient air distribution. The airflow velocity of the west-side is greater than that of the middle, which lowers the temperature in the west and fluctuates greater than that in the middle. Figure 9 shows the comparison of wind speed of B1, in which v-i is the attached airflow velocity at the measurement point i. It can be seen that the attached air velocity fluctuates under ambient wind speed. While ambient wind speed remains the same, the average airflow velocity of the west-side reaches up to 2.146 times that of the middle, which indicates that horizontally, the side of the building is more susceptible to the influence of ambient air distribution. The airflow velocity of the west-side is greater than that of the middle, which lowers the temperature in the west and fluctuates greater than that in the middle.

Vertical Analysis of Airflow Velocity of the Three Buildings
To analyze the variation law of the near-wall updraft attached to the surface, the wind speed ratio (the percentage ratio between the wind speed at the measuring point and the environmental wind speed) was defined as a comparison parameter, so that the influence of the environmental wind speed could be ignored. The calculation results were shown in Table 4, and Figure 10 was carried out according to the results. It was found that in the vertical direction, similar fluctuation rules were shown in the four sets of data. At the near-surface layer, the wind speed increased with an increase of height, while at the top layer, it came to a plateau or remained flat. This is consistent with Max's research theory on the urban gradient wind effect. He believed that the effect of outdoor wind speed and the wind pressure on the exterior surface of buildings increases gradually with the increase of height within a certain height limit.

Vertical Analysis of Airflow Velocity of the Three Buildings
To analyze the variation law of the near-wall updraft attached to the surface, the wind speed ratio (the percentage ratio between the wind speed at the measuring point and the environmental wind speed) was defined as a comparison parameter, so that the influence of the environmental wind speed could be ignored. The calculation results were shown in Table 4, and Figure 10 was carried out according to the results. It was found that in the vertical direction, similar fluctuation rules were shown in the four sets of data. At the near-surface layer, the wind speed increased with an increase of height, while at the top layer, it came to a plateau or remained flat. This is consistent with Max's research theory on the urban gradient wind effect. He believed that the effect of outdoor wind speed and the wind pressure on the exterior surface of buildings increases gradually with the increase of height within a certain height limit.  Based on the above analysis regarding the distribution of wind speed on the building's facade, it was found that the wind speed on the surface of the building presents the same trend in the vertical direction: the wind speed increases with the increase of height at the near formation, and it comes to a plateau or stayed flat at the top layer. The side of the building in the horizontal direction was more susceptible to the influence of environmental air distribution. The wind speed on the west side was greater than that present of the middle side, which reduced the temperature and caused greater fluctuations on the west. Different types of buildings showed different changes in wind speed. As shown in Table 3, the maximum difference of the average wind speed ratio of the four periods is 9.4%, 8.3%, 28.8%, 21.4%, respectively. The building's facade with a small-sized body coefficient was more likely to form a stable wind field near the wall, which made the variation range of the attached airflow velocity smaller.

Near-Wall Temperature of B3 in Summer
The variation trend of the indoor and outdoor temperature of the test room of B3 were analyzed. The outer wall temperature, indoor temperature, and the outdoor temperature of the building presented the same fluctuation trend, which was consistent with the conclusions of the winter test, and hence it will not be repeated here. To intuitively find out the temperature distribution of the outer surface, the average wall temperature difference obtained from the summer test of B3 was used for horizontal and vertical interpolation. Figure 11 was obtained for the comparison of vertical and horizontal directions.
Horizontally, the temperature of the central measuring point is higher than that of the east and west measuring points. On the topmost floor, the average temperature of the wall surface of the central measuring point was 0.43 °C higher than that of the east side and 3.11 °C higher than that of the west side. On the bottom floor, the average temperature of the wall surface of the central measuring point was 1.89 °C higher than the east side and 1.81 °C higher than the west side. In the vertical direction, the temperature showed an s-shaped fluctuation, the average temperature at the measuring points gradually increased with the increase of height in the surface layer and fluctuated, and reached the Based on the above analysis regarding the distribution of wind speed on the building's facade, it was found that the wind speed on the surface of the building presents the same trend in the vertical direction: the wind speed increases with the increase of height at the near formation, and it comes to a plateau or stayed flat at the top layer. The side of the building in the horizontal direction was more susceptible to the influence of environmental air distribution. The wind speed on the west side was greater than that present of the middle side, which reduced the temperature and caused greater fluctuations on the west. Different types of buildings showed different changes in wind speed. As shown in Table 3, the maximum difference of the average wind speed ratio of the four periods is 9.4%, 8.3%, 28.8%, 21.4%, respectively. The building's facade with a small-sized body coefficient was more likely to form a stable wind field near the wall, which made the variation range of the attached airflow velocity smaller.

Near-Wall Temperature of B3 in Summer
The variation trend of the indoor and outdoor temperature of the test room of B3 were analyzed. The outer wall temperature, indoor temperature, and the outdoor temperature of the building presented the same fluctuation trend, which was consistent with the conclusions of the winter test, and hence it will not be repeated here. To intuitively find out the temperature distribution of the outer surface, the average wall temperature difference obtained from the summer test of B3 was used for horizontal and vertical interpolation. Figure 11 was obtained for the comparison of vertical and horizontal directions.
Horizontally, the temperature of the central measuring point is higher than that of the east and west measuring points. On the topmost floor, the average temperature of the wall surface of the central measuring point was 0.43 • C higher than that of the east side and 3.11 • C higher than that of the west side. On the bottom floor, the average temperature of the wall surface of the central measuring point was 1.89 • C higher than the east side and 1.81 • C higher than the west side. In the vertical direction, the temperature showed an s-shaped fluctuation, the average temperature at the measuring points gradually increased with the increase of height in the surface layer and fluctuated, and reached the extreme value in P4 at 9th floor, which was similar to the fluctuation rule in winter. However, the amplitude in summer (0.48 • C) was larger than that in winter (0.27 • C). extreme value in P4 at 9th floor, which was similar to the fluctuation rule in winter. However, the amplitude in summer (0.48 °C) was larger than that in winter (0.27 °C).
In short, the temperature distribution of this building in summer could be described as follows: An s-shaped fluctuation occurred in the vertical direction, and its amplitude was larger than that of in winter; in the horizontal direction, the temperature in the middle was higher than that on two sides, which was related to the distribution of wind speed.

Airflow Velocity of B3 in Summer
By calculating the wind speed data obtained from the two tests, it was found that there was a major difference between the average environmental wind speed of the two. Therefore, the ratio of the wind speed at the measuring point and the environmental wind speed was shown in Table 5 and was taken as a parameter, in order to draw the distribution diagram of the attached airspeed on its building wall as shown in Figure 12.
It was found that in the horizontal direction, the wind speed on both sides of the building was larger, and the wind speed in the middle was the smallest. In the vertical direction, the wind speed on the building surface was consistent with the winter fluctuation rule, with the maximum value appearing at P4, and the amplitude was found to be smaller than the winter variation.  In short, the temperature distribution of this building in summer could be described as follows: An s-shaped fluctuation occurred in the vertical direction, and its amplitude was larger than that of in winter; in the horizontal direction, the temperature in the middle was higher than that on two sides, which was related to the distribution of wind speed.

Airflow Velocity of B3 in Summer
By calculating the wind speed data obtained from the two tests, it was found that there was a major difference between the average environmental wind speed of the two. Therefore, the ratio of the wind speed at the measuring point and the environmental wind speed was shown in Table 5 and was taken as a parameter, in order to draw the distribution diagram of the attached airspeed on its building wall as shown in Figure 12.

Mathematical Calculation of Heat Collection Wall in High Rise Apartments
The corresponding heat balance equation of heat collection wall was established in Figure 12. Airflow velocity of B3 in summer.
It was found that in the horizontal direction, the wind speed on both sides of the building was larger, and the wind speed in the middle was the smallest. In the vertical direction, the wind speed on the building surface was consistent with the winter fluctuation rule, with the maximum value appearing at P4, and the amplitude was found to be smaller than the winter variation.

Mathematical Calculation of Heat Collection Wall in High Rise Apartments
The corresponding heat balance equation of heat collection wall was established in this paper by considering the measured room to be the physical model and the mathematical model. The measured data were substituted into the calculation model as parameters of the wall envelope surrounding the wall, to study the change of heat transfer performance of the wall having the height. As the actual heat transfer process of the heat collecting wall is relatively complex with many influencing factors, the following simplified assumptions were made for the heat balance equation established:

1.
Assume that the air is uniformly incompressible; 2.
Assume that the glass temperature does not change along with thickness; 3.
Assume that the solar heat collection and storage wall system shows steady-state heat transfer; 4.
Ignore the influence of the change of relative humidity; 5.
Ignore the influence of cold air penetration on the heat transfer process; 6.
The rest of the envelope is an adiabatic surface.  Table 6, and the calculation model of the heat collection wall is shown in Figure 13.

Calculation of Attenuation Delay of Heat Collection Wall
The transfer matrix of the plate wall's thermal system expresses the relationship between the four boundary parameters of inner and outer surface temperature and the La-

Calculation of Attenuation Delay of Heat Collection Wall
The transfer matrix of the plate wall's thermal system expresses the relationship between the four boundary parameters of inner and outer surface temperature and the Laplace transform of the heat flow. Given any two parameters, the other two parameters can be obtained.
The attenuation multiples ν yn and time delay ξ yn of the wall to the sinusoidal temperature waves of different frequencies outside were calculated as follows when the temperature was kept at zero: At night in winter, the ventilation hole of the heat collection wall is closed. MATLAB software is used to program and calculate its attenuation delay. The results are shown in Table 7: It can be seen from the calculation results, the multiple attenuations and delay phases of the heat collection wall with its ventilation hole closed are higher than that of ordinary walls without heat collection structures. Within the same external disturbance, the indoor thermal environment will be more stable and comfortable.

Temperature Difference between Inlet and Outlet
Because the vents of the heat collection wall are closed during the night, the data from December 7th to December 11th are chosen as the parameters of the solar radiation, and it was found that the solar thermal wall showed poor heat collection effect 2 h after sunrise and 2 h before sunset; thus, during this time, the vents should be closed for insulation. Therefore, the calculation results from 10:00 to 16:00 which were counted every 5 min were selected to draw the following chart Figure 14 and define calculation cycle time axis as Day 1-Day 5. According to calculation results, the temperature difference between inlet and outlet in winter can reach up to 19.61 • C, and the average value of each measuring point is 10.99, 12.11, 13.13, 12.79, and 11.25 • C, respectively. and it was found that the solar thermal wall showed poor heat collection effect 2 h after sunrise and 2 h before sunset; thus, during this time, the vents should be closed for insulation. Therefore, the calculation results from 10:00 to 16:00 which were counted every 5 min were selected to draw the following chart Figure 14 and define calculation cycle time axis as Day 1-Day 5. According to calculation results, the temperature difference between inlet and outlet in winter can reach up to 19.61 °C, and the average value of each measuring point is 10.99, 12.11, 13.13, 12.79, and 11.25 °C, respectively. The variation law between the inlet and outlet temperature difference of the heat collecting wall and the outdoor wind temperature is explored, and the Figure 15 below shows the outdoor temperature at P1 and the curve chart of the inlet and outlet temperature of the heat collecting wall. It can be seen that the temperature difference between inlet and outlet is highly correlated with the ambient temperature, and the calculated correlation coefficient is 0.849, while the change of inlet and outlet temperature is slightly behind the ambient temperature. The variation law between the inlet and outlet temperature difference of the heat collecting wall and the outdoor wind temperature is explored, and the Figure 15 below shows the outdoor temperature at P1 and the curve chart of the inlet and outlet temperature of the heat collecting wall. It can be seen that the temperature difference between inlet and outlet is highly correlated with the ambient temperature, and the calculated correlation coefficient is 0.849, while the change of inlet and outlet temperature is slightly behind the ambient temperature.

Airflow Velocity in the Cavity
During winter, the vents on the glass structure of heat collection walls are closed, and the airflow is sent in from the lower tuyere and out from the upper tuyere. As shown in Figure 16, through the analysis of the calculated data, it is found that the correlation coefficient between the airflow velocity in cavity and outdoor temperature is 0.624, while the correlation coefficient between the airflow velocity in cavity and outdoor wind speed is very small. The variation curve of average air velocity and outdoor temperature in the cavity is drawn as follows:

Airflow Velocity in the Cavity
During winter, the vents on the glass structure of heat collection walls are closed, and the airflow is sent in from the lower tuyere and out from the upper tuyere. As shown in Figure 16, through the analysis of the calculated data, it is found that the correlation coefficient between the airflow velocity in cavity and outdoor temperature is 0.624, while the correlation coefficient between the airflow velocity in cavity and outdoor wind speed is very small. The variation curve of average air velocity and outdoor temperature in the cavity is drawn as follows: Figure 15. Variation of temperature difference between inlet and outlet at P1.

Airflow Velocity in the Cavity
During winter, the vents on the glass structure of heat collection walls are closed, and the airflow is sent in from the lower tuyere and out from the upper tuyere. As shown in Figure 16, through the analysis of the calculated data, it is found that the correlation coefficient between the airflow velocity in cavity and outdoor temperature is 0.624, while the correlation coefficient between the airflow velocity in cavity and outdoor wind speed is very small. The variation curve of average air velocity and outdoor temperature in the cavity is drawn as follows: Figure 16. Change of airflow velocity and outdoor temperature at P1.

Heat Collecting Efficiency
The heat supplied to the room by the heat collection wall outlet is calculated as follows: The thermic heat collecting efficiency of the heat collection wall is defined as follows: Figure 16. Change of airflow velocity and outdoor temperature at P1.

Heat Collecting Efficiency
The heat supplied to the room by the heat collection wall outlet is calculated as follows: The thermic heat collecting efficiency of the heat collection wall is defined as follows: Based on the above data calculation, the following curve of the heat supplied by the vent at the measuring point is obtained as shown in Figure 17.
Based on the above data calculation, the following curve of the heat supplied by the vent at the measuring point is obtained as shown in Figure 17. As per Table 8, the average heat collection efficiency of the heat collection wall at each measuring point is 19%, and the average heat supply of the tuyere at P1 and P2 is relatively smaller. In the future, the corresponding optimization structure of the heat collection wall is required to achieve a comfortable and ideal indoor thermal environment.  As per Table 8, the average heat collection efficiency of the heat collection wall at each measuring point is 19%, and the average heat supply of the tuyere at P1 and P2 is relatively smaller. In the future, the corresponding optimization structure of the heat collection wall is required to achieve a comfortable and ideal indoor thermal environment.  Figure 18 shows the average value of the total ventilation volume at every measured and calculated point and Figure 19 shows the ventilation quantity by thermal pressure and wind pressure at P1. It is found that the ventilation volume on the east and west sides of the building first increases and then decreases with an increase in height, while at the middle of the building, ventilation volume has no prevalent trend with the changes in height.    Figure 19 shows the effect of ventilation volume caused by hot pressure and wind pressure at measuring point 1. Ten sets of data are selected for calculation every day. It can be seen that the ventilation volume caused by wind pressure is very small. In the vertical direction, the ventilation quantity due to thermal pressure is stable, while in the horizontal direction, the total ventilation quantities of east and west are greater than the middle. Moreover, the ventilation volume of the topmost floor is larger than that of the lower floor.

Conclusions
In this paper, the near-wall microclimate of the three buildings in Zhengzhou was measured in winter and summer, trying to find the variation law of outdoor temperature and attached airflow velocity with height. Through the establishment of a typical heat Figure 19. The ventilation quantity by thermal pressure and wind pressure at P1. Figure 19 shows the effect of ventilation volume caused by hot pressure and wind pressure at measuring point 1. Ten sets of data are selected for calculation every day. It can be seen that the ventilation volume caused by wind pressure is very small. In the vertical direction, the ventilation quantity due to thermal pressure is stable, while in the horizontal direction, the total ventilation quantities of east and west are greater than the middle. Moreover, the ventilation volume of the topmost floor is larger than that of the lower floor.

Conclusions
In this paper, the near-wall microclimate of the three buildings in Zhengzhou was measured in winter and summer, trying to find the variation law of outdoor temperature and attached airflow velocity with height. Through the establishment of a typical heat collection wall mathematical model and quantitative analysis of its thermal performance, the following conclusions were drawn: 1.
In the vertical direction, the temperature of the building's near-wall showed an Sshaped fluctuation with an increase in height. The lower the building height, the smaller fluctuation amplitude. The average amplitude of the four tests in winter is 1.37 • C, 0.43 • C, 0.39 • C and 0.27 • C, respectively. The temperature of the measuring point at the middle of the building in the horizontal direction is higher than that on the side with a maximum average temperature difference of 3.11 • C.

2.
In the vertical direction, the airflow velocity attached to the building facade increases with the increase in the surface layer and falls slightly or remains flat on the top floor. Horizontally, the side of the building is more susceptible to ambient air distribution, and the wind speed reaches up to 2.146 times that of the middle part in winter. The smaller the size coefficient is, the smaller the variation range of airflow velocity is. The maximum difference of the average wind speed ratio of the four periods in winter is 9.4%, 8.3%, 28.8% and 21.4%, respectively. 3.
By numerical calculation, during daytime in winter, the average temperature difference between inlet and outlet is 12.05 • C, and the highest recorded was 20.61 • C, and the average heat collection efficiency is 0.19. At night, the attenuation coefficient and delay phase of the heat collection wall with its ventilation holes closed are higher than those of ordinary walls without heat collection structures. The feasibility of heat collection walls in the Zhengzhou area is proven.

4.
The winter calculation results show that the temperature difference between the inlet and outlet of the air layer in the heat collection wall is highly correlated with the environmental temperature, with a correlation coefficient of 0.849. The correlation coefficient between the air velocity and the outdoor temperature is 0.624.

5.
Calculation results in summer show that in vertical direction, hot pressure ventilation rate plays a major role in the ventilation process. As for horizontal direction, the total ventilation is larger on the side of the building, and the less in the middle, while the ventilation on the topmost floor is larger than that on the lower floor. In the application of heat collection walls in a high-rise building, different structures and sizes must be designed in different parts of the building to achieve the optimal indoor environment and energy-saving effect.

Institutional Review Board Statement: Not applicable.
Informed Consent Statement: Informed consent was obtained from all subjects involved in the study.

Data Availability Statement: Data available on request.
Acknowledgments: This research was supported by a grant from the National Natural Science.

Conflicts of Interest:
The authors declare no conflict of interest. The funders had no role in the design of the study; in the collection, analyses, or interpretation of data; in the writing of the manuscript, or in the decision to publish the results.

Nomenclature
Parameters t out Near-wall temperature of the five measuring points, • C T out Outdoor environmental temperature, • C t in Indoor temperature of the five measuring points, • C v1, v2, v3, v4, v5 Attached