Mortars with Crushed Lava Granulate for Repair of Damp Historical Buildings

In this paper, crushed lava granulate was used as full silica sand replacement in composition of repair mortars based on hydrated lime, natural hydraulic lime, or cement-lime binder. Lava granules were analyzed by X-ray fluorescence analysis (XRF), X-ray diffraction (XRD), and scanning electron microscopy (SEM). Particle size distribution of both silica and lava aggregates was assessed using standard sieve analysis. Hygrothermal function of the developed lightweight materials was characterized by the measurement of complete set of hygric, thermal, and structural parameters of the hardened mortar samples that were tested for both 28 days and 90 days cured specimens. As the repair mortars must also meet requirements on mechanical performance, their compressive strength, flexural strength, and dynamic Young’s modulus were tested. The newly developed mortars composed of lava aggregate and hydrated lime or natural hydraulic lime met technical, functional, compatibility, and performance criteria on masonry and rendering materials, and were found well applicable for repair of historically valuable buildings.


Introduction
Historical structures plastered with valuable and highly decorative facades are an essential part of our cultural heritage. Various kinds of mortars and plasters have been utilized all over the world from ancient times to modern days. In this sense, over time, their composition and in particular binder components have changed, from clearly natural materials, often represented by clays [1][2][3], to traditional binders, such as air lime [4][5][6][7], natural hydraulic lime [8][9][10][11][12], and their combination with natural or/and artificial pozzolans (diatomaceous earth, tuffs, zeolite, pumice, etc.) [13][14][15]. Brick dust is also considered a traditional component of mortars since its usage in lime mortars dates from the Minoan period through the ancient Greek and Roman civilizations [16]. Based on materials and production technology available, until the 1850s, air-lime blended with natural pozzolans was the main binder for rendering and plastering purposes [17]. With industry development at the end of 19th century, the first artificial hydraulic lime and later Portland cement (PC) and its decorative derivation, white cement, appeared. These made more strengthened plastering layers to resist weathering, moisture induced corrosion, and freeze/thaw cycles [18]. Based on that, PC became the prevailing binder of the construction industry and thereby also for mortars production. On the other hand, remarkably preserved buildings and ruins of structures aged hundreds or even thousand of years Incorporation of innovative high thermal insulating aggregates, e.g., aerogels, has also been studied but their presence on the market is still at a low level [48][49][50].
Because most of the commercially produced thermal insulation plasters does not meet requirements of cultural heritage authorities, new types of lightweight mortars for repair of historical buildings have been designed and tested in this study. As stated above, a general consensus accepted by the cultural heritage authorities and researchers working in the field of repairing historical valuable buildings is that the use of cement-based mortars is not a proper solution for buildings rendered and constructed from air lime-and natural hydraulic lime-based mortars. On the other hand, in buildings built from the end of the 19th century and in 20th century, PC became the prevailing binder. In these structures, the cement-based repair mortars can find use as well as cement-lime mortars and materials where part of the PC is replaced with pozzolanic admixtures. Therefore, the aim of the presented work was to use in the composition of mortars binders compatible with the original, e.g., hydrated lime, natural hydraulic lime, and PC-hydrated lime blend. As reported by Tchamdjoua [51], volcanic aggregates based on volcanic tuff can be advantageously used in mortars production. By the use of these types of aggregates, weight reduction, enhanced thermal insulation function, and improved workability can be achieved. As the use of volcanic aggregates dates back to the ancient times [52][53][54], applied lava granulate undoubtedly meets demands of the cultural heritage community on the use of natural, compatible, and functional materials in buildings repair. Moreover, the natural volcanic rock did not need any expensive and high energy demand processing compared, e.g., to the production of expanded clays-based aggregates. Based on a detailed review of published papers, no publication was found in scientific databases on the use of lava aggregates in mortars composition within the last 30 years, which is what clearly documents the novelty of the presented work. For newly developed mortars with lava aggregate, a unique set of structural, mechanical, hygric, and thermal properties was experimentally assessed, allowing assessment of the applicability of the developed mortars in repair and repointing of historical masonry and plastering.

Experimental
Hydrate lime-(HL), natural hydraulic lime-(NHL), and PC (Portland cement) -HL blend-based mortars were the subject of the extensive experimental campaign. In newly developed mortars, silica sand was fully replaced by crushed lava granulate. First, the raw materials used for mortars production were characterized in detail. Charaterization comprised assessment of their chemical and mineralogical composition, basic physical parameters, particle size distribution, and testing of lava pozzolanic activity and SEM morphology. The obtained data were then considered in mortar mix design. The casted mortar samples were cured for 28 days and 90 days, respectively. For the hardened mortar samples, the complete set of structural, mechanical, hygric, and thermal properties was experimentally assessed. Finally, the microstructure morphology of the fractured surface of the hardened samples was observed and analyzed using SEM.

Materials and Design
Commercial hydrated lime HL CL90-S (Čertovy Schody, Inc., Lhoist group, Tmaň, Czech Republic), natural hydraulic lime NHL 3.5 (Zement-und Kalkwerke Otterbein GmbH & Co. KG, Großenlüder, Germany), and laboratory prepared blend of HL CL90-S and PC CEM I 42.5 R (Českomoravský cement Inc., Radotín, Czech Republic) were used as binders in 3 prepared groups of mortar mixes. Each mortars group consisted of reference samples made of silica sand, and samples with crushed lava granulate fully replaced silica aggregate. The composition of mortar mixtures considered the constant binder/aggregate volume ratio of 1:1.15 based on a practical point of view, historical traditions, and results obtained by Lanas et al. [55]. Silica sand of particle size fraction 0-2 mm (Filtrační písky s.r.o., Chlum u Doks, Czech Republic) was mixed from three normalized sand fractions 0-0.5 mm, 0.5-1 mm, and 1-2 mm. The weight ratio of the particular sand fractions was 1:1:1. Lava granulate, the fine fraction 0/2 mm, came from Der Naturstein Garten, Hillscheid, Germany. The dosage of batch water was adjusted to get similar consistency of all studied mortars. Based on years of practical experience, the mortar mixtures were prepared using the correct amount of water required to obtain normal consistency and a good workability of the mortars (160 ± 5 mm; measured by the flow table test [56]). This consistency of lime mortars enables their easy application during rendering and good adhesion to the substrate. The composition of tested mortars is given in Table 1, where HL-R stands for a reference lime mortar, HL-LA is a lime mortar with lava granulate, PCHL-R and PCHL-LA are cement-lime mortars with silica and lava aggregates, NHL-R is a natural hydraulic lime reference mortar, and NHL-LA is a natural hydraulic lime mortar with lava aggregate. Mortar samples were prepared and tested according to European standards EN 10115-2 [57] and EN 196-1 [58]. The test specimens were standard prisms 40 mm × 40 mm × 160 mm, and circular plate specimens having 30 mm thickness and diameter of 120 mm. The freshly casted samples were covered by PE foil and sprayed for 2 days by water in order to avoid their cracking, and after demolding stored for 26 days at a highly humid environment RH (95 ± 5%) at a temperature (22 ± 2 • C). Then, they were stored freely in a laboratory. In this way, high relative humidity favored the pozzolanic reaction and the hydration of anhydrous calcium silicates. On the other hand, curing at laboratory conditions allowed carbonation of hydrated lime mortars. The experimental tests were conducted for 28 days and 90 days hardened samples.

Binders Characterization
Among the basic physical characterization of HL, NHL, and PC, their loose bulk density, specific density, specific surface, and particle size distribution were assessed. The loose bulk density was obtained on a gravimetric principle, i.e., from the measurement of dry sample mass and its volume. The specific density was determined on the helium pycnometry principle using Pycnomatic ATC (Thermo Scientific, Milan, Italy). The particle size distribution was analyzed by an Analysette 22 Micro Tec plus (Fritsch, Idar-Oberstein, Germany) working on a laser diffraction principle. The Blaine specific surface was measured in accordance with the EN 196-6 [59].
For the measurement of chemical composition of applied binders, an ARL QUANT´X EDXRF Spectrometer (Thermo Scientific, Madison, WI, USA), equipped with a Rh X-Ray tube and Si(Li) detector crystal was used. The resulting data were collected and evaluated by the UniQuant ED 6.32 software (Thermo Scientific, West Palm Beach, FL, USA). The relative accuracy was 0.5% to 5.0%, depending on the standards quantity and concentration of analyzed substances.
X-ray diffraction (XRD) data were collected by PANalytical Empyrean XRD (Malvern Panalytical Ltd., Royston, UK) with Cu-Kα as the radiation source (λ = 1.540598 Å for Kα1, accelerating voltage 45 kV, beam current 40 mA, diffraction angle 2θ in the range from 5 • to 80 • with a step scan of 0.01 • . Data evaluation was performed by HighScore Plus software 4.8 (Malvern Panalytical Ltd., Royston, UK) version 3.0 using ICDD and ICSD databases.
The basic physical properties and particles size distribution parameters of applied binders are given in Table 2. The highest Blaine fineness exhibited HL, the lowest PC, and that of NHL was in the middle. This was in agreement with the loose bulk density and specific density data. The measurement of particle size distribution revealed that NHL was coarser compared to HL and PC, but still sufficient for binding purposes. The binders' chemical and phase composition measured by XRF and XRD analyses are shown in Table 3. It complies with the nature of analyzed binders. The main constituent of HL was CaO coming from calcination of calcite. NHL was formed mainly from CaO, hydraulic oxides were present in a limited extent, only similarly as reported by Luo et al. [60]. Main oxides contained in PC were SiO 2 , Al 2 O 3 , Fe 2 O 3 , and CaO, which are typical constituents of Portland clinker [61]. NHL and PC contained significant amounts of amorphous phases. On the other hand, HL was fully crystalline. In HL, the main crystalline phase was Portlandite. In NHL, the main mineralogical phases present were Larnite, Calcite, and Portlandite. On similar NHL phase composition reported, e.g., Grilo et al. [62]. The major mineral phases in PC were Alite, Aluminate, Larnite, and Brownmillerite [61].

Aggregates Testing
For silica and lava sand, basic physical parameters (loose bulk density, specific density) and chemical composition were measured using similar methods applied for binder analyses (see Section 2.2). As the laser diffraction method working device is not designed for measurement of coarser particles, the aggregate grain size analysis was performed using the standard sieve method according to the EN 933-1 [63] with sieves of the following mesh dimensions: 0.063; 0.125; 0.25; 0.5; 1.0; 2.0 mm. The water absorption was measured for samples immersed for 24 h in water as prescribed in the EN 1097-6 [64]. Moreover, pozzolanic activity of lava fine fraction was tested. The modified Chapelle method was used for assessment of the pozzolanic activity according to the standard NF P 18-513 [65]. The test is based on the reaction of 1 g of tested material in powder form with 2 g CaO in 0.25 L of water. The results, which are expressed in mg Ca(OH) 2 fixed by 1 g of sample [66], give the straight information about the pozzolanic activity [67]. The morphology of lava particles was investigated using scanning electron microscope (SEM) Tescan Mira3 (TESCAN Brno, Ltd., Brno, Czech Republic). Elemental composition and mapping were performed using an energy dispersive spectroscopy (EDS) analyzer with XFlash 6/10 detector (Bruker AXS GmbH, Karlsruhe, Germany) and Quantax 400 software (Bruker AXS GmbH, Karlsruhe, Germany).
The loose bulk density and specific density of both used aggregates are introduced together with information on pozzolanic activity in Table 4. The ratio of loose bulk density and specific density, which was 0.63 for silica sand and 0.46 for lava granulate, gave information on lava porosity which was important for lightening of the mortar matrix and improvement of other related functional parameters, such as hygric and thermal. On lava porosity, evidence also resulted in water absorption that was 1.57% for silica sand and 8.73% for lava sand. Particle size distribution of silica and lava aggregates is graphed in Figure 1. Lava aggregate contained higher amounts of smaller particles compared to silica sand. Nevertheless, both types of aggregates had particle size in the 0-2 mm range. The results, which are expressed in mg Ca(OH)2 fixed by 1 g of sample [66], give the straight information about the pozzolanic activity [67]. The morphology of lava particles was investigated using scanning electron microscope (SEM) Tescan Mira3 (TESCAN Brno, Ltd., Brno, Czech Republic). Elemental composition and mapping were performed using an energy dispersive spectroscopy (EDS) analyzer with XFlash 6/10 detector (Bruker AXS GmbH, Karlsruhe, Germany) and Quantax 400 software (Bruker AXS GmbH, Karlsruhe, Germany). The loose bulk density and specific density of both used aggregates are introduced together with information on pozzolanic activity in Table 4. The ratio of loose bulk density and specific density, which was 0.63 for silica sand and 0.46 for lava granulate, gave information on lava porosity which was important for lightening of the mortar matrix and improvement of other related functional parameters, such as hygric and thermal. On lava porosity, evidence also resulted in water absorption that was 1.57% for silica sand and 8.73% for lava sand. Particle size distribution of silica and lava aggregates is graphed in Figure 1. Lava aggregate contained higher amounts of smaller particles compared to silica sand. Nevertheless, both types of aggregates had particle size in the 0-2 mm range. The Chapelle test showed fixation of 746 mg Ca(OH)2/g of lava aggregate fine fraction (particle size <0.063 mm), which proved its reactivity in lime-and cement-based blends. According to Raverdy et al. [68][69][70][71][72][73][74], material is considered as pozzolana active if its Chapelle reactivity is ≥650 mg of Ca(OH)2/g of material. This condition was safely fulfilled.
The chemical and phase composition of silica and lava sand measured by EDXRF spectrometer and XRD analysis is presented in Table 5. In lava sand, SiO2 and Al2O3 prevailed, which is in compliance with the Chapelle test result. According to the total alkali-silica (TAS) classification diagram (dependence of (Na2O + K2O) wt.% content on SiO2 wt.% content) for volcanic rocks, the applied lava sand belongs to ultrabasic basaltic rocks, namely, tephrites [69]. As reported, e.g., by Wakizaka [70] and Jozwiak-Niedzwiedzka [71], igneous rocks containing volcanic glass can be potentially dangerous in terms of alkali silica reaction (ASR). However, it was not this case, because alkali volcanic rocks-based aggregates are deleterious in terms of ASR, as their chemical composition expressed in wt.% exhibits the following chemical character: SiO2 > 50%, K2O > 3%, CaO < 5%, and The Chapelle test showed fixation of 746 mg Ca(OH) 2 /g of lava aggregate fine fraction (particle size <0.063 mm), which proved its reactivity in lime-and cement-based blends. According to Raverdy et al. [68][69][70][71][72][73][74], material is considered as pozzolana active if its Chapelle reactivity is ≥650 mg of Ca(OH) 2 /g of material. This condition was safely fulfilled.
The chemical and phase composition of silica and lava sand measured by EDXRF spectrometer and XRD analysis is presented in Table 5. In lava sand, SiO 2 and Al 2 O 3 prevailed, which is in compliance with the Chapelle test result. According to the total alkali-silica (TAS) classification diagram (dependence of (Na 2 O + K 2 O) wt.% content on SiO 2 wt.% content) for volcanic rocks, the applied lava sand belongs to ultrabasic basaltic rocks, namely, tephrites [69]. As reported, e.g., by Wakizaka [70] and Jozwiak-Niedzwiedzka [71], igneous rocks containing volcanic glass can be potentially dangerous in terms of alkali silica reaction (ASR). However, it was not this case, because alkali volcanic rocks-based aggregates are deleterious in terms of ASR, as their chemical composition expressed in wt.% exhibits the following chemical character: SiO 2 > 50%, K 2 O > 3%, CaO < 5%, and MgO < 3% [72]. Silica sand was fully crystalline. In lava sand, a high amount of silica and alumina amorphous phases was identified, which clearly explained its pozzolanic activity. The morphology of lava particles analyzed using SEM is apparent from Figure 2. The lava aggregate is made up of crushed volcanic rock particles of different shape, particle size, and angular edges. The high magnification made it possible to observe rugged morphology of lava particles with irregular/uneven sub-conchoidal fracture. MgO < 3% [72]. Silica sand was fully crystalline. In lava sand, a high amount of silica and alumina amorphous phases was identified, which clearly explained its pozzolanic activity. The morphology of lava particles analyzed using SEM is apparent from Figure 2. The lava aggregate is made up of crushed volcanic rock particles of different shape, particle size, and angular edges. The high magnification made it possible to observe rugged morphology of lava particles with irregular/uneven sub-conchoidal fracture.  The distribution of particular elements forming lava particles obtained by EDS is shown in Figure 3. No clustering was observed, i.e., all the analyzed elements in the studied sample were homogenously distributed. The distribution of particular elements forming lava particles obtained by EDS is shown in Figure 3. No clustering was observed, i.e., all the analyzed elements in the studied sample were homogenously distributed.

Methods for Testing Hardened Mortar Samples
The measurement of hardened mortar specimens was conducted for 28 days and 90 days for the matured samples.
The basic physical and structural characterization of hardened materials was done using the measurement of bulk density, specific density, and open porosity. In these tests, 5 samples that were vacuum dried at 60 °C were examined. The specific density ρs (kg/m 3 ) was obtained by helium pycnometry similarly as in the binders' characterization (see Section 2.2). The dry bulk density ρb (kg/m 3 ) was determined in accordance with the EN 1015-10 [73]. The expanded combined uncertainty of the bulk density test was 1.4%. The total open porosity ψ (%) was calculated based on the bulk density and specific density tests results as formulated in Equation (1):

Methods for Testing Hardened Mortar Samples
The measurement of hardened mortar specimens was conducted for 28 days and 90 days for the matured samples.
The basic physical and structural characterization of hardened materials was done using the measurement of bulk density, specific density, and open porosity. In these tests, 5 samples that were vacuum dried at 60 • C were examined. The specific density ρ s (kg/m 3 ) was obtained by helium pycnometry similarly as in the binders' characterization (see Section 2.2). The dry bulk density ρ b (kg/m 3 ) was determined in accordance with the EN 1015-10 [73]. The expanded combined uncertainty of the bulk density test was 1.4%. The total open porosity ψ (%) was calculated based on the bulk density and specific density tests results as formulated in Equation (1): The expanded combined uncertainty of the total open porosity test was 2.0%. Among the mortars' mechanical parameters, dynamic Young's modulus, flexural strength, and compressive strength were measured. For the particular mortar mixes, 5 prisms having size 40 mm × 40 mm × 160 mm were tested. First, the dynamic Young's modulus E d (GPa) was measured using a DIO 562 apparatus (Starmans Electronic, Prague, Czech Republic) working on the frequency of 50 kHz. The ultrasonic pulse method was based on measurement of the travel time of the ultrasonic wave passing through the material. The relationship between E d (GPa), wave velocity ν (m/s), and bulk density ρ b (kg/m 3 ) is given by Equation (2): As the moisture presence significantly affects propagation of ultrasonic waves, the tested specimens were dried at 60 • C in a vacuum dry kiln VACUCELL 22 ECO line (BMT Medical Technology Ltd., Brno, Czech Republic). The expanded combined uncertainty of this test was 1.7%.
Both strength tests were conducted in accordance with European standard EN 1015-11 [74]. Three-point bending strength test arrangement with a 100 mm span was used in the flexural strength f f (MPa) testing. On the fragments of broken specimens from the flexural strength test, the compressive strength f c (MPa) was assessed. The loading in the compressive strength test was 40 mm × 40 mm. The relative expanded uncertainty of these strength tests was 1.4%.
The ability of the studied mortar to absorb liquid water was described by the measurement of the water absorption coefficient and apparent moisture diffusivity. The free water intake experiment conducted in accordance with EN 1015-18 [75] was used for the determination of the water absorption coefficient A w (kg/(m 2 ·s 1/2 )) and capillary water content w cap (kg/m 3 ). The test was performed in an automatic arrangement, i.e., changes in specimen mass were continuously recorded and the contact of the sample surface with water reservoir was not interrupted throughout the test. Using the original procedure proposed by Kumaran [76], the apparent moisture diffusivity κ app (m 2 /s) was calculated [77]. The expanded combined uncertainty of the water absorption test was 2.3%, and that of the apparent moisture diffusivity test was 3.5%.
For repair mortars, the ability to transport water vapor is of the particular importance. The water vapor transmission in tested materials was characterized by the measurement of the water vapor diffusion coefficient D (m 2 /s), water vapor resistance factor µ (−), and water vapor permeability δ (s). These parameters were tested using the cup method following the standard ISO 12572 [78]. Both the dry-cup and wet-cup arrangements of the test were applied. For the cup tests, circular plater specimens of 30 mm thickness and diameter of 120 mm were used. The 28-days samples placed in alumina cups were cured in a climatic chamber CLIMACELL 111 (BMT Medical Technology Ltd., Brno, Czech Republic) at (23 ± 0.5 • C) and RH (50 ± 5%) until their constant mass was reached. In the dry cup test, the cup contained silica gel, i.e., the relative humidity ratio simulated under and above the specimen was 2%/50% RH. In the wet-cup experiment, the humidity ratio was 93%/50% RH and the high RH inside the cup was obtained by saturated solution of KNO 3 . For each tested mortar, 5 specimens in the dry-cup test and 5 specimens in the wet-cup test were examined. The expanded combined uncertainty of the water vapor diffusion test was 2.0% for D, 2.8% for µ, and 2.1% for δ.
As anticipated, the use of lava granulate in mix composition should improve mortars' thermal properties. The investigated thermal parameters, the thermal conductivity λ W/(m·K), and volumetric heat capacity C v (J/(m 3 ·K)), were tested in the dependence on moisture content, from the dry state to the fully water saturated state. These tests were done at laboratory temperature (23 ± 2 • C) using an ISOMET 2114 device (Applied Precision, Ltd., Bratislava, Slovakia). ISOMET 2114 operates on a transient technique based on recording temperature changes induced by heat impulse generated by the sensor [79]. The measurement accuracy was 5% of reading + 0.001 W/(m·K) for the thermal conductivity in the range 0.015-0.70 W/(m·K), and 10% of reading for the thermal conductivity ranging from 0.70 W/(m·K) to 6.0 W/(m·K). The accuracy of the volumetric heat capacity was 15% of reading +1 × 10 3 J/(m 3 ·K). For each mortar type, 3 cubic samples having size of 70 mm matured for 90 days were tested using circular surface probe IPS 1105 (Applied Precision Ltd., Bratislava, Slovakia).
The microstructure morphology of fractured surface of mortar samples was determined on 90-days samples using scanning electron microscope (SEM) Tescan Mira3 (TESCAN Brno, Ltd., Brno, Czech Republic).

Results and Discussion
The basic structural parameters of tested mortars cured for 28 days and 90 days are summarized in Table 6. The porosity, which was considered the main parameter affecting overall mortars performance, decreased slightly with curing time. It was due to the continuous hydration and carbonation. Nevertheless, these differences in the porosity values and thus in the bulk density and specific density, in time, can be considered as inconspicuous and have no practical sense for mortars use. On the other hand, substitution of silica sand with lava aggregate markedly increased the porosity of all examined mortars which was good for their presumed application in repair of historical damp masonry and facades. The increase in porosity of 28-days samples was approximately 27% for HL-LA, 21% for PCHL-LA, and 27% for NHL-LA. The increase in porosity was assigned to porosity of lava particles, their irregular shape, and higher amount of batch water in mixes with lava aggregate. Accordingly, the bulk density values were for all mortars with lava aggregate lower compared to that of corresponding reference mortars. It clearly demonstrated lightening of mortar structure by the use of lava aggregate. Looking at the obtained data from the point of view of the effect of applied binders, the lowest porosity values were obtained for mortars on the basis of the PC/HL blend. The use of HL and NHL gave almost similar porosity, which was about 15% higher in the case of reference mortars and about 20% higher in the case of mortars with lava aggregate compared to values obtained for PCHL-R and PCHL-LA, respectively. Similar porosity values of NHL reference mortars were obtained recently, e.g., Garijo et al. [80]. Accordingly, Pachta et al. [81] received lime mortar with sand of siliceous origin porosity of 31%, which was in agreement with porosity value of control lime mortar. Palomar at al. [82] measured cement-lime mortars porosity of 25.6%. It was close to the porosity of PCHL-R.
The mechanical parameters of the hardened mortars are summarized in Tables 7 and 8. In addition, the strength data is for the sake of comparison graphed in Figure 4. The values of the tested mechanical characteristics of the control materials corresponded with the porosity data and with the character of applied binders. The mortars with lava sand had, for all studied mixes, higher mechanical resistance than reference materials. This was due to the rigid matrix of lava particles having higher mechanical strength compared to silica sand. Also, the pozzolanic activity of the lava fine particles contributed to the total mechanical resistance of lava-based mortars. binder. In this way, the parameters of mortars can be simply modified. In literature, the values of Young's modulus of cement-lime mortars were found to be significantly different, ranging from 3 GPa to 24 GPa [84]. In this sense, the Ed values obtained for PCHL-R and PCHL-LA were approximately in the middle of this interval.  Unfortunately, as stated above, the use of PC in repair of historically valuable buildings is mostly forbidden by cultural heritage authorities. One of the reasons is mechanical incompatibility of the cement-based materials with those original [84] as rendering and masonry mortars should be considerably weaker than the old masonry to accommodate slight movements of the buildings and their structural elements. From this point of view, moderate mechanical resistance of NHL-based  The highest mechanical resistance yielded cement-lime mortar, both reference and lava modified mixes. This was mainly due to the high content of PC in the blended binder. According to Ramesh et al. [83], the open porosity of cement-lime mortar increases with the lime dosage in the binder. In this way, the parameters of mortars can be simply modified. In literature, the values of Young's modulus of cement-lime mortars were found to be significantly different, ranging from 3 GPa to 24 GPa [84]. In this sense, the E d values obtained for PCHL-R and PCHL-LA were approximately in the middle of this interval.
Unfortunately, as stated above, the use of PC in repair of historically valuable buildings is mostly forbidden by cultural heritage authorities. One of the reasons is mechanical incompatibility of the cement-based materials with those original [84] as rendering and masonry mortars should be considerably weaker than the old masonry to accommodate slight movements of the buildings and their structural elements. From this point of view, moderate mechanical resistance of NHL-based mortar is highly promising for its intended use in repair works. Building practice classifies mortars based on their 28-days compressive strength according to the European standard EN 998-1 [85]. In this respect, mortar HL-LA can be classified into category CS I (f c in the range 0.4-2.5 MPa), material NHL-LA into category CS II (f c in the range 1.5-5.0 MPa), and mortar PCHL-LA ranks into class CS IV (f c > 6.0 MPa). On the other hand, this standard does not pose any exact requirement on mechanical resistance of repair mortars. In literature, different requirements on the minimum mechanical resistance of mortars for repair or replacement of traditional lime-based rendering mortars are reported. In comprehensive review of the design and behavior of traditional lime-based renders, Nogueira et al. [86] recommended the minimum compressive strength from 0.4 to 2.5 MPa, and the minimum flexural strange in the range 0.2-0.7 MPa. In this respect, lime-based mortar with lava aggregate was acceptable for repair purposes, and NHL-based mortar even exceeded the minimum demands on mechanical resistance.
The parameters characterizing the ingress of liquid water into studied mortars are introduced in Table 9. The use of lava granulate led mostly to the slight decrease in the water absorption coefficient. This can be assigned to the changes in mortars pore size distribution by the use of lava granulate. European standard EN 998-1 [85] requires repair mortars capillary water absorption > 0.30 kg/(m 2 ·s 1/2 ), which met mortars based on HL and NHL. According to the standard EN 998-1 [85], HL-NHL-based mortars were categorized into class W I (A w ≤ 0.4 kg/(m 2 ·s 1/2 ). Quantitatively similar moisture absorption observed, e.g., Pavlíková et al. 2019 [87] who obtained lime-based repair mortar A w = 0.32 kg/(m 2 ·s1 /2 ) [84]. Also, Fusade et al. [88] obtained NHL mortars water absorption coefficient in the range 0.30-0.379 kg/(m 2 ·s1 /2 ). The lower porosity of cement-lime mortar and the structure of PC hydrates were the cause of low water absorption. Therefore, PCHL-R and PCHL-LA mortars were found to be not suitable materials for repair of damp masonry, where high water absorption in time is the positive effect, as it would enable the mortar to better absorb moisture from the surrounding masonry and help it dry out as stated by Fucade et al. [88].
As the capillary water content increased with lava aggregate use, the apparent moisture diffusivity decreased. This is an interesting feature, pointing to the presence of bigger pores in mortars with lava that allowed high water absorption, but the gravity effect decelerated the moisture ingress. In these pores, capillary activity competed with gravity force.
The data on water vapor transmission parameters obtained for 28-days cured samples are given in Table 10. As reported in other studies [87,89,90], water vapor transmission, in the case of the wet-cup test, was slightly faster compared to dry-cup test results. This can be attributed to the filling of pores with water molecules, which reduced binding forces between water vapor molecules and surface of the pores that decelerate water vapor transport in the case of dry materials. The water vapor resistance factor of repair mortars for external elements must be ≤15, which is the limit required by EN 988-1 [85]. This demand safely met mortars based on HL and NHL. Thus, the encouraging results documenting high water vapor permeability of these materials can be from the point of view of possible water evaporation from damp laden masonry recommended for restoration projects. Similar results of water vapor transmission properties measured, e.g., Silva et al. [91] who analyzed the influence of natural hydraulic lime content on the properties of aerial lime-based mortars. For lime-based mortar, the authors obtained porosity of approximately 26% and δ = 1.47 × 10 −11 s, for mortars made of lime and NHL blends, δ = 1.49-1.38 × 10 −11 s. Accordingly, Bianco at al. [92] determined that for mortar composed of NHL as binder, with the addition of 2 wt.% of metakaolin µ = 10. On the contrary, cement-lime mortars exhibited a much higher water vapor resistance factor than required by European standard. It is not surprising, as cement mortars and highly hydraulic mortars have excessive hardness, stiffness, and are impermeable for water in both liquid and gaseous forms [93]. On this account, as their use in repair of historical buildings would have adverse effects, their use in restoration application should be avoided.
Heat transport and storage parameters acquired for 90-days samples in dependence on moisture content are shown in Figures 5 and 6. As confirmed by many researchers in recent decades, the thermal properties of the porous construction materials are significantly affected by moisture content [49,94,95]. This is due to the high thermal conductivity of water (λ w = 0.56 W/(m·K) at 20 • C) compared to dry air (λ a = 0.025 W/(m·K) at 20 • C) [96] that fills the materials pores. If only a part of the pore space is filled by water, the cavities contain humid air having different thermal characteristics than the dry air.
observed differences in Cv values can be accounted as negligible, i.e., the replacement of silica sand with lava aggregate had no distinct effect on the heat storage capacity of the examined mortars. The dependence of the heat storage on the moisture presence in mortar samples was not significant and apparent as in the case of moisture dependent thermal conductivity. This was due to the volumetric heat capacity of water that is only about 3 times higher compared to the volumetric heat capacity of dry mortar samples. The microstructure morphology of the fractured surface of mortar samples determined for 90-days samples using SEM is shown in Figure 7a-c. The SEM analysis allowed identification of lava grains covered and interconnected with Portlandite, CSH-gels, and in the case of PCHL-LA also with Ettringite. At first sight, the microstructure of the particular studied mortars differed. Mortar PCHL-LA had, in comparison with the other two mortars, a denser and more compact structure, which was in agreement with its lowest porosity and binder type. On the other hand, pores having size in the m range were observed in materials HL-LA and NHL-LA. It was evident that the highly porous microstructure of HL-and NHL-based mortars was the reason behind their high water absorption, high water vapor permeability, and low thermal conductivity. with lava aggregate had no distinct effect on the heat storage capacity of the examined mortars. The dependence of the heat storage on the moisture presence in mortar samples was not significant and apparent as in the case of moisture dependent thermal conductivity. This was due to the volumetric heat capacity of water that is only about 3 times higher compared to the volumetric heat capacity of dry mortar samples. The microstructure morphology of the fractured surface of mortar samples determined for 90-days samples using SEM is shown in Figure 7a-c. The SEM analysis allowed identification of lava grains covered and interconnected with Portlandite, CSH-gels, and in the case of PCHL-LA also with Ettringite. At first sight, the microstructure of the particular studied mortars differed. Mortar PCHL-LA had, in comparison with the other two mortars, a denser and more compact structure, which was in agreement with its lowest porosity and binder type. On the other hand, pores having size in the m range were observed in materials HL-LA and NHL-LA. It was evident that the highly porous microstructure of HL-and NHL-based mortars was the reason behind their high water absorption, high water vapor permeability, and low thermal conductivity. The use of lava aggregate resulted in a considerable decrease in the thermal conductivity values compared to those of control materials. For the dry thermal conductivity, the decreases were 69% for HL-LA, 53% for PCHL-LA, and 38% for NHL-LA. This can be attributed to the higher porosity of these materials and also to the lava inner porosity itself. In accordance with the EN 998-1 [85] and the EN 1745 [97], the thermal conductivity of examined mortars met criteria for repair mortars. On similar thermal conductivity of lightweight mortar reported, e.g., Palomar and Barluenga [98] who measured cement-lime mortar with perlite and silica sand λ = 0.44 W/(m·K).
The newly developed mortars with lava granulated exhibited slightly lower dependence of the thermal conductivity on moisture despite their high porosity. This feature is advantageous for practical use in repair of historical masonry that usually suffers from excessive moisture presence, and the repair materials usually serve as substrate for moisture transport from inner parts of masonry and consequently enable water evaporation. In this case, the low dependence of the thermal conductivity on moisture content allows to maintain moderate thermal insulation function even in moisture presence.
Taking into consideration the measuring uncertainty of the volumetric heat capacity test, the observed differences in C v values can be accounted as negligible, i.e., the replacement of silica sand with lava aggregate had no distinct effect on the heat storage capacity of the examined mortars. The dependence of the heat storage on the moisture presence in mortar samples was not significant and apparent as in the case of moisture dependent thermal conductivity. This was due to the volumetric heat capacity of water that is only about 3 times higher compared to the volumetric heat capacity of dry mortar samples.
The microstructure morphology of the fractured surface of mortar samples determined for 90-days samples using SEM is shown in Figure 7a-c. The SEM analysis allowed identification of lava grains covered and interconnected with Portlandite, CSH-gels, and in the case of PCHL-LA also with Ettringite. At first sight, the microstructure of the particular studied mortars differed. Mortar PCHL-LA had, in comparison with the other two mortars, a denser and more compact structure, which was in agreement with its lowest porosity and binder type. On the other hand, pores having size in the µm range were observed in materials HL-LA and NHL-LA. It was evident that the highly porous microstructure of HL-and NHL-based mortars was the reason behind their high water absorption, high water vapor permeability, and low thermal conductivity.

Conclusions
Lava granulate was studied as a possible full replacement of silica sand in the composition of lime-, cement-lime-, and natural hydraulic lime-based mortars. In order to achieve similar workability as the reference mortar mixes with silica sand, the batch water dosage was adjusted due to the higher water absorption of lava particles in the comparison with silica sand. The use of lava sand as an aggregate greatly increased the open porosity of the developed mortars. All the mortars with incorporated lava aggregate exhibited sufficient mechanical resistance in strength classes CS I (HL-LA), CS II (NHL-LA), CS IV (PCHL-LA), and the proved pozzolanic activity of lava fine particles contributed to the total mechanical strength. Based on the tests of mechanical properties, the mortars on the basis of cement/hydrated lime blend were found to be too rigid for repair of historical masonry. These mortars also exhibited low permeability for water in both liquid and gaseous phases. However, they can be safely used in construction of contemporary buildings. On the other hand, mortars based on hydrated lime and natural hydraulic lime met the technical requirements imposed by the European standards on thermal and hygric performance of repair mortars. Therefore, they were found compatible with materials of historical masonry, and well applicable for their repair. These materials possess high water absorption capacity and low water vapor resistance that ensure possible drying of damp laden masonry which is often the case of historical and older buildings. In this sense, the interconnectivity between mortar and substrate will be of the particular importance. The lava-containing mortars had considerably lower thermal conductivity than mortars with silica sand. Also, the thermal conductivity dependence on moisture content was reduced by the use of lava aggregate. This pointed out to their possible application in moderation of thermal performance of moist historical buildings as they can find use for the rendering, repointing, and walling purposes. In summary, it can be concluded, that the lava granulate is an effective and convenient aggregate for lime-and natural hydraulic lime-based mortars, especially in regions where lava resources are abundant.

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