Construction and Demolition Residuals as Raw Materials for the Production of Novel Geopolymer Building Materials

: The increasing number of new construction projects requiring high-quality building products, which, in turn, emit enormous amounts of CO 2 , runs counter to European and global climate goals. The increasing occupation of valuable landﬁll space is also an ecological problem. To meet these challenges without having to lower living standards, more ecological building materials should be used in the future. Geopolymers or alkali-activated materials, which, unlike conventional building materials, can be produced and used without a prior burning or calcination process, offer a comparatively low-CO 2 alternative. Signiﬁcant CO 2 emissions can already be saved by using this technology. The aim of this work is to investigate whether geopolymers can also be produced from construction and demolition residuals generated by the construction industry in order to counteract the problem of the increasing use of landﬁll space and, at the same time, to further reduce greenhouse gas emissions in the production of building materials. For this purpose, various residual materials from the construction and demolition industry are investigated by means of XRF, XRD, and IR spectroscopy for their setting behavior by alkaline activation. At the same time, the characteristic values of compressive strength, ﬂexural strength, bulk density, and thermal conductivity, which are important for building materials, are determined in order to test the possible applications of the resulting materials as building materials.


Introduction
In 2019, 222,678 new construction projects were approved in Germany [1]. For the construction of new buildings on this scale, large quantities of suitable building materials are necessary in accordance with the requirements, such as concrete, aerated concrete, sand-lime bricks, and bricks. All the building materials mentioned have in common that significant raw material and energy resources have to be used for their production in thermoprocessing plants. During thermal treatment at high temperatures, corresponding amounts of CO 2 are emitted both through the combustion of primary fuels and through the decarbonation of the mineral input materials. In order to achieve climate protection targets, building materials of the future should be characterized by lower energy consumption, reduced CO 2 emissions, a feasible share of recycled material, and recyclability into the material cycle. In Germany, more than 228 million tons of construction and demolition waste were generated in 2018 [2]. For many years now, a useful recycling of valuable materials has been taking place, in which the metallic components such as iron and steel, as well as copper pipes, wood, and plastics are separated from the inorganic wall-building materials, plasters, and mortars and returned to the material cycle. However, a large proportion of the inorganic demolition materials are still sent to construction waste landfills, where they block valuable landfill space [3]. The work presented here deals with a relatively novel class of building materials called alkali-activated materials or geopolymers. These

Materials and Methods
The residual materials used here were brick sanding dust (Figure 1a (Figure 1f,g). While the brick sanding dust was already in powder form, the crumbly residual fractions of broken brick, mixed rubble, and concrete rubble were first crushed in a ball mill and then sieved to a particle size x ≤ 200 µm. Only the screened material was used for subsequent geopolymer production studies. In addition, a powdered class F fly ash from a coal-fired power plant, designated Microsit 10 ( Figure 1h), was selected as a further residual material.
Crystals 2022, 12, x FOR PEER REVIEW 2 o a relatively novel class of building materials called alkali-activated materials or geop mers. These are cold-hardening binding materials that require a comparatively sign cantly lower primary energy consumption during their production, with correspondin lower CO2 emissions [4]. From literature data, it is known that geopolymers based on takaolin, fly ash, as well as blast furnace slags have been synthesized, also saving prim energy and costs [5][6][7]. The fly ash-based geopolymers are found to be particularly e ronmentally friendly when compared with other building materials. This is mainly tributed to the fact that combustion or drying processes are no longer necessary [8] further address this environmental concern, geopolymers based on crushed brick concrete residues have also been produced [9][10][11][12][13]. In the work presented here, vari typical demolition materials and residual materials from the construction sector, such brick scrap, brick sanding dust, mixed rubble, and concrete rubble, were investigated w regard to their suitability as recycling materials for the production of novel geopoly building materials. In particular, it was examined whether the residual materials m tioned are already suitable as singular solid components for geopolymer production order to detect a reaction of the starting materials by alkaline activation, both starting terials and the resulting products were investigated by Fourier-transform infrared sp troscopy (FTIR). In addition, the material parameters of compressive strength, flex strength, bulk density, and thermal conductivity, which are important for building pr ucts, were determined. Scanning electron micrographs provided information on the m phology of the geopolymer products.

Materials and Methods
The residual materials used here were brick sanding dust (Figure 1a), brick sc (Figure 1b,c), mixed rubble (Figure 1d,e), and concrete rubble (Figure 1f,g). While the b sanding dust was already in powder form, the crumbly residual fractions of broken br mixed rubble, and concrete rubble were first crushed in a ball mill and then sieved particle size x ≤ 200 µm. Only the screened material was used for subsequent geopoly production studies. In addition, a powdered class F fly ash from a coal-fired power pl designated Microsit 10 ( Figure 1h), was selected as a further residual material.  Waste materials used in the production of geopolymers: brick sanding dust (a); unprocessed brick scrap (b); processed brick scrap (c); unprocessed mixed rubble (d); processed mixed rubble (e); unprocessed concrete rubble (f); processed concrete rubble (g); fly ash (h).

Sample Preparation
For the production of the geopolymer bricks, an alkaline activating solution of a liquid sodium silicate water glass of the grade "Betol 39 T" from Woellner-Werke, Ludwigshafen with a water glass modulus (SiO 2 /Na 2 O) of 3.0, was used. Solid NaOH pellets were slowly added under constant stirring until the solution consisted of 85.46 wt.% liquid sodium silicate and 14.54 wt.% sodium hydroxide, resulting in a water glass modulus of 1.28. During this process, the solution was stirred continuously over a period of 24 h. The activator solution thus consisted of 23.44% SiO 2 , 18.37% Na 2 O, and 57.90% H 2 O. To produce the geopolymer bricks, 1 kg of activator solution was added for every 3 kg of prepared residual powder. In this series of tests, the geopolymer bricks were produced exclusively from 100 wt.% of each of the prepared sorted residual aggregates, which can be seen in Figure 1a-h. The test batches were homogenized in a laboratory mixer over a period of 15 min each at a rotational speed of 250 rpm. The homogeneous paste was immediately poured into molds made of silicone, and air bubbles introduced in the process were expelled onto a vibrating plate over a period of 5 min. For curing, the binder samples were stored in a drying oven under defined conditions, namely always for a period of 48 h and at a temperature of 85 • C, protected against drying by PE film. After the curing process, the geopolymer test specimens were demolded and processed into suitable specimens by sawing and grinding. Compression test specimens of an edge length of (L × W × H) 40 mm × 40 mm × 40 mm, three-point bending fracture test specimens of an edge length of (L × W × H) 160 mm × 40 mm, and specimen plates for investigating thermal conductivity with the dimensions (L × W × H) 100 mm × 100 mm × 25 mm were produced ( Figure 2). All specimens that came into contact with water during sawing and grinding were dried to constant weight in the drying cabinet before the measurement of mechanical properties and then stored in the desiccator until the measurement.

Sample Preparation
For the production of the geopolymer bricks, an alkaline activating solution of a uid sodium silicate water glass of the grade "Betol 39 T" from Woellner-Werke, Ludw hafen with a water glass modulus (SiO2/Na2O) of 3.0, was used. Solid NaOH pellets w slowly added under constant stirring until the solution consisted of 85.46 wt.% liquid dium silicate and 14.54 wt.% sodium hydroxide, resulting in a water glass modulu 1.28. During this process, the solution was stirred continuously over a period of 24 h. activator solution thus consisted of 23.44% SiO2, 18.37% Na2O, and 57.90% H2O. To p duce the geopolymer bricks, 1 kg of activator solution was added for every 3 kg of p pared residual powder. In this series of tests, the geopolymer bricks were produced clusively from 100 wt.% of each of the prepared sorted residual aggregates, which can seen in Figure 1a-h. The test batches were homogenized in a laboratory mixer over a riod of 15 min each at a rotational speed of 250 rpm. The homogeneous paste was im diately poured into molds made of silicone, and air bubbles introduced in the proc were expelled onto a vibrating plate over a period of 5 min. For curing, the binder samp were stored in a drying oven under defined conditions, namely always for a period o h and at a temperature of 85 °C, protected against drying by PE film. After the cur process, the geopolymer test specimens were demolded and processed into suitable sp imens by sawing and grinding. Compression test specimens of an edge length of (L × W H) 40 mm × 40 mm × 40 mm, three-point bending fracture test specimens of an edge len of (L × W × H) 160 mm × 40 mm, and specimen plates for investigating thermal cond tivity with the dimensions (L × W × H) 100 mm × 100 mm × 25 mm were produced ( Fig  2). All specimens that came into contact with water during sawing and grinding w dried to constant weight in the drying cabinet before the measurement of mechan properties and then stored in the desiccator until the measurement.

X-ray Fluorescence Analysis
X-ray fluorescence analyses (XRF) were performed to chemically characterize the ferent residual fractions. For this purpose, an XRF instrument of the Axios type from PA alytical was used, which is a wavelength-dispersive sequence spectrometer (WDXRF) erated with a rhodium anode. For quantitative analysis of the residues, the loss on ignit (LOI) was determined at 950 °C over a period of 2 h.

X-ray Diffraction Analysis
The XRD investigations were carried out on an X'Pert PRO X-ray diffractometer fr Panalytical, whose cathode tube is operated with a copper anode. The generator setti 40 mA at 45 kV were selected. Powder-ground sample material was prepared and me ured using the back loading method.

X-ray Fluorescence Analysis
X-ray fluorescence analyses (XRF) were performed to chemically characterize the different residual fractions. For this purpose, an XRF instrument of the Axios type from PANalytical was used, which is a wavelength-dispersive sequence spectrometer (WDXRF) operated with a rhodium anode. For quantitative analysis of the residues, the loss on ignition (LOI) was determined at 950 • C over a period of 2 h.

X-ray Diffraction Analysis
The XRD investigations were carried out on an X'Pert PRO X-ray diffractometer from Panalytical, whose cathode tube is operated with a copper anode. The generator settings 40 mA at 45 kV were selected. Powder-ground sample material was prepared and measured using the back loading method.

FTIR-Spectroscopy
In order to examine the structures of the produced geopolymers, Fourier-transform infrared spectroscopy (FTIR) was performed on powders using the ATR method. IR spectroscopy is a common investigation method used to visualize the structures of geopolymers [14]. The measurements were performed on a Bruker Tensor II with a KBr beam splitter in the spectral range of 5000-400 cm −1 . The atmosphere was filtered out by automatic background measurements.

Determination of the Material Properties
The determination of the maximum compressive stresses σ d was based on the standard DIN EN 196 Part 1. For the compression test, the pressure build-up on the test surface was carried out at a constant rate of 1.5 N (mm 2 s) −1 . The maximum compressive stress σ d was calculated according to Equation (1) from the maximum applied force F at failure of the material and the cross-sectional area S of the test specimen. Fifteen test specimens of each material were tested to obtain a reliable average value.
The determination of the maximum flexural strength or bending stress σ f was based on the standart DIN EN 196 Part 1. The three-point bending test was performed at a constant pressure build-up of 0.5 kN s −1 . The maximum flexural stress σ f was calculated according to Equation (2) from the maximum applied force F, the support width L, the thickness b, and the width b of the specimens. For the determination of the mean flexural strengths, 6 specimens of each geopolymer grade were tested and the mean values and standard deviations were calculated.
For bulk density testing, the thermal conductivity test panels were first dried and cooled to room temperature. Then, the plates treated in this way were weighed and their external dimensions were determined. The calculation of the bulk density ρ roh was performed according to Equation (3), using the mass m and the volume V of the test specimens.
The thermal conductivities λ 10,dr. were determined in accordance with the test standard DIN EN ISO 8302:1991 using the so-called plate method. The thermal conductivities were calculated as a function of the respective sample medium temperatures of the area A and the layer thickness d of the sample using Equation (4) below. In order to obtain a reliable average value, three specimens of each of the geopolymer grades were tested and the average values of thermal conductivity λ 10,tr . were calculated.

Scanning Electron Microscopy
In order to gain a deeper insight into the morphology of the geopolymers obtained, images were taken using scanning electron microscopy (SEM). The fracture surfaces of the geopolymers were always examined at 2000× magnification on a Zeiss EVO 25 LS. To obtain suitable images, the samples were sputtered with gold to remove excess electrons.

X-ray Fluorescence Analysis
X-ray fluorescence (XRF) analysis was used to investigate the chemical composition of the residues. The results are shown in Table 1. The investigation showed that all the residual materials investigated contained between 52.4 and 63.4 wt.% SiO 2 . The Al 2 O 3 content of brick sanding dust, brick scrap, and the fly ash ranged from 17.9 to 25.2 wt.%. In contrast, the Al 2 O 3 contents in mixed and concrete rubble were only 5.3 and 3.1 wt.%, respectively. For the CaO content, the ratios were reversed. Here, the mixed and concrete rubble contained comparatively higher contents of 13.4 and 17.9 wt.%, respectively, while the brick sanding dust contained only 5.4 wt.%, the brick scrap only 8.6 wt.%, and the fly ash only 4.2 wt.% CaO. All residual materials contained only relatively low levels of trace constituents.

X-ray Diffraction Analysis
The results of the mineralogical analysis given in Figure 2 correlate with the results of the XRF analysis. The mineralogical analysis (XRD) showed that the brick sanding dust, Figure 3a, contained the minerals quartzite, hematite, gehlenite, albite, and microcline. In the brick scrap (Figure 3b), as a result of the same place of origin, the same minerals were contained, namely quartzite, hematite, gehlenite, albite, and microcline. Muscovite and sodium alumina silicates were also detected. The identified mineralogical phases are also presented as typical phases for fired clay in the common literature [15]. The mixed rubble ( Figure 3c) contained quartzite, calcite, dolomite, and sanidine. Other mineralogical phases that would be expected were not detectable, due to concentrations that are too low. The detected phases clearly indicated a mixture of many different materials, so phases could be detected that are assigned to clay minerals and silicate materials in the literature [15], but also classical phases from cements or concretes such as dolomite and calcite [16]. The concrete rubble (Figure 3d) was mineralogically very different from the composition of the mixed rubble. The concrete rubble contained the mineral phases quartzite, hematite, gehlenite, albite, and microcline and thus consisted of typical cement phases and typical silicate phases from the fillers gravel and sand [16]. Analysis of the fly ash ( Figure 3e) showed that it contained the minerals quartzite, hematite, gehlenite, albite, microcline, and an amorphous phase, which also correlates well with values from the literature [8].

FTIR-Spectroscopy
In order to demonstrate alkaline activation or geopolymerization, the IR spectra of the starting materials brick sanding dust, brick scrap, mixed rubble, concrete rubble, and fly ash (Figure 4) were first obtained and compared with the IR spectra of the geopolymer batches produced from them ( Figure 5). The IR spectra of the starting materials showed transmission bands at 1016, 776, and 447 cm −1 , and additionally mixed rubble and concrete rubble showed a transmission band at 3120 cm −1 . The 1016 and 447 cm −1 peaks are the main bands of the silicon-oxygen and aluminum-oxygen bonds, respectively, as has also been similarly shown by Bohra [17]. In addition, except for the fly ash, all spectra of the starting materials had an additional main band at 1415 cm −1 , which can be assigned to the asymmetric vibrational bands of the O-C-O bonds of carbonates [18,19]. The IR spectra of the investigated geopolymer batches are shown in Figure 5. The main transmission bands were located at 3380, 1429, 977, and 449 cm −1 . The broad transmission band at about 3400 cm −1 is attributed to the O-H groups of the silanols and the hydrogen bonds between attached water molecules and the silanols. The band at 1644 cm −1 is characteristic for water molecules bound to the inorganic basic structure. A particularly important band with respect to geopolymerization is the asymmetric vibrational band of the Si-O-Si and Si-O-Al compounds (abbreviated Si-O-T, where T can stand for Si and Al), which occurred in the starting materials at 1016 cm −1 . This distinct band was shifted to lower wavenumbers of 977 cm −1 in the IR spectra of the geopolymer products. It should be noted that the alkali-activated fly ash had the highest wavenumber in this peak, which, according to the literature, may indicate an increased degree of polymerization [20]. The bands of O-C-O bonds also appeared in the geopolymer products, except for the fly ash composition FA_100, at 1415 cm −1 and were more pronounced than in the starting materials.

FTIR-Spectroscopy
In order to demonstrate alkaline activation or geopolymerization, the IR spectra of the starting materials brick sanding dust, brick scrap, mixed rubble, concrete rubble, and fly ash (Figure 4) were first obtained and compared with the IR spectra of the geopolymer batches produced from them ( Figure 5). The IR spectra of the starting materials showed transmission bands at 1016, 776, and 447 cm −1 , and additionally mixed rubble and concrete rubble showed a transmission band at 3120 cm −1 . The 1016 and 447 cm −1 peaks are the main bands of the silicon-oxygen and aluminum-oxygen bonds, respectively, as has also been similarly shown by Bohra [17]. In addition, except for the fly ash, all spectra of the starting materials had an additional main band at 1415 cm −1 , which can be assigned to the asymmetric vibrational bands of the O-C-O bonds of carbonates [18,19]. The IR spectra of the investigated geopolymer batches are shown in Figure 5. The main transmission bands were located at 3380, 1429, 977, and 449 cm −1 . The broad transmission band at about 3400 cm −1 is attributed to the O-H groups of the silanols and the hydrogen bonds between attached water molecules and the silanols. The band at 1644 cm −1 is characteristic for water molecules bound to the inorganic basic structure. A particularly important band with respect to geopolymerization is the asymmetric vibrational band of the Si-O-Si and Si-O-Al compounds (abbreviated Si-O-T, where T can stand for Si and Al), which occurred in the starting materials at 1016 cm −1 . This distinct band was shifted to lower wavenumbers of 977 cm −1 in the IR spectra of the geopolymer products. It should be noted that the alkaliactivated fly ash had the highest wavenumber in this peak, which, according to the literature, may indicate an increased degree of polymerization [20]. The bands of O-C-O bonds also appeared in the geopolymer products, except for the fly ash composition FA_100, at 1415 cm −1 and were more pronounced than in the starting materials.    Figure 6 shows the results of the compressive strength tests. This shows that the geopolymers produced with fly ash (100 wt.%) achieved the highest compressive strengths with 96.6 MPa. The worst compressive strengths with 14.9 MPa were shown by the geopolymers produced from brick sanding dust (100 wt.%). When the brick sanding dust was exchanged for ground brick scrap (100 wt.%), geopolymer compressive strengths of 32.31 MPa resulted. The geopolymers prepared from mixed rubble (100 wt.%) and concrete rubble (100 wt.%) exhibited compressive strengths of 18.7 MPa and 19.3 MPa, respectively.  Figure 6 shows the results of the compressive strength tests. This shows that the geopolymers produced with fly ash (100 wt.%) achieved the highest compressive strengths with 96.6 MPa. The worst compressive strengths with 14.9 MPa were shown by the geopolymers produced from brick sanding dust (100 wt.%). When the brick sanding dust was exchanged for ground brick scrap (100 wt.%), geopolymer compressive strengths of 32.31 MPa resulted. The geopolymers prepared from mixed rubble (100 wt.%) and concrete rubble (100 wt.%) exhibited compressive strengths of 18.7 MPa and 19.3 MPa, respectively.

Determination of the Material Properties
The flexural strengths of the alkali-activated materials investigated are shown graphically in Figure 7. From the investigation, it can be seen that the flexural strengths of all geopolymer grades were in the same order of magnitude. The geopolymers prepared using fly ash (100 wt.%) showed the lowest values of 2.5 MPa; the geopolymers prepared from brick sanding dust (100 wt.%) showed the highest flexural strengths of 3.2 MPa. Figure 8 shows the results of the bulk density determination and Figure 9 shows the results of the determination of the thermal conductivities λ 10,dr. , each with their associated standard deviations. The investigations showed, for the geopolymer stones from brick sanding dust and from finely ground brick scrap, low bulk densities of 1.4 g cm −3 and 1.5 g cm −3 , respectively, and thus correlatively the lowest thermal conductivities λ 10,dr. of this test series of 0.28 W mK −1 and 0.35 W mK −1 , respectively. The alkali-activated materials from mixed and concrete rubble exhibited higher densities of 1.8 g cm −3 and, correlatively, significantly higher thermal conductivities λ 10,dr. of 0.49 W mK −1 . The geopolymer bricks from fly ash had a mean bulk density of 1.7 g cm −3 and corresponding mean thermal conductivity λ 10,dr. of 0.35 W mK −1 .      sanding dust and from finely ground brick scrap, low bulk densities of 1.4 g cm an g cm −3 , respectively, and thus correlatively the lowest thermal conductivities λ10,dr. of test series of 0.28 W mK −1 and 0.35 W mK −1 , respectively. The alkali-activated mate from mixed and concrete rubble exhibited higher densities of 1.8 g cm −3 and, correlati significantly higher thermal conductivities λ10,dr. of 0.49 W mK −1 . The geopolymer b from fly ash had a mean bulk density of 1.7 g cm −3 and corresponding mean thermal ductivity λ10,dr. of 0.35 W mK −1 .   Figures 10-14 show the SEM images of the fracture surfaces of the investigated polymer samples. In Figure 14, one can see a fly ash geopolymer. The fly ash part which had not yet fully reacted, were surrounded by matrix material and some crysta phase can be seen. A continuous matrix and crystalline material could also be dete coexisting in all construction industry residues, brick sanding dust (Figure 10), brick s (Figure 11), mixed rubble (Figure 12), and concrete rubble (Figure 13). The fly ash had highest matrix ratio, followed by the concrete rubble and the mixed rubble geopolym The surface of the brick sanding dust and the brick scrap appeared most fractal in c  Microscopy   Figures 10-14 show the SEM images of the fracture surfaces of the investigated geopolymer samples. In Figure 14, one can see a fly ash geopolymer. The fly ash particles, which had not yet fully reacted, were surrounded by matrix material and some crystalline phase can be seen. A continuous matrix and crystalline material could also be detected coexisting in all construction industry residues, brick sanding dust (Figure 10), brick scrap (Figure 11), mixed rubble (Figure 12), and concrete rubble ( Figure 13). The fly ash had the highest matrix ratio, followed by the concrete rubble and the mixed rubble geopolymers. The surface of the brick sanding dust and the brick scrap appeared most fractal in comparison.

Scanning Electron
which had not yet fully reacted, were surrounded by matrix m phase can be seen. A continuous matrix and crystalline mat coexisting in all construction industry residues, brick sanding ( Figure 11), mixed rubble (Figure 12), and concrete rubble (Fig  highest matrix ratio, followed by the concrete rubble and the The surface of the brick sanding dust and the brick scrap ap parison.

Discussion
By analyzing the chemical and mineralogical compositi brick sanding dust, brick scrap, mixed building rubble, concre shown that all these residual materials are, in principle, suit The starting materials had sufficient SiO2 as well as Al2O3 terms, fly ash showed the largest amorphous fraction of all th gated. This can favor improved setting behavior, as amorp solved more quickly by the alkaline activator solution. Fly as tive material in these investigations, as the behavior of fly as has already been studied in detail in the literature [17]. Altho Ca-poor precursor material, the mechanical properties of Ca-r rials can also be compared well.
By means of IR spectrometry, it was determined that ne numbers 3400 cm −1 and 1644 cm −1 , which can be assigned to th characteristic of geopolymers, alkaline-activated material, a there. These bands, which were not present in the starting formed silanol groups and water molecules bound into the first indicator that geopolymerization or alkaline activation h thermore, a peak shift in the Si-O-T bonds was clearly demo between the starting materials and the resulting reaction pro

Discussion
By analyzing the chemical and mineralogical composition of the starting materials brick sanding dust, brick scrap, mixed building rubble, concrete rubble, and fly ash, it was shown that all these residual materials are, in principle, suitable for alkaline activation. The starting materials had sufficient SiO 2 as well as Al 2 O 3 and CaO. In mineralogical terms, fly ash showed the largest amorphous fraction of all the starting materials investigated. This can favor improved setting behavior, as amorphous structures can be dissolved more quickly by the alkaline activator solution. Fly ash was chosen as a comparative material in these investigations, as the behavior of fly ash during alkaline activation has already been studied in detail in the literature [17]. Although fly ash corresponds to a Ca-poor precursor material, the mechanical properties of Ca-rich alkaline-activated materials can also be compared well.
By means of IR spectrometry, it was determined that new bands form at the wavenumbers 3400 cm −1 and 1644 cm −1 , which can be assigned to the O-H groups of the silanols characteristic of geopolymers, alkaline-activated material, and to the water deposited there. These bands, which were not present in the starting materials, indicate newly formed silanol groups and water molecules bound into the geopolymer and are thus a first indicator that geopolymerization or alkaline activation has taken place [21,22]. Furthermore, a peak shift in the Si-O-T bonds was clearly demonstrated in the comparison between the starting materials and the resulting reaction products. This peak shift is an unambiguous characteristic for a geopolymerization that has taken place [19,23]. It is known from the literature that this peak shift results from the structural change in the material due to the reaction. The large shift toward lower wavenumbers can be explained by the replacement of SiO4 tetrahedra by AlO4 tetrahedra. This changes the chemical environment of the Si-O bonds [13,23]. If the shift is more intense, it can be assumed that more AlO4 tetrahedra are incorporated into the SiO4 backbone, as has been observed analogously in studies of zeolites [24][25][26]. This behavior is explained by the force constant, which is higher in Si-O bonds than in Al-O bonds. A lower force constant leads accordingly to lower wavenumbers [27]. From these two clear indicators, it can be concluded that geopolymerization has occurred. It was also found that the alkali-activated fly ash had the highest wavenumbers in this peak. Thus, from previous reasoning and in agreement with the literature, it can be assumed that the fly ash geopolymer has the highest degree of Si crosslinking [20]. Comparison of the IR spectra showed that for all products except fly ash, the O-C-O band at 1415 cm −1 increased compared to the starting materials. This indicates that new carbonates were formed as a result of geopolymerization. In agreement with the literature, this can be attributed, on the one hand, to a sodium carbonate-forming reaction of the excess sodium introduced by the activator solution with CO 2 from the ambient atmosphere. As this band does not occur in the FA_100 fly ash geopolymer, it can be assumed that in this composition, the sodium is fully involved in the geopolymerization reaction [25,28]. On the other hand, these carbonates in Ca-rich alkali-activated materials can also be attributed to the reaction of free Ca cations with the CO 2 of the surrounding atmosphere [29].
From this, it can be concluded that fly ash, as already suggested by the mineralogical investigations, possibly exhibits a better solidification behavior than the other residual materials investigated. This assumption is confirmed by the fact that the fly ash geopolymer FA_100 developed the highest compressive strengths at 97 MPa. This fits in as chemical stability is usually accompanied by mechanical stability [30,31]. Moreover, the increased compressive strengths compared to the other species studied are also consistent with the stronger three-dimensional crosslinking of the Si-O-Si bands observed by IR-spectroscopy.
It was already expected from the literature that fly ash would show good setting behavior and, therefore, this material was used as a comparative material in this study. However, all other residual materials also showed suitable strengths due to alkaline activation. In particular, the geopolymer stones from ground brick scrap stood out in terms of its mechanical properties compared to the other four construction residues. The geopolymers from ground brick scrap not only exhibited the highest compressive strengths of 32 MPa, but also the second lowest bulk densities of 1.5 g cm −3 and thermal conductivities of 0.351 W mK −1 . Looking at the FTIR results, it can be observed that brick scrap has the best cross-linked Si-O-Si bands after fly ash, which results in the increased compressive strengths compared to the other residual materials. SEM results showed that brick scrap has the most fractal surface of all materials. This also indicates an increased porosity compared to the other materials, which is in good agreement with the low thermal conductivities and low density of the brick scrap-based material. This correspondence between thermal conductivity and density with the rough appearance in the SEM images can also be extrapolated to the brick sanding dust, which showed similarly low values in these areas. However, geopolymers from brick sanding dust also achieved the lowest compressive strength values with 15 MPa. In terms of bulk density and thermal conductivity, mixed rubble and concrete rubble had the worst properties for construction materials. The flexural strength was at the same level of about 3 MPa for all geopolymer samples from construction waste. Thus, flexural strength is the only mechanical property tested in this work where all geopolymers from construction waste achieved better properties than the comparative material from fly ash.
SEM images showed that the matrix phases were present in all activated materials. This is further evidence that geopolymerization or alkaline activation occurred as previously suspected. It is also evident from the images that the fly ash was able to form the most geopolymer matrix, which is consistent with the compressive strengths and the results of the IR studies. However, when comparing the SEM images, it is surprising that the brick rubble formed better strengths than the mixed rubble and concrete rubble fractions, as its fracture surface appears much more fractured than that of the rubble fractions. In fact, it can be assumed that more reactive material is present in the rubble fractions, which can be converted by the alkaline activation. This results in a more uniform and continuous matrix than is the case with the brick fractions. However, the nonreactive crystalline phases of the brick fractions, which make the fracture surfaces appear fractal, can lead to particle strengthening, which could explain the increased strengths compared to the rubble fractions.

Conclusions
The results presented here showed that it is possible to produce new building materials based on the alkaline activation process from recycled construction wastes. Due to various pretreatments and different chemical compositions of the construction waste used, the material properties of the alkaline-activated material differ considerably. For example, the use of fly ash enables the production of high-strength geopolymer bricks. This effect can be explained both by the fact that fly ashes, depending on their origin, have comparatively more activated silicate and aluminate groups, which are easily broken down by the activation solution used and are available as reaction partners for geopolymerization. It can also be explained by the fact that a more strongly three-dimensionally crosslinked polymer is formed. With regard to the bulk density of the geopolymer and the associated thermal conductivities λ 10,dr. , the geopolymers from brick sanding dust and brick scrap exhibited significantly lower and thus better values than the fly ash geopolymer in terms of thermal insulation properties. This effect can be attributed to the higher microporosity of the brick materials. Overall, the production of intact alkali-activated materials from all mineral construction residues used here was successful, and alkaline activation could be detected by IR spectroscopy. This even applies to the residual materials from mixed and concrete rubble, which may have less optimally accessible silicate and aluminate groups. Based on the present study, the main material parameters of the investigated alkali-activated construction and demolition residues are known. In further work, mixtures of these residual materials can be prepared and geopolymer stones with tailored properties can be produced from them. The presented material recycling of processed construction residues to novel substitute building materials offers the possibility to close open material cycles, to save raw material resources and valuable landfill volume, as well as unnecessary CO 2 emissions. There is a reasonable hope that used geopolymer bricks can be recycled at the end of their service life after crushing and grinding for the production of new geopolymer bricks, as was recently demonstrated for the first time for fly ash geopolymers [32].