Physicochemical and radiological characterization of kaolin and its polymerization products

M. Ivanović^a, Lj. Kljajević^a*, M. Nenadović^a, N. Bundaleski^a, I. Vukanac^a, B. Todorović^b, S. Nenadović^a

^a. Institute of Nuclear Sciences “Vinča”, University of Belgrade, (Belgrade, Serbia)

^b. Faculty of Technology of Leskovac, University of Niš, (Niš, Serbia)

*ljiljanamkljajevic@gmail.com

1. INTRODUCTIONTOP

Research on the geopolymer synthesis binders from various raw materials has been greatly accelerated in the last few years; some examples from vitreous blast furnace slags, fly ashes and other by-products are cited herein (1–6). The target was to design typically stable mixtures, either monoliths of flowable “concrete” and products which are already available in the market. In comparison to ordinary Portland cement, geopolymer concrete has better resistance to corrosion (7) and fire (up to approx. 1300°C) (8), high compressive and tensile strengths, a rapid strength gain, lower shrinkage (9) and longer durability (10). Moreover, the carbon footprint of geopolymer concrete is significantly lower and has a large greenhouse gas reduction than that of similar products from Portland cement (11). Together with a process of technology using elevated temperatures, geopolymer binders seem to be suitable for selected building materials. In the civil engineering, building materials plays different roles, so they should possess corresponding properties. Various mineralogical and chemical compositions of raw materials result in different basic properties (physical-chemical, mechanical, and durability) of building materials (12). Since these materials are usually observed as naturally occurring radioactive materials (NORM), radiological aspect in their usage as building materials should also be taken into the consideration.

Additionally, during the technologically enhanced processing of NORM, specific activity in by-products could increase significantly. These by-products are potential raw materials in manufacture of geopolymer binders (13). Determination of natural radionuclides content in building materials is important in order to estimate the exposure of humans to radiation, who can spend up to 80% of their time indoors (14). The radiation of terrestrial origin in buildings does not only originate from the soil (15–21), but also from the used building materials (22). Over the last few decades radiological research related to construction materials and buildings and their impact on the human health are supported. The building materials strongly influence indoor levels of the radioactive gas radon - direct progeny of ²²⁶Ra, and its decay products, which contribute significantly to doses through inhalation. It is shown by international studies, of the WHO (23) and ICRP (24), that building materials have a non-negligible share of radiation exposure of the public due to radon. Depending on the material, the concentration of natural radionuclides (mainly ²²⁶Ra, ²³²Th and ⁴⁰K) ranges from 1 to 4000 Bq/kg (19, 20).

The focus of this research was kaolin located below of soil that was subject of our previously published paper (25), and its polymerization products - geopolymers. Structural characteristics of the precursor materials and the geopolymer samples have been investigated by using various analytical techniques. FTIR and XPS analysis were used to monitor the forming of new chemical bonds during the synthesis of geopolymer as the potential building materials. Gamma spectroscopy measurements of the set of samples (kaolin, metakaolin and geopolymer) revealed the activity of natural radionuclides (²²⁶Ra, ²³²Th and ⁴⁰K).

2. EXPERIMENTALTOP

2.1. Materials and methodsTOP

2.1.1. MaterialsTOP

The used kaolin is high clay obtained from Rudovci, Lazarevac, Serbia. Physicochemical properties of kaolin were investigated in previous work Nenadović et al. (25). It was shown that the structural characteristics of this kaolin are suitable for both, mechanochemical and thermal treatments planned in this research. Reduction of the main particle size and changes in the ordered crystalline structure of the raw kaolin was done by mechanical milling in a Turbula Type T2C Mixer. The milling was performed under argon using ball-to-powder ratio (BRP) 4. Metakaolin (MK) was prepared by calcining kaolinite at 750 °C for 3 h. The alkaline solution was prepared from sodium silicate (volume ratio Na₂SiO₃/NaOH=1.6) and 16M NaOH (analytical grade). The reference geopolymer (GP) was formed from metakaolin and the alkaline solution (solid/liquid ratio was 0.85), which were mixed for 10 min and then left at room temperature for one day. Finally, the mixture was kept in a sample drying oven for 2 days at 50 °C. Time of 28 days is necessary to complete the process of polymerization.

2.1.2. XRD analysisTOP

All samples were characterized using X-ray diffractometry (XRD) by using Ultima IV Rigaku diffractometer, equipped by Cu Kα_1,2 radiation, with generator voltage 40.0 kV and generator current 40.0 mA. The range from 5° up to 80° 2θ angle was used for all powders in a continuous scan mode with a scanning step size of 0.02° at scan rate of 10 °/min.

2.1.3. FTIR analysisTOP

The functional groups of samples (kaolin, metakaolin, geopolymer) were studied using FTIR spectroscopy. Samples were powdered finely and dispersed evenly in anhydrous potassium bromide (KBr) pellets (1.5 mg/150 mg KBr). Spectra were taken at room temperature using a Bomem (Hartmann & Braun) MB-100 spectrometer set to give accurate spectra. The spectral data of the samples were collected in 4000–400 cm⁻¹ region.

2.1.4. XPS analysisTOP

XPS analysis has been performed using a SPECS system for surface characterization. The samples in the form of powder were fixed on an adhesive tape and analyzed ˝as received˝. Photoelectron emission has been excited by monochromatic Al K_α line having photon energy equal to 1486.67 eV. Survey spectra were taken in fixed analyzer transmission mode with pass energy of 40 eV (FAT 40) with energy step of 0.5 eV and the dwell time of 0.2 s. Detailed spectra of the main photoelectron lines were taken in FAT 20 mode with the energy step of 0.1 eV and the dwell time of 2 s. Charge compensation was performed using the electron flood gun, and the binding energy axis was fitted according to the position of the carbon C 1s line, assuming its main contribution corresponds to adventitious carbon situated at 284.8 eV. The composition analysis has been performed according to the characteristic photoelectron line intensities after background removal, using the atomic sensitivity factors provided by the manufacturer. The photoelectron lines were fitted to the superposition of peaks having pseudo-Voigt GL (30 % Lorentzian, 70 % Gaussian) profiles. Each contribution in the frame of the same line was considered to have the same width. The intensity ratio between the peaks attributed to the same bond of 2p_3/2 and 2p_1/2 lines has fixed intensity ratio 2:1, as predicted by the theory. Spin-orbit splitting of Si 2p and Al 2p lines was fixed during the fitting to 0.6 eV and 0.4 eV, respectively.

2.1.5. Gamma ray spectrometryTOP

The naturally occurring radionuclides in the samples of kaolin, metakaolin and geopolymer were determined by gamma ray spectrometry. The samples were mechanically prepared, meaning that they have been mechanically milled for the purposes of other analytical method used for sample characterization. Pulverized samples were placed in PVC cylindrical containers (125 ml) and sealed in order to reach radioactive equilibrium between ²²⁶Ra and its daughter products for six weeks.

Radiological analysis was performed by means of a coaxial semiconductor high purity germanium (HPGe) detector (AMETEK-AMT ORTEC GEM30-70, with 37% relative efficiency and 1.8 keV resolution for ⁶⁰Co at the 1332 keV line) associated with standard beam supply electronic units. Energy and efficiency calibration were performed with soil and coal standards prepared with certified solution of mixed gamma-emitting radionuclides (²⁴¹Am, ¹⁰⁹Cd, ¹³⁹Ce, ⁵⁷Co, ⁶⁰Co, ¹³⁷Cs, ²⁰³Hg, ¹¹³Sn, ⁸⁵Sr, and ⁸⁸Y), purchased from the Czech Metrology Institute (CMI). Technique of standard preparation was described in previously published paper (26). Used radioactivity standards were of the adequate density and similar chemical composition. Calibration of the spectrometer was conducted in accordance with an IAEA recommendation (27). Obtained efficiencies were corrected for coincidence summing effect using the correction factors described by Debertin and Schötzing (28).

Experimentally obtained efficiency curves had the analytical expression ε = e^−P(lnE) where ε is the detection efficiency, E is the energy and P(lnE) is the polynomial function of the fifth order. All the calculations and fitting were performed in Mathematica 5.2 software (Wolfram Research). Uncertainty of the efficiency calibration includes uncertainty of the activity of radionuclides in prepared standard, statistical uncertainty and fitting uncertainty of efficiency curve.

After reaching radioactive equilibrium, samples were measured and all spectra were recorded and analyzed using the Canberra’s Genie 2000 software. The measurement times were 80 000 s. Net areas of the relevant full energy peaks were corrected for the background, dead time and coincidence summing effects. Due to high resolution of the HPGe spectrometer used, full energy peaks were well separated, except in the cases described in below.

Activity concentration of ²³⁸U was determined indirectly by analyzing full energy peaks emitted by its descendants, ^234mPa (1001 keV) and ²³⁴Th (63.3 keV). The contribution of ²³²Th at 63.811 keV to the 63.3 keV ²³⁴Th peak was neglected. Activity of ²³⁵ U was determined directly via full energy peak at 143.767 keV. Since the samples were equilibrated, the activity of ²²⁶Ra was determined via its decay products ²¹⁴Bi (609.31 keV, 1120.3 keV, 1764.5 keV) and ²¹⁴Pb (295.21 keV, 351.92 keV). Additional testing was performed via 186.211 keV peak corrected for ²³⁵U (185.72 keV) contribution since these peaks cannot be resolved due to its close energies. The activity of ²¹⁰Pb was determined by analyzing its low energy peak at 46.54 keV.

The activity of ²³²Th was determined through the calculated activity of its progeny ²²⁸Ac (338.42 keV; 911.16 keV; 968.97 keV). Obtained results was than additionally checked through other radionuclides from the thorium series, ie. ²¹²Bi (727.25 keV) and ²¹²Pb (238.58 keV).

The activity of ⁴⁰K was determined directly by analyzing net peak area at 1460.8 keV, subtracted for the contribution of ²²⁸Ac (1459.3 keV), which could not be resolved in the recorded spectra.

Specific activities obtained are given in Table 3, expressed in Bq/kg. Presence of artificial radionuclides, gamma emitters, was not detected. Since the presence of ¹³⁷Cs could be expected in environmental samples, as a result of radio pollution, detection limits for this radionuclide are also given in Table 3.

Quoted uncertainties (the confidence level of 1σ) were calculated by error propagation calculation using the Mathematica 5.2 software (Wolfram Research). The combined standard uncertainties included the efficiency calibration uncertainty and the statistical uncertainties of the recorded peaks.

2.1.6. Dose assessmentTOP

Radium equivalent activity, Ra_eq (Bq kg⁻¹), the external hazard index, H_ex (Bq kg⁻¹), total external absorbed gamma dose rate D(nGy/h), and annual effective dose rate EDR (mSv y⁻¹) in measured samples were calculated. The radium equivalent activity was used to estimate hazard associated with materials that contain ²²⁶Ra, ²³²Th and ⁴⁰K. The external radiation hazard index reflects external radiation hazard due to the emitted gamma radiation. The values of these indicators of exposure were calculated according to Eqs. [1] and [2], (13, 29, 30):

respectively, where:

A_Ra denotes specific activity of ²²⁶Ra in Bq/kg

A_Th denotes specific activity of ²³²Th in Bq/kg, and

A_K denotes specific activity of ⁴⁰K in Bq/kg.

The external terrestrial gamma radiation absorbed dose rate, D, in air at a height of 1 m above ground level due to radionuclides ²²⁶Ra, ²³²Th and ⁴⁰K in measured samples was calculated using Eq. [3], and conversion factors: 0.462 (nGy/h)/(Bq/kg) for ²²⁶Ra, 0.604 (nGy/h)/(Bq/kg) for ²³²Th and 0.0417 (nGy/h)/(Bq/kg) for ⁴⁰K (14)

The annual outdoors effective dose rate, EDR (mSv/y) Eq. [4], was calculated utilizing a conversion coefficient of 0.7 Sv/Gy to convert the absorbed dose in air into the effective dose in the human body. This calculation takes into account that people spend about 20% of the time outdoors (outdoor occupancy factor p is 0,2) and t is 8,760 h annual exposure time. Thus, the annual effective dose rate, EDR, due to gamma radiation was calculated as, (14):

Previous calculation is performed under assumption that measured samples occurs in the environment. Based on the fact that investigated materials are row materials, and not necessarily meant for usage in construction industry, absorbed dose rate and annual effective dose rate were calculated using the equations [3] and [4], respectively.

If the examined materials are treated as a possible raw material for building material or construction material itself, different formulae should be used for dose calculation. Using the formulae given in (31), external dose rate and annual effective dose rate are calculated as [5] [6]:

Nevertheless, the percentage of examined row material, in addition to other constituents in final building material should be taken into account.

3. RESULTS AND DISCUSSIONTOP

3.1. XRD analysisTOP

Figure 1 shows the XRD patterns of the kaolin, metakaolin and geopolymer samples. According to the identified XRD patterns, the mineral phases identified in the as-received kaolin sample are kaolinite, muscovite and quartz (Fig. 1a). In the case of the thermally treated sample of kaolinite i.e. metakaolin, diffraction peaks of muscovite and in particular kaolinite were reduced, thus leaving quartz phase as the dominant one (Fig. 1b).

Metakaolin, in contrast to kaolin (25), was composed of amorphous phase and semi crystalline structure. Quartz could be identified as a component of metakaolinite. Appearance of the broad band between 18⁰ and 25⁰ indicated that the geopolymer prepared in this experiment was almost composed of amorphous structure. Obviously, quartz in the metakaolin is not solved in the geopolymerization reaction but its intensities were slightly lower due to a dilution effect. Quartz sharp peak was, most probably, the impurity in the calcined clay. According to Davidovits (32) geopolymers that harden at ambient temperatures remain X-ray amorphous and they are the geopolymers of practical interest and he works on geopolymerization mechanisms, microstructure development, properties and the application development of geopolymers as green building material.

3.2. FTIR analysisTOP

The results of the FTIR analysis of the studied samples are presented in Fig. 2. The FTIR absorption spectra were compared to known absorption lines in literature.

The FTIR spectrum of the kaolinite is typical of Al-kaolinite with four characteristic OH-stretching vibrations at 3696, 3668, 3650 and 3620 cm⁻¹ (νAl₂OH) (33, 34) . In the 1400-400 cm⁻¹ range (Figure 2), the γSi-O stretching vibrations of kaolinite are clearly observed at 1104, 1033, and 1010 cm⁻¹. Spectrum also contains a band at 798 cm⁻¹ that is attributed to quartz (35, 36). The intensity band at 913 cm⁻¹ is from the Al-Al-OH groups. The bands at 752 and 693 cm⁻¹ correspond to γSi-O stretching (37) while at 537 cm⁻¹ correspond to γSi-O-Al (octahedral) stretching, and those at 469 and 427 cm⁻¹ correspond to δSi-O and related Si-O-Si (38). This diversity of bands could be due to the presence of other aluminosilicates in the sample (illite and K-feldspars).

Heating of the kaolinite samples to metakaolin at 750 ºC, the sharp OH bands in the typical OH-stretching band range (3000-4000 cm⁻¹) have completely disappeared. Also no sharp OH peaks in this area although the 16 M NaOH was used to obtain geopolymer sample. The bands at 1104, 1033, and 1010 cm⁻¹ for Si-O stretching, those at 913, 752 and 537 cm⁻¹ also disappear. The increase in the band intensity at 1063 cm⁻¹ suggests that a three-dimensional network of amorphous Si-O-Si units is formed. These observations are in agreement with the XRD results, which demonstrate that the kaolinite structure is destroyed.

3.3. XPS analysisTOP

XPS analysis of aluminosilicates is a challenging task. The photoelectron lines are broadened due to the non-uniform surface charging, and the binding energy calibration is not always reliable. The problem becomes more elusive in case of working with natural materials, typical consisting of different phases. In this specific case, XRD analysis already shown that the kaolin sample contains significant amounts of quartz. Therefore, its presence can be expected in all samples.

Composition analysis of kaolin, metakaolin and geopolymer samples is presented in Table 1. Carbon, originating from hydrocarbon surface impurities (so-called adventitious carbon), is present in all samples. As already stated, the position of its C 1s line is used as the binding energy reference.

According to the XRD analysis, kaolin represents a mixture of different (alumino) silicate phases, in which kaolinite and quartz are dominant. Since the Si/Al ratio in kaolinite should equal 1, the difference between the amounts of silicon and aluminum can be used to estimate the atomic percentages of kaolinite (Si₂Al₂O₅(OH)₄), metakaolin (Si₂Al₂O₇) and quartz (SiO₂).The ratio between the atomic percentages of kaolinite and quartz is about 5 in the kaolin sample, whilst that of metakaolin and quartz in MK sample is about 3.9. The observed difference can be qualitatively explained by the loss of water when transforming kaolinite into metakaolin. The relative amount of quartz in GP sample (observed by XRD and FTIR) cannot be determined this way, because the chemical composition of the geopolymer is unknown at this point. As for the kaolin and MK samples, it is also clear that the relative amounts of oxygen is lower than expected, which is quantified below according to the detailed analysis of the characteristic photoelectron lines. The presence of sodium in the GP sample is an evidence of ONa groups, which, along with OH groups, typically end geopolymer chains.

Analysis of the Si 2p line confirms the presence of kaolinite and quartz contributions having Si 2p_3/2 lines at about 102.6 eV and 103.8 eV, respectively (39, 40). The ratio between the amounts of silicon in kaolinite and in quartz was used as a constraint in fitting the Si 2p line taken from kaolin and MK samples. The Si 2p line taken from the MK sample is shown in Figure 3. Al 2p line in these samples consists of a single contribution at about 75.0 eV, which can be attributed to both, Al-O and Al-OH bonds (41). Finally, O 1s line was resolved into three contributions attributed to Al-O and Al-OH bonds at about 531 eV (41), Si-O bonds at 531-532 eV (42) and to quartz at about 533 eV (40). The spectrum of the O 1s line taken from the kaolin sample is presented in Figure 4.

The corresponding fitting results for the two samples are summarized in Table 2. It can be observed that the relative intensity of the peak attributed to Al-OH bonds (contribution1) is smaller in MK as compared to kaolin. This can be explained by the loss of OH groups, which are dominantly bound to Al atoms, during the synthesis of MK. The ratio between the oxygen and silicon amounts in quartz of both samples is about 1.8, revealing already mentioned deficiency of oxygen in this phase.

Al 2p and Si 2p lines taken from the GP sample consist of a single and two contributions, respectively. Al 2p_3/2 is situated at 74.5 eV, which fits perfectly to the position of this line in geopolymers synthesized from metakaolin (43). Si 2p line was resolved to the contributions attributed to geopolymers (at 102.3 eV) and quartz (at 103.5 eV) with relative intensities of 77.8 % and 22.2 %, respectively The geopolymer contribution is above the one obtained in (43) for about 0.8 eV. However, the position of this line strongly depends on the amount of sialate bonds in the geopolymer. Indeed, in the case of pure siloxo bonds, Si 2p_3/2 line is situated at 103.8 eV (42). After subtracting the amount of silicon bound in quartz, the ratio between the Si and Al concentrations in geopolymer was evaluated to be 1.47. This ratio clearly suggests that the geopolymer sample consists of the roughly equal amounts of siloxo (Si-O-Si) and sialate (Si-O-Al) bonds.

O 1s line taken from GP samples, presented in Figure 5, was resolved into three contributions, which is usual for the geopolymers (43). Two of them can be readily attributed to Si-ONa (at 529.6eV, relative intensity of 15.9 %) and silanol Si-OH bonds (532.8eV, rel. int. 22.5 %). The latter contribution is also attributed to quartz. The peak at 531.2 eV with the relative intensity of 61.6 %, is typically related to the mixture of siloxo (Si-O-Si) and sialate (Si-O-Al) bonds. This is an additional confirmation of the conclusions made from the composition and Si 2p line analyses concerning the structure of the synthesized geopolymer. Assuming that the stoichiometry of the quartz phase in this sample is the same as in kaolin and MK samples (O:Si = 1.8), the estimated stoichiometry of the geopolymeric chains is 75.0 % of O, 14.8 % of Si and 10.2 % of Al.

3.4. Radiological analysisTOP

3.4.1. Gama spectrometric analysisTOP

Results of gamma spectrometric analysis conducted in a manner described in chapter 2.1. are given in Table 3, and based on these values dose calculations were performed.

Measured specific activity of natural radionuclides has significantly different values for three measured samples. In addition, radionuclide content showed enhancement after the first stage of polymerization, when kaolin was thermally treated on 750 °C and changed into a metakaolin phase (confirmed by FTIR analysis, XRD and XPS). The ratio of natural radionuclides content in metakaolin, compared to raw kaolin is in the range from 1.11 to 1.60. The lowest ratio is recorded for natural isotopes ⁴⁰K, while the highest ratio was recorded at the isotope ²¹⁴Pb. Further polymerization process, when it comes to alkaline activation of metakaolin (in our case with 16 M NaOH), lead to a further change (in opposite direction) of radionuclide content in measured geopolymer.

After 28 days, time necessary to complete the process of polymerization, FTIR, XPS and XRD analysis have confirmed the existence of synthesized geopolymer material. The ratio of natural radionuclides content in the synthesized material and the natural material is in the range from 0.52 to 0.72. The highest ratio of natural radioactivity is recorded for the isotopes ²¹⁴Pb, and the lowest for the isotope ²³⁵U.

The difference of the masses, i.e. densities, between kaolin and metakaolin due to loss of moisture in the sample was 8.3 %. Mass of the geopolymer sample was 8.4 % lower than mass of kaolin. These values do not correspond to measured activity ratios. This would mean that, in addition to loss of moisture, a further influence on the specific activities should be sought in the different physicochemical properties of nuclides of the uranium and thorium series, resulting in a different behavior and enrichment at the different stages of the polymerization process.

The explanation for the measured activity ratios could be over self-absorption phenomenon, but only to a certain extent. Namely, practice showed, and software for efficiency transfer calculation confirmed, that if density of the sample changes for 1 % it results in similar change in detection efficiency.

In a previously published paper Puertas et al. (44) showed that activity concentration of the hydrated or activated end product by unit of mass is slightly lower than in the anhydrous material because of the presence of moisture. The extent of the decline corresponds closely to water content in examined samples. For example, activity concentration is lower per unit of mass in hydrated cements than in their anhydrous components for 40-50%. They have confirmed this fact on a series of samples. Results presented in this paper confirmed that, but in our research we further monitored the change in radioactivity after the polymerization process. For process of polymerization we thermally treated kaolin (initiation of kaolin) to get metakaolin (the initiator) who activated and started process of polymerization in alkali environment. With heat treatment, crystalline structures appear which make the geopolymer matrix double phased, keeping the amorphous part predominant. Natural radioactivity of metakaolin is the largest, since the thermal treatment leads to water loss while during of geopolymerization process gets a final product with the lowest radioactivity.

3.4.2. Dose calculationTOP

Table 4 presents the total values of the radium equivalent activity (Ra_eq), radiation hazards (H_ex), absorbed dose rate (D), and annual effective dose rate (EDR) of kaolin (K), metakaolin (MK) and geopolymer (GP) samples.

The calculations were performed in accordance with UNSCEAR 2000 (14) under the assumption that investigated materials occurs in the environment. If these materials are treated as a raw material for building material or construction material itself, absorbed dose rate and EDR were calculated in accordance with (31), and results are given in Table 4a.

The highest values were observed for metakaolin (MK), and this can be generally explained by thermal treatment which gives higher activities values of natural radionuclides obtained by metakaolin gamma spectroscopy analysis (Table 3). The lowest values were observed for the synthesized material, and from the radiological point of view it could be recommended as a promising construction material. In the last 10 years a database of activity concentration measurements of natural radionuclides (²²⁶Ra, ²³²Th and ⁴⁰K) in building material was established. This database comprises about 10000 samples of materials used in the construction industry in 26 of 27 European Member States (45). The values of activity concentration of natural radionuclides (²²⁶Ra, ²³²Th and ⁴⁰K) in our investigated samples are in the range of results that have been published in the above reference.

4. CONCLUSIONTOP

XRD, FTIR, XPS analysis of the investigated samples showed mineralogical composition, new chemical bondings, as well as the present phase of the metakaolin that was used as a monomer in the polymerization process. Using XRD analysis mineralogical composition of samples were provided. The important thing is a quartz reflection of the raw material that remained after the polymerization process. FTIR and XPS analysis revealed formation of new chemical bonds in the geopolymer samples. XPS analysis confirmed that Si to Al ratio (Si/Al) is lowest in metakaolin (1.47) and in synthesized geopolymer material has been recorded the highest ratio of Si/Al (1.88). After alkaline activation of metakaolin, the decrease of specific activity of naturally occurring radionuclides was measured/detected in synthesized geopolymer. This research confirmed that during the polymerization process the natural radioactivity was reduced, i.e. process of metakaolin activation has an influence on natural radioactivity of precursor. The material with less natural radioactivity was obtained by polymerization process, or geopolymerization and aging this material for 28 days. From the aspect of the natural radioactivity, obtained material (geopolymer) can be recommended as a potential building material.

Presented results were obtained in the preliminary phase of a comprehensive investigation of physical-chemical and radiological characteristic of kaolin and its polymerization products. Obtained results have given the guidance for further optimization of the polymerization process in order to confirm and explain changes in radioactivity concentrations.

ACKNOWLEDGEMENTTOP

This work was supported by the Ministry of Education, Science and Technological Development of Republic of Serbia, Project numbers: [III 45012 and III 45005].

REFERENCETOP