Development of Paper Sludge Ash-Based Geopolymer and Application to Treatment of Hazardous Water Contaminated with Radioisotopes

Ambient temperature geopolymerization of paper sludge ashes (PS-ashes) discharged from paper mills was studied by means of scanning electron microscopy (SEM), X-ray diffraction (XRD), induction coupled plasma atomic emission spectrometry (ICP-AES), and X-ray absorption near edge structure (XANES). Two varieties of alkaline liquors were used in the PS-ash based geopolymers, corresponding to aqueous Na-metasilicate and Na-disilicate compositions. PS-ashes were found to be semi-crystalline and to have porous structures that make it possible to absorb much liquor. Flexural strengths of PS-ash-based geopolymers with liquor/filler ratios (L/F) of 1.0–1.5 ranged from 0.82 to 1.51 MPa at 4 weeks age, depending on PS-ashes and liquors used. The reaction process of the constituent minerals of the PS-ash is discussed. Furthermore, we attempted to solidify hazardous water contaminated with radioisotopes. Non-radioactive strontium and cesium nitrates were added as surrogates at a dosage of 1% into the PS-ash-based geopolymers. Generally, high immobilization ratios up to 99.89% and 98.77% were achieved for Sr2+ and Cs+, respectively, depending on the source of PS-ashes, alkaline liquors, and material ages. However, in some cases, poor immobilization ratios were encountered, and we further discussed the causes of the instability of derived geopolymer gels on the basis of XANES spectra.


Introduction
A geopolymerization technique may involve three categories of application. The first is the synthesis of silicates of nanometer scale at temperatures as low as 800˝C with less alkali contamination [1][2][3][4]. The second is the preparation of monolithic materials, potentially replacing Portland cement and recycling various sorts of wastes or by-products [5][6][7][8][9][10][11][12][13][14][15][16][17][18]. The third is the immobilization of hazardous heavy metals or radioisotopes contaminated in sludgy solid wastes, an application dating back to 1988 [19]. On the other hand, there is a liquid type of waste contaminated with radioisotopes awaiting to be treated [20,21]. To immobilize this type of waste by geopolymerization, the liquor/filler ratio (L/F) becomes large. However, if the geopolymer is made from general aluminosilicate powder (e.g., metakaolin and fly ash), a higher L/F would cause bleeding, and hazardous elements accordingly escape from the geopolymer. Although this problem would be solved by using coal fly ash cenospheres or porous glass ceramics [20,21], collecting or producing these materials in large quantities is very difficult and costly. Therefore, most studies are focused on the solid-liquid separation techniques based on zeolite media's absorption [22][23][24]. Incidentally, this kind of zeolite absorption technique is practically limited to Cs.

Various Analysis of PS-Ashes and Leaching Test of Surrogates
The PS-ashes as received were chemically analyzed by X-ray fluorescence (XRF), employing Philips MagixPro (Royal Philips, Amsterdam, Holland) with fundamental parameter methods (FP). Loss on ignition (LOI) was separately determined by heating with an electric furnace at 1000˝C for 2 h. Furthermore, moisture content was measured with an oven at 105˝C for 2 h. Apparent densities were determined by a pycnometer. Then, specific surface areas were measured by a conventional Blaine apparatus (Marubishi Kagaku, Tokyo, Japan). Constituent minerals were identified by X-ray diffractometry (XRD), employing Rigaku RINT-2550 (Rigaku, Tokyo, Japan). To avoid reflections from glass, window-type sample holders made of Al metal were used throughout this measurement. Scanning electron microscopy (SEM) was adopted to observe textures of the PS-ashes, employing Jeol JSM-7600F (Jeol, Tokyo, Japan). XRD technique was also used to analyze the hardened paste specimens.
After 4 weeks aging, the SC-GP and plain specimens were further cured in ambient air for 2 weeks (4 + 2 week age), 8 weeks (12 week age), and 20 weeks (24 week age), respectively, in order to examine the stability of immobilization of the surrogates. After curing, the SC-GP samples were weighted and then crushed to be finer than 4 mm in size for the leaching test. Twelve point five grams of the crushed sample was immersed into the commercially available buffer solution (pH 4.01) containing phthalic salt, meant to mimic exposure to strong acidic rainfall at disposal sites. There are several methods to evaluate dissolutions as described in literature [31], but the phthalic salt buffer method is adopted as a laboratory scale method for the convenience of our laboratory facilities. The weight of the buffer solution was 125 g, 10 times the sample weight. Then, leaching test was performed in a 250 mL plastic bottle rotated at 60 rpm for 6 h. Finally, the leachates collected by percolating with filter paper were chemically analyzed by induction coupled plasma atomic emission spectrometry (ICP-AES), employing PerkinElmer, Optima 8300 (PerkinElmer, Waltham, MA, USA). Obtained concentrations of leachates were recalculated on the basis of 125 g to get leaching weights of the surrogates, while surrogate amounts were calculated to 12.5 g of SC-GP samples on the basis of filler/Na-silicates/water proportions and the resultant bulk densities of each age shown in Tables 2  and 4, respectively. Details are as follows: (1) Bulk densities obtained were regarded as apparent densities of the sample grains with the size of under 4 mm (Table 4). (2) Density (D 0 ) at 4 week age was disintegrated into filler/Na-silicates/water ratios according to the percentages shown in Table 2. For instance, for series 0-3SC shown in Table 4 (Table 6).
(6) The procedure is the same for other prolonged age specimens of 12 and 24 week ages of which bulk densities are indicated as D 2 and D 3 , respectively (Table 4).
Thus, immobilization ratios were obtained as follows: Immobilization ratio p%q " p1´Sr 2+ or Cs + in 125 g leachate{Sr 2+ or Cs + in 12.5 g sampleqˆ100 (1) In present study, the surrogates were regarded as a part of alkaline liquors. However, the surrogates' amounts were not taken into account in the above calculations of (2) and (3) since they were very small in amounts.
In addition, X-ray absorption near edge structure (XANES) was attempted to clarify bonding and coordination circumstances of Sr 2+ and Cs + incorporated into SC-GP samples. For Cs + , however, it was technically unsuccessful at the moment, due to the duplication of the L-edge of cesium with the K-edge of titanium in X-ray spectra.

Characteristics of PS-Ashes
Chemical compositions of PS-ashes are represented in Table 1. OTo3 has a usual composition. However, the others have unusual compositions. The high content of Cl in OTs2 would be attributed to refuse derived fuel (RDF), which contains much chlorine and moisture, while the high content of MgO in N45 to recycled plastic fuel (RPF), which contains much talc, commonly used as a filler in plastic appliances. Both RDF and RPF are used widely in Japan as boiler fuels, together with oils.
To clearly grasp the features of the PS-ashes, the chemical compositions are plotted on the ternary diagram, as shown in Figure 1, in terms of CaO-Al 2 O 3 -SiO 2 mass ratio. The plots encompass a wide range of PS-ashes. OTo/OTs series are plotted alongside with a trend line parallel to the first hydraulic line running through to the metakaolin point. On the other hand, N-series showed different features, plotted in the vicinity of blast furnace slag (BFS), a member of the first hydraulic line. The former group (OTo/OTs series) can be called high-alumina PS-ash, while the latter group (N-series) can be called low-alumina PS-ash. From another point of view, the PS-ashes can be classified into two groups-Ca-rich and Ca-poor. OTo1 and OTo3 are in the latter group, but the others are in the former group. Readers are kindly requested to refer to our past publication for relevant PS-ash compositions [31]. bulk densities are indicated as D2 and D3, respectively (Table 4).
Thus, immobilization ratios were obtained as follows: Immobilization ratio (%) = (1 − Sr 2+ or Cs + in 125 g leachate/Sr 2+ or Cs + in 12.5 g sample) × 100 (1) In present study, the surrogates were regarded as a part of alkaline liquors. However, the surrogates' amounts were not taken into account in the above calculations of (2) and (3) since they were very small in amounts.
In addition, X-ray absorption near edge structure (XANES) was attempted to clarify bonding and coordination circumstances of Sr 2+ and Cs + incorporated into SC-GP samples. For Cs + , however, it was technically unsuccessful at the moment, due to the duplication of the L-edge of cesium with the K-edge of titanium in X-ray spectra.

Characteristics of PS-Ashes
Chemical compositions of PS-ashes are represented in Table 1. OTo3 has a usual composition. However, the others have unusual compositions. The high content of Cl in OTs2 would be attributed to refuse derived fuel (RDF), which contains much chlorine and moisture, while the high content of MgO in N45 to recycled plastic fuel (RPF), which contains much talc, commonly used as a filler in plastic appliances. Both RDF and RPF are used widely in Japan as boiler fuels, together with oils.
To clearly grasp the features of the PS-ashes, the chemical compositions are plotted on the ternary diagram, as shown in Figure1, in terms of CaO-Al2O3-SiO2 mass ratio. The plots encompass a wide range of PS-ashes. OTo/OTs series are plotted alongside with a trend line parallel to the first hydraulic line running through to the metakaolin point. On the other hand, N-series showed different features, plotted in the vicinity of blast furnace slag (BFS), a member of the first hydraulic line. The former group (OTo/OTs series) can be called high-alumina PS-ash, while the latter group (N-series) can be called low-alumina PS-ash. From another point of view, the PS-ashes can be classified into two groups-Ca-rich and Ca-poor. OTo1 and OTo3 are in the latter group, but the others are in the former group. Readers are kindly requested to refer to our past publication for relevant PS-ash compositions [31]. SEM images of the PS-ash are represented in Figure 2. Sponge-like porous textures peculiar to gel materials [33] can be seen for all the samples-most clearly for OTo3. Moreover, ettringite prevailed in OTo2 and N45 in acicular to prismatic forms. Particularly in OTs2, some ettringite crystals developed in stout prismatic form. SEM images of the PS-ash are represented in Figure 2. Sponge-like porous textures peculiar to gel materials [33] can be seen for all the samples-most clearly for OTo3. Moreover, ettringite prevailed in OTo2 and N45 in acicular to prismatic forms. Particularly in OTs2, some ettringite crystals developed in stout prismatic form. XRD diagrams of the PS-ash are represented in Figure 3. Calcite, quartz, and anhydrite were identified, irrespective of the PS-ash. In addition, humps are recognized around 2θ = 20°-40°. Particularly, the humps are very clear in OTo3, suggesting the presence of amorphous materials. OTo3 is characterized by less presence of ettringite, while the others (OTs2 and N45) show the pronounced presence of ettringite due to high SO3 contents, in addition to high LOI and moisture contents, as seen in Table 1. It is important to classify the identified minerals on the basis of primary and secondary origins, as classified in Table 3. In OTo3, relict portlandite was detected, indicating that primarily quick lime XRD diagrams of the PS-ash are represented in Figure 3. Calcite, quartz, and anhydrite were identified, irrespective of the PS-ash. In addition, humps are recognized around 2θ = 20˝-40˝. Particularly, the humps are very clear in OTo3, suggesting the presence of amorphous materials. OTo3 is characterized by less presence of ettringite, while the others (OTs2 and N45) show the pronounced presence of ettringite due to high SO 3 contents, in addition to high LOI and moisture contents, as seen in Table 1. XRD diagrams of the PS-ash are represented in Figure 3. Calcite, quartz, and anhydrite were identified, irrespective of the PS-ash. In addition, humps are recognized around 2θ = 20°-40°. Particularly, the humps are very clear in OTo3, suggesting the presence of amorphous materials. OTo3 is characterized by less presence of ettringite, while the others (OTs2 and N45) show the pronounced presence of ettringite due to high SO3 contents, in addition to high LOI and moisture contents, as seen in Table 1. It is important to classify the identified minerals on the basis of primary and secondary origins, as classified in Table 3. In OTo3, relict portlandite was detected, indicating that primarily quick lime  It is important to classify the identified minerals on the basis of primary and secondary origins, as classified in Table 3. In OTo3, relict portlandite was detected, indicating that primarily quick lime (CaO) formed in the boiler. Water is generally sprinkled over the ash to prevent the ash from scattering after incineration, or sometimes the ash is pelletized. Accordingly, the quick lime slakes into portlandite and finally turns to calcite, in some cases to vaterite [31], due to reaction with CO 2 in air. The ashes derived from plants and woods generally comprise K 2 O, CaO, and SiO 2 as main components, in addition to MgO, P 2 O 5 , SO 3 , and Na 2 O as subordinate components [34]. Quartz may generate during the incineration in boilers. Anhydrite is a product of desulfurization. Generally, fluidized bed-type boilers are fed by limestone together with fuel coal for desulfurization, but for paper sludge incinerations, limestone is not required, since paper sludge contains much CaO. Moreover, calcite is usually used as filler and coating materials for ordinary grade paper. Contrary, kaolin or kaolin/calcite mixtures are used for high grade paper. Waste papers are so often fed to boilers as fuel, which also act as moisture absorber of wet paper sludge, so the origin of the Al 2 O 3 component would be the kaolin. Strictly speaking, the presence of talc is because talc is so widely used as filler materials for paper and plastic appliances, so it remains in the ash of paper sludge, waste paper, and RPF combustions. A small amount of anorthite was identified, of which formation was also reported in literature for the ash from a pressurized fluidized bed-type boiler [16]. Vermiculite and hydrocalumite are secondary minerals formed during the water sprinkling. The presence of kovdorskite is also suspected other than hydrocalumite, judging from the 2θ positions. OTs2 and N45 show nearly the same XRD patterns-in which ettringite is prevailed-but talc is lacking in OTs2. It should be noted that hydrocalcite was identified in OTs2, of which the main peak is slightly different from the quartz peak, as indicated in Figure 3. Anorthite is also identified in minor quantities in both OTs2 and N45. Forsterite might be a primary origin, as discussed later in Section 3.3. Table 3. Summary of XRD results of PS-ashes. (CaO) formed in the boiler. Water is generally sprinkled over the ash to prevent the ash from scattering after incineration, or sometimes the ash is pelletized. Accordingly, the quick lime slakes into portlandite and finally turns to calcite, in some cases to vaterite [31], due to reaction with CO2 in air. The ashes derived from plants and woods generally comprise K2O, CaO, and SiO2 as main components, in addition to MgO, P2O5, SO3, and Na2O as subordinate components [34]. Quartz may generate during the incineration in boilers. Anhydrite is a product of desulfurization. Generally, fluidized bed-type boilers are fed by limestone together with fuel coal for desulfurization, but for paper sludge incinerations, limestone is not required, since paper sludge contains much CaO. Moreover, calcite is usually used as filler and coating materials for ordinary grade paper. Contrary, kaolin or kaolin/calcite mixtures are used for high grade paper. Waste papers are so often fed to boilers as fuel, which also act as moisture absorber of wet paper sludge, so the origin of the Al2O3 component would be the kaolin. Strictly speaking, the presence of talc is because talc is so widely used as filler materials for paper and plastic appliances, so it remains in the ash of paper sludge, waste paper, and RPF combustions. A small amount of anorthite was identified, of which formation was also reported in literature for the ash from a pressurized fluidized bed-type boiler [16]. Vermiculite and hydrocalumite are secondary minerals formed during the water sprinkling. The presence of kovdorskite is also suspected other than hydrocalumite, judging from the 2θ positions.

PS-ash Minerls PS-ash Remark
OTs2 and N45 show nearly the same XRD patterns-in which ettringite is prevailed-but talc is lacking in OTs2. It should be noted that hydrocalcite was identified in OTs2, of which the main peak is slightly different from the quartz peak, as indicated in Figure 3. Anorthite is also identified in minor quantities in both OTs2 and N45. Forsterite might be a primary origin, as discussed later in Section 3.3.  It should be stressed that raw PS-ashes are not completely amorphous, but abundant in crystalline phases-quite different from conventional geopolymer fillers such as metakaolin, water quenched blast furnace slag, coal fly ash, and so on.

Physical Properties of PS-Ash-Based Geopolymer
As shown in Table 4, for the #0 and #1 liquors, adequate values of L/F of PS-ash based geopolymer were from 1 to 1.5, depending on filler characters, particularly on specific surface areas and porous textures. Incidentally, a standard L/F is 0.4 for ordinary geopolymers in pastes [35]. OTs2 showed extremely slow setting with L/F 1.0, taking overnight, presumably due to the presence of so much chlorine, in addition to low specific surface area, so the specimen preparation for OTs2 was skipped in the present experiment. Other PS-ash-based geopolymer mixtures set within 40 min. Retarding effects of chlorine are recently confirmed by the experiment of using NaCl (Ichimiya, K., 2016, personal communication).  It should be stressed that raw PS-ashes are not completely amorphous, but abundant in crystalline phases-quite different from conventional geopolymer fillers such as metakaolin, water quenched blast furnace slag, coal fly ash, and so on.

Physical Properties of PS-Ash-Based Geopolymer
As shown in Table 4, for the #0 and #1 liquors, adequate values of L/F of PS-ash based geopolymer were from 1 to 1.5, depending on filler characters, particularly on specific surface areas and porous textures. Incidentally, a standard L/F is 0.4 for ordinary geopolymers in pastes [35]. OTs2 showed extremely slow setting with L/F 1.0, taking overnight, presumably due to the presence of so much chlorine, in addition to low specific surface area, so the specimen preparation for OTs2 was skipped in the present experiment. Other PS-ash-based geopolymer mixtures set within 40 min. Retarding effects of chlorine are recently confirmed by the experiment of using NaCl (Ichimiya, K., 2016, personal communication). It should be noted that when the #0 liquor was applied, the OTo3-based geopolymer mixtures swelled. Eventually, many pores of foaming origin were observed in the hardened specimens (Figure 4), resulting in smaller bulk densities, as indicated in Table 4. Presumably, free Al metal is included in this kind of PS-ash. The origin of the Al metal would be Al-laminated appliances (such as food containers), which might slip into the RDF used in the boiler plant of OTo3. However, at this moment, the Al metal could not be observed, even under the high power of scanning electron microscopy and energy dispersive spectroscopy (SEM-EDS), which is probably disseminated at the nanometer scale in the ash. Hydrogen gas is generated due to the high pH circumstances of the #0 liquor. To the contrary, no swelling was observed for the #1 liquor without mixing the caustic soda solution. Incidentally, this type of swelling is also reported for an RDF-ash [36] and hydrogen generation is confirmed by gas chromatography (Goda, H., 2012, oral communication).
Flexural strength of this lightweight material was relatively high, compared to the other non-swelled materials. It is postulated that nitride ions suppress the development of strength to a certain degree, due to the pH-lowering action of alkaline liquors [31,35]. However, in this study, this phenomenon was restricted to the specimens mixed with the #1 liquor.  It should be noted that when the #0 liquor was applied, the OTo3-based geopolymer mixtures swelled. Eventually, many pores of foaming origin were observed in the hardened specimens (Figure 4), resulting in smaller bulk densities, as indicated in Table 4. Presumably, free Al metal is included in this kind of PS-ash. The origin of the Al metal would be Al-laminated appliances (such as food containers), which might slip into the RDF used in the boiler plant of OTo3. However, at this moment, the Al metal could not be observed, even under the high power of scanning electron microscopy and energy dispersive spectroscopy (SEM-EDS), which is probably disseminated at the nanometer scale in the ash. Hydrogen gas is generated due to the high pH circumstances of the #0 liquor. To the contrary, no swelling was observed for the #1 liquor without mixing the caustic soda solution. Incidentally, this type of swelling is also reported for an RDF-ash [36] and hydrogen generation is confirmed by gas chromatography (Goda, H., 2012, oral communication).
Flexural strength of this lightweight material was relatively high, compared to the other nonswelled materials. It is postulated that nitride ions suppress the development of strength to a certain degree, due to the pH-lowering action of alkaline liquors [31,35]. However, in this study, this phenomenon was restricted to the specimens mixed with the #1 liquor.

XRD Results of Hardened Geopolymer
For the plain specimens, XRD diagrams are represented in Figure 5 for the #0 and #1 liquors, respectively. Quartz and calcite remained more or less intact, irrespective of sample species. However, judging from the variation of peak heights, some part of these minerals were reacted and diminished in highly alkaline circumstances, even for quartz. Quartz decrease was also observed in the literature [5]. Ettringite and anhydrite were not detected any more, and neither were anorthite and vermuculite. Instead, the formation of carbonate ettringite was observed, irrespective of specimen species. It is noted that magnesian calcite, (Ca, Mg)CO3, was identified for 0-1 specimen, of

XRD Results of Hardened Geopolymer
For the plain specimens, XRD diagrams are represented in Figure 5 for the #0 and #1 liquors, respectively. Quartz and calcite remained more or less intact, irrespective of sample species. However, judging from the variation of peak heights, some part of these minerals were reacted and diminished in highly alkaline circumstances, even for quartz. Quartz decrease was also observed in the literature [5]. Ettringite and anhydrite were not detected any more, and neither were anorthite and vermuculite. Instead, the formation of carbonate ettringite was observed, irrespective of specimen species. It is noted that magnesian calcite, (Ca, Mg)CO 3 , was identified for 0-1 specimen, of which peaks are located just a little bit higher than the 2θ angles of calcite, CaCO 3 , as shoulders. Peak patterns of magnesian calcite are quite different from dolomite, Ca, Mg(CO 3 ) 2 . Formation of faujasite, a member of zeolite family, was observed for 0-1 and 1-3 specimens. Other identified minerals are pirssonite, burkeite, and thenerdite, depending on specimens-all formed accompanied with the geopolymerization of mixed alkaline liquors.   Table 4, and mineral keys refer to Tables 3 and 5.
It is more plausible that the forsterite identified for specimens 0-3 and 1-3 might be a primary origin formed in the boiler. This mineral peaks might be concealed with anhydrite peaks in raw PSashes, and appeared intact according to the disappearance of anhydrite. Other than the crystalline phases mentioned above, there are amorphous phases more or less depending on specimens as so far postulated, judging from some humps around 2θ = 30°. For SC-GP specimens, no marked differences from plain specimens were observed, probably due to lower-level dosages of the surrogates. However, according to literature using metakaolin filler under higher level presence of nitrates, the formation of sodalite and cancrinite was reported as nitrate-bearing phases in addition to zeolite A and zeolite X, depending on NaOH concentrations [37].
Talking again about the faujasite, naturally-occurring faujasite generally has the chemical formula (Na2, Ca, Mg)3.5(Al7Si17O48)•32H2O, in which the S/N (SiO2/Na2O) molar ratio is 4.86. Incidentally, according to literature, naturally occurring faujasite has an S/N of around 4.5 [38]. It is well-known that synthetic faujasite is classified by S/N into zeolite X (lower than 3.0) and zeolite Y (higher than 3.0). XRD patterns represented in Figure 5 show that faujasite patterns are close to Na2Al2Si2.4O8.8•6.7H2O, where the S/N is 2.4, so the formation of zeolite X is more plausible, suggesting that the incorporation of Na-Al combination is large in the faujasite structure.

Reaction Process of PS-Ash-Based Geopolymers
Resultant minerals are summarized in Table 5, classified into three categories. The first is the  Table 4, and mineral keys refer to Tables 3 and 5.
It is more plausible that the forsterite identified for specimens 0-3 and 1-3 might be a primary origin formed in the boiler. This mineral peaks might be concealed with anhydrite peaks in raw PS-ashes, and appeared intact according to the disappearance of anhydrite. Other than the crystalline phases mentioned above, there are amorphous phases more or less depending on specimens as so far postulated, judging from some humps around 2θ = 30˝. For SC-GP specimens, no marked differences from plain specimens were observed, probably due to lower-level dosages of the surrogates. However, according to literature using metakaolin filler under higher level presence of nitrates, the formation of sodalite and cancrinite was reported as nitrate-bearing phases in addition to zeolite A and zeolite X, depending on NaOH concentrations [37].
Talking again about the faujasite, naturally-occurring faujasite generally has the chemical formula (Na 2 , Ca, Mg) 3.5 (Al 7 Si 17 O 48 )¨32H 2 O, in which the S/N (SiO 2 /Na 2 O) molar ratio is 4.86. Incidentally, according to literature, naturally occurring faujasite has an S/N of around 4.5 [38]. It is well-known that synthetic faujasite is classified by S/N into zeolite X (lower than 3.0) and zeolite Y (higher than 3.0). XRD patterns represented in Figure 5 show that faujasite patterns are close to Na 2 Al 2 Si 2.4 O 8.8¨6 .7H 2 O, where the S/N is 2.4, so the formation of zeolite X is more plausible, suggesting that the incorporation of Na-Al combination is large in the faujasite structure.

Reaction Process of PS-Ash-Based Geopolymers
Resultant minerals are summarized in Table 5, classified into three categories. The first is the intrinsic minerals of primary origin formed in boilers. The second is the extrinsic minerals of secondary origin formed due to the water sprinkling. The third is relevant to the geopolymerization of alkaline liquors with the minerals included in the PS-ashes.
Referring to the hardening process of PS-ashes, the primary and the secondary minerals react with the alkaline liquors so that the recombination takes place, and minerals peculiar to the geopolymerization form. Thereby, forsterite may remain intact, while quartz and calcite may remain partially intact. Other minerals were completely consumed to yield a group of minerals called GP-minerals in Table 5, which are carbonate ettringite, faujasite, pirssonite, burkeite, and thenerdite, and sometimes magnesian calcite, other than amorphous gels which are truly matrices. The species of GP-minerals are dependent on the PS-ashes and alkaline liquors used. It is noteworthy to refer to the amorphous phases peculiar to geopolymers, which are currently believed to consist of two distinct phases-so called C-A-S-H gels and N-A-S-H gels-where C, A, S, H, and N denote CaO, Al 2 O 3 , SiO 2 , H 2 O, and Na 2 O, respectively. It is considered that in Ca-rich geopolymer systems, C-A-S-H is stable, while N-A-S-H is unstable, due to the occurrence of an ion exchange of Ca 2+ for Na + . Accordingly, N-A-S-H turns gradually to C-A-S-H and eventually diminishes [39][40][41][42]. Strictly speaking, initial C-A-S-H and N-A-S-H may finally become (Ca, N)-A-S-H gels after the ion exchange.

Immobiization Ratios of Sr 2+ and Cs +
Results of the 4 + 2 week age samples are tabulated in Table 6, together with relevant data for calculations. High immobilization ratios of Sr 2+ and Cs + were reached for 0-1SC and 1-1SC, both using OTo3 as filler, whereas Cs + immobilization was relatively low for 0-3SC and 1-3SC, both using N45 as filler. It should be noted that specimen 1-3SC showed over-scale, indicating poor immobilization of Sr 2+ , so more detailed measurements of ICP were skipped for this specimen. Cs + will be mentioned later. Table 5. Resultant -minerals in PS-ash based geopolymers in comparison with PS-ash minerals and whole reaction process. Table 5. Resultant -minerals in PS-ash based geopolymers in comparison with PS-ash minerals and whole reaction process.  Table 5. Resultant -minerals in PS-ash based geopolymers in comparison with PS-ash minerals and whole reaction process.

PS-ash Minerals
Minerals in PS-ash based geopolymers  Table 5. Resultant -minerals in PS-ash based geopolymers in comparison with PS-ash minerals and whole reaction process.  Table 5. Resultant -minerals in PS-ash based geopolymers in comparison with PS-ash minerals and whole reaction process.   Regarding the immobilization mechanisms of Sr 2+ and Cs + , two possibilities are considered. One is that these ions are incorporated into faujasite and the other is into geopolymer gels (GP-gels). Faujasite would accommodate both Sr 2+ and Cs + , since it consists of sodalite cages with openings of 0.74 nm in diameter. Incidentally, according to Shannon and Prewitt [43], ionic radii of Sr 2+ and Cs + are 0.118-0.144 nm and 0.167-0.188 nm, respectively, depending on coordination numbers from 6-hold to 12-hold. Gobbinsite, (Na,Ca 0.5 ) 6 (Al 6 Si 10 )O 32¨1 2H 2 O-a zeolite family mineral-was also identified as a candidate mineral in a previous study [31]. However, judging from XRD peak intensities, the formation of faujasite is in very small quantities, and the formation of GP-gels is prevalent due to the polycondensation of applied alkaline liquors.

Minerals in PS-ash based geopolymers
It is postulated that there are two kinds of GP-gels-C-A-S-H and N-A-S-H [39][40][41][42]. N-A-S-H is considered to be unstable under the co-presence of C-A-S-H, due to the ion exchange of Ca 2+ for Na + . Sr 2+ may be preferentially incorporated into C-A-S-H. We considered at the moment that the high MgO content of specimens 1-3SC (Table 1) may interfere the stable formation of C-A-S-H in young ages, so 1-3SC showed over-scale for Sr 2+ . Incidentally, the stability and instability of GP-gels are also called "a complex multistep reaction process", leading to a phase-mixed product in the case of N-A-S-H [44]. That is, a non-equilibrium-to-equilibrium transition of GP-gels. However, little has been studied in the case of C-A-S-H.
For Cs + incorporation, N-A-S-H and faujasite may play an important role. However, it is predictive that N-A-S-H becomes unstable with elapsed time. Therefore, the immobilization ratio of Cs + may decrease with the ion exchange, resulting in some Cs + depletion. In the long run, however, with the formation of new C-A-S-H phase, (C, N)-A-S-H, Cs + may be again incorporated. In order to confirm this hypothesis, immobilization ratios of prolonged ages were measured up to 24 weeks, nearly 6 months. The results are shown in Table 7. For Sr 2+ , higher immobilization ratios were generally maintained, irrespective of material age. However, 1-3SC showed unstable immobilization ratios. Strangely, we found that it turned dramatically up to 91.73% at 12 week of age, but it turned down again at 24 weeks of age, suggesting unstable incorporation of Sr 2+ in this mixture. As mentioned, the high MgO content may be a cause of this instability, and there also may be some transitional stages in the evolution of C-A-S-H gels with elapsed time.
For Cs + , decreasing immobilization ratios were found at 12 weeks of age, as expected, and this phenomenon is extremely remarkable for the #0 liquor. However, these ratios again rose up at 24 weeks of age, as expected.
As a whole, 1-1SC applying #1 liquor exhibited stable immobilization ratios, irrespective of material ages. To prevent the fluctuation of immobilization ratios, one of the measures would be high-temperature curing, which accelerates the polycondensation reactions to yield stable GP-gels in a short period of time. Incidentally, high immobilization ratios were also reported for Cs + incorporated into alkali-activated fly ash matrices cured at 85˝C and 120˝C, reaching 98.56%-99.78% immobilization ratios that were analyzed by toxic characteristic leaching procedure (TCLP), using the pH 2.88 leaching solution of glacial acetic acid [35]. Retentions of 95.2% and 81.4% are reported, respectively, for Sr 2+ and Cs + in 0.01 M NaOH solution, using magnetic zeolite nanocomposites [45].
Finally, we tentatively tried to convert the hardened SC-GP into slags to reduce volumes. Fusion temperature and duration were 1400˝C-1 h for 0-1SC and 1-1SC, and 1300˝C-1 h for 0-3SC and 1-3SC, respectively. Moistures of GP-liquor origin as well as evaporates represented as LOI in Table 1 were taken into account in calculations. Results were tabulated at the right-bottom corner of Table 6, showing high immobilization ratios for both Sr 2+ and Cs + . Therefore, slag conversion would be one of the options for eternal burials as proposed in a previous study [31].

XANES
XANES spectra of the K absorption edge of strontium for SC-GP specimens of 4 + 2 week age were compared with the spectra of the standard samples of SrCl 2 , SrCO 3 , and slawsonite, (Sr, Ca)Al 2 Si 2 O 8 ). The former two are reagents, and slawsonite is a naturally-occurring mineral involving strontium in the structure from Sarusaka, Kochi, Japan. As shown in Figure 6, spectra are relatively well-separated from each other for the standard samples, indicating that the chemical states of Sr 2+ were different among SrCl 2 , SrCO 3 , and slawsonite. On the other hand, XANES spectra of strontium in the SC-GP specimens are almost in a bundle, indicating that chemical states of Sr 2+ in these specimens are nearly identical. The obtained results indicate that the chemical states of Sr 2+ in SC-GP specimens resemble that in slawsonite. Incidentally, in slawsonite, Sr 2+ is surrounded by O 2´i n 7-hold coordination with a mean M-O distance of 0.263 nm [46]. Deducting the ionic radius of O 2´, which is 0.126 nm, after Shannon and Prewitt [43], 0.137 nm is obtained as the net ionic radius of Sr 2+ . However, this ionic radius of Sr 2+ corresponds to 8-hold coordination, according to [47].
Materials 2016, 9,633 13 of 17 of this instability, and there also may be some transitional stages in the evolution of C-A-S-H gels with elapsed time. For Cs + , decreasing immobilization ratios were found at 12 weeks of age, as expected, and this phenomenon is extremely remarkable for the #0 liquor. However, these ratios again rose up at 24 weeks of age, as expected.
As a whole, 1-1SC applying #1 liquor exhibited stable immobilization ratios, irrespective of material ages. To prevent the fluctuation of immobilization ratios, one of the measures would be high-temperature curing, which accelerates the polycondensation reactions to yield stable GP-gels in a short period of time. Incidentally, high immobilization ratios were also reported for Cs + incorporated into alkali-activated fly ash matrices cured at 85 °C and 120 °C, reaching 98.56%-99.78% immobilization ratios that were analyzed by toxic characteristic leaching procedure (TCLP), using the pH 2.88 leaching solution of glacial acetic acid [35]. Retentions of 95.2% and 81.4% are reported, respectively, for Sr 2+ and Cs + in 0.01 M NaOH solution, using magnetic zeolite nanocomposites [45].
Finally, we tentatively tried to convert the hardened SC-GP into slags to reduce volumes. Fusion temperature and duration were 1400 °C-1 h for 0-1SC and 1-1SC, and 1300 °C-1 h for 0-3SC and 1-3SC, respectively. Moistures of GP-liquor origin as well as evaporates represented as LOI in Table 1 were taken into account in calculations. Results were tabulated at the right-bottom corner of Table 6, showing high immobilization ratios for both Sr 2+ and Cs + . Therefore, slag conversion would be one of the options for eternal burials as proposed in a previous study [31].

XANES
XANES spectra of the K absorption edge of strontium for SC-GP specimens of 4 + 2 week age were compared with the spectra of the standard samples of SrCl2, SrCO3, and slawsonite, (Sr, Ca)Al2Si2O8). The former two are reagents, and slawsonite is a naturally-occurring mineral involving strontium in the structure from Sarusaka, Kochi, Japan. As shown in Figure 6, spectra are relatively well-separated from each other for the standard samples, indicating that the chemical states of Sr 2+ were different among SrCl2, SrCO3, and slawsonite. On the other hand, XANES spectra of strontium in the SC-GP specimens are almost in a bundle, indicating that chemical states of Sr 2+ in these specimens are nearly identical. The obtained results indicate that the chemical states of Sr 2+ in SC-GP specimens resemble that in slawsonite. Incidentally, in slawsonite, Sr 2+ is surrounded by O 2− in 7-hold coordination with a mean M-O distance of 0.263 nm [46]. Deducting the ionic radius of O 2− , which is 0.126 nm, after Shannon and Prewitt [43], 0.137 nm is obtained as the net ionic radius of Sr 2+ . However, this ionic radius of Sr 2+ corresponds to 8-hold coordination, according to [47]. It should be stressed again that 1-3SC showed less capability of Sr 2+ at 4 + 2 and 24 weeks of age. However, it was found that the immobilization ratio became enhanced to 91.73% at the intermediate age of 12 weeks. XANES measurements were performed by using 4 + 2 week age specimens, but there is about one month time lag for the actual measurements, due to time sharing schedules of the facility. Therefore, it is difficult, at the moment, to tell the spectra of 1-3SC, whether coming from embryo stage of C-A-S-H gels due to slow coagulation or coming from well-developed and matured C-A-S- It should be stressed again that 1-3SC showed less capability of Sr 2+ at 4 + 2 and 24 weeks of age. However, it was found that the immobilization ratio became enhanced to 91.73% at the intermediate age of 12 weeks. XANES measurements were performed by using 4 + 2 week age specimens, but there is about one month time lag for the actual measurements, due to time sharing schedules of the facility. Therefore, it is difficult, at the moment, to tell the spectra of 1-3SC, whether coming from embryo stage of C-A-S-H gels due to slow coagulation or coming from well-developed and matured C-A-S-H or (C, N)-A-S-H gels. According to literature [48,49], Sr 2+ incorporations are unstable in metakaolin-based geopolymers, in which N-A-S-H gels form preferentially. In other words, depletion of Sr 2+ takes place to yield SrCO 3 in air, but no depletion of Cs + occurs, meaning 100% incorporation of Cs + into N-A-S-H. Formation of Sr(OH) 2 and as SrCO 3 is also reported in the metakaolin-based geopolymer, where the clinoptilolite zeolite encapsulating Sr 2+ and Cs + is mixed [50].
At the moment, no spectral profiles corresponding to SrCO 3 were observed in the XANES spectra, even for 1-3SC, which showed highly fluctuating immobilization ratios of Sr 2+ with elapsed time, as mentioned. Therefore, we concluded that no depletion of Sr 2+ took place in our SC-GP specimens and that the fluctuations may be attributed to the transitional GP-gel structures of C-A-S-H or (C, N)-A-S-H. That is, for instance, differences in degrees of polymerization and/or differences in tetrahedral order-disorder configurations, which would be sensitive to acidic conditions of the leaching test. The XANES technique will become a powerful measure to clarify the bonding and coordination circumstances of matrix gels in geopolymers.

Conclusions
Paper mill wastes-PS-ashes-can be solidified at ambient temperature by geopolymerization technique, by mixing with alkaline liquors designated as #0 liquor (having an aqueous Na-metasillicate composition) or #1 liquor (having aqueous Na-disilicate composition), independently. It has been found that PS-ashes consist of a high quantity of crystalline phases, accompanied with some amorphous phases such that they can be regarded as semi-crystalline fillers, quite different from the conventional fillers of metakaolin, glassy blast furnace slag, and glassy coal fly ash, which consist of almost entirely amorphous materials.
Primarily, solidification and strength tests were carried out, preparing solidified paste specimens, plain, and SC-GP-containing non-radioactive Sr(NO 3 ) 2 and CsNO 3 as surrogates. Specimens were cured at 20˝C-100% RH for 4 weeks. Subsequently, they were air-dried up to 24 weeks of age. Finally, immobilization ratios of Sr 2+ and Cs + were determined for the SC-GP specimens at 6, 12 and 24 weeks, respectively, by leaching test with pH 4.01 buffer solution. The following conclusions are summarized.
(1) Constituent minerals of the PS-ashes are classified into two groups: the primary or intrinsic minerals formed in boilers, and the secondary or extrinsic minerals due to water sprinkling. The primary and secondary minerals decompose into so-called GP-minerals during the geopolymerization process. (2) Hazardous waters contaminated with radioisotopes can be solidified by geopolymer technique, making use of the porous textures of PS-ashes, which can absorb much water. The leaching test generally showed high immobilization ratios-98%-99% and 97%-98% for Sr 2+ and Cs + , respectively, depending on material ages, alkaline liquors, and filler species. However, some specimens showed highly fluctuating immobilization ratios for both of Sr 2+ and Cs + with elapsed time. (3) XANES spectra of strontium K-edge of SC-GP specimens were measured at 6 weeks of age, and were discussed in comparison with the slawsonite spectrum. The obtained results showed that chemical environments of Sr 2+ incorporated into the PS-ash based GP-gels are similar to slawsonite.