<?xml version="1.0" encoding="UTF-8"?><!DOCTYPE article  PUBLIC "-//NLM//DTD Journal Publishing DTD v3.0 20080202//EN" "http://dtd.nlm.nih.gov/publishing/3.0/journalpublishing3.dtd"><article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" dtd-version="3.0" xml:lang="en" article-type="research article"><front><journal-meta><journal-id journal-id-type="publisher-id">ACES</journal-id><journal-title-group><journal-title>Advances in Chemical Engineering and Science</journal-title></journal-title-group><issn pub-type="epub">2160-0392</issn><publisher><publisher-name>Scientific Research Publishing</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.4236/aces.2015.52022</article-id><article-id pub-id-type="publisher-id">ACES-55736</article-id><article-categories><subj-group subj-group-type="heading"><subject>Articles</subject></subj-group><subj-group subj-group-type="Discipline-v2"><subject>Chemistry&amp;Materials Science</subject></subj-group></article-categories><title-group><article-title>
 
 
  Investigation of the Transition Reaction of Tobermorite to Xonotlite under Influence of Additives
 
</article-title></title-group><contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>ndrea</surname><given-names>Hartmann</given-names></name><xref ref-type="aff" rid="aff1"><sup>1</sup></xref></contrib><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>David</surname><given-names>Schulenberg</given-names></name><xref ref-type="aff" rid="aff1"><sup>1</sup></xref></contrib><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Josef-Christian</surname><given-names>Buhl</given-names></name><xref ref-type="aff" rid="aff1"><sup>1</sup></xref></contrib></contrib-group><aff id="aff1"><addr-line>Institute of Mineralogy, Hannover University, Hannover, Germany</addr-line></aff><pub-date pub-type="epub"><day>04</day><month>03</month><year>2015</year></pub-date><volume>05</volume><issue>02</issue><fpage>197</fpage><lpage>214</lpage><history><date date-type="received"><day>10</day>	<month>March</month>	<year>2015</year></date><date date-type="rev-recd"><day>accepted</day>	<month>12</month>	<year>April</year>	</date><date date-type="accepted"><day>16</day>	<month>April</month>	<year>2015</year></date></history><permissions><copyright-statement>&#169; Copyright  2014 by authors and Scientific Research Publishing Inc. </copyright-statement><copyright-year>2014</copyright-year><license><license-p>This work is licensed under the Creative Commons Attribution International License (CC BY). http://creativecommons.org/licenses/by/4.0/</license-p></license></permissions><abstract><p>
 
 
  The objective of the present work was to investigate the transition reaction of the calcium silicate hydrate tobermorite into xonotlite under influence of additives. Tobermorite is the main binding agent in steam hardened building materials and the appearance of xonotlite indicates the progress of hardening and an overcuring of the material. Hydrothermal experiments under addition of sucrose, calcium formate and calcium chloride dihydrate to the main components quartz and lime were done using temperatures of 220&#176;C and a reaction time of 40.5 h. All experiments were performed with powders as well as with pressed educts. The products of all syntheses were analyzed with XRD, SEM/EDX and FTIR. The references as well as the syntheses with calcium chloride dihydrate led to the formation of 11 &#197; tobermorite and xonotlite. The former showed the best results and even synthesis with pressed educts and calcium chloride dihydrate revealed an accelerating effect of the additive. In contrast syntheses with sucrose had the worst reactivity and led to the formation of calcite beside the CSH-phase scawtite. The additive calcium formate was only slightly oppressing the crystallization of tobermorite and favouring the formation of xonotlite. Syntheses with pressed pellets and sucrose or calcium formate showed generally worse results.
 
</p></abstract><kwd-group><kwd>CSH-Phases</kwd><kwd> Tobermorite</kwd><kwd> Xonotlite</kwd><kwd> Additives</kwd><kwd> Retarder</kwd><kwd> Accelerator</kwd></kwd-group></article-meta></front><body><sec id="s1"><title>1. Introduction</title><p>Additives play an important role in the production of building materials. Their accelerating or retarding effects on the course of hydraulic reactions are widely used in concrete production and cement treatment to comply the requirements of the material [<xref ref-type="bibr" rid="scirp.55736-ref1">1</xref>] -[<xref ref-type="bibr" rid="scirp.55736-ref5">5</xref>] . Basic research in building materials chemistry over decades could reveal many facets of the reaction modifications under influence of organic and inorganic additives. Retarding processes based on specific adsorption of ions of the additive on the surface of the growing phases like tricalcium silicate (C<sub>3</sub>S; C: CaO, S: SiO<sub>2</sub>) in cement was observed for classical retarders like sucrose. Rapid growth of C<sub>3</sub>S is thus inhibited [<xref ref-type="bibr" rid="scirp.55736-ref6">6</xref>] . As this process is strongly connected with consumption of calcium-ions, the C/S ratio in the system diminishes resulting in further retarding of the progress of setting and hardening of cement [<xref ref-type="bibr" rid="scirp.55736-ref7">7</xref>] - [<xref ref-type="bibr" rid="scirp.55736-ref9">9</xref>] .</p><p>In accelerators like calcium chloride the ionic potential of cations and anions contribute to the effect by influencing the ion-hydratation processes as well as the diffusion and the transport of building blocks from the solution to the growing crystals [<xref ref-type="bibr" rid="scirp.55736-ref10">10</xref>] - [<xref ref-type="bibr" rid="scirp.55736-ref12">12</xref>] . Similar effects were observed with organic accelerators like calcium formate [<xref ref-type="bibr" rid="scirp.55736-ref1">1</xref>] [<xref ref-type="bibr" rid="scirp.55736-ref13">13</xref>] . Even the simple role of decrease of pH-value has to be taken into account when additives are inserted [<xref ref-type="bibr" rid="scirp.55736-ref14">14</xref>] - [<xref ref-type="bibr" rid="scirp.55736-ref16">16</xref>] . In contrast, an increase of alkalinity was found to have no remarkable effect on C<sub>3</sub>S hydratation [<xref ref-type="bibr" rid="scirp.55736-ref13">13</xref>] [<xref ref-type="bibr" rid="scirp.55736-ref17">17</xref>] .</p><p>Compared with the comprehensive theoretical studies and experimental work connected with cement and concrete investigations on insertion of additives in the field of steam hardened building materials are much lesser numerous. Those materials were produced by autoclave curing at 160˚C - 200˚C under saturated steam pressure from quartz, burnt lime and water. Calcium-silicate-hydrate phases (CSH-phases) were formed during this reaction within a few hours [<xref ref-type="bibr" rid="scirp.55736-ref18">18</xref>] - [<xref ref-type="bibr" rid="scirp.55736-ref20">20</xref>] . The main important phase, obtained during steam curing around 180˚C is the CSH phase 11 &#197; tobermorite. The proper crystallization of this chain silicate with needle to band-like morphology is essential for a sufficient firmness of the material, as tobermorite is the main binding agent in steam hardened building materials. Tobermorite belongs to the group of chain silicates and its structure and real structure is well known [<xref ref-type="bibr" rid="scirp.55736-ref21">21</xref>] -[<xref ref-type="bibr" rid="scirp.55736-ref23">23</xref>] . The tobermorite formula depends on slight deviations in chemical composition according to differences of water molecules and hydroxyl groups per unit-cell. The compositions Ca<sub>5</sub>Si<sub>6</sub>O<sub>17</sub> &#215; 5H<sub>2</sub>O (C<sub>5</sub>S<sub>6</sub>H<sub>5</sub>; H: H<sub>2</sub>O) [<xref ref-type="bibr" rid="scirp.55736-ref20">20</xref>] and Ca<sub>5</sub>[Si<sub>6</sub>O<sub>16</sub>(OH)<sub>2</sub>] &#215; 2H<sub>2</sub>O [<xref ref-type="bibr" rid="scirp.55736-ref21">21</xref>] were usually used for tobermorite with the CaO/SiO<sub>2</sub>-ratio (C/S) of 0.83. The crystallization process of tobermorite starts with formation of calcium rich so-called pre-phases like CSHI and α-C<sub>2</sub>SH followed by 11 &#197; tobermorite. The latter transforms into xonotlite C<sub>6</sub>S<sub>6</sub>O<sub>17</sub>(OH)<sub>2</sub> at prolonged reaction time and elevated temperatures 220˚C [<xref ref-type="bibr" rid="scirp.55736-ref18">18</xref>] - [<xref ref-type="bibr" rid="scirp.55736-ref20">20</xref>] [<xref ref-type="bibr" rid="scirp.55736-ref24">24</xref>] . As mentioned above there is only a few knowledge on the effects of additives during this formation of CSH-phases in steam hardened building materials like lime sand stones and autoclaved aerated concrete. In our former experimental study the addition of sucrose [<xref ref-type="bibr" rid="scirp.55736-ref25">25</xref>] , calcium formate [<xref ref-type="bibr" rid="scirp.55736-ref26">26</xref>] and calcium chloride dehydrate [<xref ref-type="bibr" rid="scirp.55736-ref27">27</xref>] during tobermorite synthesis was investigated at 200˚C and autogeneous pressure. A retarding effect of sucrose on the tobermorite crystalli- zation was observed. The additive calcium formate indicates only a slightly retarding effect of tobermorite crystallization. However syntheses with addition of calcium chloride dihydrate resulted in an accelerating effect on the tobermorite crystallization.</p><p>In the present paper the influence of the additives sucrose, calcium formate and calcium chloride dihydrate on the transition reaction of tobermorite to xonotlite Ca<sub>6</sub>Si<sub>6</sub>O<sub>17</sub>(OH)<sub>2</sub> (C<sub>6</sub>S<sub>6</sub>H) was investigated in dependence of different mass ratios of the additive beside lime and quartz. This selected reaction is of special interest in production of steam hardened building materials as the occurrence of noticeable parts xonotlite beside tobermorite indicates the start of over curing of the material.</p></sec><sec id="s2"><title>2. Experimental</title><sec id="s2_1"><title>2.1. Syntheses</title><p>In the present paper two synthesis series were done―series a) with powder educts and b) with pressed educts. For both types first reference syntheses without additives were prepared. As in former experiments on CSH crystallization [<xref ref-type="bibr" rid="scirp.55736-ref25">25</xref>] - [<xref ref-type="bibr" rid="scirp.55736-ref28">28</xref>] for all syntheses with powders 1.5 g fine grained quartz with particle size &gt; 230 mesh (FLUKA 83340) was selected as silica source. Lime was obtained by calcination of CaCO<sub>3</sub> (Johnson Mattay GmbH) at 1000˚C for 3 h and amounts of 1.16 g (for reference syntheses) or 0.75 g for experiments with the additives were used. For additives amounts of 1.16 g sucrose C<sub>12</sub>H<sub>22</sub>O<sub>11</sub> (Aldrich S5016-500G), 0.85 g calcium formate C<sub>2</sub>H<sub>2</sub>CaO<sub>4</sub> (Sigma 21,134) or 0.96 g calcium chloride dihydrate CaCl<sub>2</sub> &#215; 2H<sub>2</sub>O (Merck 2380) were inserted. The sample numbers and the CaO/SiO<sub>2</sub> ratios of the experiments are summarized in <xref ref-type="table" rid="table1">Table 1</xref>. The individual mass ratios were selected to obtain a C/S ratio of 0.8 for the references and the experiments with calcium formate and calcium chloride dihydrate. In contrast, for the insertion of sucrose a lower C/S ratio of 0.5 resulted</p><table-wrap id="table1" ><label><xref ref-type="table" rid="table1">Table 1</xref></label><caption><title> Sample numbers and CaO/SiO<sub>2</sub> ratios (C/S) of the batches</title></caption><table><tbody><thead><tr><th align="center" valign="middle" >Sample<sup>*</sup></th><th align="center" valign="middle" >Additive</th><th align="center" valign="middle" >C/S</th></tr></thead><tr><td align="center" valign="middle" >1a + b</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >0.8</td></tr><tr><td align="center" valign="middle" >2a + b</td><td align="center" valign="middle" >Sucrose</td><td align="center" valign="middle" >0.5</td></tr><tr><td align="center" valign="middle" >3a + b</td><td align="center" valign="middle" >Calcium formate</td><td align="center" valign="middle" >0.8</td></tr><tr><td align="center" valign="middle" >4a + b</td><td align="center" valign="middle" >Calcium chloride dihydrate</td><td align="center" valign="middle" >0.8</td></tr></tbody></table></table-wrap><p><sup>*</sup>a: synthesis with powder, b: synthesis with pellet.</p><p>as it was our aim, to insert a constant amount of 0.75 g of reactive lime CaO in each of the three experiments with additives. For series a) the powdery educts were filled into 50 ml steel autoclaves with Teflon liners and 20 ml distilled water was added. For the syntheses with pellets (series b) in each case only half of the educt masses as inserted for powders were used and first pressed under a hydraulic press with special mold at 5 t for 5’ into 4 mm thick tablets of 12 mm diameter, before placed in a special Teflon sieve inlay inside each autoclave. Again 20 ml water was filled in the liners. The autoclaves were heated in an oven at 220˚C for 40.5 h. After this reaction time the products were filtered, washed with water and dried at 80˚C for 24 h.</p></sec><sec id="s2_2"><title>2.2. Analytical Methods</title><p>The synthesis products were analyzed by XRD, SEM/EDX and FTIR spectroscopy. X-ray powder data were collected on a Bruker Endeavour D4 powder diffractometer (Bragg-Brentano geometry) using Ni-filtered CuK<sub>α </sub>radiation at 40 kV and 40 mA. The measurements were performed with a step width of 0.03˚ in the range of 5˚ - 85˚ 2 Theta. 2668 steps of 1 s duration were measured. The data were analyzed using the WinXPow software of Stoe &amp; Chi.</p><p>Beside these measurements for an overview on the qualitative course of syntheses, selected products of series (a) were analysed quantitatively by Rietveld refinement of X-ray powder data. Therefore a high quality pattern was measured in the range of 2˚ - 80˚ 2θ with 0.01˚ step wide and 10 s of measurement of each step. The Topas 4.2 software (Bruker AXS) was used for data evaluation.</p><p>The morphology and chemical composition of the synthesis products were analyzed on a Jeol JSM-6390A scanning electron microscope (SEM) at an accelerating voltage of 20 kV or 30 kV. The SEM was coupled with a Bruker QUANTAX EDX Spektrometer equipped with the XFlash M410 EDX detector. The samples therefore were sputtered with a fine layer of gold to prevent electric charging during measurement. A signal of gold (Au) therefore exists in each EDX spectrum. Infrared spectra were taken on a Bruker IFS66v FTIR spectrometer. The samples therefore were diluted by KBr (about 1 mg sample in 200 mg KBr), pressed into pellets and measured relatively to the KBr as a reference.</p></sec></sec><sec id="s3"><title>3. Results</title><sec id="s3_1"><title>3.1. XRD and SEM/EDX Analysis</title><sec id="s3_1_1"><title>3.1.1. The Products of Reference Syntheses without Additives</title><p>From the XRD powder patterns of reference syntheses products with quartz powder (<xref ref-type="fig" rid="fig1">Figure 1</xref>(a)) a high amount of xonotlite (PDF 23-125) [<xref ref-type="bibr" rid="scirp.55736-ref29">29</xref>] can be derived according to intense signals at 12.7˚ (2θ), 20.9˚ (2θ) and 29.0˚ (2θ). Also 11 &#197; tobermorite (PDF 45-1480) [<xref ref-type="bibr" rid="scirp.55736-ref29">29</xref>] crystallized in this experiment. The 11 &#197; (d-value) line at diffraction angle 7.8˚ (2θ) appears and also signals at 29.0˚ (2θ) und 32.0˚ (2θ). The XRD analysis also shows quartz (PDF 46-1045) [<xref ref-type="bibr" rid="scirp.55736-ref29">29</xref>] with signals at 20.9˚ (2θ) and 26.6˚ (2θ). The powder pattern of synthesis products obtained from the synthesis with pellets (<xref ref-type="fig" rid="fig1">Figure 1</xref>(b)) shows quartz at strong signals of 20.9˚ (2θ) und 26.6˚ (2θ) beside weak ones of xonotlite and tobermorite.</p><p>A quantitative evaluation by Rietveld method is given in <xref ref-type="table" rid="table2">Table 2</xref> for the experiment with powder.</p><p>Xonotlite as main phase beside a small amount of tobermorite was detected by Rietveld analysis (<xref ref-type="table" rid="table2">Table 2</xref>). Quartz was observed only on very low scale. <xref ref-type="table" rid="table2">Table 2</xref> also includes the amounts of the CSH-phases after subtraction of the quartz fraction.</p><p><xref ref-type="fig" rid="fig2">Figure 2</xref> shows a SEM image of the reference synthesis product with quartz powder. A high amount of</p><fig id="fig1"  position="float"><label><xref ref-type="fig" rid="fig1">Figure 1</xref></label><caption><title> XRD analysis of the synthesis products without additives: (a) Powder sample; (b) Pellet sample</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/11-3700570x5.png"/></fig><fig id="fig2"  position="float"><label><xref ref-type="fig" rid="fig2">Figure 2</xref></label><caption><title> SEM image of the product of the reference synthesis (powder)</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/11-3700570x6.png"/></fig><table-wrap id="table2" ><label><xref ref-type="table" rid="table2">Table 2</xref></label><caption><title> Quantitative phase analysis of the products of reference synthesis (powder)</title></caption><table><tbody><thead><tr><th align="center" valign="middle" >Phase</th><th align="center" valign="middle" >Composition<sup>*</sup></th><th align="center" valign="middle" >Amount (M.-%)</th><th align="center" valign="middle"  colspan="2"  >Amount (without quartz) (M.-%)</th></tr></thead><tr><td align="center" valign="middle" >Xonotlite</td><td align="center" valign="middle" >C<sub>6</sub>S<sub>6</sub>H</td><td align="center" valign="middle" >80.57</td><td align="center" valign="middle" >83.27</td><td align="center" valign="middle" ></td></tr><tr><td align="center" valign="middle" >11 &#197; Tobermorite</td><td align="center" valign="middle" >C<sub>5</sub>S<sub>6</sub>H<sub>5</sub></td><td align="center" valign="middle" >16.19</td><td align="center" valign="middle" >16.73</td><td align="center" valign="middle" ></td></tr><tr><td align="center" valign="middle" >Quartz</td><td align="center" valign="middle" >SiO<sub>2 </sub></td><td align="center" valign="middle" >3.24</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" ></td></tr></tbody></table></table-wrap><p><sup>*</sup>CSH acc. [<xref ref-type="bibr" rid="scirp.55736-ref20">20</xref>] .</p><p>needle-like CSH-phases of 2 - 5 &#181;m length can be seen partly embedded in quartz powder. The EDX analysis of the surface of a needle is given in <xref ref-type="fig" rid="fig3">Figure 3</xref>. A C/S of 0.92 can be estimated from the data.</p><p>The results of SEM investigation of the reference products from synthesis with the pellet are summarized in Figures 4-6. Already the overview image (<xref ref-type="fig" rid="fig4">Figure 4</xref>) shows a high amount of CSH-phases with needle-like morphology. Higher magnification of <xref ref-type="fig" rid="fig5">Figure 5</xref> reveals a more or less connected network of the crystals. Highest</p><fig id="fig3"  position="float"><label><xref ref-type="fig" rid="fig3">Figure 3</xref></label><caption><title> EDX analysis of the product of the reference synthesis (powder)</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/11-3700570x7.png"/></fig><fig id="fig4"  position="float"><label><xref ref-type="fig" rid="fig4">Figure 4</xref></label><caption><title> SEM image of the product of reference synthesis (pellet), low magnification for overview</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/11-3700570x8.png"/></fig><fig id="fig5"  position="float"><label><xref ref-type="fig" rid="fig5">Figure 5</xref></label><caption><title> SEM image of the product of reference synthesis (pellet), crystal network at higher magnification</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/11-3700570x9.png"/></fig><fig id="fig6"  position="float"><label><xref ref-type="fig" rid="fig6">Figure 6</xref></label><caption><title> SEM image of the product of reference synthesis (pellet), fragmented crystals at highest magnification</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/11-3700570x10.png"/></fig><p>magnification (<xref ref-type="fig" rid="fig6">Figure 6</xref>) indicates a fragmented structure of the crystals and crystal sizes around 2 - 3 &#181;m and higher. The EDX analysis (see <xref ref-type="fig" rid="fig7">Figure 7</xref>) gives a C/S value of 0.75.</p></sec><sec id="s3_1_2"><title>3.1.2. The Products of Synthesis with Addition of Sucrose</title><p>The X-ray powder patterns of syntheses products obtained under addition of sucrose are summarized in <xref ref-type="fig" rid="fig8">Figure 8</xref>. A high amount of quartz can be seen in both patterns (synthesis with powder: a; synthesis with pellet: b). Lines of calcite (PDF 10 - 400) and scawtite Ca<sub>7</sub>(Si<sub>6</sub>O<sub>18</sub>)(CO<sub>3</sub>)<sup>.</sup>2H<sub>2</sub>O (C<sub>7</sub>S<sub>6</sub>H<sub>3</sub>C; PDF 31-261) were further analysed (see main reflections between 29.5˚ (2θ) and 30.5˚ (2θ)) but with higher intensities for the synthesis product from powder. Results from quantitative Rietveld refinement of the product from powder are summarized in <xref ref-type="table" rid="table3">Table 3</xref>, which also includes the amounts of scawtite and calcite after subtraction of the strong quartz fraction.</p><p>The results of the SEM investigation of the synthesis products with addition of sucrose show fine grained CSH-phases on very low scale (<xref ref-type="fig" rid="fig9">Figure 9</xref>). EDX analysis of the small CSH particles beside quartz gives a C/S value of 1.06 (<xref ref-type="fig" rid="fig1">Figure 1</xref>0).</p><p>The synthesis with the pellet under addition of sucrose shows very few but somewhat bigger CSH-crystals with needle-like morphology (<xref ref-type="fig" rid="fig1">Figure 1</xref>1), grown in the pore space between quartz particles. The EDX analysis of <xref ref-type="fig" rid="fig1">Figure 1</xref>2 reveals a C/S ratio of 0.8. As tobermorite could not detected by XRD the crystals are maybe tobermorite in a low amount under the XRD detection limit or CSH scawtite closely connected with quartz.</p><p>Also big rhombohedral crystals of calcite were observed within the product (<xref ref-type="fig" rid="fig1">Figure 1</xref>3). EDX analysis discloses a high amount of calcium (<xref ref-type="fig" rid="fig1">Figure 1</xref>4).</p></sec><sec id="s3_1_3"><title>3.1.3. The Products of Synthesis with Addition of Calcium Formate</title><p>The X-ray powder pattern of the product from powder under addition of calcium formate (<xref ref-type="fig" rid="fig1">Figure 1</xref>5(a)) shows quartz and xonotlite as the main phases. Some weak signals of calcite were also detected. Quantitative results according to Rietveld refinement of the pattern of this product from powder are summarized in <xref ref-type="table" rid="table4">Table 4</xref>, which also includes the amounts of xonotlite and calcite after subtraction of the quartz fraction.</p><p>In the XRD pattern of the product from the pellet (<xref ref-type="fig" rid="fig1">Figure 1</xref>5(b)) mainly quartz beside lower amounts of xonotlite and somewhat more calcite were detected.</p><p>SEM investigation of the synthesis product with powder and addition of calcium formate shows crystallisation of CSH-phases with needle-like morphology (<xref ref-type="fig" rid="fig1">Figure 1</xref>6). The crystals have a size of 20 &#181;m up to 50 &#181;m. XRD results and also the morphology exhibits the formation of xonotlite. Beside separated xonotlite crystals also smaller more net-like CSH-phases were observed. If these phases are former tobermorites under advanced degradation or pre-stage xonotlites is unclear up to now. The low C/S ratio of 0.56, obtained from the EDX analysis of a needle-like crystal, given in <xref ref-type="fig" rid="fig1">Figure 1</xref>7, clearly indicate a covering of the crystal surface with silicate.</p><p>SEM analysis of the synthesis product with the pellet and addition of calcium formate shows xonotlite beside</p><fig id="fig7"  position="float"><label><xref ref-type="fig" rid="fig7">Figure 7</xref></label><caption><title> EDX analysis of the products of the reference synthesis (pellet)</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/11-3700570x11.png"/></fig><fig id="fig8"  position="float"><label><xref ref-type="fig" rid="fig8">Figure 8</xref></label><caption><title> XRD analysis of the synthesis products with addition of sucrose: (a) Powder sample; (b) Pellet sample</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/11-3700570x12.png"/></fig><fig id="fig9"  position="float"><label><xref ref-type="fig" rid="fig9">Figure 9</xref></label><caption><title> SEM image of the product of synthesis with addition of sucrose (powder)</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/11-3700570x13.png"/></fig><fig id="fig10"  position="float"><label><xref ref-type="fig" rid="fig1">Figure 1</xref>0</label><caption><title> EDX analysis of the fine grained CSH particles between quartz in the product of synthesis with addition of sucrose</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/11-3700570x14.png"/></fig><fig id="fig11"  position="float"><label><xref ref-type="fig" rid="fig1">Figure 1</xref>1</label><caption><title> SEM image of the products of synthesis with addition of sucrose (pellet)</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/11-3700570x15.png"/></fig><fig id="fig12"  position="float"><label><xref ref-type="fig" rid="fig1">Figure 1</xref>2</label><caption><title> EDX analysis of the products of synthesis with addition of sucrose (pellet)</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/11-3700570x16.png"/></fig><fig id="fig13"  position="float"><label><xref ref-type="fig" rid="fig1">Figure 1</xref>3</label><caption><title> SEM image of the product of synthesis with addition of sucrose (pellet)</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/11-3700570x17.png"/></fig><fig id="fig14"  position="float"><label><xref ref-type="fig" rid="fig1">Figure 1</xref>4</label><caption><title> EDX analysis of the product of synthesis with addition of sucrose (pellet)</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/11-3700570x18.png"/></fig><fig id="fig15"  position="float"><label><xref ref-type="fig" rid="fig1">Figure 1</xref>5</label><caption><title> XRD analysis of the synthesis products with addition of calcium formate: (a) Powder sample; (b) Pellet sample</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/11-3700570x19.png"/></fig><fig id="fig16"  position="float"><label><xref ref-type="fig" rid="fig1">Figure 1</xref>6</label><caption><title> SEM image of the product of synthesis with addition of calcium formate (powder)</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/11-3700570x20.png"/></fig><fig id="fig17"  position="float"><label><xref ref-type="fig" rid="fig1">Figure 1</xref>7</label><caption><title> EDX analysis of the product (CSH needle) of synthesis with addition of calcium formate (powder)</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/11-3700570x21.png"/></fig><table-wrap id="table3" ><label><xref ref-type="table" rid="table3">Table 3</xref></label><caption><title> Quantitative phase analysis of the products from synthesis with sucrose (powder)</title></caption><table><tbody><thead><tr><th align="center" valign="middle" >Phase</th><th align="center" valign="middle" >Formula<sup>*</sup></th><th align="center" valign="middle" >Amount (M.-%)</th><th align="center" valign="middle" >Amount, without quartz (M.-%)</th></tr></thead><tr><td align="center" valign="middle" >Quartz</td><td align="center" valign="middle" >SiO<sub>2</sub></td><td align="center" valign="middle" >50.35</td><td align="center" valign="middle" >-</td></tr><tr><td align="center" valign="middle" >Scawtite</td><td align="center" valign="middle" >C<sub>7</sub>S<sub>6</sub>H<sub>3</sub>C</td><td align="center" valign="middle" >25.20</td><td align="center" valign="middle" >50.76</td></tr><tr><td align="center" valign="middle" >Calcite</td><td align="center" valign="middle" >CaCO<sub>3 </sub></td><td align="center" valign="middle" >24.45</td><td align="center" valign="middle" >49.24</td></tr></tbody></table></table-wrap><p><sup>*</sup>CSH acc. [<xref ref-type="bibr" rid="scirp.55736-ref20">20</xref>] .</p><table-wrap id="table4" ><label><xref ref-type="table" rid="table4">Table 4</xref></label><caption><title> Quantitative phase analysis of the products from synthesis with calcium formate (powder)</title></caption><table><tbody><thead><tr><th align="center" valign="middle" >Phase</th><th align="center" valign="middle" >Formula<sup>*</sup></th><th align="center" valign="middle" >Amount (M.-%)</th><th align="center" valign="middle" >Amount, without quartz (M.-%)</th></tr></thead><tr><td align="center" valign="middle" >Xonotlite</td><td align="center" valign="middle" >C<sub>6</sub>S<sub>6</sub>H<sub>2</sub></td><td align="center" valign="middle" >51.26</td><td align="center" valign="middle" >71.11</td></tr><tr><td align="center" valign="middle" >Quartz</td><td align="center" valign="middle" >SiO<sub>2</sub></td><td align="center" valign="middle" >27.92</td><td align="center" valign="middle" >-</td></tr><tr><td align="center" valign="middle" >Calcite</td><td align="center" valign="middle" >CaCO<sub>3 </sub></td><td align="center" valign="middle" >20.83</td><td align="center" valign="middle" >28.89</td></tr></tbody></table></table-wrap><p><sup>*</sup>CSH acc. [<xref ref-type="bibr" rid="scirp.55736-ref20">20</xref>] .</p><p>small amounts of to bermorite in band-shaped crystals up to 5 &#181;m, which grow into the pore space (see <xref ref-type="fig" rid="fig1">Figure 1</xref>8). The EDX measurement given in <xref ref-type="fig" rid="fig1">Figure 1</xref>9, exhibits a C/S ratio of 1.36 according to intergrowths with calcite in agreement with XRD analysis.</p></sec><sec id="s3_1_4"><title>3.1.4. The Products of Synthesis with Addition of Calcium Chloride Dihydrate</title><p>Formation of mainly xonotlite beside somewhat fewer amount of tobermorite and quartz can be derived from the XRD results of the synthesis with powder, given in <xref ref-type="fig" rid="fig2">Figure 2</xref>0(a). Quantitative results according to Rietveld refinement of the pattern of this product from powder are summarized in <xref ref-type="table" rid="table5">Table 5</xref>, which also includes the amounts of xonotlite and tobermorite after subtraction of the quartz fraction.</p><fig id="fig18"  position="float"><label><xref ref-type="fig" rid="fig1">Figure 1</xref>8</label><caption><title> SEM image of the product of synthesis with addition of calcium formate (pellet)</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/11-3700570x22.png"/></fig><fig id="fig19"  position="float"><label><xref ref-type="fig" rid="fig1">Figure 1</xref>9</label><caption><title> EDX analysis of CSH needles of synthesis with addition of calcium formate (pellet)</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/11-3700570x23.png"/></fig><table-wrap id="table5" ><label><xref ref-type="table" rid="table5">Table 5</xref></label><caption><title> Quantitative phase analysis of the products from synthesis with calcium chloride dihydrate (powder)</title></caption><table><tbody><thead><tr><th align="center" valign="middle" >Phase</th><th align="center" valign="middle" >Formula<sup>*</sup></th><th align="center" valign="middle" >Amount (M.-%)</th><th align="center" valign="middle" >Amount, without quartz (M.-%)</th></tr></thead><tr><td align="center" valign="middle" >Xonotlite</td><td align="center" valign="middle" >C<sub>6</sub>S<sub>6</sub>H<sub>2</sub></td><td align="center" valign="middle" >56.58</td><td align="center" valign="middle" >65.57</td></tr><tr><td align="center" valign="middle" >11 &#197; Tobermorite</td><td align="center" valign="middle" >C<sub>5</sub>Si<sub>6</sub>H<sub>5</sub></td><td align="center" valign="middle" >29.71</td><td align="center" valign="middle" >34.43</td></tr><tr><td align="center" valign="middle" >Quartz</td><td align="center" valign="middle" >SiO<sub>2 </sub></td><td align="center" valign="middle" >13.70</td><td align="center" valign="middle" >-</td></tr></tbody></table></table-wrap><p><sup>*</sup>CSH acc. [<xref ref-type="bibr" rid="scirp.55736-ref20">20</xref>] .</p><fig id="fig20"  position="float"><label><xref ref-type="fig" rid="fig2">Figure 2</xref>0</label><caption><title> XRD analysis of the synthesis products with addition of calcium chloride dehydrate: (a) Powder sample; (b) Pellet sample</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/11-3700570x24.png"/></fig><p>In contrast qualitative estimation of the XRD pattern of the product from pellet synthesis crystallization of somewhat more tobermorite can be found compared with xonotlite, beside the usual parts of quartz.</p><p><xref ref-type="fig" rid="fig2">Figure 2</xref>1 shows a typical SEM image of the synthesis product, obtained from powder under addition of calcium chloride dihydrate. In accordance with XRD, high amounts of CSH-phases were observed. The CSH crystals show a needle-like morphology of 3 - 4 &#181;m in size.</p><p>The EDX analysis, given in <xref ref-type="fig" rid="fig2">Figure 2</xref>2 indicates a C/S ratio of 1.0, as to be expected for xonotlite. Also an amount of 2.55 M. % chlorine was detected, resulting from the additive calcium chloride dihydrate.</p><p>SEM investigation of the product of synthesis with the pellet under addition of calcium chloride dihydrate, shown in <xref ref-type="fig" rid="fig2">Figure 2</xref>3, reveals CSH-phases similar to the synthesis with powder. The crystals have a needle-like morphology with a size of about 10 &#181;m (<xref ref-type="fig" rid="fig2">Figure 2</xref>3). EDX analysis, given in <xref ref-type="fig" rid="fig2">Figure 2</xref>4, indicates a C/S ratio of 0.91 for this material.</p><p>A further SEM image at somewhat higher magnification is shown in <xref ref-type="fig" rid="fig2">Figure 2</xref>5. Large crystals, which mainly grew inside the pore space with a card-shaped morphology can be seen. The EDX analysis of these crystals reveals a C/S ratio of 0.83 characteristic for tobermorite (see <xref ref-type="fig" rid="fig2">Figure 2</xref>6).</p></sec></sec><sec id="s3_2"><title>3.2. FTIR Spectroscopy</title><p><xref ref-type="fig" rid="fig2">Figure 2</xref>7 summarizes the FTIR-spectra of the products of all experiments. The spectra of the syntheses with powder (a) always exhibited a higher degree of absorption as well as more distinct signals compared to the spectra of the products synthesized with pellets (b). The spectrum of synthesis with powder and without additives (<xref ref-type="fig" rid="fig2">Figure 2</xref>7, sample 1a) reveals two strong absorption bands in the range of the deformation vibrations of SiO<sub>4</sub>-tetrahedra (400 - 540 cm<sup>−1</sup>) and three signals with shoulders due to Si-O stretching vibrations (900 - 1200 cm<sup>−1</sup>) [<xref ref-type="bibr" rid="scirp.55736-ref30">30</xref>] . Also Si-O-Si bending vibrations induce a signal at 671 cm<sup>−1</sup>.</p><p>Those absorption bands occur quite similar in all the spectra of this study and indicate silicate chain structures [<xref ref-type="bibr" rid="scirp.55736-ref30">30</xref>] . All samples show <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/11-3700570x25.png" xlink:type="simple"/></inline-formula> vibrations of carbonate in the range of 1400 - 1500 cm<sup>−1</sup> and at 876 cm<sup>−1</sup> as a shoulder [<xref ref-type="bibr" rid="scirp.55736-ref31">31</xref>] . For the pellets of the reference (1b) and the products of the syntheses with addition of calcium formate (3b) the signals of carbonates have a higher intensity compared to the powder samples (1a and 3a). The</p><fig id="fig21"  position="float"><label><xref ref-type="fig" rid="fig2">Figure 2</xref>1</label><caption><title> SEM image of the product of synthesis with addition of calcium chloride dihydrate (powder)</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/11-3700570x26.png"/></fig><fig id="fig22"  position="float"><label><xref ref-type="fig" rid="fig2">Figure 2</xref>2</label><caption><title> EDX Analysis of the product of synthesis with addition of calcium chloride dihydrate (powder)</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/11-3700570x27.png"/></fig><fig id="fig23"  position="float"><label><xref ref-type="fig" rid="fig2">Figure 2</xref>3</label><caption><title> SEM image of the product of synthesis with addition of calcium chloride dihydrate (pellet)</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/11-3700570x28.png"/></fig><fig id="fig24"  position="float"><label><xref ref-type="fig" rid="fig2">Figure 2</xref>4</label><caption><title> EDX analysis of the crystals according to <xref ref-type="fig" rid="fig2">Figure 2</xref>3 of synthesis with addition of calcium chloride dihydrate (pellet)</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/11-3700570x29.png"/></fig><fig id="fig25"  position="float"><label><xref ref-type="fig" rid="fig2">Figure 2</xref>5</label><caption><title> SEM image of the product of synthesis with addition of calcium chloride dihydrate (pellet). Crystals within the pore</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/11-3700570x30.png"/></fig><fig id="fig26"  position="float"><label><xref ref-type="fig" rid="fig2">Figure 2</xref>6</label><caption><title> EDX analysis of the crystals according to <xref ref-type="fig" rid="fig2">Figure 2</xref>5 of pro- duct of synthesis with addition of calcium chloride dihydrate (pellet)</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/11-3700570x31.png"/></fig><fig id="fig27"  position="float"><label><xref ref-type="fig" rid="fig2">Figure 2</xref>7</label><caption><title> FTIR-spectra of the products of synthesis with powder (a) and pellet (b) and without additives (1), with addition of sucrose (2), calcium formate (3) and calcium chloride dihydrate (4)</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/11-3700570x32.png"/></fig><p>absorption bands of water occur at about 1634 cm<sup>−1</sup> and between 2800 - 3700 cm<sup>−1</sup> [<xref ref-type="bibr" rid="scirp.55736-ref31">31</xref>] . They are present in all the spectra but the spectrum of the products of synthesis with addition of calcium chloride dihydrate (4a) has a much higher intensity. Signals around 3600 cm<sup>−1</sup> are due to vibrations of hydroxyl groups [<xref ref-type="bibr" rid="scirp.55736-ref31">31</xref>] . Possible types of vibrations are Si-OH, Ca-OH and OH<sup>−</sup> [<xref ref-type="bibr" rid="scirp.55736-ref31">31</xref>] . The OH-absorption band in the spectra of sample 1a, 3a, 3b and 4a is distinct and has a high intensity. The spectra of the syntheses with sucrose do not show OH-vibrations. Also the Si-O stretching and the SiO<sub>4</sub> bending vibrations of the spectra 2a and 2b indicate broad, overlapping signals in contrast to distinct absorption bands of the other samples. The spectra of the products of syntheses with addition of calcium formate (3a and 3b) and calcium chloride dihydrate (4a and 4b) have a strong correlation to the spectra of the reference (1a and 1b). But the absorption bands of the reference are more distinctive and have a higher intensity.</p></sec></sec><sec id="s4"><title>4. Discussion and Conclusion</title><p>For the general evaluation of the influence of the different additives studied in the present work, the qualitative estimation of phase formation for all experiments is summarized in <xref ref-type="table" rid="table6">Table 6</xref>. From this overview, based on XRD, it can be derived, that the insertions of additives have a remarkable effect on the progress of CSH-phase formation during the hydrothermal process.</p><p>The following aspects have to be discussed for a comparative characterization individual behavior of an additive on the reaction process:</p><p>(i) the degree of conversion during the whole reaction;</p><p>(ii) the overall amounts of CSH phase formation, independent of an individual phase;</p><p>(iii) the ratio of xonotlite/other CSH (tobermorite, scawtite); and last not least</p><p>(iv) the crystal quality according to morphology and size of the crystals.</p><p>The amount of remaining quartz after each reaction is representative for the degree of conversion (i). The quantitative values from Rietveld refinements for products under use of powdery educts show the following ranking order (starting with the best result):</p><p>reference → calcium chloride dehydrate → calcium formate → succrose</p><p>The same ranking can be estimated qualitatively from XRD (<xref ref-type="table" rid="table6">Table 6</xref>) for synthesis with pellets.</p><table-wrap id="table6" ><label><xref ref-type="table" rid="table6">Table 6</xref></label><caption><title> Results of the X-ray diffraction</title></caption><table><tbody><thead><tr><th align="center" valign="middle" >Additive</th><th align="center" valign="middle" ><sup>* </sup></th><th align="center" valign="middle" >(C + A)/S</th><th align="center" valign="middle" >A/C</th><th align="center" valign="middle" >Tob</th><th align="center" valign="middle" >Xo</th><th align="center" valign="middle" >Sc</th><th align="center" valign="middle" >Qz</th><th align="center" valign="middle" >Cal</th></tr></thead><tr><td align="center" valign="middle"  rowspan="2"  >Reference</td><td align="center" valign="middle" >1a</td><td align="center" valign="middle" >0.83</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >○</td><td align="center" valign="middle" >●</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >(∙)</td><td align="center" valign="middle" ></td></tr><tr><td align="center" valign="middle" >1b</td><td align="center" valign="middle" >0.83</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >○</td><td align="center" valign="middle" >○</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >●</td><td align="center" valign="middle" ></td></tr><tr><td align="center" valign="middle"  rowspan="2"  >Sucrose</td><td align="center" valign="middle" >2a</td><td align="center" valign="middle" >0.54</td><td align="center" valign="middle" >0.24</td><td align="center" valign="middle" ></td><td align="center" valign="middle" ></td><td align="center" valign="middle" >○</td><td align="center" valign="middle" >●</td><td align="center" valign="middle" >○</td></tr><tr><td align="center" valign="middle" >2b</td><td align="center" valign="middle" >0.54</td><td align="center" valign="middle" >0.24</td><td align="center" valign="middle" >○</td><td align="center" valign="middle" >○</td><td align="center" valign="middle" >○</td><td align="center" valign="middle" >●</td><td align="center" valign="middle" ></td></tr><tr><td align="center" valign="middle"  rowspan="2"  >Calcium formate</td><td align="center" valign="middle" >3a</td><td align="center" valign="middle" >0.80</td><td align="center" valign="middle" >0.49</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >●</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >○</td><td align="center" valign="middle" >○</td></tr><tr><td align="center" valign="middle" >3b</td><td align="center" valign="middle" >0.80</td><td align="center" valign="middle" >0.49</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >○</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >●</td><td align="center" valign="middle" >○</td></tr><tr><td align="center" valign="middle"  rowspan="2"  >Calcium chloride dihydrate</td><td align="center" valign="middle" >4a</td><td align="center" valign="middle" >0.80</td><td align="center" valign="middle" >0.49</td><td align="center" valign="middle" >○</td><td align="center" valign="middle" >●</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >(∙)</td><td align="center" valign="middle" ></td></tr><tr><td align="center" valign="middle" >4b</td><td align="center" valign="middle" >0.80</td><td align="center" valign="middle" >0.49</td><td align="center" valign="middle" >○</td><td align="center" valign="middle" >○</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >●</td><td align="center" valign="middle" ></td></tr></tbody></table></table-wrap><p><sup>*</sup>a = powdered, b = pressed educts; ● = high, ○ = low amount; (∙) very low amount, Tob = 11-&#197; tobermorite, Xo = xonotlite, Sc = scawtite, Qz = quartz, Cal = calcite.</p><p>Again an equal sequence is found for the overall amounts of CSH phase formation, independent of an individual phase (ii) and for the ratio of xonotlite: tobermorite or scawtite (iii), again for synthesis with powder as well as with pellet.</p><p>It has to be mentioned here, that the comparison of reactions with powders or pellets shows general lower reaction rates for pellets and hence more quartz and fewer CSH within these products. Here the reduced reaction space compared with crystallization within the liquid phase under use of powders and 20 ml water is responsible for the lower conversion into CSH-phases. However, a reduced reaction area introduces a formation of CSH in card-shaped structure resulting in a high stability of the building material, like, e.g. limesand stone [<xref ref-type="bibr" rid="scirp.55736-ref20">20</xref>] .</p><p>According to (iv) the ranking is somewhat deviating. As the morphology is relative similar as both synthesis products from powders with calcium chloride dehydrate and calcium formate appear as needles, the crystal size differs. Were needles of 5 - 10 &#181;m in size were found for powder syntheses with formate, much longer ones (10- 20 &#181;m) were observed with calcium chloride dehydrate. Using pellets again more band or card shaped crystals of uniform size between 5 - 10 &#181;m occurred.</p><p>In contrast syntheses with sucrose yield to the CSH-phase scawtite C<sub>7</sub>S<sub>6</sub>H<sub>3</sub>C instead of tobermorite and xonotlite. From the literature it is known that at low temperatures sucrose and calcium ions form a Ca-saccharate complex, whereby further reactions with SiO<sub>2</sub> and H<sub>2</sub>O to CSH-phases could be prevented [<xref ref-type="bibr" rid="scirp.55736-ref32">32</xref>] . At higher temperatures (160˚C - 180˚C) sucrose dissociates. The solubility of quartz depends on alkaline conditions, ruled by the availability of Ca(OH)<sub>2</sub>. Therefore at the beginning of the reaction calcium is consumed by sucrose and the solubility of quartz is lower and a less amount of SiO<sub>2</sub> is available for the formation of CSH-phases. At elevated temperatures dissolution products of the Ca-saccharate complex like calcium ions and carbonate groups seem to favour the formation of scawtite.</p><p>The results with calcium formate are surprising. Former experiments on tobermorite synthesis at 200˚C already showed the retarding effect of this additive on the formation of C<sub>5</sub>S<sub>6</sub>H<sub>5</sub> [<xref ref-type="bibr" rid="scirp.55736-ref26">26</xref>] . The results of the present study of synthesis at 220˚C confirm this observation for tobermorite but show in contrast a surprisingly high amount of xonotlite and calcite. Remaining parts of portlandite and quartz, as during 200˚C syntheses in [<xref ref-type="bibr" rid="scirp.55736-ref26">26</xref>] , were not found in the present study. Future experiments must clarify the role of higher temperature and the question if the formation of xonotlite is more insensitive against the Ca-formate effect.</p><p>From all three additives calcium chloride dihydrate yield to highest amounts of CSH in close resemblance to the results of the reference syntheses but with higher portions of tobermorite than xonotlite. Further experiments must clarify if this behavior is ruled by pH-value [<xref ref-type="bibr" rid="scirp.55736-ref14">14</xref>] - [<xref ref-type="bibr" rid="scirp.55736-ref16">16</xref>] hand in hand with the ionic potential of the additional Ca and Cl ions in the reaction system [<xref ref-type="bibr" rid="scirp.55736-ref10">10</xref>] -[<xref ref-type="bibr" rid="scirp.55736-ref12">12</xref>] .</p></sec></body><back><ref-list><title>References</title><ref id="scirp.55736-ref1"><label>1</label><mixed-citation publication-type="other" xlink:type="simple">Taylor, H.F.W. (1990) Cement Chemistry. 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