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Atomistic Simulation studies of the Cement Paste Components

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<strong>Atomistic</strong> <strong>Simulation</strong> <strong>studies</strong> <strong>of</strong> <strong>the</strong> <strong>Cement</strong> <strong>Paste</strong> <strong>Components</strong><br />

⎡<br />

4 ⋅⎢<br />

⎣<br />

⎤<br />

Ca2 nH wSi(3n−1) O(9n− 2)<br />

OH Ca ⋅<br />

w+ n( y−2)<br />

n y<br />

m H<br />

2O⎥<br />

2 ⎦<br />

{ }( )<br />

{ }<br />

n= 1; w= 0; y = 2; m= 0 →4⋅⎡⎣<br />

Ca2Si2O7 ⋅Ca1⎤⎦<br />

(3.3.3)<br />

The relaxed structure after <strong>the</strong> optimization (figure 3.2.3) has a very poor symmetry,<br />

in comparison with <strong>the</strong> low C/S ratio case. Consequently, <strong>the</strong> total dipolar moment <strong>of</strong><br />

<strong>the</strong> particle is very high, 13.72 D. It can be suggested that <strong>the</strong> energy gain <strong>of</strong> <strong>the</strong><br />

multiple bond formation primes over <strong>the</strong> dipole cancellation in <strong>the</strong> present case. Each<br />

precursor can be still distinguished, although <strong>the</strong>ir structure is distorted. The added<br />

calcium atoms are coordinated not only to <strong>the</strong> terminal oxygen atoms <strong>of</strong> <strong>the</strong> silicate<br />

chains, but also to those <strong>of</strong> <strong>the</strong> Ca-O layer <strong>of</strong> each precursor. Thus, <strong>the</strong> silicate dimers<br />

are now linked to two different Ca-O layers, within <strong>the</strong> precursors and between <strong>the</strong>m.<br />

The mean charge <strong>of</strong> <strong>the</strong> calcium ion <strong>of</strong> <strong>the</strong> layer formed between <strong>the</strong> units is slightly<br />

smaller than <strong>the</strong> one within <strong>the</strong> precursor, just about 0.1 e - lower. This small decrease<br />

indicates that <strong>the</strong> iono-covalent nature <strong>of</strong> both layers is similar.<br />

3.5. Discussion <strong>of</strong> <strong>the</strong> assembly mechanism<br />

The formed structures after <strong>the</strong> assembly <strong>of</strong> precursors can be related to <strong>the</strong> crystalline<br />

species tobermorite 14 Å and jennite. A schematic representation is presented in figure<br />

3.2.4. When <strong>the</strong> dipole-dipole interaction is <strong>the</strong> responsible <strong>of</strong> <strong>the</strong> system organization, a<br />

tobermorite-like structure is formed. The configuration can be identified as a precursor<br />

assembly in <strong>the</strong> perpendicular direction <strong>of</strong> <strong>the</strong> silicate chains, with <strong>the</strong> Ca +2 ion acting as<br />

a linker between layers. However, when <strong>the</strong> formation <strong>of</strong> multiple Ca-O bonds primes,<br />

<strong>the</strong> silicate chains rearrange <strong>the</strong>mselves and are coordinated to two Ca-O layers. This<br />

would be equivalent to a jennite-like structure, growing in <strong>the</strong> laminar plane and<br />

perpendicular to <strong>the</strong> silicate chain direction. Thus, starting from a single precursor,<br />

tobermorite or jennite-like structures can be reached, depending on <strong>the</strong> mechanism,<br />

which in its turn depends on <strong>the</strong> calcium to silicon ratio. The growth mechanisms are<br />

consistent, <strong>the</strong>refore, with <strong>the</strong> calcium content <strong>of</strong> <strong>the</strong> crystalline species.<br />

82

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