The Role of Al in C-S-H: NMR, XRD, and Compositional Results for Precipitated Samples

X-ray diffraction, compositional analysis, and 29Si and 27Al MAS NMR spectroscopy of Al-substituted tobermorite-type C�S�H made by precipitation from solution provide significant new insight into the structural mechanisms of Al-substitution in this important and complicated phase. Al occurs in 4-, 5-, and 6-coordination (Al[4], Al[5], and Al[6]) and plays multiple structural roles. Al[4] occurs on the bridging tetrahedra of the drierkette Al�silicate chains, and Al[5] and Al[6] occur in the interlayer and perhaps on particle surfaces. Al does not enter either the central Ca�O sheet or the pairing tetrahedra of the tobermorite-type layers. Al[4] occurs on three types of bridging sites, Q3 sites that bridge across the interlayer; Q2 sites that are charge balanced by interlayer Ca+2, Na+, or H+; and Q2 sites that are most likely charge balanced by interlayer or surface Al[5] and Al[6] through Al[4]�O�Al[5,6] linkages. Although the data presented here are for relatively well-crystallized tobermorite-type C�S�H with C/S ratios less than or equal to 1.2, comparable spectral features for hydrated white cement pastes indicate the presence of similar structural environments in the C�S�H of such pastes, and by implication OPC pastes.

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  • Supplemental Notes:
    • Abstract reprinted with permission from Elsevier.
  • Authors:
    • Sun, G K
    • Young, J Francis
    • Kirkpatrick, R James
  • Publication Date: 2006-1

Language

  • English

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  • Accession Number: 01019350
  • Record Type: Publication
  • Files: TRIS
  • Created Date: Mar 1 2006 9:04AM