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Volumn 28, Issue 2, 2001, Pages 130-141

Modeling of diotahedral 2:1 phyllosilicates by means of transferable empirical potentials

Author keywords

Catio substitution effect; Crystal structure; Diotahedral 2:1 phyllosilicates; Mica; Pyrophyllite; Smectite illite; Theoretical study

Indexed keywords

CATION EXCHANGE CAPACITY; CRYSTAL STRUCTURE; PHYLLOSILICATE; PYROPHYLLITE; SMECTITE; THEORETICAL STUDY;

EID: 0034915435     PISSN: 03421791     EISSN: None     Source Type: Journal    
DOI: 10.1007/s002690000139     Document Type: Article
Times cited : (79)

References (37)
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    • (1989) Am Mineral , vol.74 , pp. 774-779
    • Dove, M.T.1
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    • 3+ co-ordination sites in iron oxides. Application to spectra, bonding and magnetism
    • (1985) Phys Chem Miner , vol.12 , pp. 161-175
    • Sherman, D.M.1
  • 35
    • 0021335069 scopus 로고
    • The distribution of octahedral cations in the 2:1 layers of dioctahedral smectites studied by oblique-texture electron diffraction
    • (1984) Clay Miner , vol.19 , pp. 177-193
    • Tsipursky, S.I.1    Drits, V.A.2


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.