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Volumn 65, Issue 7, 2001, Pages 1059-1070

Are quartz dissolution rates proportional to B.E.T. surface areas?

Author keywords

[No Author keywords available]

Indexed keywords

DISSOLUTION; QUARTZ; SURFACE AREA; WEATHERING;

EID: 0035012922     PISSN: 00167037     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0016-7037(00)00570-6     Document Type: Article
Times cited : (222)

References (63)
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    • Calculation of the thermodynamic and transport properties of aqueous species at high pressures and temperatures: Aqueous tracer diffusion coefficients of ions to 1000°C and 5 kb
    • (1988) Geochim. Cosmochim. Acta , vol.52 , pp. 63-85
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  • 61
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    • Calculations of the thermodynamic properties of aqueous silica and the solubility of quartz an its polymorphs at high pressures and temperatures
    • (1977) Am. Jour. Sci , vol.277 , pp. 1315-1351
    • Walther, J.V.1    Helgeson, H.C.2
  • 62
    • 0001503674 scopus 로고
    • Chemical weathering of silicates in nature: A microscopic perspective with theoretical considerations
    • (eds. A.F. White and S.L. Brantley), Washington, D.C
    • (1995) Rev. Mineral. Mineral Soc. Am , vol.31 , pp. 407-461
    • White, A.F.1
  • 63
    • 84934727565 scopus 로고
    • Chemical weathering of some primary rock-forming minerals
    • (1975) Soil Sci , vol.119 , pp. 349-355
    • Wilson, M.J.1


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.