Change of black shale organic material surface area during oxidative weathering: Implications for rock-water surface evolution

作者: Cornelius Fischer , Reinhard Gaupp

DOI: 10.1016/J.GCA.2004.09.021

关键词:

摘要: Black shale oxidative weathering plays a significant role in a variety of processes including acid mine drainage and atmospheric CO2 control. The modeling of weathering is highly …

参考文章(46)
Gerd Seidel, Geologie von Thüringen Schweizerbart'sche Verlagsbuchhandlung. ,(2003)
C. M. Schmidt, K. Heide, Thermal Analysis of Hydrocarbons in Paleozoic Black Shales Journal of Thermal Analysis and Calorimetry. ,vol. 64, pp. 1297- 1302 ,(2001) , 10.1023/A:1011530020564
The Iron Oxides Wiley‐VCH Verlag GmbH. pp. 5- 18 ,(2003) , 10.1002/9783527613229.CH01
Michael F. Hochella, Art F. White, Mineral-Water Interface Geochemistry ,(2018)
Carlos M. Pina, Udo Becker, Peter Risthaus, Dirk Bosbach, Andrew Putnis, Molecular-scale mechanisms of crystal growth in barite Nature. ,vol. 395, pp. 483- 486 ,(1998) , 10.1038/26718
A Lttge, U Winkler, A.C Lasaga, Interferometric study of the dolomite dissolution: a new conceptual model for mineral dissolution Geochimica et Cosmochimica Acta. ,vol. 67, pp. 1099- 1116 ,(2003) , 10.1016/S0016-7037(02)00914-6