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Singurindy & Berkowitz 2004

Singurindy, O. and Berkowitz, B. (2004). Dedolomitization and flow in fractures. Geophysical Research Letters 31: doi: 10.1029/2004GL021594. issn: 0094-8276.

An experimental study was carried out to examine the evolution of flow patterns in both time and space under different flow regimes, caused by incongruent dissolution of fractured dolomite. Analysis of oscillatory behavior of the overall hydraulic conductivity was based on the fluid residence time, which influences strongly aragonite and calcite precipitation in fractured dolomite rocks. The results are in accordance with field observations.

BACKGROUND DATA FILES

	Abstract

Keywords
Geochemistry, Chemical evolution, Global Change, Biogeochemical processes, Hydrology, Groundwater quality, Hydrology, Groundwater transport, Hydrology, Groundwater hydrology

Journal
Geophysical Research Letters
http://www.agu.org/journals/gl/

Publisher
American Geophysical Union
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