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Geoelectrical characterization of carbonate and silicate porous media in the presence of supercritical CO2-water flow

机译：超临界CO2-水流作用下碳酸盐和硅酸盐多孔介质的地电特征

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This article has been accepted for publication in Geophysical Journal International ©: 2015 The authors. Published by Oxford University Press on behalf of the Royal Astronomical Society. All rights reserved.

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Abidoye Luqman K.; Das Diganta Bhusan;
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1. pH, geoelectrical and membrane flux parameters for the monitoring of water-saturated silicate and carbonate porous media contaminated by CO2 [J] . Abidoye Luqman K., Das Diganta B. Chemical engineering journal . 2015 ,第Null期

机译：pH，地电和膜通量参数，用于监测被CO2污染的水饱和硅酸盐和碳酸盐多孔介质
2. Quantifying the flow dynamics of supercritical CO2-water displacement in a 2D porous micromodel using fluorescent microscopy and microscopic PIV [J] . Kazemifar Farzan, Blois Gianluca, Kyritsis Dimitrios C., Advances in Water Resources . 2016 ,第sepa期

机译：使用荧光显微镜和显微镜PIV量化二维多孔微模型中超临界CO2-水驱替的流动动力学
3. Porous Biomaterials Obtained Using Supercritical CO2-Water Emulsions [J] . Cleofe Palocci, Andrea Barbetta, Angelo La Grotta Langmuir: The ACS Journal of Surfaces and Colloids . 2007 ,第15期

机译：使用超临界CO2-水乳液获得的多孔生物材料
4. The Research of Waterflow in Porous Carbonate Rocks of the Nowa Wioska Dolomite Mine Using Geoelectrical Methods [C] . Justyna GIBAS Polish-Czech-Slovakian symposium on mining geophysics . 2002

机译：用电气方法研究日式纤维岩矿井多孔碳酸岩岩石水流研究
5. Supercritical fluids, oscillatory flow, and partially saturated porous media by magnetic resonance microscopy. [D] . Rassi, Erik Michael. 2011

机译：超临界流体，振荡流和部分饱和的多孔介质（通过磁共振显微镜检查）。
6. Efficiency and Compatibility of Selected Alkoxysilanes on Porous Carbonate and Silicate Stones [O] . Matea Ban, Elisabeth Mascha, Johannes Weber, 2019

机译：所选烷氧基硅烷在多孔碳酸盐和硅酸盐石上的效率和相容性
7. pH, geoelectrical and membrane flux parameters for the monitoring of water-saturated silicate and carbonate porous media contaminated by CO2 [O] . Abidoye Luqman K., Das Diganta Bhusan 2015

机译：pH，地电和膜通量参数，用于监测被CO2污染的水饱和硅酸盐和碳酸盐多孔介质

Geoelectrical characterization of carbonate and silicate porous media in the presence of supercritical CO2-water flow

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