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Reservoir-scale faults in a priori low-deformed reservoirs targeted for CO2 storage can present high complex architecture, which might influence the hydro-mechanical behaviour of the fault system; 2. Chemical interactions (dissolution and precipitation processes, chemically-induced weakening, etc).
The results of plotted chemical data on Durov's diagram is used to identify the geochemical evolution of groundwater where the groundwater is initially recharged by Ca HCO3 water (rain water) and undergo water rock interactions (dissolution) and mixing with pre-existing groundwater in karstified dolomitic limestone that may be of saline nature.
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Hydrogen bonding interactions and dissolution behavior of salt in supramolecular electrolytes are investigated.
This is a cluster based on rock water interaction, mineral dissolution and anthropogenic pollution source.
Some examples are rock water interaction, mineral dissolution, agriculture and industrial effluents, mixing water, cation exchange and saltwater intrusion (Appelo and Postma 2005; Reddy et al. 2010; Thilagavathi 2012).
These interactions involve mainly dissolution and precipitation processes, which are controlled by the solubility products of different mineral phases involved.
Cations in the Marcellus Shale waters can participate in multiple water rock interactions, including mineral dissolution and precipitation, ion exchange, and surface complexation when clay minerals are abundant.
The control of mineralogy and water chemistry in oil recovery highlight the importance of considering simultaneous water rock interactions, including mineral dissolution, desorption, and ion exchange during the low-salinity waterflooding of sandstone rocks.
High conc. of Na+ from most local water samples could be due to long rock water interactions, high ET, dissolution of halite minerals and weathering of plagioclase feldspar (Pazand et al. 2012).
To realistically simulate dissolved xylene migration at this site, a three-dimensional numerical flow and transport model incorporating biochemical multispecies interactions and xylene dissolution from the NAPL has been developed.
The principal water type depicts rock water interaction involving the dissolution of carbonates by weathered zone above the underlying rocks.
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