The groundwater head in the brine-saline water area will also decrease about 1.8 m by the end of forecasting period, caused by excessive brine mining.
In this paper, we are aiming to comprehensively study the effects of formation brine salinity and reservoir temperature on convection mechanism and on CO2 storage in saline aquifers.
Popularly, brine or saline aquifers, oceans, depleted oil reservoirs, and coal beds are considered potential geological formations for CO2 storage.
The geologic sequestration of CO2 in pressure-constrained formations may generate large volumes of extracted brine, or saline water formations with total dissolved salts up to 85,000 ppm.
The model profile is perpendicular to the coastal line with two interfaces, freshwater-saline water interface near the shore and inland brine water-saline water-seawater interface.
Rhodizite is a rare mineral found in low concentrations in lepidolite and in salt brines and saline deposits.
The proximity of coastal aquifer to the sea, the presence of brines and saline soils in the region, the agriculture activities and the hydraulic properties of the aquifer are also important factors which can become the sources of salinity of this aquifer.
Any remaining water on the surface may have formed saline brine pockets within the permafrost.
It is suggested that the stability of bassanite is attributed to the elevated ambient temperatures in the presence of highly saline brine and organic acids.
With highly saline brine feed water (NaCl, 70,000 mg/L of TDS) and utilizing two different cation exchange membranes, we measured electrical responses of unit fluidic cell, and monitored the product water salinity changes over a wide ranges of flow velocities and electric current densities.
