The elevated Na+ concentrations coupled to low Ca2+ suggesting that Ca2+ and Na+ ion exchange process is an important geochemical process for the Na Cl type of groundwater.
Elevated Na+ concentrations coupled with low Ca2+ suggest that Ca2+ and Na+ ion exchange process is an important geochemical process for the Na Cl type of groundwater.
and contributed to the neoformation and dissolution of minerals over the long term, as well as to the generation of gaseous byproducts (e.g., H2S, CH4, CO2) that could be important for geochemical processes on the surface and ultimately for distant communities and global biogeochemical recycling.
Adsorption of uranium to bacterial surfaces is an important aqueous geochemical process (see [108]).
The solid solution aqueous solution (SSAS) interaction plays an important role in the geochemical processes in water, rock and soil.
These microbially linked geochemical processes have important ramifications for bulk system geochemistry that were previously unknown.
Geochemical processes are important as they decide on the composition of groundwater and are the cause for spatial and temporal variation in groundwater quality.
All together our results demonstrate that SBSE-TD-GC-MS analyses of hydrothermal fluids will make important contributions to the understanding of geochemical processes, geomicrobiological interactions and formation of mineral deposits.
Simulation of geochemical processes in bentonite is therefore important for long-term safety assessment of those repositories.
