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Hydrochemical data, δ34S values of dissolved SO42− and 87Sr/86Sr ratios have been analyzed to identify the predominant geochemical processes that control the arsenic mobilization within the aquifers.
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The large variations in EC are attributed mainly to geochemical processes prevailing in this region.
The large variation in EC is mainly attributed to geochemical processes prevailing in this region.
The large variations in EC are mainly attributed to anthropogenic activities and to geochemical processes prevailing in this region.
Future studies of the effect of aquifer heterogeneity on geochemical processes and isotopic fractionation may benefit from careful processes-oriented isotopic work prior to analytical or numerical modeling.
Many diagenetic processes such as cementation, recrystallization, and dolomitization are essentially geochemical processes; others like compaction are fundamentally physical processes.
Authigenic minerals, like calcite, halite, and gypsum, form in situ within the depositional site in response to geochemical processes.
This setting generates deep geochemical processes, inducing intense chemical weathering.
The separation of crust from mantle has involved rather different geochemical processes than those of the segregation of the core.
Life has played a key role in shaping global geochemical processes over billions of years.
The interplay between molecular, physiological, ecological, evolutionary, and geochemical processes that constitute, cause, and maintain microbial diversity.
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