Sentence examples for main geochemical processes from inspiring English sources

The other main geochemical processes differentiating the pedons were chemical weathering of carbonates and accumulation of residual elements.

Results corroborated that the mixing of surface waters, as well as calcite dissolution and CO2 dissolution/exsolution, are the main geochemical processes constraining Fuensanta spring hydrochemistry.

The dissolution of halite and gypsum has proved to be the main geochemical processes, which are favored by the great ionic strength of groundwater.

Hydrogeochemical modelling of porewaters indicate that the main geochemical processes controlling the chemistry of the bentonite are acid-base reactions, aqueous complexation, cation exchange, dissolution/ex-solution of CO2, and dissolution and precipitation of highly soluble minerals such as calcite, dolomite, chalcedony, and gypsum/anhydrite.

Samples from both seasons mostly fall in Field 2 depicting reverse ion exchange as the main geochemical process modifying the water type of groundwater.

Multivariate statistics reveal the main geochemical process controlling the groundwater chemistry as silicate weathering due to high Na+ and HCO3-; contributions from humic acid indicated by low pH and poor waste management indicated by low DO and high K.   5.

Multivariate statistics reveal the main geochemical process controlling the groundwater chemistry as silicate weathering due to high Na+ and HCO3-; contributions from humic acid indicated by low pH and poor waste management indicated by low DO and high K. Sodium adsorption ratio (SAR), magnesium hazard (MH) and magnesium ratio indicated the excellent quality of these waters for irrigation use.

However, constituents such as dissolved solids are affected by many geochemical processes.

A total of 47 groundwater wells were sampled and analyzed to detect the main hydrochemical facies associated geochemical processes.

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.