Sentence examples for major geochemical processes from inspiring English sources

Multivariate statistical analysis undertaken using PCA of major hydrochemical ions identified three major geochemical processes with 85.45% of TV.

This review summarizes the major geochemical processes controlling the release, speciation, fate, and distribution of inorganic arsenic in mine drainage and natural systems.

Thus, the strong positive loadings of the major ions together with EC and TDS in Component 1 are expected and suggest their contribution to major geochemical processes through mineralogical influence.

Bacterial groups or processes associated with major geochemical processes, such as methanogenesis, sulphate reduction and denitrification, that have the potential to drive contaminant degradation, were detected at various borehole levels.

Component 1 explains nearly 51.9% of the total variance (Table 6) and has strong positive loadings (>0.75) for EC, TDS, Mg2+, Ca2+, Na+, K+, Cl− and SO4 2− and a weak positive loading for HCO3 − (Table 5) suggesting that the major ions contribute positively to the total dissolved solids of the groundwater and can be accounted for by major geochemical processes within the aquifer.

Apart from fluoride, it is important to classify the water in respect of suitability for drinking for rest of the chemical constituents (Haritash et al. 2016); and to determine the major geochemical processes responsible for regulating groundwater chemistry (Haritash et al. 2017).

Water rock interaction (chemical weathering) is the major geochemical process that controls the groundwater chemistry followed by anthropogenic activities.

The rock water interaction was the major geochemical process controlling the chemistry of groundwater in the study area.

Type I groundwater is mostly located in a mountainous recharge area where pyrite oxidation is the major geochemical process.

The analysis results indicated that the carbonate weathering due to calcite dissolution was the major geochemical process contributing to the cations and anions of the aquifer water.

This observation indicates that evaporation may not be the major geochemical process controlling the chemistry of groundwater in this study region or ion exchange reaction dominating over evaporation.