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- W4306696601 abstract "Proper assessment of mixing with shallow groundwater is key to understanding the state and hydrochemical composition of deep groundwater. Each tracer technique (hydrochemistry, isotopes, temperature, etc.) used to evaluate mixing has its own applicability and disadvantages. Microorganisms in groundwater record the environment they experience and respond quickly to environmental changes, making them potential tracers. Three groups of groundwater (nine samples) from three different hydrogeological conditions in a hydrothermal system in Suining (southern China) were selected and assessed as a case study. The three groups of groundwater have similar hydrochemical types, but the chemical compositions are different. Moreover, the deep warm groundwater experiences a temperature of 66.5–74.6 °C and a circulation depth of 1.93 km. Species-level operational taxonomic unit (OTU) classification and principal component analysis (PCA) were performed for the microorganisms. Although Proteobacteria and Cyanobacteria are dominant, the microbial communities are significantly different in the three groups of groundwater. Moreover, Firmicutes, Fusobacteria and Cyanobacteria are positively correlated with Na+, SO42–, Cl– and F–, as well as the corresponding OTUs at the species level. The ratio of geothermal water mixed with shallow groundwater is evaluated by water chemistry (Cl–, SO42– and Na+) and the average value is 46.46%, while the mixing ratio evaluated by the microbial community is 44.68 and 43.71% at the phylum and species level, respectively. Similar assessment results indicate that the microbial community can be used as an effective tracer to estimate the mixing of deep geothermal water with shallow groundwater." @default.
- W4306696601 created "2022-10-19" @default.
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- W4306696601 date "2022-10-18" @default.
- W4306696601 modified "2023-09-27" @default.
- W4306696601 title "Use of microbial communities to assess the mixing of deep and shallow groundwater: case study from southern China" @default.
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- W4306696601 doi "https://doi.org/10.1007/s10040-022-02555-9" @default.
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