2018
DOI: 10.1007/s12665-017-7212-6
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Hydrochemical characteristics and quality assessment of shallow groundwater and CBM co-produced water in the Shizhuangnan block, Qinshui Basin, China

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Cited by 15 publications
(3 citation statements)
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“…The plot of Ca 2+ + Mg 2+ vs. HCO 3 − + SO 4 2− also confirmed that the presence of HCO 3 − and SO 4 2− (63.89% of samples) was associated with the soil system that majorly affects the nature of groundwater in the study area (Figure 7c). This was supported by plotting HCO 3 − vs. Cl − + SO 4 2− graph, indicating that 61.1% of the samples (Figure 7d) fell below the equiline; this also confirmed that weathering and the influence of anthropogenic activities are the primary source of excess concentrations of ions in groundwater [59]. In particular, an excess amount of HCO 3 − in the groundwater indicates that physical weathering of Na + and K + silicates along with anthropogenic activities of organic waste decomposition are significant sources of groundwater contamination in the study region.…”
Section: Contamination Source Identification (Csi)supporting
confidence: 57%
“…The plot of Ca 2+ + Mg 2+ vs. HCO 3 − + SO 4 2− also confirmed that the presence of HCO 3 − and SO 4 2− (63.89% of samples) was associated with the soil system that majorly affects the nature of groundwater in the study area (Figure 7c). This was supported by plotting HCO 3 − vs. Cl − + SO 4 2− graph, indicating that 61.1% of the samples (Figure 7d) fell below the equiline; this also confirmed that weathering and the influence of anthropogenic activities are the primary source of excess concentrations of ions in groundwater [59]. In particular, an excess amount of HCO 3 − in the groundwater indicates that physical weathering of Na + and K + silicates along with anthropogenic activities of organic waste decomposition are significant sources of groundwater contamination in the study region.…”
Section: Contamination Source Identification (Csi)supporting
confidence: 57%
“…This can be challenging and cost-prohibitive. Re-use for irrigation purposes is theoretically appealing; however, prolonged application of CBM-produced waters can result in salt alkalization and salinization of agricultural soils, and these effects are exacerbated by significant transpiration and/or water stagnation due to poor drainage (Mallants et al 2017;Wang et al 2018). Other disposal mechanisms are expensive-costing as high as US$ 0.3 per m 3 (where corresponding value of gas is of the order $ 10 2 -10 3 ) (Boysen et al 2002).…”
Section: Cbm Challenges Pertaining To Produced Water Qualitymentioning
confidence: 99%
“…Moreover, where groundwater is available, obtaining shallow groundwater is more economical and convenient than deep groundwater [13][14][15]. However, the shallow groundwater has direct recharging and discharging relationships with local precipitation and surface water and is greatly affected by anthropogenic activities due to shallow buried conditions and rapid circulation [16][17][18]. Therefore, the quality and safety of shallow groundwater have drawn global attention.…”
Section: Introductionmentioning
confidence: 99%