2016
DOI: 10.1080/15324982.2015.1056326
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Hydrochemical and isotopic characters of surface water in agricultural oases of the Tianshan Mountains, Northwest China

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Cited by 6 publications
(5 citation statements)
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“…In spring, dryness, less precipitation and vigorous evaporation led to the enrichment of stable isotopes in the river water. In summer, more precipitation and a large amount of ice melt water (with low isotopes) recharged to river water, which resulted in the dilution of stable isotopes in river water samples [4,17,26]. The stable isotope composition of river water samples in the study area showed an obvious spatial variation (Figure 4).…”
Section: δD and δ 18 O In River Watermentioning
confidence: 99%
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“…In spring, dryness, less precipitation and vigorous evaporation led to the enrichment of stable isotopes in the river water. In summer, more precipitation and a large amount of ice melt water (with low isotopes) recharged to river water, which resulted in the dilution of stable isotopes in river water samples [4,17,26]. The stable isotope composition of river water samples in the study area showed an obvious spatial variation (Figure 4).…”
Section: δD and δ 18 O In River Watermentioning
confidence: 99%
“…The measurement results were reported by the Vienna Standard Mean Ocean Water (V−SMOW). Dual−column instrument (Dionex DX−100, Dionex, Sunnyvale, CA, USA, analytical errors were: Ca 2+ (±0.4 mg/L), Mg 2+ (±0.7 mg/L), Na + (±0.1 mg/L), K + (±0.1 mg/L), Cl − (±0.1 mg/L), SO 4 2− (±0.3 mg/L), HCO 3 − (±0.3 mg/L)) was used to measure the major ion concentration of surface and ground water. Some parameters (pH, water temperature and the total dissolved solids (TDS)) were tested in situ using a portable multiparameter instrument (Manta 2) adjusted with a standard solution.…”
Section: Sample Testing and Laboratory Analysismentioning
confidence: 99%
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