Xianyang City, located about twenty kilometers to the north of Xi'an, the capital city of Shannxi,China, is rich in geothermal resources. Geothermal resources are characterized by relative high temperature,high hydraulic pressure, and high quality. Our hydrochemical study shows that: (1) Geothermal anomaly is controlled by faults; (2) Na+ is major cation in the thermal waters, order of anions based on their concentration is [Cl-] >^s[HCO3-] >^s[SO42-] and, as a result, Na-Cl type accounts for 50% of sampled thermal waters; (3)Evolution law of hydrochemical characteristics shows a general trend: Na-Cl type of high TDS water mainly distributes near the intersection of fractures; from southern to northern part of the field, with increase of [HCO3-]and [SO42-], water type evolves from Na-Cl type of high TDS to Na-HCO3-SO4 and Na-SO4-HCO3 type of intermediate TDS.
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机译:咸阳市位于中国陕西省山西首都西安北部约20公里,丰富地热资源。地热资源的特点是相对高温,液压压力和高质量。我们的水利化学研究表明:(1)地热异常由断层控制; (2)Na +是热水中的主要阳离子,基于它们的浓度的阴离子顺序是[Cl-]> ^ S [HCO3-] 结果,因此,Na-Cl型占据50%的采样热水; (3)水利化特征的演化法显示了一般趋势:Na-Cl型高TDS水主要分布在裂缝的交叉点附近;从南部到该领域的北部,随着[HCO3-]和[SO42-]的增加,水型从Na-Cl型高TDS到Na-HCO3-SO4和NA-SO4-HCO3中间TDS的中间TDS。
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