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昆明市黑龙潭岩溶泉氢氧稳定同位素分析

黄华诚 刘 宏

黄华诚, 刘 宏. 昆明市黑龙潭岩溶泉氢氧稳定同位素分析[J]. 中国岩溶, 2015, 34(5): 445-451. doi: 10.11932/karst20150504
引用本文: 黄华诚, 刘 宏. 昆明市黑龙潭岩溶泉氢氧稳定同位素分析[J]. 中国岩溶, 2015, 34(5): 445-451. doi: 10.11932/karst20150504
HUANG Hua-cheng, LIU Hong. The hydrogen and oxygen stable isotope analysis of the karst spring in Heilongtan[J]. CARSOLOGICA SINICA, 2015, 34(5): 445-451. doi: 10.11932/karst20150504
Citation: HUANG Hua-cheng, LIU Hong. The hydrogen and oxygen stable isotope analysis of the karst spring in Heilongtan[J]. CARSOLOGICA SINICA, 2015, 34(5): 445-451. doi: 10.11932/karst20150504

昆明市黑龙潭岩溶泉氢氧稳定同位素分析

doi: 10.11932/karst20150504
基金项目: 国家自然科学基金(41371040)

The hydrogen and oxygen stable isotope analysis of the karst spring in Heilongtan

  • 摘要: 黑龙潭位于昆明市北缘的五老山山麓,沿黑龙潭东支断裂带出露地表,该区分布三个岩溶泉,分别是:清水潭、浑水潭、小水潭,文章运用氢氧稳定同位素方法对它们进行连续的观测研究。通过对大气降水和泉水氢氧稳定同位素特征进行分析,揭示研究区岩溶泉水的来源及泉域含水层特征。得出以下结论:(1)通过大气降水δ18O -δD 关系建立当地大气降水线,大气降水线和泉水的稳定同位素分析表明泉水来源于大气降水,而且主要来源于夏季降水。(2)高斯混合模型分析结果表明,清水潭的补给不仅来源于野猫山地区,还包括径流过程中的入渗补给,而且入渗补给量并不小。浑水潭旱雨两季补给类型有所区别。小水潭除受北部二叠系灰岩含水层补给之外,很有可能也受东北部玄武岩山地的孔洞裂隙水补给。

     

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  • 刊出日期:  2015-10-25

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