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黄河水主要化学组分与δ13C的沿程变化特征

Main Chemical Constituent of the Yellow River Water and Characteristics of δ13C Streamwise Variation

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【作者】 苏小四吴晓芳林学钰廖资生王金生

【Author】 SU Xiao-si~1,WU Xiao-fang~1,LIN Xue-yu~1,LIAO Zi-sheng~1,WANG Jin-sheng~2(1.Institute of Water Resources and Environmental Research,Jilin University,Changchun,Jilin 130026;2.Beijing Normal University,Beijing 100875)

【机构】 吉林大学水资源与环境研究所北京师范大学水科学研究院 吉林长春130026教育部城市环境与可持续发展研究中心吉林大学分中心吉林长春130026北京100875

【摘要】 在系统采集从黄河源头至入海口的17条河谷断面上的黄河水、地下水和地表水水样,并测定其主要化学组分含量和1δ3C同位素组成的基础上,对黄河水主要化学组分含量及同位素组成沿程变化特征进行了综合分析。黄河水具有从源头到入海口水化学变化大,δ13C比值波状下降的总体变化特点。研究认为,地表径流和岩溶地下水等水体对河水的补给以及灌溉回归水是导致河水水化学组成和同位素变化的最主要因素。

【Abstract】 The paper comprehensively analyzes the main chemical constituent content of the Yellow River water and characteristic of isotope streamwise variation based on samples of the Yellow River,groundwater and surface water systematically collected from 17 valley sections from the river head to river mouth and the observation of its main chemical constituent content and δ13C isotope component.The Yellow River water has the characteristics of overall variation of great hydrochemical variation and undulating fall of δ13C proportionality from the river head to river mouth.It considers through study that the replenishment of surface runoff and karsk groundwater to the river and irrigation return flow are the most important factors for conducing hydrochemical composition and isotope variation of the river.

【基金】 国家重点基础研究发展规划项目(G1999043606);吉林大学“985计划”项目
  • 【分类号】X832
  • 【被引频次】20
  • 【下载频次】382
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