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珠江下游泗合水流域降雨事件环境同位素特征及水汽来源分析

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利用珠江下游泗合水流域雨季6场降雨事件中采集的降雨、河水、地下水水样,结合同位素示踪技术、HYSPLIT模式及同位素二元混合模型,对各水样中的氢氧同位素特征、降雨水汽来源及两场降雨事件中径流的不同水源比例进行了分析.结果表明:(1)降雨δD与δ18O的变化范围分别为-98.05‰~-24.16‰与-13.33‰~-4.54‰,泗合水流域局地大气降水线为δD=8.22δ18O+13.64;δ18O与氘盈余之间呈现负相关关系,氘盈余值表现为"高-低-高"的走向.(2)降雨水汽主要来源于印度洋的西南季风以及太平洋的东南季风;20140916场次降雨事件气团输送路径较长,水汽中的氢氧同位素较为贫化.(3)20140916场次降雨事件地下径流变化幅度较小,地表径流与总径流同步涨落,地下、地表径流量比例分别约为60%与40%;20150509场次地下径流、地表径流与总径流均同步涨落,地下、地表径流量比例分别约为40%与60%.
Analysis of the Characteristics of Environmental Isotopes and Water Vapor Sources of Precipitation Events in Sihe River Basin of Lower Pearl River
The characteristics of hydrogen and oxygen isotopes in each water samples,the water vapor sources of precipitation and the proportion of different water sources of the runoff in two precipitation events were analyzed based on precipitation,river water and groundwater samples collected during six precipitation events in Sihe River basin of lower Pearl River,using stable isotope tracer technique,HYSPLIT model and isotope-based two-component mixing model.The results show that:(1)The δD and δ18O in precipitation range from-98.05‰ to-24.16‰ and-13.33‰ to-4.54‰ respectively,and the local meteoric water line of Sihe River basin is δD=8.22δ18O+13.64(R2=0.98,n=19);δ18O is negatively related to the deuterium surplus,and the values of deute-rium surplus show a"high-low-high"trend approximately.(2)The water vapor of precipitation are mainly from the southwest mon-soon from the Indian Ocean and the southeast monsoon from the Pacific Ocean;the transport pathway of the water vapor trajec-tory of 20140916 precipitation event is quite long,and the hydrogen and oxygen isotopes in the water vapor are relatively de-pleted.(3)The variation range of the underground runoff of 20140916 precipitation event is relatively small,while the surface run-off and total runoff fluctuate synchronously,and the proportion of the underground and surface runoff is about 60%and 40%re-spectively;the underground runoff,surface runoff and total runoff of 20150509 precipitation event all fluctuate synchronously,and the proportion of the underground and surface runoff is about 40%and 60%respectively.

precipitation eventsthe characteristics of isotopeswater vapor sourcestwo-component mixing modelSihe River Basin

刘俊达、胡海英、卢义亮

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华南理工大学土木与交通学院,广东广州 510640

降雨事件 同位素特征 水汽来源 二元混合模型 泗合水流域

国家自然科学基金国家重点研发计划资助项目

512090962018YFC1508203

2023

水文
水利部水文局 水利部水利信息中心

水文

CSTPCDCSCD北大核心
影响因子:0.742
ISSN:1000-0852
年,卷(期):2023.43(6)
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