首页|青藏高原西北部班公湖流域夏季主要水体H-O同位素组成及其影响因素

青藏高原西北部班公湖流域夏季主要水体H-O同位素组成及其影响因素

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作为高寒内陆区的青藏高原西北部班公湖流域水文数据资料较为匮乏,导致对区域水循环过程和气候环境的认识不够深入,氢氧稳定同位素示踪技术可为解决该问题提供理想途径.本文系统分析班公湖流域夏季含湖水、河水、冰川融水和地下水4种不同类型的水体中氢氧同位素的组成,阐释水体氢氧同位素、氘盈余参数沿程变化的特征及其与水体矿化度、高程、经纬度和全球大气降雨线之间的关系,并进一步剖析同位素组成变化的控制因素.结果显示,水体中δ2H和δ18O的波动范围分别为-112.37‰~-24.90‰和-14.84‰~2.01‰,平均值及标准差分别为-76.73‰±26.49‰和-8.43‰±5.24‰.湖水δ2H和δ18O相对其他水体富集,测定结果更偏正值,冰川融水δ2H和δ18O相对其他水体更为贫化.流域水体氢氧同位素的大陆效应总体不明显,部分水体有一定高程效应体现.水体氢氧同位素演化趋势表明,冰川融水与全球大气水线接近,易受大气降雨影响.同时其他水体线的较小截距和斜率值,表明大气降雨不是这些水体的直接补给源.河流沿程的水体δ2H和δ18O呈递增趋势,越远离冰川融水补给端的河水和湖水值越偏正,反映强蒸发的特点.水体氘盈余参数及其与矿化度之间的关系也指示蒸发作用是影响该区域水体氢氧同位素变化的主要因素.
Characteristics and Influencing Factors of the Hydrogen and Oxygen Isotopes in Summer Water Bodies in the Bangong Lake Basin,Northwest Tibetan Plateau
The Bangong Lake basin in northwestern Tibetan Plateau is geographically challenging to access and lacks effective hydrological data.In order to understand the regional water cycle and climate,a total of 34 water samples,including lake water,river water,glacial meltwater,and groundwater,were collected from this region during the summer.Moreover,the study revealed the variation characteristics of hydrogen and oxygen isotopes,deuterium excess parameters,and their relationships with the water salinity,elevation,longitude,latitude,and global rainfall patterns,as to investigate the environmental indications of hydrogen and oxygen isotopes in the regional water cycles.The results show that the values of δ2 H and δ18 O in the water samples ranged from-112.37‰ to-24.90‰ and from-14.84‰ to 2.01‰,respectively.The mean values and standard devia-tions were-76.73‰±26.49‰ for δ2H and-8.43‰±5.24‰ for δ18O.Among them,the values of δ2H and δ18O were found to be the highest in lake water samples and the lowest in the glacial meltwater samples.The continental effect of hydrogen and oxygen isotopes was not evident in the study area,and certain water bodies exhibit an elevation effect.The hydrogen and oxygen isotope lines of each water body show that meltwater in the study area was more susceptible to atmospheric rainfall compared to other water bodies.The smaller inter-cept and slope values for the other water bodies indicate that atmospheric rainfall was not a major source of recharge and was characterized by evapotranspiration.The δ2H and δ18O values of rivers exhibit an increasing trend along the course,also reflecting the characteristics of strong evaporation.The relationship between deute-rium excess parameters and salinity indicated that evaporation was the main factor affecting the variation of hydrogen and oxygen isotopes.

Bangong Lake basinhydrogen and oxygen isotopedeuterium excess parameterspatial distribu-tionisotopic effect

邵玉祥、严步青、刘旭、蒋钦、陈文彬、龚康、易海洋、李博

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中国地质调查局军民融合地质调查中心,四川成都 610036

中国地质大学(武汉)地球科学学院,湖北武汉 430073

中国地质大学(北京)地球科学与资源学院,北京 100083

班公湖流域 氢氧同位素 氘盈余参数 空间特征 同位素效应

中国地质调查局项目中国地质调查局项目

[2023]10-02-01ZD20220199

2024

现代地质
中国地质大学(北京)

现代地质

CSTPCD北大核心
影响因子:1.2
ISSN:1000-8527
年,卷(期):2024.38(2)
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