Wu Huawu;Li Xiaoyan;Li Jing;Jiang Zhiyun;Li Guangyong;Liu Lei

 

[Wu Huawu; Li Xiaoyan] Beijing Normal Univ, State Key Lab Earth Surface Proc & Resource Ecol, Beijing 100875, Peoples R China.

[Wu Huawu; Li Xiaoyan; Jiang Zhiyun; Li Guangyong; Liu Lei] Beijing Normal Univ, Coll Resources Sci & Technol, Beijing 100875, Peoples R China.

[Li Jing] Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China.

[Li Jing] Univ Chinese Acad Sci, Beijing 100049, Peoples R China.

ABSTRACT: Stable isotopic compositions (delta O-18 and delta D) have been utilized as a useful indicator for evaluating the current and historical climatic and environmental changes. Therefore, it is vital to understand the relationship between the stable isotopic contents in lake water and the variations of lake level, particularly in Lake Qinghai, China. In this study, we analyzed the variations of isotope compositions (delta O-18, delta D and d-excess) in lake water and precipitation by using the samples that were collected from Lake Qinghai region during the period from 2009 to 2012. The results showed that the average isotopic contents of delta O-18 and delta D in lake water were higher than those in precipitation, which were contrary to the variations of d-excess. The linear regression correlations between delta O-18 and delta D in lake water and precipitation showed that the local evaporative line (LEL) in lake water (delta D=5.88 delta O-18-2.41) deviated significantly from the local meteoric water line (LMWL) in precipitation (delta D=8.26 delta O-18+16.91), indicating that evaporative enrichment had a significant impact on isotopic contents in lake water. Moreover, we also quantified the E/I ratio (evaporation-to-input ratio) in Lake Qinghai based on the lake water isotopic enrichment model derived from the Rayleigh equation. The changes of E/I ratios (ranging from 0.29 to 0.36 between 2009 and 2012) clearly revealed the shifts of lake levels in Lake Qinghai in recent years. The average E/I ratio of 0.40 reflected that water budget in Lake Qinghai was positive, and consistent with the rising lake levels and the increasing lake areas in many lakes of the Tibetan Plateau. These findings provide some evidences for studying the hydrological balance or water budget by using delta O-18 values of lake sedimentary materials and contribute to the reconstruction of paleolake water level and paleoclimate from an isotopic enrichment model in Lake Qinghai.

Published in JOURNAL OF ARID LAND.2015,7(5):623-635, DOI: 10.1007/s40333-015-0048-6