达里诺尔湖水体稳定氢、氧同位素组成变化对结冰过程的响应

李文宝; 李畅游; 刘晓旭; 甄志磊; 胡其图; 刘志娇

doi:10.3799/dqkx.2015.184

Volume 40 Issue 12

Dec. 2015

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Article Navigation > Earth Science > 2015 > 40(12): 2081-2090

Li Wenbao, Li Changyou, Liu Xiaoxu, Zhen Zhilei, Hu Qitu, Liu Zhijiao, 2015. Changes of Stable Oxygen and Hydrogen Isotopes and Their Responses to Freezing Process in Dali-Nor Lake in Cold-Arid Areas of China. Earth Science, 40(12): 2081-2090. doi: 10.3799/dqkx.2015.184

Citation:

Li Wenbao, Li Changyou, Liu Xiaoxu, Zhen Zhilei, Hu Qitu, Liu Zhijiao, 2015. Changes of Stable Oxygen and Hydrogen Isotopes and Their Responses to Freezing Process in Dali-Nor Lake in Cold-Arid Areas of China. Earth Science, 40(12): 2081-2090. doi: 10.3799/dqkx.2015.184

Citation:

Li Wenbao, Li Changyou, Liu Xiaoxu, Zhen Zhilei, Hu Qitu, Liu Zhijiao, 2015. Changes of Stable Oxygen and Hydrogen Isotopes and Their Responses to Freezing Process in Dali-Nor Lake in Cold-Arid Areas of China. Earth Science, 40(12): 2081-2090. doi: 10.3799/dqkx.2015.184

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Changes of Stable Oxygen and Hydrogen Isotopes and Their Responses to Freezing Process in Dali-Nor Lake in Cold-Arid Areas of China

doi: 10.3799/dqkx.2015.184

1.
Key Laboratory of Water Resources Protection and Utilization, Inner Mongolia Agricultural University, Hohhot 010018, China
2.
National Nature Reserve Ecological Tourism Co., Ltd. of Keshenketeng Dali-Nor Lake, Chifeng 025373, China

Received Date: 2015-04-03
Publish Date: 2015-12-15

Abstract

Abstract

Utilizing the environmental isotopes, which exist widely as one proxy of lake water evolution process, has become one important direction in lake sciences.In this paper, a total of 77 samples of lake water, ice and precipitation water were collected in Dali-Nor Lake, which locates in cold-arid areas of Inner Mongolia; and changes of δD and δ¹⁸O and their responses to freezing process in Dali-Nor Lake are analyzed. The comparison of the changes of δD and δ¹⁸O among lake ice, lake water and precipitate water shows that: (1) Following the freezing process, the values of ΔδD, Δδ¹⁸O between bottom (65 cm) and surface (15 cm) ice layers are both above zero.But in fast stage and stable stage during lake ice forming, the change range of water stable isotopes is different.Meanwhile, the values of δD and δ¹⁸O in water under the ice are about 13.85 ‰ and 2.23 ‰ lighter than those in lake ice.In addition, the river inflows have more obvious influence on value changes of δD and δ¹⁸O among different sites in winter than in summer. (2) The δD and δ¹⁸O values of water (both summer and winter) and ice are both in right side of the global meteoric water line (GMWL) and local meteoric water line (LMWL), which shows that the evaporation process has certain influence on the fractional distillation of water stable isotopes before the lake ice formed. On the other hand, the values of δD and δ¹⁸O in lake ice and winter lake water have the same slope range and both in right side of the values of δD and δ¹⁸O in summer lake water, which shows that the freezing process has obvious influence on the fractional distillation of water stable isotopes during the lake ice forming process.
- hydrogen isotope,
- oxygen isotope,
- freezing process,
- Dali-Nor Lake,
- cold-arid area,
- geochemistry

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Changes of Stable Oxygen and Hydrogen Isotopes and Their Responses to Freezing Process in Dali-Nor Lake in Cold-Arid Areas of China

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