巴丹吉林沙漠降水稳定同位素特征与水汽再循环

曹乐; 申建梅; 聂振龙; 孟令群; 刘敏; 王哲

doi:10.3799/dqkx.2020.273

Volume 46 Issue 8

Aug. 2021

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Article Navigation > Earth Science > 2021 > 46(8): 2973-2983

Cao Le, Shen Jianmei, Nie Zhenlong, Meng Lingqun, Liu Min, Wang Zhe, 2021. Stable Isotopic Characteristics of Precipitation and Moisture Recycling in Badain Jaran Desert. Earth Science, 46(8): 2973-2983. doi: 10.3799/dqkx.2020.273

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Cao Le, Shen Jianmei, Nie Zhenlong, Meng Lingqun, Liu Min, Wang Zhe, 2021. Stable Isotopic Characteristics of Precipitation and Moisture Recycling in Badain Jaran Desert. Earth Science, 46(8): 2973-2983. doi: 10.3799/dqkx.2020.273

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Stable Isotopic Characteristics of Precipitation and Moisture Recycling in Badain Jaran Desert

doi: 10.3799/dqkx.2020.273

Cao Le^{1, 2, 3
,
,},
Shen Jianmei^{1
,
,
,},
Nie Zhenlong¹,
Meng Lingqun¹,
Liu Min¹,
Wang Zhe¹

1.
Institute of Hydrogeology and Environmental Geology, CAGS, Shijiazhuang 050061, China
2.
China University of Geosciences, Beijing 100083, China
3.
Key Laboratory of Groundwater Sciences and Engineering of Ministry of Natural Resources, Shijiazhuang 050061, China

Received Date: 2020-06-19
Available Online: 2021-09-14
Publish Date: 2021-08-15

Abstract

Abstract

Understanding the isotopic characteristics of precipitation in desert is helpful to study the water cycle process in arid areas. According to the precipitation samples from 4 stations in the Badain Jaran Desert from 2015 to 2016, the temporal and spatial distribution characteristics and influencing factors of δ²H and δ¹⁸O were analyzed. The source of precipitation moisture was analyzed with the backward air mass trajectory model and the recycled moisture fractions were calculated with deuterium excess. The results show that the precipitations of δ²H and δ¹⁸O show seasonal effect, which are higher in summer and lower in winter. The precipitations of δ²H and δ¹⁸O in the hinterland of desert are more positive and d-excess is more negative than that in the surrounding mountainous areas, reflecting the stronger evaporation of precipitation in the hinterland. The annual precipitation is mainly from the westerly moisture, and the summer precipitation is affected by the southeast monsoon. The recycled moisture fraction in desert is 10.3%-10.9%, which is slightly larger than 8.5% of mountainous area; the recycled moisture accounts for 11.1% of the total evaporation, which reflects that the contribution of strong evaporation in desert to local precipitation is relatively limited.
- precipitation,
- stable isotope,
- d-excess,
- moisture recycling,
- Badain Jaran Desert,
- atmospheric science

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References(41)

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Stable Isotopic Characteristics of Precipitation and Moisture Recycling in Badain Jaran Desert

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