Articles | Volume 21, issue 9
https://doi.org/10.5194/hess-21-4419-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/hess-21-4419-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Origin of water in the Badain Jaran Desert, China: new insight from isotopes
Xiujie Wu
School of Water Resources and Environment, China University of
Geosciences (Beijing), Beijing, 100083, P. R. China
Department of Earth, Ocean, and Atmospheric Science, Florida State University, Tallahassee, FL,
32306, USA
High National Magnetic Field Laboratory, Tallahassee, FL, 32310, USA
Xu-Sheng Wang
School of Water Resources and Environment, China University of
Geosciences (Beijing), Beijing, 100083, P. R. China
Yang Wang
CORRESPONDING AUTHOR
Department of Earth, Ocean, and Atmospheric Science, Florida State University, Tallahassee, FL,
32306, USA
High National Magnetic Field Laboratory, Tallahassee, FL, 32310, USA
Institute of Groundwater and Earth
Sciences, The Jinan University, Guangzhou, Guangdong Province,
510632, P. R. China
Bill X. Hu
CORRESPONDING AUTHOR
School of Water Resources and Environment, China University of
Geosciences (Beijing), Beijing, 100083, P. R. China
Department of Earth, Ocean, and Atmospheric Science, Florida State University, Tallahassee, FL,
32306, USA
Institute of Groundwater and Earth
Sciences, The Jinan University, Guangzhou, Guangdong Province,
510632, P. R. China
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33 citations as recorded by crossref.
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- Identifying the recharge and salinization mechanisms of the Shekastian saline spring in southern Iran J. Mohammadzadeh-Habili et al. 10.1007/s11356-023-27308-3
- Stable isotopes reveal the lake shrinkage and groundwater recharge to lakes in the Badain Jaran Desert, NW China L. Cao et al. 10.1016/j.jhydrol.2022.128289
- Identifying the spatio-seasonal pattern of hydrochemical evolution and surface water-groundwater interaction in a large urban river basin, Northwest China L. Duan et al. 10.1016/j.scitotenv.2024.173989
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- Trace element distribution, sources, toxicity risk characteristics associated with lacustrine groundwater discharge in boreal lakes: Implications for the eco-environmental security in the Yellow River Basin, China X. Yang et al. 10.1016/j.ecolind.2024.112600
- Hydrogeochemistry and fractionation of boron isotopes in the inter-dune aquifer system of Badain Jaran Desert, China X. Zhang et al. 10.1016/j.jhydrol.2021.125984
- Key hydrological processes in the Del Azul Creek basin, sub-humid Pampean Plain M. Zabala et al. 10.1016/j.scitotenv.2020.142258
- Radiocarbon age discrepancies between the carbonate cement and the root relics of rhizoliths from the Badain Jaran and the Tengeri deserts, Northwest China Q. Sun et al. 10.1016/j.catena.2019.04.011
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- The Study of Hydrogeochemical Environments and Microbial Communities along a Groundwater Salinity Gradient in the Pearl River Delta, China S. Sang et al. 10.3390/w11040804
- Climate change during the last glacial period on the southeast margin of Badain Jaran Desert, Northwest China X. Fan et al. 10.1007/s11629-018-5186-9
- Large-scale surface water-groundwater origins and connectivity in the Ordos Basin, China: Insight from hydrogen and oxygen isotopes S. Qu et al. 10.1016/j.envres.2023.116837
- Groundwater quality assessment and hydrogeochemical processes in typical watersheds in Zhangjiakou region, northern China W. Jiang et al. 10.1007/s11356-021-15644-1
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- Spatiotemporal Variation of Groundwater Recharge in the Lower Reaches of the Poyang Lake Basin, China: Insights From Stable Hydrogen and Oxygen Isotopes H. Mao et al. 10.1029/2020JD033760
- Lake dynamics in an Early Jurassic desert: Evidence from the Clarens Formation in southern Africa H. Head & E. Bordy 10.1111/sed.13066
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- Using 222Rn temporal and spatial distributions to estimate the groundwater discharge rate and associated nutrient fluxes into high salinity lakes in Badain Jaran Desert, Northwest China X. Su et al. 10.1016/j.scitotenv.2022.159359
- Groundwater Age and Origin and Its Relation with Anthropogenic and Climatic Factors U. Iqbal et al. 10.3390/w16020287
- Groundwater net discharge rates estimated from lake level change in Badain Jaran Desert, Northwest China X. Wang et al. 10.1007/s11430-019-9533-8
- Spatio-seasonal characteristics and controlling factors of surface water stable isotope values (δ18O and δD) across the Inner Mongolia Reaches of the Yellow River Basin, China: Implication for hydrological cycle S. Qu et al. 10.1016/j.ejrh.2024.101843
- Comment on “Origin of water in the Badain Jaran Desert, China: new insight from isotopes” by Wu et al. (2017) L. Zhan et al. 10.5194/hess-22-4449-2018
- Understanding recharge of soil water in a sand dune at the Nuoertu of Badain Jaran Desert using isotopes of H and O K. Jin et al. 10.1007/s10967-018-6204-7
- Contrasting groundwater depletion patterns induced by anthropogenic and climate-driven factors on Alxa Plateau, northwestern China T. Wang et al. 10.1016/j.jhydrol.2019.06.057
- Moisture sources and climate evolution during the last 30 kyr in northeastern Tibetan Plateau: Insights from groundwater isotopes (2H, 18O, 3H and 14C) and water vapour trajectories modeling N. Yang & G. Wang 10.1016/j.quascirev.2020.106426
- Hydrologic partition and maintenance mechanism of Badain Jaran Desert lake group indicated by hydrogen and oxygen stable isotopes, northwest China X. Su et al. 10.1007/s12665-022-10686-1
- Cryospheric processes in Quaternary and Cretaceous hyper‐arid plateau desert oases C. Wu et al. 10.1111/sed.12804
1 citations as recorded by crossref.
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Short summary
It is critical to identify the origins of water in arid and semiarid regions for management and protection of the water resources. The D, 18O, 3H and 14C in water samples from the Badain Jaran Desert, China, were analyzed. The results show that groundwater supplies the lakes and originates from local precipitation and adjacent mountains. Negative d-excess values of water in the area were the result of evaporation. The 14C ages do not represent the residence time of local groundwater.
It is critical to identify the origins of water in arid and semiarid regions for management and...