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    Volume 48 Issue 3
    Mar.  2023
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    Article Navigation >  Earth Science  > 2023  >  48(3): 1156-1178
    Li Zongxing, Zhang Baijuan, Feng Qi, Gui Juan, Zhang Baiting, 2023. A Review of Isotope Ecohydrology in the Cold Regions of Western China. Earth Science, 48(3): 1156-1178. doi: 10.3799/dqkx.2022.264
    Citation: Li Zongxing, Zhang Baijuan, Feng Qi, Gui Juan, Zhang Baiting, 2023. A Review of Isotope Ecohydrology in the Cold Regions of Western China. Earth Science, 48(3): 1156-1178. doi: 10.3799/dqkx.2022.264
    shu

    A Review of Isotope Ecohydrology in the Cold Regions of Western China

    doi: 10.3799/dqkx.2022.264
    • 1.

      Observation and Research Station of Eco-Hydrology and National Park by Stable Isotope Tracing in Alpine Region/Key Laboratory of Ecohydrology of Inland River Basin/Ecological Environment Research Center of Qilian Mountain, Gansu Province, Northwest Institute of Eco-environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China

    • 2.

      University of Chinese Academy of Sciences, Beijing 100049, China

    • Received Date: 2022-05-09
      Available Online: 2023-03-27
    • Publish Date: 2023-03-25
      Abstract
    • The mountainous alpine area in western China is an Asian water tower and is an important ecological barrier area. With the development of environmental isotope test technology and the maturity of the related theories, stabilizing isotope technology has become a technique integrating many functions such as tracing, integration, and indication. Based on the previous research results, this study sorts out and summarizes the isotopic ecohydrology of the alpine mountains in a western area. It is found that the atmospheric precipitation line in the west of the alpine mountains is δD=7.44δ18O+5.23 (R2=0.86). The temperature effect shows an increasing trend from the south to north, while the precipitation effect shows an opposite direction. The water vapor sources in the western alpine mountains are complex. When the temperature coefficient is less than 0, the water vapor source is dominated by the southwest monsoon; when the temperature coefficient is 0-0.3, the water vapor source is jointly dominated by the southwest monsoon and the westerly wind; when the temperature coefficient is more significant than 0.3, the water vapor source is dominated by the westerly wind. Different water bodies are affected by water supply and evaporation differences. The slope of the local evaporation lines of stable isotope in each water body is in the following order: river water > ice and snow melt water > groundwater. The altitude effect of δ18O in precipitation in the western alpine mountains is -1.3‰/100m, and the altitude effect of δ18O in river water is -0.17‰/100m. The primary source of plant water in the study area is soil water, and the utilization rate of water is closely related to plant types and the regional environment. Water vapor recycling has become an essential part of regional precipitation water vapor sources. However, with the deepening of the major national strategy of ecological civilization construction, the western alpine mountainous area, which is an essential national ecological barrier, is undergoing profound and drastic changes in the ecological and hydrological processes under the changing environment. It poses challenges to regional water resources security, ecological security and sustainable development, which in turn provides a broad stage for the development of isotope ecohydrology in cold regions. In the future, it is urgent to further advances in the four aspects involving the observation, sampling, modeling, and theory in this domain.

       

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