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[Assessing the "two water worlds" hypothesis by stable isotope method: Progress and prospect].
1State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Chinese Academy of Sciences and the Ministry of Water Resources, Yangling 712100, Shaanxi, China.
Summary
The two water worlds hypothesis proposes distinct soil water pools for plants and runoff. Further research is needed to clarify its theoretical basis and formation conditions, moving beyond current isotope-based methods.
Area of Science:
- Soil science
- Hydrology
- Ecology
Background:
- The two water worlds (TWW) hypothesis posits two independent soil water pools: bound water for plants and mobile water for runoff/recharge.
- This contrasts with traditional models assuming complete soil water mixing and is crucial for developing new hydrological models.
Purpose of the Study:
- To review the research progress, discrimination methods, controversies, and future prospects of the TWW hypothesis.
- To highlight the current lack of clarity regarding the theoretical underpinnings and formation conditions of the TWW hypothesis, especially in China.
Main Methods:
- Evaluation of existing studies primarily relies on hydrogen and oxygen stable isotope (²H, ¹⁸O) techniques.
- Methods include direct comparison, precipitation intersection point, precipitation residual, and precipitation migration methods.
Main Results:
- Research shows three viewpoints on the TWW hypothesis: support, partial support, and rejection.
- Discrepancies in results are attributed to the representativeness of isotope samples and limitations of isotope technology.
Conclusions:
- Developing non-isotope-based methods is essential for future research.
- Clarifying the theoretical basis of the TWW hypothesis is critical.
- Future studies should integrate multi-disciplinary approaches, multi-scale assessments, and multi-factor analyses to understand the ecological hydrological coupling.
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