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应用生态学报 ›› 2020, Vol. 31 ›› Issue (4): 1417-1424.doi: 10.13287/j.1001-9332.202004.015

• 综合评述 • 上一篇    

稳定同位素方法评估“两个水世界”假设的研究现状与展望

赵影1,2, 王力1,3*   

  1. 1中国科学院水利部水土保持研究所黄土高原土壤侵蚀与旱地农业国家重点实验室, 陕西杨凌 712100;
    2中国科学院大学, 北京 100049;
    3西北农林科技大学资源环境学院, 陕西杨凌 712100
  • 收稿日期:2020-01-01 出版日期:2020-04-20 发布日期:2020-04-20
  • 通讯作者: *E-mail: wangli5208@nwsuaf.edu.cn
  • 作者简介:赵 影, 女, 1993年生, 博士研究生。主要从事同位素水文研究。E-mail: 13898159705@163.com
  • 基金资助:
    国家自然科学基金项目(41771545,41977012,41530854)和中国科学院地球环境研究所黄土与第四纪地质国家重点实验室(SKLLQG1718)资助

Assessing the “two water worlds” hypothesis by stable isotope method: Progress and prospect

ZHAO Ying1,2, WANG Li1,3*   

  1. 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;
    2University of Chinese Academy of Sciences, Beijing 100049, China;
    3College of Resources and Environment, Northwest A&F University, Yangling 712100, Shaanxi, China.
  • Received:2020-01-01 Online:2020-04-20 Published:2020-04-20
  • Contact: *E-mail: wangli5208@nwsuaf.edu.cn
  • Supported by:
    This work was supported by the National Natural Science Foundation of China (41771545, 41977012, 41530854) and the State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences (SKLLQG1718).

摘要: “两个水世界”的假设(two water worlds hypothesis,TWW)认为,土壤中存在两个相互独立且功能不同的水库,束缚水库用于植物生存生长,移动水库补给河川径流及地下水。该假设区别于传统水文模型中一个土壤水库的理论,对构建新的水文模型意义重大。目前,TWW假设的理论基础及形成条件仍不明确,尤其国内研究尚不多见。因此,本文总结了TWW假设的研究现状、判别方法、争议点以及未来的研究方向。目前,关于TWW假设的研究结果分为3种:支持、部分支持以及拒绝该假说,所有的评估方法都是基于氢、氧同位素(2H, 18O)方法实现的,如直接比较法、降水交结点法、降水残差法和降水偏移法等。束缚水与移动水同位素样品的代表性以及同位素技术的局限性可能是产生不同结果的重要原因,发展不同于稳定同位素手段的方法是未来研究的一个重要方向。另外,该假设的理论基础尚不清楚是当前面临的最关键的科学问题。TWW假设涉及到降水、土壤和植被三者耦合所形成的连续的生态水文过程,多学科融合、多尺度评估、多因素分析是深入研究该假设的有效途径,也将是水文学与生态学领域的重要研究方向。

Abstract: According to the two water worlds hypothesis (TWW), there are two independent water pools with different functions in the soil matrix, bound water world used by plants and mobile water world contributed to runoff and groundwater recharge. The TWW hypothesis is different from the original hydrological model that soil water is completely mixed, and is of significance for establishing new hydrological models. Currently, the theorical basis and formation conditions of TWW hypothesis are still unclear, with less reaserch from China. Here, we summarized research process, discrimination method, controversial points and prospect of TWW hypothesis. There are three views regarding the hypothesis: support, partial support, and rejection. All evaluation methods are based on hydrogen and oxygen isotope (2H, 18O) methods, such as direct comparison, precipitation intersection point method, precipitation residual method, and precipitation migration method. The representativeness of isotope samples of bound water and mobile water and the limitation of isotope technology may be the important reasons for different results across all the studies. The development of methods different from stable isotope ones is an important direction of future research. In addition, the theoretical basis of TWW hypothesis remains unclear, which is the most critical issue. The hypothesis is about a continuous ecological hydrological process coupling of precipitation, soil, and vegetation. Multi-disciplinary integration, multi-scale assessment and multi-factor analysis would be the effective ways to study this hypothesis, and would be an important research direction in the field of hydrology and ecology.