壤中流形成机制及其生态水文效应研究进展

赵宇寒; 曹建生; 朱春雨; 阳辉

doi:10.12357/cjea.20210277

壤中流形成机制及其生态水文效应研究进展

doi: 10.12357/cjea.20210277

赵宇寒^{1, 2,},
曹建生^1, ,,
朱春雨¹,
阳辉¹

1.
中国科学院遗传与发育生物学研究所农业资源研究中心/河北省土壤生态学重点实验室/中国科学院农业水资源重点实验室　石家庄　050022
2.
中国科学院大学　北京　100049

基金项目: 河北省重点研发计划项目(20324203D)、河北省创新能力提升计划项目(20536001D)和国家自然科学基金项目(4187072165)资助

详细信息

作者简介:
赵宇寒, 主要研究方向为生态水文学。E-mail: 1219886686@qq.com

通讯作者:
曹建生, 主要从事山地生态水文过程与降水资源调控机制研究。E-mail: caojs@sjziam.ac.cn

中图分类号: S157.2
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- 文章访问数: 270
- HTML全文浏览量: 102
- PDF下载量: 59
- 被引次数: 0
出版历程
- 收稿日期: 2021-05-08
- 录用日期: 2021-09-26
- 网络出版日期: 2021-11-17
- 刊出日期: 2022-01-08

Research progress on the formation mechanism of subsurface flow and its eco-hydrological effects

ZHAO Yuhan^{1, 2
,},
CAO Jiansheng^{1
, ,},
ZHU Chunyu¹,
YANG Hui¹

1.
Center for Agricultural Resources Research, Institute of Genetics and Developmental Biology, Chinese Academy of Sciences / Hebei Key Laboratory of Soil Ecology / Key Laboratory of Agricultural Water Resources, Chinese Academy of Sciences, Shijiazhuang 050022, China
2.
University of Chinese Academy of Sciences, Beijing 100049, China

Funds: This study was supported by the Key R & D Project of Hebei Province (20324203D), Hebei Province Innovation Ability Promotion Project (20536001D) and the National Natural Science Foundation of China (4187072165)

More Information

Corresponding author: E-mail: caojs@sjziam.ac.cn

摘要

摘要: 水是人类生存和经济社会发展的重要基础资源, 在气候变化和人类活动的双重影响下, 陆地水循环发生了深刻变化。壤中流是水循环的重要环节, 径流过程的重要组成部分, 河湖水的重要补给来源, 对流域径流形成、水源涵养、养分运移等过程产生重要影响, 是水文学和土壤学及生态水文学的研究热点、难点与重要科学问题。文章分析发现1990—2020年中国壤中流的发文数量和被引频次均逐渐增多，研究方向主要集中在环境、工程、水资源以及农业等方面, 主题分布在紫色土、湿地、氮素等方面。壤中流形成的主要影响因素包括土壤、地形、植被、降雨等。壤中流的几种生态水文效应包括土壤养分运移效应、水土保持、径流调节、水文预报效应等。最后文章提出了目前壤中流研究中的一些局限性, 并对未来的研究重点进行了展望，为重要生态系统修复与水源涵养功能提升提供参考。
- 壤中流 /
- 土壤 /
- 降雨入渗 /
- 生态水文效应
Abstract: Water is an important basic resource for human survival and economic and social development. However, the water cycle has undergone profound changes under the dual influence of climate change and human activities. Subsurface flow, a key part of the runoff process and a major replenishment source for rivers and lakes, has a critical impact on runoff formation, water conservation, and nutrient transport. The understanding of subsurface flow processes is an important and popular topic in the fields of hydrology, soil science, and ecohydrology, however, it is a complex scientific problem that is difficult to disentangle. In this article, it was found that from 1990 to 2020, the number citation frequency of published articles related to subsurface flow in China have gradually increased. The researches mainly focused on the environment, engineering, water resources, and agriculture, focusing on topics such as purplish soil, wetlands, and nitrogen. In addition, we analyzed the main factors affecting subsurface flow formation, including soil, topography, vegetation, rainfall, etc. Furthermore, we summarized several ecological and hydrological effects of interflow, including the soil nutrient transport effect, soil and water conservation, runoff regulation, and hydrological forecasting effect. Finally, we highlighted some limitations in current research on interflow and discussed future research priorities, ultimately providing an important scientific basis for crucial ecosystem restoration and water conservation improvements.
- Subsurface flow /
- Soil /
- Rainfall infiltration /
- Eco-hydrological effect

HTML全文

图 1 1990—2020年Web of Science (a)和中国知网(b)检索的中国壤中流论文发表数量及被引频次变化趋势

Figure 1. Trends in the number and citation of the published papers about researches of subsurface flow of China in Web of Science (a) and CNKI (b) from 1990 to 2020

下载: 全尺寸图片幻灯片

图 2 1990—2020年中国知网(A)和Web of Science (B)壤中流研究的主要主题分布

Figure 2. Distribution of main themes of published papers on subsurface flow researches in CNKI (A) and Web of Science (B) from 1990 to 2020

下载: 全尺寸图片幻灯片

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