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首页|期刊导航|灌溉排水学报|宁南黄土高原退耕还林(草)区包气带土壤水分运移特征及对降水的响应

宁南黄土高原退耕还林(草)区包气带土壤水分运移特征及对降水的响应

马玉学 杨凡 公亮 杨丽虎 吉卫波 孙变变 张晓东

灌溉排水学报2026,Vol.45Issue(1):35-44,10.
灌溉排水学报2026,Vol.45Issue(1):35-44,10.DOI:10.13522/j.cnki.ggps.2024391

宁南黄土高原退耕还林(草)区包气带土壤水分运移特征及对降水的响应

Characteristics of soil water flow in naturalized farmland and their response to rainfall in the Loess Plateau of South Ningxia

马玉学 1杨凡 2公亮 1杨丽虎 3吉卫波 1孙变变 1张晓东1

作者信息

  • 1. 宁夏回族自治区基础地质调查院(宁夏回族自治区地质矿产中心实验室),银川 750021
  • 2. 中国科学院地理科学与资源研究所/陆地水循环及地表过程重点实验室,北京 100101||中国科学院大学资源与环境学院,北京 100049
  • 3. 中国科学院地理科学与资源研究所/陆地水循环及地表过程重点实验室,北京 100101||中国科学院大学资源与环境学院,北京 100049||中国地质学会永定河下游地区自然资源监测技术创新基地,河北廊坊 065000
  • 折叠

摘要

Abstract

[Objective]The loess hilly region in southern Ningxia is ecologically fragile and naturalising farmland is a way to restore its ecological functions.While soil water is a key factor regulating ecosystem functions and stability,its response to rainfall in naturalised farmlands is not well understood.This paper investigates the spatiotemporal soil water dynamics and its response to rainfall in such ecosystems.[Method]Based on rainfall and soil moisture data measured from April to October 2023 in the vadose zone of a typical grassland(CD)and farmland(NT)in the southern Ningxia,we analysed the characteristics of soil water movement and their response to rainfall in the two ecosystems.[Result]① Light rainfall events only replenished the top 10 cm soil layer,while moderate rainfall events replenished the 0-30 cm soil layer.Under moderate rainfalls,noticeable soil moisture changes were observed mainly in the 10 cm and 30 cm layers in both ecosystems.② There were significant differences in the response time and magnitude of soil moisture change to rainfall events between the two ecosystems.The maximum average soil moisture content in NT and CD was in the 30 cm layer and the 10 cm layer,respectively.The effect of rainfall on soil moisture content dwindled as soil depth increased.③ Soil water balance analysis showed that the evapotranspiration of NT was significantly lower than that of CD,while its water percolation into deep soil was higher than that in CD.It was found that NT enhanced water infiltration into deep soil,thereby increasing groundwater recharge.[Conclusion]Our results unveiled the fundamental mechanisms underlying soil water movement in farmland and naturalised farmland in loess hilly region of southern Ningxia;they provide guidances for restoring the ecological functions of ecologically fragile areas in this region.

关键词

退耕还林(草)/土壤水运移/土壤水势/土壤水量平衡

Key words

the returned farmlands/soil water movement/soil potential/soil water balance

分类

农业科技

引用本文复制引用

马玉学,杨凡,公亮,杨丽虎,吉卫波,孙变变,张晓东..宁南黄土高原退耕还林(草)区包气带土壤水分运移特征及对降水的响应[J].灌溉排水学报,2026,45(1):35-44,10.

基金项目

宁夏自然科学基金项目(2023AAC03769) (2023AAC03769)

国家自然科学基金联合基金项目(U24A20571) (U24A20571)

宁夏生态地质调查示范项目(NXCZ20220201) (NXCZ20220201)

灌溉排水学报

1672-3317

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