Arid
DOI10.1002/hyp.14397
Vertical variations and transport mechanism of soil moisture in response to vegetation restoration on the Loess Plateau of China
Qiu, Dexun; Gao, Peng; Mu, Xingmin; Zhao, Baili
通讯作者Gao, P ; Mu, XM (corresponding author), Chinese Acad Sci & Minist Water Resources, Inst Soil & Water Conservat, Yangling 712100, Shaanxi, Peoples R China.
来源期刊HYDROLOGICAL PROCESSES
ISSN0885-6087
EISSN1099-1085
出版年2021
卷号35期号:10
英文摘要Soil moisture is essential for vegetation restoration in arid and semi-arid regions. Ascertaining the vertical distribution and transportation of soil moisture under different vegetation types has a profound effect on the ecological construction. In this study, the soil moisture at a depth of 500 cm for four typical vegetation types, including Robinia pseudoacacia, Caragana korshinskii, Stipa bungeana, and corn, were investigated and compared in the Zhifanggou watershed of the Loess plateau. Additionally, hydrogen and oxygen stable isotopes were detected to identify the transport mechanism of soil moisture. The results showed vertical distribution and transportation of soil moisture were different under different vegetation types. Depth-averaged soil moisture under S. bungeana and corn generally increased along the profile, while C. korshinskii and R. pseudoacacia showed weakly increasing and relatively stable after an obvious decreasing trend (0-40 cm). The soil moisture under R. pseudoacacia was lower than that under other vegetation types, especially in deep layer. However, the effect of R. pseudoacacia on soil moisture in the topsoil (< 30 cm) could be positive. For R. pseudoacacia (160-500 cm), C. korshinskii (0-500 cm), and S. bungeana (0-100 cm), the soil moisture declined with increased in vegetation age. Planting arbor species such as R. pseudoacacia intensified the decline of soil moisture on the Loess Plateau. The capacity of evaporation fractionation of soil moisture followed the sequence: corn > S. bungeana > R. pseudoacacia > C. korshinskii. The delta O-18 values in soil water fluctuated across the profile. The delta O-18 values changed sharply in upper layer and generally remained stable in deep layer. However, in middle layer, the vertical distribution characteristics of the delta O-18 values were different under different vegetation types. We estimated that piston flow was the main mode of precipitation infiltration, and the occurrence of preferential flow was related to vegetation types. These results were helpful to improve the understanding of the response of deep soil moisture to vegetation restoration and inform practices for sustainable water management.
英文关键词hydrogen and oxygen stable isotopes Loess Plateau soil moisture vegetation restoration
类型Article
语种英语
收录类别SCI-E
WOS记录号WOS:000711813100007
WOS关键词WATER CONSERVATION ; GULLY REGION ; YELLOW-RIVER ; PATTERNS ; O-18 ; DYNAMICS ; DEUTERIUM ; DEPLETION ; DROUGHT ; ISOTOPE
WOS类目Water Resources
WOS研究方向Water Resources
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/373655
作者单位[Qiu, Dexun; Gao, Peng; Mu, Xingmin; Zhao, Baili] Chinese Acad Sci & Minist Water Resources, Inst Soil & Water Conservat, State Key Lab Soil Eros & Dryland Farming Loess P, Yangling, Shaanxi, Peoples R China; [Gao, Peng; Mu, Xingmin; Zhao, Baili] Northwest A&F Univ, Inst Soil & Water Conservat, State Key Lab Soil Eros & Dryland Farming Loess P, Yangling, Shaanxi, Peoples R China; [Qiu, Dexun; Gao, Peng; Mu, Xingmin] Univ Chinese Acad Sci, Coll Adv Agr Sci, Beijing, Peoples R China
推荐引用方式
GB/T 7714
Qiu, Dexun,Gao, Peng,Mu, Xingmin,et al. Vertical variations and transport mechanism of soil moisture in response to vegetation restoration on the Loess Plateau of China[J],2021,35(10).
APA Qiu, Dexun,Gao, Peng,Mu, Xingmin,&Zhao, Baili.(2021).Vertical variations and transport mechanism of soil moisture in response to vegetation restoration on the Loess Plateau of China.HYDROLOGICAL PROCESSES,35(10).
MLA Qiu, Dexun,et al."Vertical variations and transport mechanism of soil moisture in response to vegetation restoration on the Loess Plateau of China".HYDROLOGICAL PROCESSES 35.10(2021).
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