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DOI | 10.1007/s10040-021-02372-6 |
Evolution of soil-water states in the vadose zone of a desert soil after an extreme rainfall event and its impact on the ecosystem | |
Zhou, Hong; Zhao, Wen Zhi | |
通讯作者 | Zhao, WZ (通讯作者),Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, Key Lab Inland River Basin Ecohydrol, Linze Inland River Basin Res Stn, Lanzhou 730000, Peoples R China. |
发表日期 | 2021 |
ISSN | 1431-2174 |
EISSN | 1435-0157 |
起始页码 | 2127 |
结束页码 | 2147 |
卷号 | 29期号:6 |
英文摘要 | Evolution of soil-water movement patterns following rare and extreme rainfall events in arid climates is not well understood, but it has significant effects on water availability for desert plants and on the hydrological cycle at small scale. Here, field data and the Hydrus-1D model were used to simulate the mechanisms of soil water and vapor transport, and the control factors associated with temporal variability in the soil water and temperature were analyzed. The results showed that thermal vapor transport with a no rainfall scenario determined daily variability in water content at the soil surface. During rainfall, isothermal liquid water fluctuated as a result of dry sandy soils and matric potential in the upper soil (0-25 cm), and thermally driven vapor played a key role in soil-water transport at 40-60 cm soil depth. After an extreme rainfall event, thermal vapor flux increased and accounted for 11.8% of total liquid and vapor fluxes in daytime with a steep temperature gradient; this was very effective in improving long-term soil-water content after the rain. The simulated results revealed that thermal water vapor greatly contributed to the soil-water balance in the vadose zone of desert soil. This study provided an alternative approach to describing soil-water movement processes in arid environments, and it increased understanding of the availability of water for a desert plant community. |
关键词 | VAPOR MOVEMENTHALOXYLON-AMMODENDRONHEAT-TRANSPORTPOROUS-MEDIALIQUID WATEREVAPORATIONOASISDIFFUSIONFLOWRESPONSES |
英文关键词 | Unsaturated zone; Liquid water and water vapor movement; Rainfall; Desert system; Hydrus-1D |
语种 | 英语 |
WOS研究方向 | Geology ; Water Resources |
WOS类目 | Geosciences, Multidisciplinary ; Water Resources |
WOS记录号 | WOS:000661401100001 |
来源期刊 | HYDROGEOLOGY JOURNAL |
来源机构 | 中国科学院西北生态环境资源研究院 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/253717 |
作者单位 | [Zhou, Hong] Northwest Normal Univ, Coll Tourism, Lanzhou 730070, Peoples R China; [Zhou, Hong; Zhao, Wen Zhi] Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, Key Lab Inland River Basin Ecohydrol, Linze Inland River Basin Res Stn, Lanzhou 730000, Peoples R China |
推荐引用方式 GB/T 7714 | Zhou, Hong,Zhao, Wen Zhi. Evolution of soil-water states in the vadose zone of a desert soil after an extreme rainfall event and its impact on the ecosystem[J]. 中国科学院西北生态环境资源研究院,2021,29(6). |
APA | Zhou, Hong,&Zhao, Wen Zhi.(2021).Evolution of soil-water states in the vadose zone of a desert soil after an extreme rainfall event and its impact on the ecosystem.HYDROGEOLOGY JOURNAL,29(6). |
MLA | Zhou, Hong,et al."Evolution of soil-water states in the vadose zone of a desert soil after an extreme rainfall event and its impact on the ecosystem".HYDROGEOLOGY JOURNAL 29.6(2021). |
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