中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Internal evaporation and condensation characteristics in the shallow soil layer of an oasis

文献类型:期刊论文

作者Ao, Yinhuan1; Han, Bo1; Lu, Shihua1; Li, Zhaoguo1,2
刊名THEORETICAL AND APPLIED CLIMATOLOGY
出版日期2016-07-01
卷号125期号:1-2页码:281-293
ISSN号0177-798X
DOI10.1007/s00704-015-1510-2
通讯作者Han, Bo(hanbo@lzb.ac.cn)
英文摘要The surface energy balance was analyzed using observations from the Jinta oasis experiment in the summer of 2005. A negative imbalance energy flux was found during daytime that could not be attributed to the soil heat storage process. Rather, the imbalance was related to the evaporation within the soil. The soil heat storage rate and the soil moisture variability always showed similar variations at a depth of 0.05 m between 0800 and 1000 (local standard time), while the observed imbalanced energy flux was very small, which implied that water vapor condensation occurred within the soil. Therefore, the distillation in shallow soil can be derived using reliable surface energy flux observations. In order to show that the importance of internal evaporation and condensation in the shallow soil layer, the soil temperatures at the depths of 0.05, 0.10, and 0.20 m were reproduced using a one-dimensional thermal diffusion equation, with the observed soil temperature at the surface and at 0.40 m as the boundary conditions. It was found that the simulated soil temperature improves substantially in the shallow layer when the water distillation is added as a sink/source term, even after the soil effective thermal conductivity has been optimized. This result demonstrates that the process of water distillation may be a dominant cause of both the temperature and moisture variability in the shallow soil layer.
收录类别SCI
WOS关键词ENERGY-BALANCE CLOSURE ; VADOSE ZONE ; HEAT-FLUX ; THERMAL-CONDUCTIVITY ; DEW DEPOSITION ; POROUS-MEDIA ; DESERT SOILS ; HYDROLOGIC BALANCE ; WATER TRANSPORT ; CLIMATE-CHANGE
WOS研究方向Meteorology & Atmospheric Sciences
WOS类目Meteorology & Atmospheric Sciences
语种英语
WOS记录号WOS:000378884600022
出版者SPRINGER WIEN
URI标识http://www.irgrid.ac.cn/handle/1471x/2557236
专题寒区旱区环境与工程研究所
通讯作者Han, Bo
作者单位1.Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, Key Lab Land Surface Proc & Climate Change Cold &, Lanzhou 730000, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
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GB/T 7714
Ao, Yinhuan,Han, Bo,Lu, Shihua,et al. Internal evaporation and condensation characteristics in the shallow soil layer of an oasis[J]. THEORETICAL AND APPLIED CLIMATOLOGY,2016,125(1-2):281-293.
APA Ao, Yinhuan,Han, Bo,Lu, Shihua,&Li, Zhaoguo.(2016).Internal evaporation and condensation characteristics in the shallow soil layer of an oasis.THEORETICAL AND APPLIED CLIMATOLOGY,125(1-2),281-293.
MLA Ao, Yinhuan,et al."Internal evaporation and condensation characteristics in the shallow soil layer of an oasis".THEORETICAL AND APPLIED CLIMATOLOGY 125.1-2(2016):281-293.

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来源:寒区旱区环境与工程研究所

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