干旱区生态环境知识资源中心(Arid): The Soil Water Evaporation Process from Mountains Based on the Stable Isotope Composition in a Headwater Basin and Northwest China

Arid

DOI	10.3390/w12102711
	The Soil Water Evaporation Process from Mountains Based on the Stable Isotope Composition in a Headwater Basin and Northwest China
	Yong, Leilei; Zhu, Guofeng; Wan, Qiaozhuo; Xu, Yuanxiao; Zhang, Zhuanxia; Sun, Zhigang; Ma, Huiying; Sang, Liyuan; Liu, Yuwei; Guo, Huiwen; Zhang, Yu
通讯作者	Zhu, GF
来源期刊	WATER
EISSN	2073-4441
出版年	2020
卷号	12 期号:10
英文摘要	Soil water is a link between different water bodies. The study of soil water evaporation is of great significance to understand the regional hydrological process, promote environmental remediation in arid areas, and rationalize ecological water use. On the basis of soil water delta H-2 and delta O-18 data from April to October 2017 in the Xiying River basin in the upper reaches of the Qilian mountains, the lc-excess and Craig-Gordon model were applied to reflect the evaporating fractionation of soil water. The results show that the change in evaporation loss drives the enrichment of soil water isotopes. The signal of evaporative fractionation of soil water isotopes at different elevations has spatiotemporal heterogeneity. From the perspective of time dynamics, the evaporation loss of the whole region during the observation period was affected by temperature before July, while after July, it was controlled jointly by temperature and humidity, evaporation was weakened. Soil salt content and vegetation played an important role in evaporation loss. In terms of spatial dynamics, the soil moisture evaporation at the Xiying (2097 m) and Huajian (2390 m) stations in the foothills area is larger than that at the Nichan station (2721 m) on the hillside and Lenglong station (3637 m) on the mountain top. The surface soil water evaporation is strong, and the evaporation becomes weak with the increase of depth. The research has guiding significance for the restoration and protection of vegetation in arid areas and the formulation of reasonable animal husbandry policies.
英文关键词	Qilian Mountains stable isotope evaporation loss lc-excess Craig-Gordon model
类型	Article
语种	英语
开放获取类型	gold
收录类别	SCI-E
WOS记录号	WOS:000585301100001
WOS关键词	HYDROGEN ISOTOPES ; UNSATURATED ZONE ; MOISTURE ; OXYGEN ; FRACTIONATION ; DEUTERIUM ; BALANCE ; SURFACE ; O-18 ; PRECIPITATION
WOS类目	Environmental Sciences ; Water Resources
WOS研究方向	Environmental Sciences & Ecology ; Water Resources
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/327285
作者单位	[Yong, Leilei; Zhu, Guofeng; Wan, Qiaozhuo; Xu, Yuanxiao; Zhang, Zhuanxia; Sun, Zhigang; Ma, Huiying; Sang, Liyuan; Liu, Yuwei; Guo, Huiwen; Zhang, Yu] Northwest Normal Univ, Coll Geog & Environm Sci, Lanzhou 730070, Peoples R China; [Zhu, Guofeng] Gansu Engn Res Ctr Land Utilizat & Comprehens Con, Lanzhou 730070, Peoples R China
推荐引用方式 GB/T 7714	Yong, Leilei,Zhu, Guofeng,Wan, Qiaozhuo,et al. The Soil Water Evaporation Process from Mountains Based on the Stable Isotope Composition in a Headwater Basin and Northwest China[J],2020,12(10).
APA	Yong, Leilei.,Zhu, Guofeng.,Wan, Qiaozhuo.,Xu, Yuanxiao.,Zhang, Zhuanxia.,...&Zhang, Yu.(2020).The Soil Water Evaporation Process from Mountains Based on the Stable Isotope Composition in a Headwater Basin and Northwest China.WATER,12(10).
MLA	Yong, Leilei,et al."The Soil Water Evaporation Process from Mountains Based on the Stable Isotope Composition in a Headwater Basin and Northwest China".WATER 12.10(2020).