Temporal stability of surface soil moisture of different vegetation types in the Loess Plateau of China

CORC > 生态环境研究中心 > 中国科学院生态环境研究中心 > 城市与区域生态国家重点实验室

	Temporal stability of surface soil moisture of different vegetation types in the Loess Plateau of China
	Zhou, Ji; Fu, Bojie; Gao, Guangyao; Lu, Nan; Lu, Yihe; Wang, Shuai
刊名	CATENA
	2015-05
卷号	128 页码:1-15
关键词	Temporal stability Soil moisture Vegetation type Hydrological processes
英文摘要	The temporal stability of soil moisture (TSSM) was widely applied to optimize the soil moisture sampling scheme on a catchment or even larger spatial scale over wet and dry observational periods. However, the integration of the TSSM feature with specific hydrological response at a small plot scale has not been sufficiently researched. This study analyzed the temporal stability of surface soil moisture (0-10 cm) characteristics and corresponding influencing factors of different vegetation types under two typical soil moisture changing processes including wet-to-dry (WTD) and dry-to-wet (DTW), and determined the representative points. A total of 16 microplots (60 x 60 cm each) that were composed of three vegetation types containing Andropogon, Artemisia scoparia and Spiraea pubescens and bare land cover were selected. And the soil moisture in the central point (CP) and four ambient points (APs) of each microplot were measured during the WTD and DTW processes. The results showed that, 1) from DTW to WTD processes, the distribution of the soil water content in different vegetation types indicated a significant difference. Compared with the soil moisture in the AP or CP area of other vegetation types, the soil water content in tall shrub types (S. pubescens) was the lowest. 2) The autocorrelation coefficient indicated that both in the AP and CP areas, the soil moisture of the low shrub types (A. scoparia) had a higher temporal stability than that of other vegetation types. However, the soil water content in bare land had the highest temporal fluctuation from the DTW to WTD processes. Additionally, in the CP area, the TSSM of all the vegetation types tended to decrease during the WTD process. 3) Based on the TSSM analysis system that was derived from the principle of probability and statistics, the soil moisture in the low shrub types (A. scoparia) most likely provides the best representativeness of the spatial average soil water content of heterogeneous vegetation types. The determination of the representative soil moisture point via the hydrological-trait sampling method could be supplementary and significant for a TSSM study of the available soil water resources in an arid and semi-arid ecosystem. (C) 2015 Elsevier B.V. All rights reserved.
研究领域[WOS]	Geosciences, Multidisciplinary ; Soil Science ; Water Resources
WOS记录号	WOS:000351806600001
公开日期	2016-03-08
内容类型	期刊论文
源URL	[http://ir.rcees.ac.cn/handle/311016/32389]
专题	生态环境研究中心_城市与区域生态国家重点实验室
推荐引用方式 GB/T 7714	Zhou, Ji,Fu, Bojie,Gao, Guangyao,et al. Temporal stability of surface soil moisture of different vegetation types in the Loess Plateau of China[J]. CATENA,2015,128:1-15.
APA	Zhou, Ji,Fu, Bojie,Gao, Guangyao,Lu, Nan,Lu, Yihe,&Wang, Shuai.(2015).Temporal stability of surface soil moisture of different vegetation types in the Loess Plateau of China.CATENA,128,1-15.
MLA	Zhou, Ji,et al."Temporal stability of surface soil moisture of different vegetation types in the Loess Plateau of China".CATENA 128(2015):1-15.