Arid
DOI10.1007/s11368-017-1656-x
Spatial continuity and local conditions determine spatial pattern of dried soil layers on the Chinese Loess Plateau
Zhang, Chencheng1,2; Shao, Ming’an3; Jia, Xiaoxu3
通讯作者Shao, Ming’an ; Jia, Xiaoxu
来源期刊JOURNAL OF SOILS AND SEDIMENTS
ISSN1439-0108
EISSN1614-7480
出版年2017
卷号17期号:8页码:2030-2039
英文摘要

Purpose Many efforts of restoring vegetation have ignored the feedbacks between biotic and abiotic factors that have developed in water-limited ecosystem. Dried soil layers (DSLs) have formed extensively on the Chinese Loess Plateau (CLP). The objective of this study was to identify the primary factors controlling spatial pattern of DSLs on the CLP.


Materials and methods Two DSL indices (DSL thickness (DSLT) and soil water content in a DSL (DSL-SWC)) were estimated by measuring SWC to a depth of 5 m at 86 sites along a south-north transect on the CLP in 2013. The correlation between the spatial pattern of DSLs and environmental factors was determined with redundancy analysis (RDA).


Result and discussion DSLs had formed at most of the sites (66 of the 86 sites) along the transect. The sites without DSLs were primarily in an irrigated agricultural zone. DSLT was > 400 cm and generally increased from south to north, and DSL-SWC was 2.54% (v/v) in the semi-arid zone of the transect. The connected features of DSLs between connected neighboring sampling units exhibited a much wider extent. A total of nine environmental variables were the primary contributors to the spatial pattern of the DSLs, explaining approximately 47.3% of the variability. Local conditions were responsible for the higher proportion of explained variability than climatic factors. In addition, field capacity was the most important factor in all environmental factors, which may have influenced water-holding capacity.


Conclusion This study concludes that spatial continuity and local conditions determine the spatial pattern of DSLs at a regional scale. Understanding the characteristic of DSLs is useful for efficiency of vegetation restoration and soil water management.


英文关键词Dried soil layer Feedback Spatial continuity The Loess Plateau Water-limited region
类型Article
语种英语
国家Peoples R China
收录类别SCI-E
WOS记录号WOS:000405581200003
WOS关键词RESTORATION ECOLOGY ; WATER STORAGE ; COMMUNITY STRUCTURE ; TEMPORAL STABILITY ; SCALE ; MOISTURE ; VEGETATION ; VARIABILITY ; ECOSYSTEMS ; FEEDBACKS
WOS类目Environmental Sciences ; Soil Science
WOS研究方向Environmental Sciences & Ecology ; Agriculture
来源机构中国科学院地理科学与资源研究所 ; 西北农林科技大学
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/200803
作者单位1.Chinese Acad Sci & Minist Water Resources, Inst Soil & Water Conservat, State Key Lab Soil Eros & Dryland Farming Loess P, Yangling 712100, Shaanxi, Peoples R China;
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China;
3.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Ecosyst Network Observat & Modeling, Beijing 100101, Peoples R China
推荐引用方式
GB/T 7714
Zhang, Chencheng,Shao, Ming’an,Jia, Xiaoxu. Spatial continuity and local conditions determine spatial pattern of dried soil layers on the Chinese Loess Plateau[J]. 中国科学院地理科学与资源研究所, 西北农林科技大学,2017,17(8):2030-2039.
APA Zhang, Chencheng,Shao, Ming’an,&Jia, Xiaoxu.(2017).Spatial continuity and local conditions determine spatial pattern of dried soil layers on the Chinese Loess Plateau.JOURNAL OF SOILS AND SEDIMENTS,17(8),2030-2039.
MLA Zhang, Chencheng,et al."Spatial continuity and local conditions determine spatial pattern of dried soil layers on the Chinese Loess Plateau".JOURNAL OF SOILS AND SEDIMENTS 17.8(2017):2030-2039.
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