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Permanent dry soil layer a critical control on soil desiccation on China’s Loess Plateau
by
Gongadze, Kate
, Shao, Ming’an
, Zhao, Chunlei
, Zhu, Yuanjun
, Jia, Xiaoxu
, Wu, Lianhai
in
631/158
/ 704/242
/ Desiccation
/ Ecosystem assessment
/ Ecosystems
/ Humanities and Social Sciences
/ Moisture content
/ multidisciplinary
/ Science
/ Science (multidisciplinary)
/ Soil degradation
/ Soil water
/ Water content
/ Water depth
2019
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Permanent dry soil layer a critical control on soil desiccation on China’s Loess Plateau
by
Gongadze, Kate
, Shao, Ming’an
, Zhao, Chunlei
, Zhu, Yuanjun
, Jia, Xiaoxu
, Wu, Lianhai
in
631/158
/ 704/242
/ Desiccation
/ Ecosystem assessment
/ Ecosystems
/ Humanities and Social Sciences
/ Moisture content
/ multidisciplinary
/ Science
/ Science (multidisciplinary)
/ Soil degradation
/ Soil water
/ Water content
/ Water depth
2019
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Permanent dry soil layer a critical control on soil desiccation on China’s Loess Plateau
by
Gongadze, Kate
, Shao, Ming’an
, Zhao, Chunlei
, Zhu, Yuanjun
, Jia, Xiaoxu
, Wu, Lianhai
in
631/158
/ 704/242
/ Desiccation
/ Ecosystem assessment
/ Ecosystems
/ Humanities and Social Sciences
/ Moisture content
/ multidisciplinary
/ Science
/ Science (multidisciplinary)
/ Soil degradation
/ Soil water
/ Water content
/ Water depth
2019
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Permanent dry soil layer a critical control on soil desiccation on China’s Loess Plateau
Journal Article
Permanent dry soil layer a critical control on soil desiccation on China’s Loess Plateau
2019
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Overview
The wide spread of dry soil layers (DSL) in China’s Loess Plateau region has negative effects on the ecosystem, including soil degradation and vegetation failure. To understand the temporal persistence of DSL, a ca. 860 km south-north transect was established and soil water content of the 0–5 m depth soil layer repeatedly measured for a period of four years. The results indicated that DSL varied with time and had a distribution area over 21.5–47.0% in the 860 km transect during the study period. The DSL could be divided into temporary and permanent types based on the length of period for which the soil remains dry. While temporary DSL is recoverable, permanent DSL (which existed in 47 out of 86 sites) was apparently unrecoverable as it persisted throughout the observation period. Permanent DSL was characterized by high temporal persistence, severe soil desiccation and thick dry layers; all of which suggested severe negative effect on the ecosystem. Non-climatic factors, rather than climate factors, contributed more to the formation of permanent DSL in the study area. Thus, it was suggested that policies and measures should be enacted to control especially permanent DSL formation in the region.
Publisher
Nature Publishing Group UK,Nature Publishing Group
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