Abstract
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.
Highlights
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
While under the wet condition, only 21.5% of the area in the transect had DSL, this proportion increased to 47.0% under the dry condition
DSL mainly occurred in the central region of the transect
Summary
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. The formation of dry soil layer (DSL) is a global hydrological process that has been reported in China[1], Russia[2], Eastern Amazonia[3] and Southern Australia[4] It generally occurs in arid, semi-arid and semi-humid regions, mainly due to excessive depletion of deep soil water by vegetation, evapotranspiration and scarce precipitation recharge over a long time[5,6]. DSL can hamper water movement and exchange in the soil profile and can cause severe eco-hydrological problems This is a common occurrence in China’s Loess Plateau (CLP) region, where frequent water shortage and high soil erosion has made the ecosystem highly fragile[6,11,12]. Soil water can be replenished in temporary DSL conditions by precipitation[22,23]
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