Abstract

The effects of water erosion (including long-term historical erosion and single erosion event) on soil properties and productivity in different farming systems were investigated. A typical sloping cropland with homogeneous soil properties was designed in 2009 and then protected from other external disturbances except natural water erosion. In 2012, this cropland was divided in three equally sized blocks. Three treatments were performed on these blocks with different simulated rainfall intensities and farming methods: (1) high rainfall intensity (1.5 - 1.7 mm min−1), no-tillage operation; (2) low rainfall intensity (0.5 - 0.7 mm min−1), no-tillage operation; and (3) low rainfall intensity, tillage operation. All of the blocks were divided in five equally sized subplots along the slope to characterize the three-year effects of historical erosion quantitatively. Redundancy analysis showed that the effects of long-term historical erosion significantly caused most of the variations in soil productivity in no-tillage and low rainfall erosion intensity systems. The intensities of the simulated rainfall did not exhibit significant effects on soil productivity in no-tillage systems. By contrast, different farming operations induced a statistical difference in soil productivity at the same single erosion intensity. Soil organic carbon (SOC) was the major limiting variable that influenced soil productivity. Most explanations of long-term historical erosion for the variation in soil productivity arose from its sharing with SOC. SOC, total nitrogen, and total phosphorus were found as the regressors of soil productivity because of tillage operation. In general, this study provided strong evidence that single erosion event could also impose significant constraints on soil productivity by integrating with tillage operation, although single erosion is not the dominant effect relative to the long-term historical erosion. Our study demonstrated that an effective management of organic carbon pool should be the preferred option to maintain soil productivity in subtropical red soil hilly region.

Highlights

  • Soil erosion, including tillage, wind, and water erosion, is a main type of soil degradation considered as a widespread natural geological phenomenon and a major factor causing the reduction of soil productivity and organic matter content [1,2,3,4]

  • The effects of water erosion including long-term historical erosion and a single rainfall–erosion event on soil properties and productivity in different farming systems in the subtropical red soil hilly region in south China were investigated

  • Our data showed that the effects of long-term historical erosion significantly explained most of the variation in soil productivity in no-tillage and tillage systems

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Summary

Introduction

Soil erosion, including tillage, wind, and water erosion, is a main type of soil degradation considered as a widespread natural geological phenomenon and a major factor causing the reduction of soil productivity and organic matter content [1,2,3,4]. More than two billion ha of biologically productive land have been irreversibly degraded since 1000 AD [3]. As global warming adversely affects the environment and extreme rainfall events frequently occur [6], soil erosion continuously poses environmental risks [7]. Soil erosion and its threat to the environment [4], to food security [8], should be addressed. Adverse effects of erosion on soil productivity have been identified and a qualitative consensus has been obtained [9,10]. The factors or mechanisms that determine the soil productivity reduction influenced by soil erosion in a small-scale spatio-temporal study have not been clearly elucidated [11]

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