Abstract

Raindrops disperse large soil aggregates into smaller particles, which can clog soil pores, cause soil crusting, reduce rainfall infiltration and increase soil loss. It was found that natural polymer derivatives were effective in improving soil physical properties and decreasing soil erosion on an experimental loess hillslope. This study investigated the effect of new natural polymer derivatives (Jag S and Jag C162) on soil properties, rainfall infiltration and sediment yield at four rates of sprayed polymers (0, 1, 3 and 5 g/m2), three rainfall intensities (1, 1.5 and 2 mm/min) and a slope gradient of 15° with a silt loam soil through simulated rain. The results showed that both Jag S and Jag C162 significantly increased the shear strength and improved the aggregates composition of the soil surface. The water-stable soil aggregates >0.25 mm increased from 9% to 50% with increasing rates of Jag S and Jag C162. Jag S and Jag C162 also effectively increased rainfall infiltration and final infiltration rate, and reduced erosion compared to controls without natural polymer derivatives added. However, higher rates of Jag S produced lower infiltration rates. Although both Jag S and Jag C162 effectively influenced soil physical properties and erosion, the effect of Jag C162 was more significant than that of Jag S.

Highlights

  • Drought and soil erosion are two environmental problems on loess hillslopes

  • The results indicated that the amendment applications could decrease the erosive forces of raindrops, increase the water-stable soil aggregates contents, reduce surface crusting and improve rainfall infiltration

  • The objectives of this research were to: (i) determine the effects of Jag S and Jag C162, two new natural polymer derivatives, at different rates on soil loss and rainfall infiltration; (ii) reveal the mechanisms responsible for their effects by analyzing the proportions of water-stable soil aggregates of different sizes and shear strength after Jag S and Jag C162 were spread under simulated rainfall on experimental loess hillslope

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Summary

Introduction

Crust formation at the surface of cultivated soils exposed to the impact of raindrops is a common phenomenon, which is formed by the combined effect of physical disintegration of soil aggregates on the surface by the impact energy of raindrops and physicochemical dispersion of soil clays. It can disperse cultivated soils aggregates into micro-aggregates, reduce infiltration rate and increase runoff and erosion [1,2,3], which causes negative effects on the survival and growth of plants in arid and semiarid regions. Public Health 2018, 15, 9; doi:10.3390/ijerph15010009 www.mdpi.com/journal/ijerph

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