Abstract

The distribution of soil particle sizes is closely related to soil health condition. In this study, grasslands under different grazing intensities and different cultivation ages grasslands were selected to evaluate the dynamics of soil particle size redistribution in different soil layers. When the grazing intensity increased, the percentage of 2000~150-μm soil particles in the 0–10-cm soil layer decreased; 150~53-μm soil particles remained relatively stable among the grazing intensities—approximately 28.52%~35.39%. However, the percentage of less than 53-μm soil particles increased. In cultivated grasslands, the larger sizes (>53 μm) of soil particles increased and the smaller sizes (<53 μm) decreased significantly (p < 0.05) in the 0–10 cm-soil layer with increasing cultivation ages. The increase in small soil particles (<53 μm) in topsoil associated with grazing intensity increased the potential risk of further degradation by wind erosion. The increase in big soil particles (>53 μm) in topsoil associated with cultivation ages decreased the soil capacity of holding water and nutrient. Therefore, to maintain the sustainability of grassland uses, grazing grasslands need to avoid heavy grazing, and cultivated grasslands need to change current cultivation practices.

Highlights

  • Grasslands are the largest terrestrial landform in China, accounting for nearly 40% of the total land area [1]

  • When the grassland type changed from 10-year enclosure grassland (G10) to heavy grazing grassland (HG), the quantity of larger (>53 μm) soil particles decreased, and the quantity of smaller (

  • In the 10–60-cm soil layer, the percentage of 2000~250-μm soil particles underwent no significant change between moderate grazing grasslands (MG) and G10 but underwent a significant decrease from MG to HG (p < 0.05)

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Summary

Introduction

Grasslands are the largest terrestrial landform in China, accounting for nearly 40% of the total land area [1]. During the past half century, approximately 8 × 106 ha of native grasslands in China have been converted to croplands [2]. These different grassland uses affect soil nutrients, soil structure, and the distribution and stability of soil aggregates [3]. The fates of different grassland utilization methods are closely linked to the redistribution of soil particles, which regulates the states of the soil water, gas and heat [7,8]; affects the activity and type of soil microbes and other soil fauna [9,10]; and determines the nutrient levels of the soil [11].

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