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ORIGINAL RESEARCH article

Front. Environ. Sci.
Sec. Drylands
Volume 12 - 2024 | doi: 10.3389/fenvs.2024.1535193
This article is part of the Research Topic Drylands under the Influence of Climate Change and Human Activities View all 13 articles

Soil Porosity as a Key Factor of Soil Aggregate Stability: Insights from Restricted Grazing

Provisionally accepted
Yi Yang Yi Yang 1,2,3Zhongju Meng Zhongju Meng 1,2,3*Haonian Li Haonian Li 1,2,3Yue Gao Yue Gao 1,2,3Tianyang Li Tianyang Li 1,2,3Lei Qin Lei Qin 4
  • 1 College of Desert Control and Engineering, Inner Mongolia Agricultural University, Hohhot, China
  • 2 Key Laboratory of Aeolian Physics and Desertification Control Engineering from Inner Mongolia Autonomous Region, Hohhot, China
  • 3 Key Laboratory of Desert Ecosystem Conservation and Restoration, State Forestry and Grassland Administration of China, hohhot, China
  • 4 Water Conservancy Development Center of Inner Mongolia Ancient Autonomous Region, Hohhot, Inner Mongolia Autonomous Region, China

The final, formatted version of the article will be published soon.

    Overgrazing leads to steppe degradation and soil structure deterioration, which is common in desert steppes. Restricted grazing is a sustainable practice, but the mechanisms by which soil structure responds to restricted grazing have received little attention. This study examined the effects of two different grazing management strategies, namely restricted grazing and free grazing (CK), on soil structure indicators in the desert steppe. The restricted grazing further included grazing exclusion (GE) and seasonal grazing (SG). Additionally, a preliminary exploration was conducted to identify the main factors affecting the soil aggregate stability. Our results demonstrated that GE significantly increased clay (<0.002 mm) and silt (0.002-0.02 mm) in the 0-10 cm and 10-20 cm layers by an average of 71.27% and 70.64%, respectively. Additionally, SG significantly increased clay (<0.002mm), silt(0.002-0.02mm), and macroaggregates (>0.25mm) in the 0-10 cm layer. GE significantly increased soil organic carbon in the 0-10 cm and 10-20 cm layers by 7.02 g/kg and 7.45 g/kg, respectively. In addition, SG had no significant effect on soil organic carbon. The findings obtained from the computations using the enhanced regression tree (BRT) demonstrated that, within the study period, soil porosity significantly affects soil aggregate stability compared to other factors. Moreover, it possessed an average explanatory power that surpassed 45%. Overall, the soil structure is better under GE than under SG, and GE is the key to improving the soil structure of desert steppe. The research will contribute to a more profound comprehension of the impact of grazing on soil structure. Therefore, it is recommended that grazing closures be prioritized in desert grasslands to promote coordination between grassland restoration and livestock development.

    Keywords: Soil aggregate stability, Desert steppe, Soil Organic Carbon, Grazing exclusion, Soil porosity

    Received: 27 Nov 2024; Accepted: 27 Dec 2024.

    Copyright: © 2024 Yang, Meng, Li, Gao, Li and Qin. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) or licensor are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.

    * Correspondence: Zhongju Meng, College of Desert Control and Engineering, Inner Mongolia Agricultural University, Hohhot, China

    Disclaimer: All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article or claim that may be made by its manufacturer is not guaranteed or endorsed by the publisher.