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Research Article

Hydrological responses of pine needle litter to rainfall erosional processes on Chinese karst hillslopes

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Received 26 May 2023, Accepted 08 Apr 2024, Accepted author version posted online: 29 Apr 2024
 
Accepted author version

Abstract

Native vegetation restoration, such as pines, is an effective measure for mitigating soil erosion. However, the impact of pine needle litter on runoff, soil erosion, and hydrological responses on karst hillslopes remains unclear. This study investigated these factors during the rainy season from June to August 2021 under six distinct treatments (flat, gentle, and steep slopes with and without pine needle coverings). The results showed that pine needle litter significantly increased the soil water content, particularly on steeper slopes, by improving the water-holding capacity. It also substantially reduced runoff (by 23.8%) and soil erosion (by 92.5%). The critical rainfall threshold for generating runoff did not occur in the pine needle covering treatment, whereas it was 19.3 ± 8.8 mm in the bare soil treatment under wet conditions. These findings highlight the efficacy of pine needle cover in mitigating runoff and soil erosion in karst areas, suggesting it as a sustainable alternative against erosion, and underscoring the importance of pine plantations in degraded soil restoration efforts.

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As a service to authors and researchers we are providing this version of an accepted manuscript (AM). Copyediting, typesetting, and review of the resulting proofs will be undertaken on this manuscript before final publication of the Version of Record (VoR). During production and pre-press, errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal relate to these versions also.

Supplementary material

Supplemental data for this article can be accessed online at https://doi.org/10.1080/02626667.2024.2349261.

Disclosure statement

No potential conflict of interest was reported by the authors.

Additional information

Funding

We acknowledge and are grateful for the financial support provided by the National Natural Science Foundation of China through grant no. 42067004, Guizhou Provincial Science and Technology Foundation (YQK[2023]005), and China Scholarship Council.

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