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Effects of thinning and understory removal on the soil water-holding capacity in Pinus massoniana plantations

Forest management practices play an important role in regulating the soil water-holding capacity of plantation. However, most studies focus on soil water dynamics present during large-scale forest loss and afforestation events, while little is known about how soil water under different forest manage...

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Autores principales: Wang, Ting, Xu, Qing, Gao, Deqiang, Zhang, Beibei, Zuo, Haijun, Jiang, Jing
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2021
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8219692/
https://www.ncbi.nlm.nih.gov/pubmed/34158581
http://dx.doi.org/10.1038/s41598-021-92423-5
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author Wang, Ting
Xu, Qing
Gao, Deqiang
Zhang, Beibei
Zuo, Haijun
Jiang, Jing
author_facet Wang, Ting
Xu, Qing
Gao, Deqiang
Zhang, Beibei
Zuo, Haijun
Jiang, Jing
author_sort Wang, Ting
collection PubMed
description Forest management practices play an important role in regulating the soil water-holding capacity of plantation. However, most studies focus on soil water dynamics present during large-scale forest loss and afforestation events, while little is known about how soil water under different forest management practices responds to rainfall events and which factors mainly regulate soil water-holding capacity. In this study, a stable hydrogen isotope was used to explore the contribution of three natural rainfall events (8.9, 13.3 and 67.7 mm) to soil water (CRSW) in a Pinus massoniana plantation under four forest management practices (no thinning (NTN), understory removal (USR), light-intensity thinning (LIT) and heavy-intensity thinning (HIT)) in the Three Gorges Reservoir Area of the Yangtze River Basin in China. Furthermore, a structural equation model was employed to determine the effects of vegetation biomass and soil properties on the CRSW. The results showed that plantation soil under different forest management practices exhibited different water-holding capacities. Following light (8.9 mm) and moderate (13.3 mm) rainfall events, the CRSW in the HIT stand was slightly higher than that in the other stands. Following heavy (66.7 mm) rainfall event, the CRSW of most layers in USR stand was not different from the other three stands, while the CRSW in the LIT and NTN stands was significantly higher than that in the HIT stand in the 0–100 cm soil layers, suggesting that soil in the LIT and NTN stands had a greater water-holding capacity than that in the HIT stand. In addition, soil properties were the main factors directly affecting the CRSW, explaining 60% and 37% of the variation in the CRSW on the first and seventh days after heavy rainfall, respectively. Overall, compared to the HIT stand, the LIT and NTN stands showed greater capacity in retaining rainwater. Therefore, under expected global changes with frequent occurrences of extreme precipitation events, methods involving light-intensity and no thinning should be employed to build up soil and water conservation functions, which will be critical for keeping water-holding capacity and moderating floods.
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spelling pubmed-82196922021-06-24 Effects of thinning and understory removal on the soil water-holding capacity in Pinus massoniana plantations Wang, Ting Xu, Qing Gao, Deqiang Zhang, Beibei Zuo, Haijun Jiang, Jing Sci Rep Article Forest management practices play an important role in regulating the soil water-holding capacity of plantation. However, most studies focus on soil water dynamics present during large-scale forest loss and afforestation events, while little is known about how soil water under different forest management practices responds to rainfall events and which factors mainly regulate soil water-holding capacity. In this study, a stable hydrogen isotope was used to explore the contribution of three natural rainfall events (8.9, 13.3 and 67.7 mm) to soil water (CRSW) in a Pinus massoniana plantation under four forest management practices (no thinning (NTN), understory removal (USR), light-intensity thinning (LIT) and heavy-intensity thinning (HIT)) in the Three Gorges Reservoir Area of the Yangtze River Basin in China. Furthermore, a structural equation model was employed to determine the effects of vegetation biomass and soil properties on the CRSW. The results showed that plantation soil under different forest management practices exhibited different water-holding capacities. Following light (8.9 mm) and moderate (13.3 mm) rainfall events, the CRSW in the HIT stand was slightly higher than that in the other stands. Following heavy (66.7 mm) rainfall event, the CRSW of most layers in USR stand was not different from the other three stands, while the CRSW in the LIT and NTN stands was significantly higher than that in the HIT stand in the 0–100 cm soil layers, suggesting that soil in the LIT and NTN stands had a greater water-holding capacity than that in the HIT stand. In addition, soil properties were the main factors directly affecting the CRSW, explaining 60% and 37% of the variation in the CRSW on the first and seventh days after heavy rainfall, respectively. Overall, compared to the HIT stand, the LIT and NTN stands showed greater capacity in retaining rainwater. Therefore, under expected global changes with frequent occurrences of extreme precipitation events, methods involving light-intensity and no thinning should be employed to build up soil and water conservation functions, which will be critical for keeping water-holding capacity and moderating floods. Nature Publishing Group UK 2021-06-22 /pmc/articles/PMC8219692/ /pubmed/34158581 http://dx.doi.org/10.1038/s41598-021-92423-5 Text en © The Author(s) 2021 https://creativecommons.org/licenses/by/4.0/Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/ (https://creativecommons.org/licenses/by/4.0/) .
spellingShingle Article
Wang, Ting
Xu, Qing
Gao, Deqiang
Zhang, Beibei
Zuo, Haijun
Jiang, Jing
Effects of thinning and understory removal on the soil water-holding capacity in Pinus massoniana plantations
title Effects of thinning and understory removal on the soil water-holding capacity in Pinus massoniana plantations
title_full Effects of thinning and understory removal on the soil water-holding capacity in Pinus massoniana plantations
title_fullStr Effects of thinning and understory removal on the soil water-holding capacity in Pinus massoniana plantations
title_full_unstemmed Effects of thinning and understory removal on the soil water-holding capacity in Pinus massoniana plantations
title_short Effects of thinning and understory removal on the soil water-holding capacity in Pinus massoniana plantations
title_sort effects of thinning and understory removal on the soil water-holding capacity in pinus massoniana plantations
topic Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8219692/
https://www.ncbi.nlm.nih.gov/pubmed/34158581
http://dx.doi.org/10.1038/s41598-021-92423-5
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