Runoff and sediment reduction effects of different Paspalum wettsteinii-planting measures on the slopes of Masson pine plantation in the red soil region of southern China

IF 2.8 3区 地球科学 Q2 GEOGRAPHY, PHYSICAL Earth Surface Processes and Landforms Pub Date : 2024-09-23 DOI:10.1002/esp.5959
Feihua Zhou, Ruibo Zha, Zehua Wu, Juan Wu, Qiang Lin, Jieling Wu, Liu Zhang, Liyuan Wang, Xuan Zha
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Abstract

Grass-planting measure is a crucial vegetation approach to mitigate understory soil erosion and improve ecological environment in the red soil region of southern China. This study aimed to quantify the effects of grass (Paspalum wettsteinii Hackel.)-planting measures on runoff and sediment reduction on slopes of Masson pine plantations under rainstorm conditions. We conducted a rainfall simulation experiment at a rainfall intensity of 2.0 mm/min, comparing single strip (MT1, strip spacing: 145 cm), double strips (MT2, strip spacing: 70 cm), and triple strips (MT3, strip spacing: 45 cm) grass-planting measures on slope surface runoff generation and soil erosion processes of the young Masson pine (MT0, no grass strip) plantation, and the bare slope (CK) was selected as the control. Results revealed that grass-planting measures significantly decreased slope erosion parameters compared to CK and MT0. As the average grass coverage increased (MT1 from 10% to 25%, MT2 from 7.5% to 22.5%, MT3 from 7.3% to 25%), the slope surface erosion parameters under the grass-planting measures decreased, resulting in significantly improved runoff and sediment reduction benefits. The runoff reduction effect could reach 32%, while the sediment reduction effect could reach 88%. Moreover, MT3 demonstrated superior performance over MT2 and MT1, with minimal runoff and sediment reduction effects observed for the MT0. Overall, this study suggests that grass-planting measures, coupled with the increasing of grass coverage rates, significantly improve runoff and sediment reduction benefits on slopes in regions experiencing heavy rainfall. Among the tested configurations, MT3 emerged as most effective measure for controlling understory soil erosion in Masson pine plantations, especially when its average grass coverage rate reached 25%. These findings provide valuable insights for selecting appropriate grass-planting strategies, as well as for understanding the underlying mechanisms of how these measures mitigate soil erosion. This scientific reference will aid in the design and implementation of soil and water conservation measures in the region.

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在中国南方红壤地区的马尾松种植园山坡上采用不同的覆盆子种植措施对减少径流和泥沙的影响
在中国南方红壤地区,植草措施是减轻林下水土流失、改善生态环境的重要植被措施。本研究旨在量化暴雨条件下马尾松种植园坡面植草措施对径流和泥沙减少的影响。我们在降雨强度为 2.0 毫米/分钟的条件下进行了降雨模拟实验,比较了单带(MT1,带间距:145 厘米)、双带(MT2,带间距:70 厘米)和三带(MT3,带间距:45 厘米)植草措施对幼年马松(MT0,无草带)种植园坡面径流产生和土壤侵蚀过程的影响,并选择裸坡(CK)作为对照。结果表明,与 CK 和 MT0 相比,植草措施显著降低了坡面侵蚀参数。随着平均植草覆盖率的增加(MT1 从 10% 增加到 25%,MT2 从 7.5% 增加到 22.5%,MT3 从 7.3% 增加到 25%),植草措施下的坡面侵蚀参数也随之降低,从而显著提高了径流和沉积物的减少效果。径流减少效果可达 32%,泥沙减少效果可达 88%。此外,MT3 的表现优于 MT2 和 MT1,而 MT0 的径流和泥沙减少效果则微乎其微。总之,这项研究表明,在暴雨地区的斜坡上,植草措施与提高草覆盖率相结合,可显著提高径流和泥沙减少效果。在测试的配置中,MT3 是控制马松种植园林下土壤侵蚀最有效的措施,尤其是当其平均植草覆盖率达到 25% 时。这些发现为选择适当的植草策略以及了解这些措施如何减轻土壤侵蚀的内在机制提供了宝贵的见解。这一科学参考资料将有助于该地区水土保持措施的设计和实施。
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来源期刊
Earth Surface Processes and Landforms
Earth Surface Processes and Landforms 地学-地球科学综合
CiteScore
6.40
自引率
12.10%
发文量
215
审稿时长
4 months
期刊介绍: Earth Surface Processes and Landforms is an interdisciplinary international journal concerned with: the interactions between surface processes and landforms and landscapes; that lead to physical, chemical and biological changes; and which in turn create; current landscapes and the geological record of past landscapes. Its focus is core to both physical geographical and geological communities, and also the wider geosciences
期刊最新文献
Morphology and dynamics of thermokarst ponds in a subarctic permafrost peatland, northern Sweden Issue Information Runoff and sediment reduction effects of different Paspalum wettsteinii-planting measures on the slopes of Masson pine plantation in the red soil region of southern China Holocene hillslope evolution through extreme rainfall induced landslides in the mountainous region of Rio de Janeiro, Brazil: Geochronology and paleoenvironmental evidence Issue Information
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