Varied root effects on soil detachment with growth time and hydrodynamic characteristics

IF 2.8 3区 地球科学 Q2 GEOGRAPHY, PHYSICAL Earth Surface Processes and Landforms Pub Date : 2024-05-26 DOI:10.1002/esp.5839
Junyang Liu, Zhengchao Zhou, Hao Chen, Weixiao Han
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Abstract

Plant roots significantly reduce soil detachment by overland flow. However, there have been few studies on how plant growth time and hydrodynamic characteristics affect the erosion-reducing potential of plant roots. This study cultivated ryegrass (Lolium perenne L.) and alfalfa (Medicago sativa L.) as representative of plants possessing fibrous roots and taproots, respectively, in silty soil from the Loess Plateau, China. Root-soil composites were collected monthly from March to September 2021 and subjected to flow scouring in a hydraulic flume at a 15° slope using five different flow discharges (0.05, 0.1, 0.15, 0.2 and 0.3 L s−1). The results of the study indicated that root length density, root surface area density and root mass density exhibited a significant increase during the early growth phase, followed by a slight decrease. All parameters of fibrous roots revealed greater values than those of taproots, except for root mass density. The reduction in soil detachment under varying flow shear stresses showed a significant increase during the early phases of growth, followed by a gradual decline. Notably, fibrous roots demonstrated a greater impact on soil detachment than taproots, and this discrepancy fluctuated over time. Moreover, the contributions of fibrous and taproots to reducing soil detachment decreased from 55.81% to 39.66% and from 38.21% to 20.99% with increasing flow shear stress, respectively. It indicated that the erosion-reducing potential of plant roots was greater when subjected to low-flow shear stress compared to high-flow shear stress. This study can provide a scientific basis for understanding the erosion-reducing potential of plant roots at different growing stages and under varying hydrodynamic characteristics.

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根系随生长时间和水动力特性对土壤剥离的不同影响
植物根系可大大减少陆地水流对土壤的冲刷。然而,有关植物生长时间和水动力特性如何影响植物根系减少侵蚀潜力的研究却很少。本研究以黑麦草(Lolium perenne L.)和紫花苜蓿(Medicago sativa L.)为代表,分别在中国黄土高原的淤泥土壤中栽培具有须根和直根的植物。从 2021 年 3 月到 9 月,每月采集根-土复合材料,并在坡度为 15°的水槽中使用五种不同的流量(0.05、0.1、0.15、0.2 和 0.3 L s-1)进行水流冲刷。研究结果表明,根长密度、根表面积密度和根质量密度在生长初期显著增加,随后略有下降。除根质量密度外,须根的所有参数值都高于直根。在不同的流动剪切应力下,土壤剥离的减少量在生长初期显著增加,随后逐渐减少。值得注意的是,与直根相比,须根对土壤剥离的影响更大,而且这种差异随着时间的推移而波动。此外,随着流动剪应力的增加,须根和直根对减少土壤剥离的贡献率分别从 55.81% 降至 39.66%,从 38.21% 降至 20.99%。这表明,与高水流剪切应力相比,植物根系在低水流剪切应力下的侵蚀减少潜力更大。这项研究为了解植物根系在不同生长阶段和不同水动力特性下的侵蚀消减潜力提供了科学依据。
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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
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