Influence of crop rotation, irrigation, fertilization, and tillage on the aggregate property and soil wind erosion potential in the floodplain of the Yellow River

IF 3.1 3区 地球科学 Q2 GEOGRAPHY, PHYSICAL Aeolian Research Pub Date : 2024-04-25 DOI:10.1016/j.aeolia.2024.100925
Huawei Pi , Xiuli Zhang , Sisi Li , Nicholas P. Webb
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Abstract

The floodplain of the Yellow River (FPYR) is threatened by severe soil erosion. Soils are often susceptible to wind erosion owing to their coarse-textures and weak aggregation, yet studies are yet to describe the ability of soils to resist wind erosion in this region. Accordingly, this study aimed to quantify how soil wind erosion potential is affected by soil aggregate properties, such as dry aggregate geometric mean diameter (GMD), aggregate geometric standard deviation (GSD), aggregate stability, and soil bulk density, and to assess the effects of soil type, crop rotation, irrigation, fertilization, and tillage treatments on these aggregate properties in the main wind erosion area across the FPYR. Significant differences in GMD and aggregate stability were found between crop rotation treatments, whereas crop rotation marginally affected the soil bulk density. Further, the impact of management practices on aggregate properties differed for each soil type. The soil aggregate erodible fraction (EF) in the FPYR ranged from 1.14 to 82.73% across sites, with a mean of 26.14% across soil types and management practices, which was lower than that previously reported in other wind erosion regions. We incorporated these measured EFs into the Revised Wind Erosion Equation (RWEQ) to evaluate the wind erosion risk of the FPYR. The results indicated that the central FPYR was more susceptible to wind erosion than the other regions, although the total wind erosion potential in the FPYR was small. Adoption of soil conservation practices could help minimize wind erosion and improve atmospheric quality in the region.

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轮作、灌溉、施肥和耕作对黄河冲积平原集料性质和土壤风蚀潜力的影响
黄河泛滥平原(FPYR)受到严重水土流失的威胁。由于土壤质地粗、聚集性弱,通常容易受到风力侵蚀,但有关该地区土壤抵御风力侵蚀能力的研究尚不多见。因此,本研究旨在量化土壤风蚀潜力如何受到干集料几何平均直径(GMD)、集料几何标准偏差(GSD)、集料稳定性和土壤容重等土壤集料特性的影响,并评估整个山南地区主要风蚀区的土壤类型、轮作、灌溉、施肥和耕作处理对这些集料特性的影响。结果发现,不同轮作处理之间的全球降水量和集料稳定性存在显著差异,而轮作对土壤容重的影响微乎其微。此外,每种土壤类型的管理方法对骨料特性的影响也不尽相同。青藏高原各地点的土壤团聚体可侵蚀率(EF)从 1.14% 到 82.73% 不等,不同土壤类型和管理措施的平均值为 26.14%,低于其他风蚀地区的报告值。我们将这些测得的 EF 值纳入修订的风蚀方程 (RWEQ),以评估该地区的风蚀风险。结果表明,与其他地区相比,山南地区中部更容易遭受风蚀,尽管山南地区的总风蚀潜力很小。采用水土保持措施有助于最大限度地减少风蚀,改善该地区的大气质量。
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来源期刊
Aeolian Research
Aeolian Research GEOGRAPHY, PHYSICAL-
CiteScore
7.10
自引率
6.10%
发文量
43
审稿时长
>12 weeks
期刊介绍: The scope of Aeolian Research includes the following topics: • Fundamental Aeolian processes, including sand and dust entrainment, transport and deposition of sediment • Modeling and field studies of Aeolian processes • Instrumentation/measurement in the field and lab • Practical applications including environmental impacts and erosion control • Aeolian landforms, geomorphology and paleoenvironments • Dust-atmosphere/cloud interactions.
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