EVALUATION OF THE EFFECTS OF SOIL COMPACTION ON HYDROLOGY AND SOIL EROSION

土壤压实对水文和土壤侵蚀影响的评价

• 批准号: RGPIN-2014-05506
• 负责人: Gumiere, Silvio
• 金额: $ 1.89万
• 依托单位: Université Laval
• 依托单位国家: 加拿大
• 项目类别: Discovery Grants Program - Individual
• 财政年份: 2019
• 资助国家: 加拿大
• 起止时间: 2019-01-01 至 2020-12-31
• 项目状态: 已结题
• 来源: https://www.nserc-crsng.gc.ca/ase-oro/Details-Detailles_eng.asp?id=681483
• 关键词: EVALUATION; EFFECTS; SOIL; COMPACTION; HYDROLOGY

Soil compaction presents a major issue in modern day farming, and it is suspected that this process is to a large extent responsible for losses in productivity associated with yield reduction in precision agriculture. Commonly defined as the process by which soil grains are rearranged, soil compaction decreases the void between them and brings them into closer contact. The spatial extent of compacted soil is estimated at 68 million hectares worldwide, and in Europe alone soil compaction is responsible for the degradation of 33 million hectares of arable land. Similar problems have been reported in Canada and the USA.*Although compaction is viewed as one of the severest environmental problems in conventional agriculture, it is also the most difficult type of degradation to identify because the symptoms are not always apparent at the surface. Soil compaction reduces infiltration rates, which leads to increased runoff, enhanced erosion and loss of nutrients and pesticides to surface water. It is very well possible that the spatial distribution of compacted areas alters hydrological and sediment connectivity. In addition, reduced infiltration indirectly affects the efficiency of surface and subsurface drainage systems and increases flood risk. Therefore, in order to prevent damage and rehabilitate affected areas, it is essential to develop more advanced modeling tools, create mapping tools, and optimize tillage practices and agricultural machinery.*The long-term objective of the proposed research program is to increase our understanding of how the spatial distribution of soil compaction affects the hydrology and soil erosion at the watershed scale. Outcomes will provide a solid scientific support for improving regulatory government policies related to the application of beneficial management practices (BMPs), and establish methods of identifying contamination sources with better precision.*Short-term objectives of this research program are: (i) to increase our comprehension of the effects of soil compaction on runoff production and erosion at the scale of the soil pedon; (ii) to understand the spatially distributed impact of compacted areas on hydrological and sedimentological connectivity at the watershed scale; and (iii) based on the findings of objectives (i) and (ii), to develop a distributed water erosion model able to account for the effects of soil compaction on watershed hydrological and sedimentological connectivity.*These research program will significantly improve our understanding on how soil compaction contributes to changes in watershed hydrology. Addressing this issue is of paramount importance to ongoing agricultural and earth science research because very few studies to date have attempted to illustrate how soil compaction can influence diffuse and concentrated sediment and nutrient transport during storm events. Research of this topic is essential for developing management strategies in areas where sediment and nutrient losses are significant and present serious risks for the quality of surface waters. However, the manner in which connectivity and associated nutrient and sediment transport are modified by the process of soil compaction remains unclear and may be specific to each watershed. For Canada, Outcomes will provide a solid scientific support for improving regulatory government policies related to the application of (BMPs), and establish new methods for the identification of contamination sources of agricultural watersheds with better precision.

土壤压实是现代农业中的一个主要问题，人们怀疑这一过程在很大程度上导致了与精准农业产量下降相关的生产力损失。通常定义为土壤颗粒重新排列的过程，土壤压实减少了它们之间的空隙，使它们更紧密地接触。据估计，全世界压实土壤的空间范围为6 800万公顷，仅在欧洲，土壤压实就造成3 300万公顷可耕地的退化。加拿大和美国也报告了类似的问题。虽然压实被认为是传统农业中最严重的环境问题之一，但它也是最难识别的退化类型，因为症状并不总是在表面很明显。土壤压实降低了渗透率，导致径流增加，侵蚀加剧，养分和农药流失到地表水中。 压实区的空间分布很可能改变水文和沉积物的连通性。此外，渗透减少间接影响了地表和地下排水系统的效率，增加了洪水风险。因此，为了防止损害和恢复受影响地区，必须开发更先进的建模工具，创建绘图工具，并优化耕作方法和农业机械。拟议的研究计划的长期目标是增加我们的理解土壤压实的空间分布如何影响水文和土壤侵蚀在流域尺度。研究结果将为改善与有益管理实践（BMPs）应用相关的政府监管政策提供坚实的科学支持，并建立更精确地识别污染源的方法。本研究计划的短期目标是：（i）增加我们对土壤压实对土壤层径流产生和侵蚀的影响的理解;（ii）了解压实区域在流域尺度上对水文和沉积连通性的空间分布影响;以及（iii）根据目标（i）和（ii）的调查结果，开发一个能够说明土壤压实对流域水文和沉积连通性影响的分布式水蚀模型。这些研究计划将显着提高我们对土壤压实如何有助于流域水文变化的理解。解决这个问题是至关重要的，正在进行的农业和地球科学研究，因为很少有研究迄今已试图说明土壤压实如何影响扩散和集中的沉积物和养分运输在风暴事件。在沉积物和营养物流失严重并对地表沃茨质量构成严重威胁的地区，研究这一专题对于制定管理战略至关重要。然而，在土壤压实过程中，连接和相关的养分和沉积物运输的修改方式仍然不清楚，可能是具体到每个流域。对加拿大而言，成果项目将为改进与应用最佳管理计划（BMPs）有关的政府监管政策提供坚实的科学支持，并为更精确地确定农业流域污染源建立新的方法。