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

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:
依托单位国家:
加拿大
项目类别:
Discovery Grants Program - Individual
财政年份:
2017
资助国家:
加拿大
项目状态:
已结题
起止时间:
2017-01-01 至 2018-12-31

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中文摘要
翻译
土壤压实是现代农业的一个主要问题,人们怀疑这一过程在很大程度上导致了精准农业中与产量减少相关的生产力损失。土壤压实通常被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面积为6800万公顷,仅在欧洲,土壤压实就造成了3300万公顷耕地的退化。类似的问题在加拿大和美国也有报道。虽然压实被视为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,因为表面上的症状并不总是很明显。土壤压实降低了入渗速率,从而导致径流增加,侵蚀加剧,营养物质和农药流失到地表水中。压实区域的空间分布很可能改变水文和沉积物的连通性。此外,入渗减少间接影响地表和地下排水系统的效率,增加洪水风险。因此,为了防止破坏和恢复受灾地区,必须开发更先进的建模工具,创建地图工具,优化耕作方法和农业机械。该研究计划的长期目标是增加我们对土壤压实的空间分布如何影响流域尺度上的水文和土壤侵蚀的理解。研究结果将为完善与有益管理实践(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)增加我们对土壤土壤压实对土壤土壤侵蚀和径流生产的影响的理解;(ii)在流域尺度上了解压实区对水文和沉积连通性的空间分布影响;(iii)基于目标(i)和(ii)的结果,开发一个能够解释土壤压实对流域水文和沉积连通性影响的分布式水侵蚀模型。这些研究项目将大大提高我们对土壤压实对流域水文变化的理解。解决这一问题对正在进行的农业和地球科学研究至关重要,因为迄今为止很少有研究试图说明土壤压实如何影响风暴事件期间弥散和集中的沉积物和营养物质的运输。在沉积物和养分损失严重并对地表水质量构成严重威胁的地区,研究这一主题对于制定管理战略至关重要。然而,连通性和相关的养分和沉积物运输如何被土壤压实过程所改变的方式尚不清楚,可能是每个流域特有的。对加拿大而言,成果将为改善与bmp应用相关的政府监管政策提供坚实的科学支持,并建立新的方法,以更精确地识别农业流域的污染源。
英文摘要
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.
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Mechanics of soil erosion by water: Mathematical modelling and laboratory experimentation
  • 批准号:
    RGPIN-2020-06271
  • 项目类别:
    Discovery Grants Program - Individual
  • 资助金额:
    $1.89万
  • 财政年份:
    2022
  • 负责人:
    Gumiere, Silvio
  • 依托单位:
Mechanics of soil erosion by water: Mathematical modelling and laboratory experimentation
  • 批准号:
    RGPIN-2020-06271
  • 项目类别:
    Discovery Grants Program - Individual
  • 资助金额:
    $1.89万
  • 财政年份:
    2021
  • 负责人:
    Gumiere, Silvio
  • 依托单位:
Irrigation de précision et gestion intégrée de l'eau en production de pommes de terre
  • 批准号:
    514551-2017
  • 项目类别:
    Collaborative Research and Development Grants
  • 资助金额:
    $14.5万
  • 财政年份:
    2021
  • 负责人:
    Gumiere, Silvio
  • 依托单位:
Mechanics of soil erosion by water: Mathematical modelling and laboratory experimentation
  • 批准号:
    RGPIN-2020-06271
  • 项目类别:
    Discovery Grants Program - Individual
  • 资助金额:
    $1.89万
  • 财政年份:
    2020
  • 负责人:
    Gumiere, Silvio
  • 依托单位:
国内基金
海外基金
Dynamic Credit Rating with Feedback Effects
  • 批准号:
    --
  • 项目类别:
    外国学者研究基金项目
  • 资助金额:
    --
  • 批准年份:
    2024
  • 负责人:
    Christian Martin Hilpert
  • 依托单位:
水环境中新兴污染物类抗生素效应(Like-Antibiotic Effects,L-AE)作用机制研究
  • 批准号:
    21477024
  • 项目类别:
    面上项目
  • 资助金额:
    86.0万元
  • 批准年份:
    2014
  • 负责人:
    李丹
  • 依托单位: