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Use of an Integrated Approach for Assessing Soil Redistribution in the River Vorobzha Basin

机译:使用综合方法评估河流河流域河河河河

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Significant climate and crop rotation changes have taken place over the last few decades in the Central Chernozem zone of European i Russia. These have considerably influenced sediment redistribution rates within agricultural catchments. Quantitativeassessments of soil losses from cultivated lands and sediment redistribution intensity have been made using an integrated approach for typical catchments of Central Russia located near the city of Kursk in the River Vorobzha basin. Combined application of the caesium-137 (~(137)Cs) technique, erosion models, the soil morphological method and large-scale geomorphic mapping with detailed evaluation of the area of each typical morphological unit indicated that soil erosion rates on arable hill slopes decreased by about 1.5 times during the last 25 years (yr) compared with rates during the previous quarter century. Sediment delivery from cultivated fields into the River Vorobzha valley also decreased by up to three-fold over the same timeframes. The main reason for these changes was the considerably reduced surface runoff during the spring snowmelt period. In addition, the approach employed made it possible to quantify the effectiveness of soil conservation measures (SCMs) introduced within the small experimental sub-catchments occupying part of the study area. Application of SCMs reduced soil losses from cultivated fields by 2.5 times. Most of the eroded sediment and sediment-associated ~(137)Cs has been rede-posited within the cultivated fields and adjacent dry valley bottoms. It can be concluded that taking an integrated approach is the most appropriate strategyfor assessing soil degradation and determining both localized and off-site soil and nutrient sinks.
机译:在欧洲I俄罗斯中央Chernozem区的过去几十年中,已经发生了重大的气候和作物轮换变化。这些在农业集水区内的沉积物再分配率方面具有很大影响。使用俄罗斯中部典型集水区的综合方法制定了来自耕地和沉积物再分配强度的土壤损失的量化,位于Vorobzha河河河河河河河河克斯克市附近。铯-137(〜(137)CS)技术,腐蚀模型,土壤形态学方法和大型地貌测绘,对每个典型形态单位的面积进行详细评价的综合应用表明,耕地山坡上的土壤侵蚀率降低在过去的25年(YR)期间与前一季度世纪的比率约为1.5倍。从栽培领域进入Vorobzha山谷的沉积物递送也在相同的时间范围内降低了三倍。这些变化的主要原因是春季雪花期间的表面径流相当减少。此外,采用的方法使得可以量化在占据研究区域的小型实验小组中引入的土壤保护措施(SCM)的有效性。 SCM的应用减少了2.5次耕田的土壤损失。大多数侵蚀的沉积物和沉积物相关的〜(137)CS已经在耕地和相邻的干燥谷底部进行了重新定位。可以得出结论,采取综合方法是评估土壤退化和确定本地化和场外土壤和营养水池的最合适的策略。

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