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首页> 外文期刊>Bulletin of University of Agricultural Sciences and Veterinary Medicine Cluj-Napoca: Agriculture >Soil - Land Use Correlations in the Jijia Upper Catchment Focus on Land Degradation
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Soil - Land Use Correlations in the Jijia Upper Catchment Focus on Land Degradation

机译:积家上游流域的土壤-土地利用相关性以土地退化为中心。

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The distribution of zonal soils from Jijiaa€?s upper catchment is the result of the development in time of all soil forming and evolution processes. The problems regarding the soil cover and its capitalization become often a€?complicateda€?, being constantly subjected to the land use. For this paper, was used the methodology for establishing classes of land use based on the Romanian System of Soil Taxonomy (2012) nomenclature. Based on GIS software was conducted the assessment and classification, by statistical and spatial methods, of soil basic features in relation to the present land use. In terms of pedogenesis, Jijia upper catchment represents an area with high complexity in relation to the environmental variability. On the overall is confirmed the area-elevation distribution of the main types and soil classes, marking the transition from Chernisols (through Phaeozems) to Luvisols. For the entire basin, forested areas exceed the national average (36% of the studied zone), to these being added the territories under constructions that occupy considerable area (11%). Regarding the land used as arable (27%), it can be pointed out the strong capitalization of Chernisols (Chernozems and Phaeozems), including also those located on slope conditions. Uncontrolled extensions on stable terrains with high pedological potential creates an anthropogenic pressure on the soil background, the arable lands being specific also to some areas with soils less favorable (Luvisols, formed and evolved in the forest, but gradually taken into the agricultural utilization). Moreover, in this way it is noticed an incresead percent of territories affected by landslides and other current geomorphological processes.
机译:吉家河上游流域的地带性土壤分布是所有土壤形成和演化过程随时间发展的结果。关于土壤覆盖及其资本化的问题经常变得很复杂,并且经常受到土地利用的影响。在本文中,使用了基于罗马尼亚土壤分类法(2012)命名法建立土地利用类别的方法。基于GIS软件,通过统计和空间方法对与当前土地利用相关的土壤基本特征进行了评估和分类。就成岩作用而言,集家上游流域是一个相对于环境变化而言具有高度复杂性的地区。总体上可以确定主要类型和土壤类别的高程分布,标志着从切尔尼索尔(通过辉菌)到路维索尔的过渡。对于整个流域,森林面积超过了全国平均水平(占研究区域的36%),此外,这些森林还在建设中,占据了相当大的面积(11%)。关于可耕地(27%),可以指出切尔尼索尔(Chernozems和Phaeozems)的资本化能力强,包括那些位于斜坡条件下的土地。在具有高生态学潜力的稳定地形上不受控制的扩展会在土壤背景上造成人为压力,耕地也特定于某些土壤条件较差的地区(Luvisols在森林中形成和演化,但逐渐被农业利用)。此外,以这种方式注意到,受滑坡和其他当前地貌过程影响的领土比例增加了。

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