多布罗斯洛维尼县可持续农业土壤理化性质研究

A. Stănilă
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引用次数: 0

摘要

研究区域位于Olt县的中西部,属于Caracal平原,西南部分的Leu-Rotunda油田很少,都是Romanati平原的分区。局部以低空平原为主,以冲积-洪积平原为特征,适度破碎,局部有阶地,覆盖着黄土样沉积物,但有碟状起伏。所研究领土的土壤覆盖是所有环境因素的直接反映,每一个因素都在成土过程中起作用。气候作为一个成土因子,由其组成部分,即:温度、降水、蒸散发、全球辐射起作用。森林草原植被是有机物质和生物量的供应,因为水文制度是缺乏的,但特别是岩性基质(黄土样复合体),以引导固化到cernisols类的特征类型。在环境因素和土成过程的影响下,多布罗斯洛维尼亚地区形成了种类繁多的土壤,即:原生土、石质土、腐质土和水解土。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Research on the Physico-Chemical Properties of Soils Locality Dobrosloveni, Olt County for Sustainable Agriculture
The studied territory located in the central-western part of Olt County, belongs to the Caracal Plain and extremely little in the Leu-Rotunda Field in the SW part, both as divisions of the Romanati Plain.Locality presents a predominant relief of plain low altitude that is characterized by alluvio-proluvial plains moderately fragmented with local terraces, covered with loess-like deposit but relief of saucer.The soil cover of the territory under study is the direct reflection of all environmental factors, each having a role in the pedogenetic processes. Climate, as a pedogenetic factor, acted by its components, namely: temperature, precipitation, evapotranspiration, global radiation.Forest steppe vegetation was the supply of organic matter and biomass, because the hydrological regime is deficient, but especially the lithological substrate (loess-like complex) to steer solification to types characteristic of the cernisols class.Under the influence of environmental factors and pedogenetic processes within the locality Dobrosloveni it formed a wide range of soils, namely: protisols, cernisols, luvisols and hydrisols.
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