Abstract

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.

Highlights

  • Locality Dobrosloveni is among the regions nature and diversity of natural territorial complex components ensures optimum user to obtain agricultural production and income, the more they are exploited effectively, economically and environmentally existing technologies

  • Marls, sands and gravels appears at base of slopes of Teslui Valley

  • On the lands that have not been subjected to agricultural crops, we find elements of

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Summary

Introduction

Locality Dobrosloveni is among the regions nature and diversity of natural territorial complex components ensures optimum user to obtain agricultural production and income, the more they are exploited effectively, economically and environmentally existing technologies. A productive agriculture is essential prerequisite for sustainable development of agriculture with multiple objectives, improve livelihoods, with preserving and protecting the natural resource base. All this is not possible without special research, extensive and often lengthy. Withen the territory studied is presented formation, development, soils distribution, physical and geographical conditions, main physico-chemical properties of the soils, as well as agro-pedoameliorative works. Related to formation, development and distribution of soils in the territory, was intended at the outset how the appearance of each factor of the complex territorial analyzing on all the structure, dynamics and function of each of them, as their role directly or indirectly in the soils genesis

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