THE SOIL – FORMING PROCESSES THAT CONTRIBUTED TO THE FORMATION AND EVOLUTION OF THE SOILS FROM THE PICIOR DE MUNTE PLAIN
Journal Title: The Annals of Valahia University of Târgoviste, Geographical Series - Year 2007, Vol 7, Issue 1
Abstract
Inside the Picior de Munte Plain, the bioaccumulation, eluviation-illuviation, specific weathering, gleyzation-stagnation-gleyzation and vertic processes had a very important role in the formation of soil cover. The bioaccumulation is a general process, characteristical for all the soils. The eluviation -illuviation processes determined the formation of the albic luvosols, that are very spread inside the Picior de Munte Plain. Weathering is a general process, that takes part in all the soils formation. But there are some cases when the weathering leads to the formation of some specific horizons, like the B cambic horizon (Bv), characteristical for typical eutricambosols and alluvic eutricambosols.. The gleyzation and stagno-gleyzation processes are typical for the gleysols in the rivers plains and for the stagno-sols formed on the clayey lands, with global imperfect drainage. The vertic processes are typical for the soils formed on clayey layings with swelling character, such as (in the researched area) the vertic subtypes of the soils in the luvisols class.
Authors and Affiliations
Stefan ISPAS
Keywords
Related Articles
- EP ID EP143427
- DOI -
- Views 92
- Downloads 0
THE TYPOLOGY OF THE HUMAN SETTLEMENTS FROM DÂMBOVIŢA VALLEY IN THE AREA OF HIGH SUB-MOUNTAINOUS PLAIN
The area under analysis is situated in the center of Dâmboviţa County, its relief being that of high sub-mountainous plain, with a protecting temperate-continental climate and fertile soils that favored the develop...
SOIL MOISTURE RATIO AND VARIOUS DEPTHS, PÅTÂRLAGELE STATION AREA, BUZĂU SUBCARPATHIANS
THE CHLORIDE MINERAL WATERS FROM THE GLODENI LOCALITY, DÂMBOVIŢA
The geotehtonic evolution of the internal extended depression situated in-between the mountains and the plateau area, along the lower Miocene deposits allow to create the hydrogeological conditions who forms the mi...
ACTUAL AND PROSPECTIVE SOCIO-ECONOMIC ELEMENTS CONCERNING EUROPEAN TOURISM
Tourism represents, both for its content and for its role, a phenomenon that has become widely spread during the contemporary period, its spectacular development being a characteristic feature of the present centur...
THE PRESENT-DAY MODELLING PROCESSES IN THE CÂNDESTI PIEDMONT