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Title:Voda kot pedogenetski dejavnik v porečju Sotle
Authors:Prah, Klemen (Author)
Oddelek za geografijo, Filozofska fakulteta Univerze v Mariboru (Authorship owner)
Files:.pdf Revija_za_geografijo_2012_Prah_Voda_kot_pedogenetski_dejavnik_v_porecju_Sotle.pdf (577,91 KB)
 
URL http://www.ff.um.si/zalozba-in-knjigarna/ponudba/zbirke-in-revije/revija-za-geografijo/clanki/stevilka-7-1-2012/071-08_prah.pdf
 
Language:Slovenian
Work type:Scientific work (r2)
Typology:1.01 - Original Scientific Article
Organization:FL - Faculty of Logistic
Abstract:Prst nastaja in se razvija na stiku prepletanja in medsebojnega delovanja vseh sestavin pokrajine, tudi hidrosfere. Ugotoviti želimo, kako vodni viri v porečju Sotle vplivajo na značilnosti prsti, saj je poznavanje teh zakonitosti pomembno za usmerjanje rabe tal in s tem za varovanje prsti. V ta namen smo porečje Sotle razdelili v pet hidrografskih območij in jih primerjali glede na vodne in pedološke značilnosti ter pri tem upoštevali značilnosti rabe tal. Glavni poudarek smo dali metodi analize z GIS-i. Porečje Sotle leži ob slovensko-hrvaški meji in je izrazito asimetrično. Rečna mreža je gosta, prisotne pa so tudi številne stoječe vode. Od rabe tal prevladuje gozd, sledijo travniki in pašniki, njive, pozidana zemljišča, vinogradi, sadovnjaki, drevesa in grmičevje, mokrišča in barjanski travniki. Od prsti prevladujejo evtrične in distrične rjave, medtem ko hriboviti svet prekrivajo rendzine, rankerji in rjave pokarbonatne prsti. Vinogradniške lege označujejo rigolane prsti, v rečnih dolinah pa prevladujejo obrečne prsti na ilovnatem aluviju, oglejene in psevdooglejene prsti. Površinske vode, ki so v veliki meri podvržene človekovemu delovanju, imajo v porečju Sotle velik učinek na prsti, kar se odraža tudi v rabi zemljišč. Tako se v porečju Sotle pojavlja velik delež njivskih zemljišč, ki so najobsežnejša na holocenskih ravnicah ob Sotli, Mestinjščici in Bistrici, kjer prevladujejo hidromorfne prsti.
Keywords:geografija, vodni viri, prst, porečje Sotle
Year of publishing:2012
Number of pages:str. 81-87
Numbering:št. 1, Letn. 7
ISSN:1854-665X
UDC:551.435.1
ISSN on article:1854-665X
COBISS_ID:512475453 Link is opened in a new window
NUK URN:URN:SI:UM:DK:K6P8JSFK
Copyright:Oddelek za geografijo, Filozofska fakulteta Univerze v Mariboru
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Record is a part of a journal

Title:Revija za geografijo
Publisher:Oddelek za geografijo, Filozofska fakulteta Univerze v Mariboru
ISSN:1854-665X
COBISS.SI-ID:229718016 New window

Secondary language

Language:English
Title:Water as a pedogenetical factor in the river basin of Sotla
Abstract:Soil develops on the contact of all components of the landscape, including hydrosphere. We want to find out, how water resources in Sotla river basin contribute to soil characteristics. This knowledge is important for land use orientation and consequently for soil protection. For this purpose we studied Sotla river basin as region, which is divided on five hydrographical areas. We compared them according to water and pedological characteristics considering land use. The accent was on GIS methodology. Sotla river basin is located along Slovenian-Croatian border and is very asymmetric. The river network is very dense, present are also many standing waters. From land use predominate forests followed by grasslands, fields, built-up areas, vineyards, orchards, trees and bushes, swamps and marsh grasslands. From the soils predominate eutric and distric brown soils, in hills rendzina, ranker and brown soils on limestone. Vineyard sites cover anthropogenic soils. In river valleys are spread riverine soils on clay, gleyed and pseudogleyed soils. Surface waters in Sotla river basin are highly subjected to human act and have great influence on soils. That reflects in land use. It can be recognized in high percent of agriculture fields, the most extensive on holocen flat lands along rivers Sotla, Mestinjščica and Bistrica, where predominate hydromorfic soils.
Keywords:geography, water resources, soil, Sotla river basin


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This document is a part of these collections:
  1. Revija za geografijo

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