Spatial and temporal distribution of potential vulnerability to wind erosion processes in Vojvodina

Wind erosion represents a significant type of degradation of arable agricultural soil. Natural and anthropogenic factors in Vojvodina are favourable for the occurance and development of intensive wind erosive processes. Along with the numerous causal factors of a complex process of wind erosion (rel...

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Main Authors: Savić Radovan, Letić Ljubomir, Benka Pavel, Ondrašek Gabrijel, Nikolić Vesna
Format: Article
Language:English
Published: University of Banja Luka - Faculty of Agriculture, Banja Luka 2012-01-01
Series:Agroznanje
Subjects:
Online Access:https://scindeks-clanci.ceon.rs/data/pdf/2233-0070/2012/2233-00701202191S.pdf
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author Savić Radovan
Letić Ljubomir
Benka Pavel
Ondrašek Gabrijel
Nikolić Vesna
author_facet Savić Radovan
Letić Ljubomir
Benka Pavel
Ondrašek Gabrijel
Nikolić Vesna
author_sort Savić Radovan
collection DOAJ
description Wind erosion represents a significant type of degradation of arable agricultural soil. Natural and anthropogenic factors in Vojvodina are favourable for the occurance and development of intensive wind erosive processes. Along with the numerous causal factors of a complex process of wind erosion (relief, climate, soil, vegetation, manner of land usage, land consolidation, etc.), the accent in this paper is especially on climate as an aggressive component of wind erosion processes. Primarily wind, and then precipitation and temperatures, i.e. unfavourable coincidence of the aforementioned climatic elements, directly or indirectly affects the potential occurence and development of wind erosion. Actual realization of the process, that is, forming of wind deposits, depends on all the other relevant factors. Based on unfavourable coincidence of climatic factors, one can distinguish areas and periods when the conditions of potential occurrence of wind erosion are at its most aggressive. It has been determined that, according to the climatic factors, the area of Banat is more endangered than other areas in Vojvodina (3 to 4 times more). The most intensive processes are possible in early spring (April) and in autumn (October), especially in extremely dry years.
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spelling doaj.art-ba30837dff9a4e53a9add30d14498e632024-04-16T13:30:17ZengUniversity of Banja Luka - Faculty of Agriculture, Banja LukaAgroznanje2233-00702012-01-0113219119810.7251/AGRSR1202191S2233-00701202191SSpatial and temporal distribution of potential vulnerability to wind erosion processes in VojvodinaSavić Radovan0https://orcid.org/0000-0002-9256-3139Letić Ljubomir1Benka Pavel2https://orcid.org/0000-0001-6229-5180Ondrašek Gabrijel3Nikolić Vesna4https://orcid.org/0000-0003-3393-9981Univerzitet u Novom Sadu, poljoprivredni fakultet, Departman za uređenje voda, Novi Sad, SerbiaUniverzitet u Beogradu, Šumarski fakultet, Beograd, SerbiaUniverzitet u Novom Sadu, poljoprivredni fakultet, Departman za uređenje voda, Novi Sad, SerbiaSveučilište u Zagrebu, Agronomski fakultet, Zagreb, HrvatskaUniverzitet u Beogradu, Šumarski fakultet, Beograd, SerbiaWind erosion represents a significant type of degradation of arable agricultural soil. Natural and anthropogenic factors in Vojvodina are favourable for the occurance and development of intensive wind erosive processes. Along with the numerous causal factors of a complex process of wind erosion (relief, climate, soil, vegetation, manner of land usage, land consolidation, etc.), the accent in this paper is especially on climate as an aggressive component of wind erosion processes. Primarily wind, and then precipitation and temperatures, i.e. unfavourable coincidence of the aforementioned climatic elements, directly or indirectly affects the potential occurence and development of wind erosion. Actual realization of the process, that is, forming of wind deposits, depends on all the other relevant factors. Based on unfavourable coincidence of climatic factors, one can distinguish areas and periods when the conditions of potential occurrence of wind erosion are at its most aggressive. It has been determined that, according to the climatic factors, the area of Banat is more endangered than other areas in Vojvodina (3 to 4 times more). The most intensive processes are possible in early spring (April) and in autumn (October), especially in extremely dry years.https://scindeks-clanci.ceon.rs/data/pdf/2233-0070/2012/2233-00701202191S.pdfwind erosionerosion factorsintensity of erosionsoil degradation
spellingShingle Savić Radovan
Letić Ljubomir
Benka Pavel
Ondrašek Gabrijel
Nikolić Vesna
Spatial and temporal distribution of potential vulnerability to wind erosion processes in Vojvodina
Agroznanje
wind erosion
erosion factors
intensity of erosion
soil degradation
title Spatial and temporal distribution of potential vulnerability to wind erosion processes in Vojvodina
title_full Spatial and temporal distribution of potential vulnerability to wind erosion processes in Vojvodina
title_fullStr Spatial and temporal distribution of potential vulnerability to wind erosion processes in Vojvodina
title_full_unstemmed Spatial and temporal distribution of potential vulnerability to wind erosion processes in Vojvodina
title_short Spatial and temporal distribution of potential vulnerability to wind erosion processes in Vojvodina
title_sort spatial and temporal distribution of potential vulnerability to wind erosion processes in vojvodina
topic wind erosion
erosion factors
intensity of erosion
soil degradation
url https://scindeks-clanci.ceon.rs/data/pdf/2233-0070/2012/2233-00701202191S.pdf
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AT leticljubomir spatialandtemporaldistributionofpotentialvulnerabilitytowinderosionprocessesinvojvodina
AT benkapavel spatialandtemporaldistributionofpotentialvulnerabilitytowinderosionprocessesinvojvodina
AT ondrasekgabrijel spatialandtemporaldistributionofpotentialvulnerabilitytowinderosionprocessesinvojvodina
AT nikolicvesna spatialandtemporaldistributionofpotentialvulnerabilitytowinderosionprocessesinvojvodina