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dc.creatorKašanin-Grubin, Milica
dc.creatorHukić, Emira
dc.creatorBellan, Michal
dc.creatorBialek, Kamil
dc.creatorBosela, Michal
dc.creatorColl, Lluis
dc.creatorCzacharowski, Marcin
dc.creatorGajica, Gordana
dc.creatorGiammarchi, Francesco
dc.creatorGömöryová, Erika
dc.creatordel Rio, Miren
dc.creatorDinca, Lucian
dc.creatorĐogo Mračević, Svetlana
dc.creatorKlopčić, Matija
dc.creatorMitrović, Suzana
dc.creatorPach, Maciej
dc.creatorRanđelović, Dragana
dc.creatorRuiz-Peinado, Ricardo
dc.creatorSkrzyszewski, Jerzy
dc.creatorOrlić, Jovana
dc.creatorŠtrbac, Snežana
dc.creatorStojadinović, Sanja M.
dc.creatorTonon, Giustino
dc.creatorTosti, Tomislav
dc.creatorUhl, Enno
dc.creatorVeselinović, Gorica
dc.creatorVeselinović, Milorad
dc.creatorZlatanov, Tzvetan
dc.creatorTognetti, Roberto
dc.date.accessioned2022-02-21T10:41:25Z
dc.date.available2022-02-21T10:41:25Z
dc.date.issued2021
dc.identifier.issn0045-5067
dc.identifier.urihttp://cherry.chem.bg.ac.rs/handle/123456789/4840
dc.identifier.urihttp://cherry.chem.bg.ac.rs/handle/123456789/4891
dc.description.abstractForests in Europe are currently not endangered by soil erosion. However, this can change with climate change orwith intensified forest management practices. Using a newly established network of plots in beech forests across Europe,the aims of this study were to (i) distinguish soil properties and erodibility indices in relation to bedrock, (ii) determine geochemicalproperties and organic carbon (Corg) influencing erodibility, and (iii) assess the effect of soil depth on erodibilityindices. Seventy-six soil samples from 20 beech forests were collected in 11 countries to quantify soil properties influencingerodibility indices: clay ratio, modified clay ratio, sodium adsorption ratio, and oxides ratio. The results indicate that thedominant soil properties, determined by bedrock, that correlate with forest soil erodibility indices are Corg, pH, electricalconductivity, calcium and sodium ions concentrations, total water-soluble cations, and the percentage of sand. Accordingto the tested indices, soil susceptibility to erosion follows the order granite > andesite > sandstone > quartzite > limestone.Deeper soil horizons on granite are more susceptible to erosion than surface horizons are, but this is not the case forsoils on limestones. In conclusion, forest management should consider the predisposition of different soil types to erosion.
dc.publisherCanadian Science Publishing
dc.relationinfo:eu-repo/grantAgreement/MESTD/Basic Research (BR or ON)/176006/RS//
dc.relationinfo:eu-repo/grantAgreement/MESTD/Integrated and Interdisciplinary Research (IIR or III)/43009/RS//
dc.relationinfo:eu-repo/grantAgreement/MESTD/inst-2020/200026/RS//
dc.relationBulgarian National Science Fund (BNSF) via project No. DCOST 01/3/19.10.2018.
dc.relationMinistry of Civil Affairs of Bosnia and Herzegovina project No. 10-02- 2-1769/20-36.
dc.relation.isversionofhttps://cherry.chem.bg.ac.rs/handle/123456789/4841
dc.relation.isreferencedbyhttps://cherry.chem.bg.ac.rs/handle/123456789/4840
dc.rightsopenAccess
dc.sourceCanadian Journal of Forest Research
dc.subjectbedrock
dc.subjectenvironmental change
dc.subjecttexture
dc.subjectorganic matter
dc.subjectgeochemistry
dc.subjectCLIMO COST Action
dc.titleErratum: Soil erodibility in European mountain beech forests (Can. J. For. Res. 51, 12, 1846–1855, 2021, 10.1139/cjfr-2020-0361)
dc.typecontributionToPeriodicalen
dc.rights.licenseARR
dc.citation.volume51
dc.citation.issue12
dc.citation.spage1846
dc.citation.epage1855
dc.identifier.wos000740357500001
dc.identifier.doi10.1139/cjfr-2021-0347
dc.citation.rankM22~
dc.description.otherRelated to accepted version: [https://cherry.chem.bg.ac.rs/handle/123456789/4841]
dc.description.otherLink to the corrected article: [https://cherry.chem.bg.ac.rs/handle/123456789/4840]
dc.type.versionpublishedVersion
dc.identifier.scopus2-s2.0-85122812878


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