A. Michno, K. Wasak, M. Stolarczyk, D. Strzyżowski, Dominika Wrońska-Wałach, J. Fidelus, M. Sobucki, M. Żelazny
{"title":"Wpływ wiatrowałów na zróżnicowanie cech osadów aluwialnych w dolinach tatrzańskich o różnym stopniu wylesienia","authors":"A. Michno, K. Wasak, M. Stolarczyk, D. Strzyżowski, Dominika Wrońska-Wałach, J. Fidelus, M. Sobucki, M. Żelazny","doi":"10.12657/LANDFANA.031.003","DOIUrl":null,"url":null,"abstract":": The aim of the research was to recognize the diversity of the textural and chemical characteristics of the sedi - ments removed from the catchments of the Tatra Mts., which were affected by the windthrow event in 2013. The diver sity was related to the morphometry of the catchments and the effects of the windthrow event. In catchments sediments deposited during low transport dynamics dominated, two of the catchments were characterized by some percentage (up to 10%) of the sediments deposited in the high-energy environment. However, this diversity is connected to the mor - phometry of the studied catchments and up to this time impact of the windthrows is not clearly reflected in the textural characteristics of the sediments.","PeriodicalId":30719,"journal":{"name":"Landform Analysis","volume":"31 1","pages":"35-48"},"PeriodicalIF":0.0000,"publicationDate":"2017-03-09","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Landform Analysis","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.12657/LANDFANA.031.003","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 1
Abstract
: The aim of the research was to recognize the diversity of the textural and chemical characteristics of the sedi - ments removed from the catchments of the Tatra Mts., which were affected by the windthrow event in 2013. The diver sity was related to the morphometry of the catchments and the effects of the windthrow event. In catchments sediments deposited during low transport dynamics dominated, two of the catchments were characterized by some percentage (up to 10%) of the sediments deposited in the high-energy environment. However, this diversity is connected to the mor - phometry of the studied catchments and up to this time impact of the windthrows is not clearly reflected in the textural characteristics of the sediments.