Biogeomorphological effects of leaf accumulations in stepped-bed channels: Exploratory study, Moravskoslezské Beskydy Mountains, Czech Republic

The stepped-bed system, with a step-like longitudinal profile, is typical morphology in steep headwater streams. These systems are created by a series of coarse sediments or instream wood (steps with supercritical flows) interspaced with finer material (forming pools with subcritical flows). In the...

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Main Authors: Přibyla Zdeněk, Galia Tomáš, Hradecký Jan
Format: Article
Language:English
Published: Sciendo 2016-09-01
Series:Moravian Geographical Reports
Subjects:
Online Access:http://www.degruyter.com/view/j/mgr.2016.24.issue-3/mgr-2016-0013/mgr-2016-0013.xml?format=INT
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author Přibyla Zdeněk
Galia Tomáš
Hradecký Jan
author_facet Přibyla Zdeněk
Galia Tomáš
Hradecký Jan
author_sort Přibyla Zdeněk
collection DOAJ
description The stepped-bed system, with a step-like longitudinal profile, is typical morphology in steep headwater streams. These systems are created by a series of coarse sediments or instream wood (steps with supercritical flows) interspaced with finer material (forming pools with subcritical flows). In the case of well-developed steps and pools, the resulting channel-reach morphology is referred to as “step-pool” morphology. In this study, we identify a previously undescribed type of step-pool formation, the “foliaged step-pool”, in the high-gradient Stoligy Stream of the Moravskoslezské Beskydy Mountains. The defining feature of this formation is the significant presence of leaves in the step structure. The geometry of the steps and pools was measured and the parameters that characterise the distribution, amount and function of leaves acting in these areas were defined. Statistical results showed differences between non-foliaged and foliaged step-pool formations, in which the latter showed a significant increase in storage level, influencing the channel’s hydrodynamics. Particle-size analyses demonstrated that foliaged step-pool formations had finer sediment in the pools, which indicates that there are differences in sediment transport processes between foliaged and non-foliaged formations. These results offer new insights into stepped-bed and step-pool morphology, providing directions for further research on small streams in deciduous forested regions.
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spelling doaj.art-0efc00257ac24929a08d7a3713569a5b2022-12-22T03:13:59ZengSciendoMoravian Geographical Reports1210-88122016-09-01243132310.1515/mgr-2016-0013mgr-2016-0013Biogeomorphological effects of leaf accumulations in stepped-bed channels: Exploratory study, Moravskoslezské Beskydy Mountains, Czech RepublicPřibyla Zdeněk0Galia Tomáš1Hradecký Jan2Department of Physical Geography and Geoecology, University of Ostrava, Ostrava, Czech RepublicDepartment of Physical Geography and Geoecology, University of Ostrava, Ostrava, Czech RepublicDepartment of Physical Geography and Geoecology, University of Ostrava, Ostrava, Czech RepublicThe stepped-bed system, with a step-like longitudinal profile, is typical morphology in steep headwater streams. These systems are created by a series of coarse sediments or instream wood (steps with supercritical flows) interspaced with finer material (forming pools with subcritical flows). In the case of well-developed steps and pools, the resulting channel-reach morphology is referred to as “step-pool” morphology. In this study, we identify a previously undescribed type of step-pool formation, the “foliaged step-pool”, in the high-gradient Stoligy Stream of the Moravskoslezské Beskydy Mountains. The defining feature of this formation is the significant presence of leaves in the step structure. The geometry of the steps and pools was measured and the parameters that characterise the distribution, amount and function of leaves acting in these areas were defined. Statistical results showed differences between non-foliaged and foliaged step-pool formations, in which the latter showed a significant increase in storage level, influencing the channel’s hydrodynamics. Particle-size analyses demonstrated that foliaged step-pool formations had finer sediment in the pools, which indicates that there are differences in sediment transport processes between foliaged and non-foliaged formations. These results offer new insights into stepped-bed and step-pool morphology, providing directions for further research on small streams in deciduous forested regions.http://www.degruyter.com/view/j/mgr.2016.24.issue-3/mgr-2016-0013/mgr-2016-0013.xml?format=INTmountain streamsfoliaged step-poolleaf accumulationinstream woodMoravskoslezské Beskydy Mts.Czech Republic
spellingShingle Přibyla Zdeněk
Galia Tomáš
Hradecký Jan
Biogeomorphological effects of leaf accumulations in stepped-bed channels: Exploratory study, Moravskoslezské Beskydy Mountains, Czech Republic
Moravian Geographical Reports
mountain streams
foliaged step-pool
leaf accumulation
instream wood
Moravskoslezské Beskydy Mts.
Czech Republic
title Biogeomorphological effects of leaf accumulations in stepped-bed channels: Exploratory study, Moravskoslezské Beskydy Mountains, Czech Republic
title_full Biogeomorphological effects of leaf accumulations in stepped-bed channels: Exploratory study, Moravskoslezské Beskydy Mountains, Czech Republic
title_fullStr Biogeomorphological effects of leaf accumulations in stepped-bed channels: Exploratory study, Moravskoslezské Beskydy Mountains, Czech Republic
title_full_unstemmed Biogeomorphological effects of leaf accumulations in stepped-bed channels: Exploratory study, Moravskoslezské Beskydy Mountains, Czech Republic
title_short Biogeomorphological effects of leaf accumulations in stepped-bed channels: Exploratory study, Moravskoslezské Beskydy Mountains, Czech Republic
title_sort biogeomorphological effects of leaf accumulations in stepped bed channels exploratory study moravskoslezske beskydy mountains czech republic
topic mountain streams
foliaged step-pool
leaf accumulation
instream wood
Moravskoslezské Beskydy Mts.
Czech Republic
url http://www.degruyter.com/view/j/mgr.2016.24.issue-3/mgr-2016-0013/mgr-2016-0013.xml?format=INT
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AT galiatomas biogeomorphologicaleffectsofleafaccumulationsinsteppedbedchannelsexploratorystudymoravskoslezskebeskydymountainsczechrepublic
AT hradeckyjan biogeomorphologicaleffectsofleafaccumulationsinsteppedbedchannelsexploratorystudymoravskoslezskebeskydymountainsczechrepublic