RECENT RIVER CHANNEL CHANGE DETECTIONS IN THE SECTION OF THE RIVER TISZA ABOVE TISZAÚJLAK (BИЛОК)

In the section above Tiszaújlak, despite the presence of embankments, the River Tisza shows active meandering tendency and it splits into branches resulting in side channels, dead channels and backwaters that follow the main channel. In our work we examined the right- and the left-side riverbank s...

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Main Authors: ISTVÁN KOLOZSVÁRI, JÓZSEF MOLNÁR, GYÖRGY DÉVAI
Format: Article
Language:English
Published: University of Debrecen 2016-08-01
Series:Acta Geographica Debrecina: Landscape and Environment Series
Subjects:
Online Access:http://landscape.geo.klte.hu/pdf/agd/2016/2016v10is3_4_4.pdf
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spelling doaj-67a92824411b4773bbde2fc5620eb0da2020-11-25T00:10:47ZengUniversity of DebrecenActa Geographica Debrecina: Landscape and Environment Series1789-49211789-75562016-08-01103-4123130DOI:10.21120/LE/10/3-4/4RECENT RIVER CHANNEL CHANGE DETECTIONS IN THE SECTION OF THE RIVER TISZA ABOVE TISZAÚJLAK (BИЛОК)ISTVÁN KOLOZSVÁRI0JÓZSEF MOLNÁR1GYÖRGY DÉVAI2kolozsvaros@gmail.comjozsi@kmf.uz.uadevai.gyorgy@science.unideb.huIn the section above Tiszaújlak, despite the presence of embankments, the River Tisza shows active meandering tendency and it splits into branches resulting in side channels, dead channels and backwaters that follow the main channel. In our work we examined the right- and the left-side riverbank sections of the River Tisza, between Tiszaújlak (Вилок) and Tiszasásvár (Тросник), as well as between Tiszaújlak and Tiszapéterfalva (Пийтерфолво), to reveal the extent of bar depositions between 2006 and 2015, and to what extent the intensity and direction of the riverbank formation processes were influenced by the material of the bank and the plant coverage, its rate and characteristics. We tried to reveal which sections were eroded by the river and what security risks they have for the safety of the settlements along the Tisza River. On the right side of the Tisza River riverbank 51, and on the left side 62 main measuring points were recorded by GPS positioning satellite in 2009, 2010 and 2015. Our results were compared to the satellite images of Google Earth taken in 2006, too. According to our experience, in several bends of the examined sections of the river, active bar deposition can be observed; in some cases more than 100 m of bar depositions were detected.http://landscape.geo.klte.hu/pdf/agd/2016/2016v10is3_4_4.pdfUkraineUpper-Tiszaanastomosing channel typelateral erosioncut bankplant coverageriverbank materials
collection DOAJ
language English
format Article
sources DOAJ
author ISTVÁN KOLOZSVÁRI
JÓZSEF MOLNÁR
GYÖRGY DÉVAI
spellingShingle ISTVÁN KOLOZSVÁRI
JÓZSEF MOLNÁR
GYÖRGY DÉVAI
RECENT RIVER CHANNEL CHANGE DETECTIONS IN THE SECTION OF THE RIVER TISZA ABOVE TISZAÚJLAK (BИЛОК)
Acta Geographica Debrecina: Landscape and Environment Series
Ukraine
Upper-Tisza
anastomosing channel type
lateral erosion
cut bank
plant coverage
riverbank materials
author_facet ISTVÁN KOLOZSVÁRI
JÓZSEF MOLNÁR
GYÖRGY DÉVAI
author_sort ISTVÁN KOLOZSVÁRI
title RECENT RIVER CHANNEL CHANGE DETECTIONS IN THE SECTION OF THE RIVER TISZA ABOVE TISZAÚJLAK (BИЛОК)
title_short RECENT RIVER CHANNEL CHANGE DETECTIONS IN THE SECTION OF THE RIVER TISZA ABOVE TISZAÚJLAK (BИЛОК)
title_full RECENT RIVER CHANNEL CHANGE DETECTIONS IN THE SECTION OF THE RIVER TISZA ABOVE TISZAÚJLAK (BИЛОК)
title_fullStr RECENT RIVER CHANNEL CHANGE DETECTIONS IN THE SECTION OF THE RIVER TISZA ABOVE TISZAÚJLAK (BИЛОК)
title_full_unstemmed RECENT RIVER CHANNEL CHANGE DETECTIONS IN THE SECTION OF THE RIVER TISZA ABOVE TISZAÚJLAK (BИЛОК)
title_sort recent river channel change detections in the section of the river tisza above tiszaújlak (bилок)
publisher University of Debrecen
series Acta Geographica Debrecina: Landscape and Environment Series
issn 1789-4921
1789-7556
publishDate 2016-08-01
description In the section above Tiszaújlak, despite the presence of embankments, the River Tisza shows active meandering tendency and it splits into branches resulting in side channels, dead channels and backwaters that follow the main channel. In our work we examined the right- and the left-side riverbank sections of the River Tisza, between Tiszaújlak (Вилок) and Tiszasásvár (Тросник), as well as between Tiszaújlak and Tiszapéterfalva (Пийтерфолво), to reveal the extent of bar depositions between 2006 and 2015, and to what extent the intensity and direction of the riverbank formation processes were influenced by the material of the bank and the plant coverage, its rate and characteristics. We tried to reveal which sections were eroded by the river and what security risks they have for the safety of the settlements along the Tisza River. On the right side of the Tisza River riverbank 51, and on the left side 62 main measuring points were recorded by GPS positioning satellite in 2009, 2010 and 2015. Our results were compared to the satellite images of Google Earth taken in 2006, too. According to our experience, in several bends of the examined sections of the river, active bar deposition can be observed; in some cases more than 100 m of bar depositions were detected.
topic Ukraine
Upper-Tisza
anastomosing channel type
lateral erosion
cut bank
plant coverage
riverbank materials
url http://landscape.geo.klte.hu/pdf/agd/2016/2016v10is3_4_4.pdf
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