Please use this identifier to cite or link to this item: https://hdl.handle.net/1959.11/22233
Title: Bank instability along a weir pool of the River Murray
Contributor(s): Thoms, Martin  (author)orcid 
Publication Date: 2017
DOI: 10.1080/03721426.2017.1374158
Handle Link: https://hdl.handle.net/1959.11/22233
Abstract: River banks are an important transition zone between aquatic and terrestrial environments. This ecotone is highly vulnerable to natural and anthropogenic disturbances. Bank erosion is a common occurrence along the River Murray. Morphological features reflecting river bank instability form a near-continuous pattern along large tracts of the river. This study investigates the character and extent of bank instability along the Torrumbarry Weir Pool. Over 90% of the bank length in this weir pool was assessed as being actively eroding. Notch development was the dominant instability mechanism and it promoted other forms of bank instability. Erosion notches result from stable water levels and inherent soil instability of the river banks along the weir pool. The character and extent of river bank erosion recorded along this section of the River Murray is an artefact of flow regulation and not a reflection of the natural occurrence of bank erosion in river networks. Water level management in the upstream weir pool has significant implications for the management of river banks along regulated reaches of the River Murray.
Publication Type: Journal Article
Source of Publication: Transactions of the Royal Society of South Australia, 141(2), p. 151-168
Publisher: Taylor & Francis Australasia
Place of Publication: Australia
ISSN: 0372-1426
2204-0293
Field of Research (FOR): 040699 Physical Geography and Environmental Geoscience not elsewhere classified
040601 Geomorphology and Regolith and Landscape Evolution
Peer Reviewed: Yes
HERDC Category Description: C1 Refereed Article in a Scholarly Journal
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Appears in Collections:Journal Article
School of Humanities, Arts and Social Sciences

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