Investigation of the lateral channel migration: A case study of the South Morava River (Serbia)

Q4 Social Sciences
Marko Langović
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引用次数: 1

Abstract

The morphological evolution of the fluvial relief in the lowland areas is determined by the dynamic of the lateral channel migration process. River meandering and lateral channel migration represent continuous, dynamic and complex processes, which intensity modifies alluvial plains. Accordingly, it is a current topic observed from the domain of various scientific disciplines and practices, including the geographical aspect of the study. Directly or indirectly, variations of natural and anthropogenic processes affect changes in the lateral migration intensity, which is later manifested through permanent consequences for the environment. The aim of this paper is to investigate the process of lateral channel migration, through the review and interpretation of theoretical and methodological concepts and results of contemporary scientific literature. In this paper, on specific sections of the South Morava River (Serbia), the values of maximum lateral migration over different time periods are determined. Three representative river sectors were singled out, spatial and temporal dynamic was determined, while the process of lateral channel migration was presented quantitatively and graphically. Based on the obtained data, a comparative analysis showed significant riverbank changes for the observed meanders, within the period 1924-2020. Special emphasis is on the analysis of the lateral channel migration in the last decade of the mentioned period. The obtained results can be further used in order to develop and implement plans of water and land management, environmental protection and socio-economic development strategies.
横向河道迁移研究——以南莫拉瓦河(塞尔维亚)为例
低地河流起伏的形态演化是由侧向河道迁移过程的动力决定的。河流曲流和横向河道迁移是一个连续的、动态的、复杂的过程,其强度改变了冲积平原。因此,这是一个从各种科学学科和实践领域观察到的当前主题,包括研究的地理方面。自然和人为过程的变化直接或间接地影响横向迁移强度的变化,这种变化后来通过对环境的永久性后果表现出来。本文的目的是通过对当代科学文献的理论和方法概念和结果的回顾和解释来研究横向河道迁移的过程。本文以南莫拉瓦河(塞尔维亚)的特定河段为例,确定了不同时期的最大横向迁移值。选取了3个具有代表性的河段,确定了河段的时空动态,并定量、图解地描述了河段横向迁移的过程。根据获得的数据,对比分析表明,在1924-2020年期间,观测到的曲流发生了显著的河岸变化。特别着重分析了上述时期最后十年的侧向河道运移。所取得的成果可进一步用于制定和执行水和土地管理、环境保护和社会经济发展战略的计划。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Glasnik - Srpskog Geografskog Drustva
Glasnik - Srpskog Geografskog Drustva Social Sciences-Education
CiteScore
0.70
自引率
0.00%
发文量
11
审稿时长
18 weeks
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