## Abstract The inner delta of the River Niger receives runoff from both the River Niger and the River Bani (249 000 km^2^) and is divided into a northern part (15 000 km^2^) and a southern part (58 000 km^2^). The average input and output discharges are approximately 1490 and 900 m^3^ s^β1^ (1955/
Factors affecting distribution of instability of river banks in the Niger delta
β Scribed by T.K.S. Abam
- Publisher
- Elsevier Science
- Year
- 1993
- Tongue
- English
- Weight
- 626 KB
- Volume
- 35
- Category
- Article
- ISSN
- 0013-7952
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β¦ Synopsis
The Niger delta is intensely dissected by a network of rivers which erode and continuously reshape their banks resulting in net riverbank recessions. The rates of bank recession depend on season, soil type, bank height and stratigraphy, flow velocity and relative location along the river system. Bank failures occur by several mechanisms. These include; rotational, translational, overhang/toppling and flow mechanisms. Bank failure episodes are concentrated at the early stages of lowering of channel water level due to the sensitivity of banks to removal of passive resistance. High ground-water level accentuates seepage erosion which reduces bank stability. To realistically predict the behaviour of river banks, the method of evaluation must recognise the dynamic nature of the controlling factors.
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## Abstract This article describes a multidisciplinary approach to assessing potential vegetation types. The relation between vegetation distribution as derived from field survey and habitat characteristics in the Yellow River Delta (YRD) was analyzed using detrended canonical correspondence analys