Observing Spatiotemporal Inconsistency of Erosion and Accretion in the Barak River Using Remote Sensing and GIS Techniques

Наблюдение за пространственно-временной неоднородностью эрозии и аккумуляции в реке Барак с использованием методов дистанционного зондирования и ГИС
Briti Sundar Sil, Kumar Ashwini, Wajahat Annayat, Jatan Debnath, Majid Farooq, Gowhar Meraj
2022-12-26

Barak Riverland use/land coverremote sensing and GISriverbank erosionsediment deposition
Alluvial rivers all over the world have one common problem, which is their meandering pattern. This meander formation is because of natural and anthropogenic processes. Barak River is dynamic, and due to this, it is exposed to regular shifting and creates many problems for the people who reside near the river. The livelihood of many people depends on agriculture, which they conduct on the nearby sides of the river. However, the regular shifting of riverbanks makes their life miserable and leads to severe economic losses. Further, roadways and railways run along the banks of the Barak River, and during monsoon, Assam (Silchar), along with three states, Mizoram, Manipur, and Tripura, become disconnected from the rest of India because the road and rail connections fail due to riverbank erosion. Therefore, considering the catchment area and the importance of this river, we have tried to understand the spatiotemporal changes (erosion, deposition, and unchanged area) in the Barak River. From our analysis, we found that the maximum and minimum amount of erosion occurred from 2012–2017 and 2002–2012 and were 727.56 ha and 332.69 ha, respectively. While the highest amount of deposition that occurred during 1984–2017 was 1054.21 ha, the minimum amount of deposition that occurred during 2012–2017 was 351.32. Overall, it was identified that the area under the deposition was more dynamic than the erosion from 1984–2017. Moreover, from the temporal analysis of land use/land cover from 1984–2017, it was found that the area that comes under the settlement and arable land has increased by 10.47% and 5.05%, respectively. The dynamic factors, such as the nature of channel gradient, land use/land cover, and riparian vegetative cover, could be the probable driving forces that cause changes in the erosional and depositional areas. This study will help us understand the dynamics of the Barak River and other rivers of this type worldwide. This study shall help implement strategies that will help manage bank erosion by adapting scientific bank protection measures.
1
Deposition peaked at 1054.21 ha during 1984–2017 and was lowest during 2012–2017 at 351.32 ha.
2
Deposition was more spatially and temporally dynamic than erosion across the Barak River during 1984–2017.
3
Maximum erosion occurred during 2012–2017, covering 727.56 ha, while minimum erosion occurred during 2002–2012, covering 332.69 ha.
4
Settlement and arable land increased by 10.47% and 5.05%, respectively, between 1984 and 2017; channel gradient, land use, and riparian vegetation may drive observed changes.
5
The study uses remote sensing and GIS to quantify spatiotemporal erosion, deposition, and unchanged areas along the dynamic Barak River from 1984–2017.

the Barak River and its riverbanks within the catchment area

spatiotemporal changes and driving factors of riverbank erosion, deposition, and unchanged areas during 1984–2017

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2022-12-26
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Briti Sundar Sil
Kumar Ashwini
Wajahat Annayat
Jatan Debnath
Majid Farooq
Gowhar Meraj
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