Briti Sundar Sil

Dr. Briti Sundar Sil


Research Focus & Metrics

Academic Career Length

17Years (2010-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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11 July 2020 in Bulletin of Engineering Geology and the Environment
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Journal Article
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wajahat Annayatwajahat Annayat
wajahat Annayat
BSBriti Sundar Sil
Briti Sundar Sil

26 December 2022 in Conservation
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Journal Article
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BSBriti Sundar Sil
Briti Sundar Sil
Kumar AshwiniKumar Ashwini
Kumar Ashwini
wajahat Annayatwajahat Annayat
wajahat Annayat
JDJatan Debnath
Jatan Debnath
Majid FarooqMajid Farooq
Majid Farooq
Gowhar MerajGowhar Meraj
Gowhar Meraj
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.

8 November 2017 in Meteorology Hydrology and Water Management
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Journal Article
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VBViolina Basumatary
Violina Basumatary
BSBriti Sundar Sil
Briti Sundar Sil
Analysis of a design storm, explained as the expected rainfall intensity for a given storm duration and return period is carried out to establish Rainfall Intensity-Duration Frequency (IDF) relationships. The IDF relationships are essential for the designing of hydraulic structures for future...


1 May 2010 in Journal of Hydrology
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Journal Article
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PCParthasarathi Choudhury
Parthasarathi Choudhury
BSBriti Sundar Sil
Briti Sundar Sil

1 June 2016 in International Journal of Sediment Research
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Journal Article
Closed access
BSBriti Sundar Sil
Briti Sundar Sil
PCParthasarathi Choudhury
Parthasarathi Choudhury