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Updated Current Affairs (. The committee was constituted in July 2. Ministry of Water Resources River Development and Ganga Rejuvenation to prepare guidelines for desiltation of river Ganga from Bhimgauda (Uttarakhand) to Farakka (West Bengal). Shri Madhav Chitale (Expert Member, NGRBA) was appointed as Chairman of the committee.

The other members of the committee were: Secretary, Ministry of Water Resources, River Development & Ganga Rejuvenation, Secretary, Ministry of Environment, Forests & Climate Change and Dr. Mukesh Sinha, Director, Central Water and Power Research Station, Pune. The committee was asked to establish difference between desilting and sand mining and also to establish need for desilting for ecology and e- flow of the river Ganga. The committee in its report says erosion, sediment transport and siltation are very complex phenomena. It is impossible to apply a “one- size- fits- all.

Local factors such as topography, river control structures, soil and water conservation measures, tree cover, and riparian land- use or land disturbance (for example agriculture, mining, etc.) can have a large impact on sediment loads in rivers. River control structures (such as reservoirs), soil conservation measures and sediment control programmes can cause downstream sediment loads to decrease, while factors such as land disturbance (clearing of vegetation, for example) or agricultural practices can cause increased sediment loads. At the same time, indiscriminate de- siltation works may result into more harm to ecology and environment flow. Thus, there is a need to evolve Guidelines, better broad principles, which should be kept in mind while planning and implementing de- silting works.

According to the report erosion, sediment transport and siltation in large rivers like Ganga are very complex phenomena and their estimation has inherent limitations and uncertainties. A reconnaissance of Main River Ganga on Google earth map reveal that different reaches are in a dynamic equilibrium phase.

Sedimentation is mainly seen downstream of Bhimgauda barrage and near the confluences of tributary rivers with Ganga. The discharge congestion, large scale sediment deposition and its negative effects are mainly seen downstream of the confluence of Ghagra and beyond. The river flood plain drastically widens beyond the confluence of Ghagra and is estimated to be around 1.

The committee says though de- siltation works can improve hydraulic performance of the river and this itself can justify undertaking de- siltation, these have no direct role in improving environment flow in the river. On the other hand, indiscriminate de- silting or sand mining would cause adverse impacts on river e- flow.

Recognizing the importance of sediment transport in rivers, following basic principles of siltation in rivers should be kept in mind while considering de- siltation works: 1. Catchment Area Treatment and Watershed Development works, along with good agricultural practices and river bank protection/anti- erosion works, are necessary to reduce silt inflow into the river system and must be undertaken in a comprehensive way. Erosion, movement and deposition of sediment are natural regulating functions of river and Sediment equilibrium of river should be maintained. Rivers should be provided with sufficient flood plains (lateral connectivity) without any hindrance to the flow.

Instead of “keeping the silt away”, strategy to “giving the silt way” should be adopted. In specific reference to de- siltation works in river Ganga, in addition to Mo. EF& CC Sand Mining Guidelines, which are statutory in nature, and the GSI Guidelines, the committee has suggested following Guidelines; 1.

It is necessary to provide the river sufficient areas of flood plain and lakes along the river to moderate the flood level. Any encroachment of flood plain, reclamation of lakes or disconnection of lakes from river should be avoided; rather adjoining lakes/depressions may be de- silted to increase their storage capacities.

The de- silting of lakes, etc., should be in such a manner that the sediment continuity is maintained and should not lead to head cut that creates safety issues for the river crossings, water intakes or river training works locally, downstream or upstream. Possibly river training, cut- off developments and provision of extra water way near the constrictions could be tried after proper assessment without impacting the morphology of river elsewhere. The area freed from the development in the form of oxbow lakes should be used for flood moderation rather than reclaiming it for other purposes. The dredged material may be dumped along the alternate channel which was to be closed to avoid bank erosion. Freebsd Installing Dig Host Nslookup Syntax. Care shall be taken to develop stable channel which do not affect the flow either on upstream or downstream. Efforts should be made to provide silt continuity along the weirs and barrages.

It should invariably be associated with sediment flux studies and morphological studies to confirm no significant adverse effect on downstream or upstream reach of the river including the safety and effectiveness of river crossings, water intakes, existing river bank / flood protection measures etc. This would require quantitative long term forecast with decision support system to be established for optimum reservoir operations. It shall be ensured that the head cut induced upstream should automatically de- silt the reach. The headcut induced should progress upstream slowly so that the flora and fauna will have sufficient time to re- adjust its habitat. River gravels/sands/silts could be used gainfully in construction works, including housing, roads, embankment and reclamation works.

Under no circumstances, disposal should create any contamination of the water bodies, harmful to the flora and fauna existing adjacent to the disposal sites. It should also be ensured that disposed material should not come back into the river again. The sediment removed may be used for re- grading the Farakka Feeder Canal or may be used for strengthening the existing embankments around the barrage pond. Sediment sluicing may be incorporated to maintain sediment continuity from upstream to downstream reaches after carrying out necessary studies. The de- silting / dredging works of the barrage pond shall not cause any structural problem to the barrage by excessive erosion on the downstream. In view of this the dredging shall be restricted only up to original bed level or higher.

It shall also be ensured that the concentrated sediment flux passed downstream will not create any major morphological changes on the downstream reaches. Restrictions as presented in Appendix IV of this Report need to be enforced before planning and executing any dredging/ de- silting / mining activities. These restrictions may be modified only after proper study and monitoring the effects of dredging / de- silting / mining. These integrated plans could serve as base documents for Central, State and District Level Authorities for considering proposals for environment clearances for works related to river Ganga.

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