Lingza - Ministry of Power
Lingza - Ministry of Power
Lingza - Ministry of Power
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CHAPTER-IV<br />
26<br />
Preliminary Feasibility Report<br />
<strong>Lingza</strong> HE Project (3 x 40 MW)<br />
TOPOGRAPHIC AND GEOTECHNICAL ASPECTS<br />
4.1 INTRODUCTION<br />
Central Electricity Authority proposed construction <strong>of</strong> <strong>Lingza</strong> hydroelectric scheme on<br />
Ringpi Chu near Ishana in order to generate hydroelectricity from its water potential. The<br />
scheme envisaged construction <strong>of</strong> a diversion structure upstream <strong>of</strong> Ishana, a water<br />
conductor system in the left bank <strong>of</strong> Ringpi Chhu and a powerhouse downstream <strong>of</strong><br />
confluence <strong>of</strong> Ringpi Chu and Rangyong Chu. The scheme was expected to generate<br />
approximately 160 MW <strong>of</strong> power. The task <strong>of</strong> preparation <strong>of</strong> pre-feasibility report was<br />
assigned to NHPC. As per the MOU, GSI reports and site visits <strong>of</strong> experts would form<br />
major in puts for topographic and geotechnical aspects. The present appraisal is based on<br />
study <strong>of</strong> topographic sheet 78 A/6 and reconnaissance traverse that was undertaken by<br />
mid October.<br />
A study <strong>of</strong> the area was undertaken and a few modifications were made in layout <strong>of</strong> the<br />
project, because <strong>of</strong> Panan scheme, which has been proposed in the downstream. Now, a<br />
diversion structure shall be constructed approximately 700m upstream <strong>of</strong> Ishana, a 4 km<br />
long water conductor system in the right hill and an underground powerhouse upstream<br />
<strong>of</strong> confluence <strong>of</strong> Ringpi and Rangyong Chhu. The tail water shall be discharged above<br />
the FRL <strong>of</strong> Panan Scheme. The geological report from GSI has been received and placed<br />
as annexure 4.1.<br />
4.2 REGIONAL TOPOGRAPHIC AND GEOTECHNICAL FEATURES<br />
River Teesta in Sikkim is a major river originating from Zemeu glaciers and generally<br />
flows in north-south direction, at a steeper gradient. The river is joined by several<br />
tributaries major amongst them being Yumthang Chu, Zemu Chu, Talung Chu, Dik Chu<br />
and Rangpo Chu, apart from others join the river. The river valleys in this region are u-<br />
shaped while, as the tributaries had developed deep gorges, which are bound by steep