04.08.2013 Views

Lingza - Ministry of Power

Lingza - Ministry of Power

Lingza - Ministry of Power

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

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

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!