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Why settling basins are essential in Nepal
Short answer
Nepal's young Himalayas cause high sediment with hard quartz, leading to severe turbine abrasion and headrace filling in run-of-river plants. Settling basins remove particles (0.15-0.5 mm) by reducing velocity to 0.2-0.4 m/s with ≥90% efficiency, using two chambers for continuous flushing.
Why settling basin is essential in hydropower electric project in Nepal? Draw a layout plan and section of typical settling basin along with its design criteria.
Why a settling basin is essential in Nepal
A settling basin (desander) is an enlarged chamber after the intake where flow velocity is reduced so that suspended sediment settles and is flushed back to the river. In Nepal it is essential because:
- Young, fragile Himalaya: rivers carry very high sediment loads, especially in the monsoon (often several thousand ppm).
- Hard, sharp quartz particles: quartz and feldspar content is high, so turbines (especially high-head Pelton and Francis) suffer severe abrasion/erosion of runners, needles, guide vanes and seals.
- Most plants are run-of-river: there is no large reservoir to trap sediment.
- Sediment fills headrace canals and tunnels, reducing capacity and increasing head loss.
- Wear causes loss of efficiency, frequent shutdowns and costly repairs (e.g. Jhimruk, Khimti, Kaligandaki A).
Typical layout
PLAN
inlet settling zone outlet
from +-----+--------------------------+-----+ to
intake| / | ==== chamber 1 ==== | \ |headrace
----> |< |--------------------------| >|---->
| \ | ==== chamber 2 ==== | / |
+-----+--------------------------+-----+
transition |flushing| spill transition
v channel v weir
SECTION (longitudinal)
WL ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~
\ inlet outlet|
\___ ____weir__|
\______________________/
bed slope 1:20-1:50 --> flushing
gate/pipe
Design criteria
- Particle size to remove: 0.15–0.2 mm for high-head plants (> 100 m) and 0.2–0.5 mm for low/medium heads.
- Trap efficiency: usually ≥ 90% of the design particle size.
- Flow velocity: less than critical (scour) velocity, by Camp: cm/s (d in mm, a = 44 for 0.1–1 mm), normally 0.2–0.4 m/s.
- Size: settling length (w = fall velocity), increased for turbulence (Vetter/Camp efficiency); about 4–10.
- Inlet and outlet transitions: gradual (about 1:5 to 1:8) to give uniform flow; baffles or flow-straightening walls.
- Number of chambers: at least two, so one can be flushed or repaired while the other works.
- Flushing: continuous or intermittent (hydraulic flushing gates, Serpent/SSSS systems, pipes); bed slope 2–5% towards the flushing outlet.
- Spillway: to pass excess water during floods or load rejection.
- Provision for sediment monitoring and bypass of flood flows.
✓ Answer checked by Claude Opus 5.5 (high effort)
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