ISH Journal of Hydraulic Engineering
ISSN: 0971-5010 (Print) 2164-3040 (Online) Journal homepage: http://www.tandfonline.com/loi/tish20
Performance evaluation of desilting basins of
small hydropower projects
Gurdeep Singh & Arun Kumar
To cite this article: Gurdeep Singh & Arun Kumar (2016): Performance evaluation of
desilting basins of small hydropower projects, ISH Journal of Hydraulic Engineering, DOI:
10.1080/09715010.2015.1094750
To link to this article: http://dx.doi.org/10.1080/09715010.2015.1094750
Published online: 05 Jan 2016.
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Date: 06 January 2016, At: 18:54
ISH Journal of HydraulIc EngInEErIng, 2016
http://dx.doi.org/10.1080/09715010.2015.1094750
Performance evaluation of desilting basins of small hydropower projects
Gurdeep Singh and Arun Kumar
Downloaded by [gurdeep singh] at 18:54 06 January 2016
alternate Hydro Energy centre, Indian Institute of Technology roorkee, roorkee, India
ABSTRACT
ARTICLE HISTORY
There are many silt removing devices/methods used in small hydropower projects. Selection of these
devices/methods depends upon the size and quantity of incoming sediments, land utilization for
construction, size of sediment to be removed, and sequent of sediment lushing. The settling basin
is the most widely used desilting device for small hydropower project (SHP). Vortex sediment settling
basin developed recently is other cost-efective and eicient desilting device. This paper presents
performance evaluation of settling basins and vortex sediment desilting devices constructed at SHP
stations through ield investigations at number of SHP stations in almost similar type of climatic and
physiographic conditions. Silt removal eiciency has been compared using diferent methods for
computing eiciency provided by diferent investigators. For SHP stations, eicient and economic
desilting basin has been also suggested.
received 26 november 2014
accepted 13 September 2015
KEYWORDS
Vortex sediment settling
basin; SHP; performance
Introduction
Settling basin
Small hydropower (SHP) stations in mountainous streams are
generally run-of-river types, where the catchments are steep
and vulnerable to high soil erosion. Heavy rains, especially
in tropics and monsoon regions produce large sediment yield
from these catchments and the streams experience high sediment concentrations during seasonal loods. he desilting
basin constructed in series with the headrace channel play an
important role for hydropower stations. he design dimensions of the desilting basin are the major factor for their sand
trapping eiciency. he sediment, not only cause erosion on
turbine, capital cost of replacement, but also leads to loss of
generation (due to reduced eiciency). hough it may not be
possible to remove all sediments, even sediments should be
removed to the extent to maintain hydraulic carrying capacity
of the waterway and to prevent the abrasion of turbines. he
desilting devices allow suspended particles to settle down and
deposit on the bottom of the basin by reducing the velocity of
the water low. Deposited sediments are removed, by lushing or by dredging manually or mechanically. In recent years,
desilting basins based on diferent methods for the removal of
sediments have been developed and are in use. hese desilting
devices are:-
Settling basins are used on irrigation and hydropower channels
to remove sediment of speciied size and quantity. he channel
is expanded into the basin by widening its width and lowering
its loor (increasing depth) through an expansion transition
and restored back through a contraction transition at the end
of the basin (Athar et al. 2002).he deposited sediments are
removed through one or more duct(s) unit continuous or intermittent generally based lushing or manually. he schematic
sketch of Settling basin is shown in Figure 1(a) and (b).
Where B1 – width of the channel; B2 – width of the settling
basin; D – depth of low in the settling basin; D1 – depth of
low in the channel; L – length of the settling basin; Qsi – Inlet
Discharge; Qse – Outlet Discharge; U1 – Flow Velocity in channel; U – Flow Velocity in desilting basin.
(a)
(b)
(c)
(d)
Vortex tubes,
Desilting basin,
Tunnel extractor,
Hydro cyclone.
he desilting basin is the most commonly and preferred
desilting devices used in SHP stations. here are two types of
desilting basins:
(i) Settling basin and
(ii) Vortex sediment settling basin.
CONTACT gurdeep Singh
© 2016 Indian Society for Hydraulics
gurdeep5206@gmail.com, gsj5206@yahoo.com
Vortex sediment settling basin
The vortex chamber-type sediment basin is a fluidic device
which is used to extract bed load and suspended load sediment from the diverted water by the vortices of flow (Paul
et al. 1991). A higher velocity flow is introduced tangentially
into a circular basin having an orifice at the center of its
bottom, which removes highly concentrated sediment flow.
The secondary flow resulting from this phenomenon causes
the fluid layers near the basin floor to move towards the
outlet orifice at the centre. The sediment particles present
in the flow move along a helicoidal path towards the orifice,
thereby obtaining a long settling length compared to the
basin dimensions (Paul et al. 1991). The sediment reaching
the centre can be flushed out through the orifice outlet channel/pipe. The schematic diagram of vortex settling basin is
shown in Figure 2(a) and (b).
2
G. SinGH And A. KumAr
(a)
(b)
Figure 1. (a) Plan (garde et al. 1990); (b) section a-a (garde et al. 1990).
(b)
(a)
Downloaded by [gurdeep singh] at 18:54 06 January 2016
Figure 2. (a) Plan (Paul et al. 1991); (b) section X-X (Paul et al. 1991).
Table 1. Vortex settling basin eiciency relations (athar et al. 2002).
Investigator
curie et al. (1979)
Mashauri (1986)
Paul et al. (1991)
relationship
�
(
athar et al. (2002)
�0.88
⎞
⎛ do0.11 𝛾s
𝛾
⎟
𝜂O = 1.74 + ln ⎜ Q0.58f
⎟
⎜
⎠
⎝
( )
( )
)
(
+ (1.71 × 10−2 dd − 5.93 × 10−4 d dk
𝜂O = 0.835 − 0.0292
k1
o
o 1
( )
𝜔o
𝜂O = 73.4 + 8 Log W
𝜔o
)
𝜂O = 98 + 0.92 Log W
[
]
( )0.25 ( )0.35 (
)0.15 ( 2 )0.11
Qo
𝜔o ds
Zh
Qw
𝜂O = ko
Q
h
𝜈
gR3 h2
i
p
( )0.04 ( )1.27
𝜔
Qo
𝜂O = 2.16 Vo
Q
t
𝜂O =
(
𝜔o
Vto
t
)0.0045 ( )0.01
Qo
Qi
T P
Where h1 – height of diaphragm from bed of inlet canal; h2 –
basin depth at its periphery from inlet canal bed; h – low depth
in inlet canal, full-supply depth; h0 – depth of low over oriice;
hp – water depth at basin periphery; d0 – lushing pipe diameter; d – basin diameter; d – basin diameter; Qc – inlet-canal
discharge, full-supply discharge; Qcc – discharge entering basin;
Qs – Overlow Discharge; Q0 – Flushing Discharge; S – bed
slope (S horizontal to one vertical); Sc – radial slope of basin
loor (Sc horizontal to one vertical).
developed relationships for sediment removal eiciency assessment are given in Table 1.
he SHP plant owners design these settling basins based
on limited data, as for SHP stations installed on small streams
data available are very poor and limited. Many desilting basins
get choked with deposited silt during heavy rainfall or lash
Vortex sediment settling basin has the following advantages:(a) Land area required for sedimentation is less.
(b) Require lower lushing water.
(c) Cost of construction is much low compared to settling
basin.
(d) Hydraulic eiciency as compared to settling basin is
high.
(e) In vortex settling basin, water may be diverted directly
to power channel during lean season when water is
almost free of sediments. his is important in cold
region, where settling basin freezes due to lower velocity and causes the shutting down of plants.
However, design of vortex sediment settling basin needs to
be supported with model study for performance assessment
before execution at site. Paul et al. (1991) and Ather et al. (2002)
Figure 3. camp and dobbins’ relation for eiciency of settling basin (camp 1946).
iSH JournAl oF HydrAulic EnGinEErinG
3
quite common). he design parameters used at each SHP station under study was collected including the design details by
contacting plant owners and visiting the SHP stations. Samples
of sediment were also collected from head works (natural
stream) as well as at silt lushing outlets of several SHP stations.
For settling basin, the eiciency of basins computed using
Camp Dobbins curve, as well as Garde method were compared
with eiciency observed at each desilting basin. he eiciency
observed at site was by comparing grain size distribution (GSD)
curve at inlet and lushing outlet. Similarly, for vortex settling
basin the eiciency of basins was computed using Paul and
Ather method, and was compared with the eiciency of desilting basin observed at site.
Evaluation of Settling basin eiciency
Eiciency computation using Camp-Dobbins method
Camp-Dobbins curve used for silt removal eiciency is given
in Figure 3.
Where L is the length of the basin, D is the depth of the
basin, w and u are settling velocity of particle and low velocity
in basin, respectively, n is the regosity cofecient, and g is the
acceleration due to gravity 9.81 m/s2. Using basin dimension,
low, and sediment characterstics, the eiciency is assumed.
Downloaded by [gurdeep singh] at 18:54 06 January 2016
Figure 4. Variation of k and η0 with w/u* (garde et al. 1990).
loods. heir eiciency gets reduced and did not perform well.
here are not many studies reported on performance evaluation of desilting basins on SHP stations. hus, the performance
of these basins is evaluated, proper design is carried out, and
corrective measures are undertaken so that sediment efects
on SHP stations can be minimized.
Eiciency computation using Grade method
An inherent limitation of the Camp-Dobbins relationship is
that it gives an eiciency of nearly 100% if the settling basin is
very long, even if it has not been widened or deepened, to give
a signiicant decrease in velocity (Cecen and Akmandor 1973).
Grade designed a new relationship for assuming the sediment
removal eiciency of settling basin (Garde et al. 1990), and is
as follows:
Methodology
he performance evaluation of desilting basins has been carried out by studying a number of desilting basins constructed
recently at SHP stations in the state of Himanchal Pradesh (a
Himalayan state where sediment problem for power stations is
𝜂 = 𝜂0 (1 − e
−kL
D
(1)
)
Table 2(a). Settling basin features (Singh and Kumar 2013).
name of name of
Sr. no station
stream
1
Tarila
Tareila
nallah
2
Tarila-ii
Tareila
nallah
3
Baner-iii Baner
khad
4
Iku-ii
Iku khad
5
upper
Khauli
khauli
Khad
6
drinidhar Brahl
Khad
7
aleo
allain
manali
stream
8
Baragoan Sanjoin
nallah
9
Sarbari
Sarbari
khad
10
Jirah
Jirah
nallah
11
Toss
Toss
nallah
12
Brahma- Bharamganga
gana
13
gurahan gurahan
Khud
14
Patkari
Bakhli
khad
inlet
channel
Head discharge width
(m)
(cumec)
(m)
184
6.00
2.0
installed
capacity
(mW)
2 × 2.5
Type of
turbine
francis
2 × 2.5
francis
133
6.10
2 × 2.5
Pelton
302
2 × 2.5
2 × 2.5
Pelton
Pelton
2 × 2.5
desilting basin dimensions (m)
u/S
transition
10.4
depth
4.5
d/S
transition
7.8
no. of
outlet
1
Flushing
conduit
(mm)
600Ø
length
54.7
Width
7.5
2.0
5.0
36.0
8.5
3.1
5.0
1
600Ø
2.70
1.8
7.5
30.0
5.0
2.5
1
500 × 500
362
430
3.96
2.34
1.8
1.8
7.7
8.0
52.0
51.5
5.0
4.5
2.5
4.1
4.0
4.0
1
1
500 × 500
500 × 500
Pelton
249
3.10
1.8
10.5
45.0
5.0
2.5
5.0
1
500 × 500
2 × 1.5
Pelton
290
1.60
1Ø
–
25.0
5.0
2.0
–
5
300Ø
1 × 1.9
francis
170
4.25
2.3
18.0
62.0
6.0
3.0
–
1
1000Ø
2 × 2.25
Pelton
202
4.50
n.a
–
43.9
9.4
4.1
–
4
300Ø
2×2
Pelton
348
1.31
1.2Ø
9.5
30.0
5.0
6.0
–
3
800Ø
2×5
Pelton
186
4.32
n.a
–
45.0
7.0
3.0
–
n.a
n.a
2 × 2.5
Pelton
230
3.15
1.6Ø
20.6
40.0
7.0
3.0
6.0
1
500Ø
1 × 1.5
Pelton
216
1.10
1.2
4.5
40.0
3.0
1.0
4.5
1
300Ø
2×8
Pelton
375
5.83
3.5
10.0
54.0
7.0
3.5
–
3
500Ø
4
G. SinGH And A. KumAr
Table 2(b). Vortex settling basin features (Singh and Kumar 2013).
Sr. no
15
name of
station
gaj
16
Khauli
17
Bhuri
singh
name of
stream
gaj &
leond
Khauli
Khad
Sal
nallah
discharge
(cumec)
6.93
inlet
channel
width
(m)
3.4
diameter
17
475
3.19
2.4
13.72
5.14
3.4
installed
capacity
(mW)
3 × 3.5
Type of
turbine
Pelton
Head
(m)
213
2×6
Pelton
0.45
francis
where η0 is the limiting eiciency obtained for a given w/u* at
large values of L/D and k is a coeicient. he values of k and
η0 are determined using the mean curves and their variation
with w/u*is shown in Figure 4.
Where u* is the shear velocity in the settling basin, w is the
settling velocity in settling basin, and L and D are length and
depth of basin, respectively.
Downloaded by [gurdeep singh] at 18:54 06 January 2016
Evaluation of vortex settling basin eiciency
Eiciency of vortex type settling basin is evaluated using relation given by diferent investigators and is described as follows:
Computation of eiciency by Paul method
he Eiciency computation relation given by Paul’s relation
(Paul et al. 1991):
( )
Vs
P = 98 + 0.92 log
W
(2)
Figure 5. SHP stations studied in Himachal Pradesh, India (Singh and Kumar 2013).
desilting basin
dimensions (m)
depth
2.05
Slope
(1V:H)
01:10
no. of
outlet
1
Flushing
conduit
(mm)
600Ø
12
2.00
01:10
1
450Ø
17
2.15
01:10
1
600Ø
where P is the efficiency in (%), D t is the diameter of the
tank, S c is the slope adopted at all project sites (10H:1V),
V s is the settling velocity of the particle, W is the vertically upward velocity (W = (4Q s/πd 2), Q s is overflow
discharge (Q i–Q 0), Q i is inlet discharge, and Q 0 is flushing
discharge.
Computation of eiciency by Ather method
he eiciency computation method using M. Ather relation
(Athar et al. 2002) is as follows:)]
[( ) ( ) ( ) (
Zh
Qw2
Qu
𝜔d
,
,
,
𝜂0 = f
(3)
Qi
hp
𝜈
gRT3 hp2
where Qi is discharge in the inlet channel, Qu is discharge
flushed out through the under flow, ω is fall velocity of
sediment, d is the sediment size, hp is the depth of flow
at periphery of the chamber, Zh is the elevation difference
between inlet and outlet channel beds at their junctions with
iSH JournAl oF HydrAulic EnGinEErinG
Tareila SHP
60%
Efficiency
from G.S.D
Curve
40%
20%
0%
0.5
1
Particle size (mm)
Efficiency in (%)
100%
80%
60%
Efficiency
from G.S.D
curve
40%
20%
0%
0.5
1
Downloaded by [gurdeep singh] at 18:54 06 January 2016
Particle size (mm)
Efficiency
from Camp
dobbins
curve
Efficiency
from G.S.D
curve
Efficiency in (%)
80%
60%
40%
20%
0%
0.5
1
Efficieny
from Garde
et al
method
Aleo Manali SHP
Iku-II SHP
80%
60%
Efficiency in (%)
60%
40%
20%
0%
0
0.5
1
Efficiency
from G.S.D
curve
40%
20%
0%
0
Efficieny
from Garde
et al method
Particle size (mm)
0.5
1
Particle size (mm)
Efficieny
from Garde
et al method
DrinidharSHP
Efficiency
from camp
dobbins
curve
Efficiency
from G.S.D
curve
100%
80%
60%
40%
20%
1
Efficieny
From Garde
et al method
1
Efficiency
from camp
dobbins
curve
Efficiency
from
G.S.D
curve
Efficiency
from
Garde et al
method
0%
0
0.5
Particle size (mm)
Baragran SHP
100%
Efficiency in (%)
Efficiency
from camp
dobbins
curve
Efficiency
from G.S.D
curve
80%
Efficiency
from camp
dobbins
curve
100%
(h)
100%
1
Efficieny from
Garde et al
method
Particle size (mm)
Particle size (mm)
(g)
0.5
0
(f)
100%
0
20%
0%
Efficiency
From Garde et
al method
Upper Khauli SHP
(e)
Efficiency
from G.S.D
curve
40%
(d)
Efficiency
from Camp
dobbins curve
0
60%
Efficiency
from Garde
et al method
Baner-III SHP
(c)
Efficiency
from Camp
dobbins curve
80%
Efficiency in (%)
80%
100%
Efficiency in (%)
Efficiency in (%)
100%
0
Tareila-II SHP
(b)
Efficiency
from Camp
doddins
curve
Efficiency in (%)
(a)
5
80%
60%
40%
20%
0%
0
0.5
Particle size (mm)
Figure 6. (a)–(n) Eiciency vs. particle size (mm) of settling basin at diferent SHP station (Singh and Kumar 2013).
the vortex chamber, RT is the radius of the vortex chamber, g
is the gravitational acceleration, v is the kinematic viscosity,
and k is a coefficient.
Evaluation of eiciency of settling/vortex settling basin
observed data
Eiciency of settling/vortex settling basin at project sites is
evaluated by comparing the GSD curve at inlet and lushing
outlet of the basin. Eiciency at project sites (Singh and Kumar
2013) is computed as follows:-
𝜂site =
% of particular dia of particle at flushing outlet
(4)
% of particular dia of particle at inlet
SHP stations for study
Diferent SHP project stations of medium and high head with
diferent designed discharge, diferent installed capacity in
Himalayan region located mainly in Himachal Pradesh, India
were selected and visited.
Features of Settling basin and Vortex sediment settling
basins are given in Table 2(a), and (b), Figure 3 shows the
locations of SHP stations in Himachal Pradesh, India (Singh
and Kumar 2013) (Figure 5).
G. SinGH And A. KumAr
Sarbari SHP
(i)
100%
Efficiency in (%)
Jirah SHP
(j)
Efficiency
from camp
dobbins curve
80%
Efficiency
from G.S.D
curve
60%
40%
Efficieny from
Garde et al
method
20%
Efficiency
from camp
dobbins
method
100%
80%
Efficiency in (%)
6
Efficiency
from G.S.D
curve
60%
40%
0%
0%
0
0.5
1
0
Particle size (mm)
(k)
(l)
Tosh SHP
Efficiency
from camp
dobbins
curve
40%
20%
Efficieny
from
Garde et al
method
0%
0.5
1
Particle size (mm)
60%
Efficiency
from Garde et
al method
40%
20%
0
0.5
1
Particle size (mm)
Patikari SHP
(n)
100%
100%
Efficeincy
from camp
dobbins
curve
80%
60%
Efficiency in (%)
Efficiency in (%)
Efficiency
from G.S.D
curve
80%
0%
Gurhan SHP
Efficiency
from G.S.D
curve
40%
20%
0.5
1
Efficency from
camp dobbins
curve
80%
60%
Efficiency from
G.S.D curve
40%
Efficiency from
Garde et al
method
20%
Efficieny
from Garde et
al method
0%
0
Efficiency
from camp
dobbins curve
100%
Efficiency
from
G.S.D
curve
60%
(m)
1
Bramganga SHP
Efficiency in (%)
Efficiency in (%)
80%
0
0.5
Particle size (mm)
100%
0%
0
0.5
1
Particle size (mm)
Particle size (mm)
Figure 6. (continued)
Bhuri singh SHP
(a)
Efficiency
from Ather
Relation
60%
40%
Efficiency
from G.S.D
curve
20%
0%
0.2
0.4
0.6
0.8
Efficiency
from Paul
relation
100%
80%
Efficiency in (%)
80%
0
Gaj SHP
(b)
Efficiency
From Paul
RElation
100%
Efficiency in (%)
Efficiency
from Ather
Relation
60%
40%
Efficiency
from G.S.D
curve
20%
0%
1
0
Particle dia (mm)
0.2
0.4
0.6
0.8
1
Particle dia (mm)
Khauli SHP
(c)
Efficiency
from Paul
relation
100%
Efficiency in (%)
Downloaded by [gurdeep singh] at 18:54 06 January 2016
Efficiency
from Garde
et al
method
20%
80%
60%
Efficiency
from Ather
Relation
40%
20%
0%
0
0.2
0.4
0.6
0.8
1
Efficiency
from G.S.D
method
Particle dia (mm)
Figure 7. (a)–(c) Eiciency vs. sediment size (mm) of vortex sediment settling basin at diferent SHP station (Singh and Kumar 2013).
iSH JournAl oF HydrAulic EnGinEErinG
Results and discussion
Comparative eiciency of settling basins
he eiciency of settling basin for each SHP station computed using diferent methods described above is shown as
Figure 6(a)–(n).
From above, it is observed that actual eiciency of most of
the settling basin is less than the eiciency computed using
diferent relationships.
Comparative eiciency of vortex sediment settling
basins
he eiciency of vortex sediment settling basins computed
using diferent methods described above is shown in Figure
7(a)–(c).
Downloaded by [gurdeep singh] at 18:54 06 January 2016
Conclusions
Performance evaluation of desilting basins was carried out for
a number of desilting basins in various locations of Himachal
Pradesh, India. Following conclusions may be drawn for both
types of desilting basin respectively.
Settling basin
(a) hough dimensions of the settling basin under study
were suicient to trap the particles less than 0.2 mm
(mostly recommended minimum size for removal),
observed eiciency of settling basin was found to be less
and may be attributed to:(i) Turbulence in water leading sediment in suspension.
(ii) Transitions were not designed and executed properly.
(iii) Inadequate sediment lushing arrangements.
(b) hese settling basins mostly were designed for continuous lushing specially during monsoon which mostly
time was not observed resulting in choking the lushing
ducts and decreasing eiciency of the basins.
Adequate design and execution of transitions as well as proper
arrangement operation of silt removal of silt removal arrangements be ensured for eicient operation of settling basin (Singh
and Kumar 2013).
Vortex settling basin
he observed eiciency of vortex settling basin at site is close
to designed eiciency computed using diferent methods for
all particles. Further, these basins required less volume of water
to remove the sediment and prove to be economical and eicient desilting device, especially for the removal of particle size
0.1–0.2 mm (Singh and Kumar 2013).
In settling basin, the length of the basin should be such that
the particle will settle on covering that much distance, whereas
in Vortex settling basin, the diameter of basin is kept that much
so that sediment particles present in the low would cover a
7
helicoidal path towards the oriice, thereby obtaining a long
settling length compared to the basin dimensions.
By keeping discharge (Q), Sediment concentration (ppm)
low velocity (v), settling velocity (w) constant for a given type
of sediment particle the length of Basin (in case of settling
basin) and diameter of basin (in case of vortex settling basin)
will govern the eiciency of desilting basin.
A comparative study by Badrinath and Bhardwaj “Vortex
Desilting Tanks for Sediment Exclusion For small Hydro
Projects” proceedings of design of hydraulic structures Dept.
of civil egg. UOR, Roorkee pp. 283–291 (1994) concluded that
vortex settling tanks are highly eicient, 55% cheaper and lesser
land.
As criteria for designing the most of desilting basin (under
study) designed to remove 0.25 mm particle completely, but
from the eiciency curves it has been shown that the most of
desilting basins do not perform with 100% eiciency removal
of 0.25 mm particle but removal eiciency of Vortex settling
basin was found higher that settling basin. To achieve more
accurate results, model studies should be carried out for a project having same parameters for both types of desilting Basin.
hus, the comparative study of settling basin and vortex
settling basin shows that vortex settling basin is eicient and
economical desilting device as compared to settling basin for
small hydropower stations.
Acknowledgment
he author express the gratitude to SHP plant owners for providing the
details of their SHP stations and allowing the access to their SHP station
for ield observation and investigations. he corresponding author is
thankful to IITR administration and MHRD for providing assistantship
for carrying out the study as Master of Technology dissertation work.
Disclosure statement
No potential conlict of interest was reported by the authors.
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