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Langtang Water To Kulekhani Via Kathmandu By AB Thapa The Melamchi Water Supply
Office had brought out in their web site
comments on the articles on Melamchi
project published in this journal some time
back. Such prompt reaction of the Melamchi
Office in defense of their plan deserves
to be taken up positively. It has
provided an opportunity to bring forward to
the notice of the general public various
technical, economic and policy issues related
to this project. This article is the
continuation of the previous article published
very recently in this journal on April
25 on Melamchi Office comments. Is It Only A
Dream ? It is not a
surprise that many people would have
apprehension that the proposed Langtang
water diversion into the Kulekhani reservoir
through Kathmandu could be nothing more
than a dream. The grandiose of the title
of the total plan itself can confuse
anybody. They can easily be misled.. The
whole concept can be much more easily
understood if each element of this
diversion plan is explained separately. Before
going any further to present the plan
to divert the Langtang river into the
Kulekhani we need to be very clear
that according to the existing Melamchi project
plan about 40 kilometers long tunnel would
have to be built anyhow to cater the
demand for water supply in Kathmandu
valley from 2011 onward. Out of such
total length of the tunnel, the length of
the Melamchi tunnel would be 28 kilometers
and the length of the Yangri and Larke
diversion tunnel about 12 kilometers. The
Melamchi tunnel hydropower is also
a component of the original Melamchi
water supply project plan prepared under
the UNDP assistance though. it is now
considered to drop this component despite
the fact that the UNDP study had
recommended to provide the hydropower because
it could contribute to reducing the cost of
drinking water to Kathmandu residents. Let us now look
into the NEAís plan to divert
the Langtang river at Ghore Tabela for
power generation. Even according to the
Melamchi Water Supply Officeís reporting the
Langtang diversion is an excellent power
project. It is proposed to discharge the
Langtang water after the power generation
directly into the Trisuli river. Now we
come to the crux of the problem. What
is going to happen if the plan of
the water resources ministry to divert
the Langtang river at Ghore Tabela for
the generation of electricity is combined
with the plan of the water
supply ministry to deliver additional water to
Kathmandu valley on top of the Melamchi
water? Will such plan to generate
electricity nicely dovetail with that of
the water supply ministry ? What would be
the comparative advantage of such multipurpose project
vis--vis two separate projects delinked with
one another ? It can hardly be denied
that it is the duty of the NATIONAL
PLANNING COMMISSION to examine such
possibilities. Nonetheless it also is the
obligation of each individual ministry to
insure that every aspect of the project
within its jurisdiction is honestly examined
in the broader interest of the country. If the alignment
of the tunnel to draw Langtang
water at Ghore Tabela for power
generation is changed and the water after
the power generation is led into the
Melamchi river as against the original plan to
discharge into the Trisuli river, there might
be even slight decrease in the total
combined cost of the Melamchi water supply
project and the Langtang power project.
However, such rerouting of the Langtang power
tunnel could open up completely new
vistas of possibilities for the generation of
cheap electricity. In this brief article
three separate components of the Langtang
diversion into the Kulekhani have been
examined. To a certain extent each of these
three components can also be seen as
a separate project independent of one
another. The first would be the Langtang
diversion at Ghore Tabela. What would
happen if the Langtang river is diverted
into the Melamchi instead of the
Trisuli river ? The next would be the
Langtang storage dam at Jaithang and its contribution
towards the augmentation of the dry season
flow of the Melamchi and Kulekhani rivers.
The third is the diversion of the
combined flow of the Langtang and Melamchi
rivers into the Kulekhani reservoir. Langtang Diversion into
Melamchi According to the NEA
study the minimum flow of the Langtang
river at Ghode Tabela is about 4 cumecs.
Such flow could be more than the
combined flow of the Yangri and Larke
rivers. There is a level difference of
about 1600 meters between Ghore Tabela and the
Trisuli river. It is planned to utilize
this big head to generate power and for
this purpose a 12 km long power
tunnel would be necessary. It would be possible
to obtain a total gross head
of about 1600 meters or even more
if the Langtang water is conveyed
to the Melamchi river instead of diverting it into
the water surplus Trisuli river. Such diversion could be
a substitute for the diversion of the Yangri and Larke rivers to
augment the flow of the Melamchi. It could, thus, spare us the trouble to cut off
the Larke and Yangri water supply to Indrawati hydropower stations for power generation.
A 20 km long power tunnel would be
needed to deliver the Langtang water
from Ghore Tabala to the Melamchi project intake
and such tunnel would have been 8
km longer than the power tunnel needed to
divert the Langtang water into the Trisuli
river. We should not forget that it would
be necessary by 2011 according to the
UNDP feasibility study of the Melamchi
project to build the 12 km long Larke and
Yangri diversion tunnels to augment
the dry season flow of the Melamchi
river. If the Langtang water is diverted
into the Melamchi river, it would not be
necessary neither to build the 12 km
long diversion tunnel to deliver the Yangri and
Larke waters into the Melamchi nor
to build the expensive headworks across those
two rivers to divert the water. Thus the
utilization of the Melamchi route for the Langtang river
power project would have involved
the construction of power tunnel 4 km
shorter in length and would also have
allowed to dispense with the construction of
expensive headworks across those two
rivers( Yangri and Larke). There would not be
any reduction in total gross head
for the power generation despite the
changes of the Langtang diversion
route from Ghore Tabela- Trisuli to Ghore
Tabela ñMelamchi. Out of the total gross head of 1620 m between the Ghore Tabela
and the Sundarijal tailrace, about 1300 m head would
be used by the Langtang hydropower that discharges water into the
Melamchi intake and the rest by the hydropower to be provided
near the entry point of the Melamchi tunnel into the
Kathmandu valley. Langtang Storage Dam at Jaithang The Langtang storage project is one of the
schemes identified in the UNDP supported Gandak Basin Master Plan study. According to the
UNDP study report a dam about 120-m in height is proposed on the Langtang river near
Jaithang. The total drainage area of the Langtang at Jaithang is 150 sq. km. as against a
drainage area of 250 sq. km. at Ghore Tabela. The volume of the reservoir would be about
180 million cubic meters. The elevation of the FSL would be 3995 meters which is well
below the permanent snow line. The Melamchi Water Supply office has provided information
in their web page that the height of the proposed Langtang storage dam at Jaithang should
be raised to 300 meters to arrive at a total storage volume of 180 million cubic meters.
It would be very much appreciated if they could provide further information in more
detailed form about the recalculated height of the Langtang storage dam that completely
disproves the findings of the UNDP supported Gandak basin study. According to the UNDP
study the regulated flow of the Langtang river is proposed to be tapped for power
generation only at Ghore Tabela about 15 km downstream at an elevation of 3028 meters.
However, it appears to be worthwhile to build another hydropower near the Ghore Tabela to
utilize the potential of the Langtang river between the diversion dam at Ghore Tabela and
the storage dam at Jaithang. The hydropower would be directly drawing water from the
storage reservoir. There can be some concern about the
thickness of the river bed materials wherever a storage dam is proposed to be built.
Fortunately in case of the Langtang high dam, the bed rock might be found at lesser
depth because the gradient of the river is too steep. Another equally important
issue could be the glaciological problems which are briefly described hereinafter.
Threat From Langtang
Glaciers Glaciers occur exclusively
in mountainous regions above the snow line. Mountains
below the snow line carry only seasonal snow.
The snow line of the southern Himalayan region
is approximately at an elevation of 5000 meters
above the sea level. Snow accumulates and
glaciers are formed at heights above the
snow line. Constant avalanches of snow from the
slopes feed the upper reaches of the
glaciers. The surface layers of ice and
snow grow thicker. The glacier begins to
slide under its own weight and enters the
valley like tongue of moving ice. The part of
the glacier at elevation below the snow
line melts into water and such melted water is
drained into the river. The position of the
termini of the glaciers remains almost
unchanged if the phenomena such as the
retreating ( or advancing if it is opposite) of
the glaciers recently observed in the Himalayan
region are discounted. In case of the
Langtang storage dam at Jaithang
and its environs the full supply
water level in the storage reservoir
would be well below the level of
the snow line and thus at a
distance from the tongue of the Langtang
glacier. It is difficult to find any direct
relationship between the reservoir water level and
the existence of the Langtang glacier. However, it would
have been a completely different matter had
there been a glacier lake in between
the storage dam and the termini
of the glacier as in case of the Dig Tsho
glacier. In 1985 the Dig Tsho glacier lake outburst
flood (GLOF) completely destroyed the Namche
Hydropower station. Nonetheless it can not be
denied that a study of the Langtang
glaciers in full detail would have to be
an important part of the future feasibility
study of the Langtang storage dam project. Diversion from
Kathmandu to Kulekhani The diversion of the
surplus Melamchi and Langtang waters( initially without a
storage dam at Jaithang) from Kathmandu valley to the
Kulekhani reservoir could be a very simple
and at the same time the most cost effective
proposition despite the fact that at first
glance it might appear to be a highly complicated
engineering task. Let us take a hypothetical
case that we are going to draw only
4 cumecs water somewhere near Chobar out
of the combined flow of the Bagmati. Melamchi
and Langtang rivers. We might have to
build a 15 MW pump station to lift
the water to a height of about 300
meters above the river water level which
might be in height equivalent to the full
supply level (FSL) of the Kulekhani storage reservoir.
It is equally possible that instead of
one big pump station we might need several
small pump stations with a total
capacity of about 15 MW that would
be completely dependant on topography. A
15 km long waterway might be needed to
carry the water into the Kulekhani storage
reservoir out of it the length of the
tunnel could be about 9 kilometers. The
total cost of such diversion could be
about US $ 20 million After the completion of
the above described Langtang diversion into the
Kulekhani reservoir, there would be a net
increase of about 250 GWh firm power in
annual generation of the Kulekhani Nos 1,2&3
hydropower stations even after subtracting the energy
spent on pumping. Thus the additional
generation of the Kulekhani hydropower stations after
the Langtang diversion would be two times
greater than the present annual generation of
Kulekhani No 1 Station. It would be possible to
increase to such a great extent the
electricity generation absolutely without any
additional investment in civil structures and
electrical equipments of the Kulekhani dam
and hydropower stations. At present the NEA is
paying to the private developers at an average
rate of about US Cents 6 per KWh.
Out of such purchase, the firm energy is only
about 50% and the rest is secondary
energy. The purchase rate of the exclusively
firm energy could be about US Cents 9 per
KWh if it is presumed that 3 KWh
secondary energy would be equivalent 1 KWh firm
energy though in the World Bank supported Upper
Karnali Project feasibility study the seasonal
energy has been valued only at 10% of
the firm energy based on the expected net value
of such energy for the thermal fuel displacement. Thus
even a small scale Langtang diversion into
the Kulekhani could help to increase
the annual income of the Kulekhani hydropower
stations by a wide margin of US $ 22.5
million whereas the total investment in
the pumping system to deliver the water
into the Kulekhani reservoir could be only
about US $ 20 million. |
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editor: spotligh@mos.com.np |