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Fresh concerns over safety of Mullaperiyar dam
By Our Special Correspondent
THIRUVANANTHAPURAM, DEC. 13. The occurrence of an earthquake of
the magnitude of about 5 on the Richter scale has raised fresh
concerns about the safety of the Mullaperiyar dam.
While some experts are of the view that the dam has long
outlived its normal life, others maintain that it can continue in
service because of the strengthening works undertaken by the
Tamil Nadu Government. However, engineers of Kerala and Tamil
Nadu do not see eye to eye on the subject. And the earthquake has
changed the position further.
Tremors had been occurring in and around the Idukki reservoir
ever since the dam was filled. There is not much data on whether
tremors had occurred before the commissioning of the dam.
Seismographs had been put up at Kulamavu and other places only
with the construction of the Kulamavu dam.
Most of the tremors recorded there were of such low magnitude
that the local people had not come to notice them. As a
correlation had been noticed between the filling and emptying of
the reservoir, scientists had suggested that these could be
reservoir-induced. However, subsequent tremors put certain
questions marks on this assumption. The magnitude of the tremors
was expected to come down as the geological formations under the
reservoir had `settled down'. However, this was not happening.
The tremor at Nedumkandam in 1988 measured 4.5 on the logarithmic
Richter scale. The after-shocks measured 4.1 and 3.8 on the
scale. It has been more or less confirmed now that yesterdays's
shock was of the magnitude of 5 on the scale. The after-shocks
also came close to this reading. In 1994, a shock of the
magnitude of 4.3 on the Richter scale occurred at Wadakkanchery
followed by another of the magnitude 3.0 in 1996. In between, a
number of tremors of lower magnitudes have occurred in different
parts of Kerala and Tamil Nadu. This pointed to tectonic activity
in the area.
Idukki and its surrounding areas now have about a dozen large
reservoirs, the oldest being Mullaperiyar. Most of them are over
geological fault lines. Moreover, many of the slopes in the
catchment areas are unstable. This increases the risk of large
chunks of earth falling into reservoirs leading to dam failure.
(The failure of the arch dam at Viont in Italy had occurred this
way). The Mullaperiyar, which was built before tectonic studies
became a norm for dam design, is prone to damage from quakes.
This is especially true of the Baby dam. In the recent non-
destructive testing of Baby dam by the Central Soil and Material
Research Station, fissures had been found inside the dam
structure. Further studies would be required to see how far the
main dam structure would withstand quakes.
The risk here is not the collapse of the Mullaperiyar dam alone.
If the dam gives way when the reservoir level is high in both
Idukki dam and Mullaperiyar, Idukki would not be able to hold the
inflow. Idukki dams are designed to withstand earthquakes.
However, the spillways at Cheruthoni do not have the capacity to
release such a flow and keep the dam safe. Many dam failures
across the world had occurred because of deficiency of spillways.
In the case, earthquakes and landslides can compound the problem.
Meanwhile, the Kerala State Electricity Board authorities are
examining the dams under it for any damage from the quakes.
However, their observations would be severely limited from the
fact that several of the instruments for monitoring the dams are
not functional. Some have malfunctioned in the past and gave
wrong readings. The stress strain meters in the Idukki arch dam,
for example, gave values in the nineties that suggested that the
dam would burst.
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