dc.contributor.advisor |
Bhuiyan, Dr. Muhammed Ali |
|
dc.contributor.author |
Zakir Ahmad |
|
dc.date.accessioned |
2015-05-18T09:25:40Z |
|
dc.date.available |
2015-05-18T09:25:40Z |
|
dc.date.issued |
2006-08 |
|
dc.identifier.uri |
http://lib.buet.ac.bd:8080/xmlui/handle/123456789/375 |
|
dc.description.abstract |
Groundwater is the primary source of safe water to meet the essential demands of
people in Bangladesh. Dhaka the capital city, with its enOlmous population takes a huge
toll on its groundwater resources. In order to meet this growing demand various
organizations mainly DWASA and private users have already installed nearly 2000 high
capacity DTWs. Continuous pumping with so many wells from an area less than 450 km2
has rendered the groundwater resources in stressed condition. This is likely to cause some
adverse environmental impact like land subsidence. Many countries of the world have
already experienced land subsidence of severe magnitude due to excessive groundwater
pumping. Formation beneath the city of Dhaka is also susceptible to such phenomenon.
This gives an early indication for an urgent need to alleviate pressure on the upper aquifers
being exploited and explore for more suitable and sustainable sources to supplement the
present water supply.
DWASA is entrusted with supply of piped water to Dhaka Metropolitan City and
its adjacent area. At present 75% city area is under DWASA water supply coverage, out of
which 82% is from groundwater sources. In an attempt to find alternate sources DWASA
has started exploiting the deep aquifer at a depth of around 300 m. But the source and
recharge mechanism of this aquifer is yet unknown and can not support the development of
.J a long tenn strategy for water supply of Dhaka City.
From the previous studies, the development of Ground Water and Land Subsidence
Model by EPC and MMP (1991) and its updating by BUET (2000) have been the most
important and relevant to the present study. In the wake of recent development the
previous model has become an inadequate tool to simulate the deep aquifer. So the current
A, study was undertaken to setup a groundwater and land subsidence model that is flexible
enough to simulate deep aquifer system and any other new changes. A versatile
groundwater modeling tool called 'MODFLOW-2000 with Argus ONE' has been used for
the current study.
MODFLOW-2000 uses the coupling of law of conservation of mass and Darcy's
equation to simulate groundwater flow. The subsidence module is integrated into
MODFLOW -2000 to compute the land subsidence using the groundwater model. The
subsidence is computed basing on the Terzaghi's theory of one dimensional consolidation.
The groundwater model under the current study covers an area of 8,778 km2 and
includes the districts of Dhaka, Manikganj, Gazipur, Narshindi, Narayanganj and
Munshiganj. The model area is discretized to 500 m grid inside Dhaka City. In the vertical
direction the model is defined by 6 geologic layers. The model was calibrated by matching
the hydro graphs within and outside the Dhaka Region. The calibrated model was then used
to estimate the land subsidence in and around Dhaka City.
The simulated hydrographs at important places of Dhaka City confirms the
declining trend of groundwater level. The piezometric levels at Motijheel and Gulshan are
found to be -52 and -43 m PWD respectively in December 2004. The corresponding
subsidence as estimated by the model is maximum 4.9 cm. Results of model scenario runs
indicate that the groundwater in the upper Dupi Tila aquifer would stabilize by April 2006
if no increase of abstraction is allowed after December 2004. Subsidence results for the
same scenario shows that subsidence almost ceases with the stabilization of groundwater.
Results of another scenario shows abstraction from deep aquifer with 94 wells in operation
would deplete the groundwater by 20 m in 2020. But the situation in deep aquifer can only
be confirmed after collecting observed data for a complete hydrological cycle.
If the current situation prevails the condition in the upper aquifers will worsen and
many existing wells will go inoperative. Recharge from rainfall has become negligible due
to lowering of water level and increased urbanization. The reduced storage capacity of the
aquifers may cause land subsidence of such magnitude that may affect life and property.
All these facts suggest that a comprehensive policy must be undertaken to counter/prevent
the possible adverse effects on groundwater resource of Dhaka City. |
en_US |
dc.language.iso |
en |
en_US |
dc.publisher |
Department of Water Resources Engineering |
en_US |
dc.subject |
Water,Underground-Dhaka city |
en_US |
dc.title |
Study on groundwater depletion and land subsidence in Dhaka city |
en_US |
dc.type |
Thesis-MSc |
en_US |
dc.contributor.id |
040416019 F |
en_US |
dc.identifier.accessionNumber |
102847 |
|
dc.contributor.callno |
551.490954922/ZAK/2006 |
en_US |