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Abstracts
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Tuesday, 17 February 2009 10:56 |
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Bacterial Study of Groundwater in Sub-Himalayan Region of Muzaffarabad, Azad Kashmir. Pakistan J. Environ. Sci. Vol 1; N0. 2; Jan. 2002. Geologically the area of study is located at the core of the Hazara Kashmir Syntaxis where Precambrian to Recent rock units are exposed. The drinking water in Muzaffarabad is available from three main sources; 1) The Springs; 2) The River; 3) The Streams. Among all these sources, the spring water is usually considered the most economic and reliable source of potable water, but the springs are polluted by fecal contaminations marked by coliform organisms and trace elements i.e. P, B and Pb. The most apparent reason of groundwater contamination is frequent use of septic tanks (for domestic water disposal) and uncontrolled disposed off liquid and solid wastes generated by the community. The springs presents at the lower topographic level and those emerging from alluvial terraces are mainly affected by sewage system in the area. Not only groundwater but also the treated water is not free from micro-organisms which arises a variety of health based problems in the community. Diarrhea, enteric fever and Bicolli dysentery are the mot common water born infections which become more serious in summer when receptivity of infectious bacteria is increased in human recipients. It was concluded that geology of the area provides environment for bacterial growth, even in treated water in terms of suspended load derived from different geological formations. The suspended load reduces the efficiency of Chlorination operation in the treatment process which provides space for bacterial growth. Author(s): M. Arshad Khan, M. Ashraf and Tariq Bashir Institute of Geology, University of AJ & K, Muzaffarabad. |
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Last Updated on Tuesday, 28 April 2009 12:48 |
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Friday, 13 February 2009 11:17 |
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Investigation of Toxic Elements in Groundwater of Kalalanwala Area near Lahore The section of news appeared in media in last week of July 2000 that deformed bones in children of village Kalalanwala are causing unrest among the people and scared villagers are seeking help. The fluoride content in some drinking water samples reportedly analyzed by PCSIR were as high as 40 ppm. A group of environmental researchers from Geoscience Laboratory, Geological Survey of Pakistan made a program to investigate the possible contamination of geological importance in the groundwater of the area. The sample collected from the village Kalalanwala/Kot Asadullah near Manga Mandi, Lahore were analyzed for fluoride and arsenic in water, being used by residents of the locality. The area under investigation is a flood plain of river Ravi, where the fine silt and clay deposits during flood-seasons and it encourages the agriculturist to use the fields to cultivate for common crops. Since two decades the area is being developed as industrial zone specially Chunian and Kasur, and for the last five years the Kalalanwala and nearby area are being exploited for various industries. Modern instrumentation facilities of the high-tech Geoscience Laboratory were used to analyze the samples. The concentration of fluoride was found in the range of 1.4 to 22 mg/L and the As contents ranged from 50 to 920 ug/L, both being beyond the threshold EQS (environmental quality standards) values (i.e., F=0.8mg/L and As 20ug/L) and thus this water is not suitable for life. The investigations were also carried out for other elements like Zn, Cr, Cd, Ni, Co, Pb and Hg in addition to the usual parameters. Whereas the other laboratories were emphasizing on fluoride only, this team discovered the presence of another important toxic element arsenic in the samples collected from the affected area, which poses the real threat to the human life. The contents of Ca were found less than usual, thus deficiency of calcium is probably one of the possible factor in deforming the bones. By the time it is established that the bone deformity cases are being reported from whole of the area stretching through Shanki Bhattian to Kot Radha Kishan. This research will definitely open new venues for other scientists around the globe. Author(s): Muhammad Naseem, Abida Mumtaz Farooqi, Dilshad Masih and Muhammad Anwar Geoscience Lab, GSP, Islamabad, Pakistan. |
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Last Updated on Monday, 17 August 2009 12:06 |
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Friday, 13 February 2009 11:15 |
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An Account of Waterlogging and Salinity Problems and Remedial Measures in Pakistan Irrigation in the Indus Plain is being practiced along Indus River since the earliest settlements, thousands of years ago. Before the induction of weir controlled irrigation in the nineteenth and early twentieth century, the water table was quite deep in the Indus plain. But due to deep percolation of seepage water from the unlined canals and on-farm irrigation, and without adequate drainage, a new increment of recharge was added to the groundwater regime of the Indus basin resulting into creation of severe perils of waterlogging and salinization of the soils in many parts of the country, affecting agricultural production. This problem was further aggravated due to construction infra structures, semi-arid climatic conditions, flat topography, poor natural drainage, porous soils, seepage from unlined irrigation channels and inefficient irrigation management. During late fifties, these problems became so serious that these became the biggest environmental issues and gigantic threat to the sustainability of irrigated agriculture in the country. It was estimated that about 40,000 ha of irrigated land was being lost due to waterlogging and salinity every year.
The responsibility for tackling this problem was assigned to Water and Power Development Authority (WAPDA) by the Government of Pakistan in 1958. Since then, a number of Salinity Control and Reclamation Projects (SCARPs) were launched by WAPDA and 57 SCARPs were completed so far. In addition to these completed SCARPs, a number of drainage projects in all provinces are in various stages of completion. The SCARPs mainly consisted of installation of tubewells, construction of surface and pipe drains and construction of intercepter drains. The paper gives brief information on the extent of problems of waterlogging and salinity in the country, the remedial measures undertaken and the results achieved so far. author(s): G. Sarwar, Muhammad Ramzan Ch. And Muhammad Nawaz Bhutta International Waterlogging and Salinity Research Institute (IWASRI) 13 West Wood Colony, Thokar Niaz Baig, Lahore. |
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Last Updated on Tuesday, 28 April 2009 12:49 |
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Friday, 13 February 2009 11:13 |
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Effect of Biological Contamination on the Water Quality in Wah Cantt. Area, Pakisatn. Third South Asia Geological Congress Lahore, Pakistan. Four aquifer layers exist in the area. Shallow aquifer layers are being contaminated through dug wells. A number of water samples tested for biological contamination using Double Tube Method reveal the migration of coliform bacteria through soil and disposed off water to the nearby dug wells used for domestic supply. On the basis of MNP (Bacteria Count) the area has been divided into four sectors. These sectors can be related with geological and hydro-geological conditions. An infra-formational fault detected in the area is ‘preventing’ migration of coliform from shallow to deeper aquifer layers. Fresh water hyphomycetes have been detected for the first time in the area. All the layers especially shallow aquifers show severe level of biological contamination that has crossed the WHO and USEPA recommended limits. Author(s): M. H. Malik and Sajid Rashid Institute of Geology Punjab University Lahore Pakistan M. Saleem Khan Khanpur Dam, Pakistan.
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Last Updated on Tuesday, 28 April 2009 12:49 |
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Friday, 13 February 2009 11:12 |
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Need for a Rational Water Policy in South Asia South Asia is a contiguous terrain where one ecosystem smoothly transgresses into another. The Himalayan Mountain Range is a common pivotal feature to all South Asian nations, barring Sri Lanka and Maldives, which is both a blessing and a curse. Blessing as it is the mother source of many important waterways providing enormous benefits to all the nations, through which they traverse, and a curse, as harnessing these water-bodies almost always become a bone of contention among the riparian nations Harnessing these water-bodies too has played its crucial role in perpetuating preexisting suspicion and betterness among the countries of the South Asia. In this context, an in depth analysis of a few bilateral treaties and agreements on international rivers, flowing in South Asia, sharply brings out the fact that there is an acute need for a rational water policy in South Asia. The treaty agreements between India-Bangladesh, India-Nepal, India-Pakistan and India-Bhutan have been discussed and analyzed for this purpose. The analysis also reveals that India, irrespective of its position as lower or upper reparian state, has taken the maximum possible advantage while harnessing the international rivers of South Asia, true to its image of regional superpower in this part of the globe, at the cost of undermining the interests of people of its smaller neighboring countries. As a matter of fact, the Indian water policy in South Asia is merely an extension of its domestic water policy (if such a thing really exists), which has resulted in deprivation and dispossession of poor people and benefited and enriched upper rural and urban elite. In the case of Nepal and Bhutan, it has succeeded in getting itself maximum benefits, in the case of Bangladesh it has used water of Farraka as a tool to harass ruling party whenever they acquire anti-India posture and in the case of Pakistan it has started making its own interpretation to the international Indus Treaty. By taking all this into account, one cannot escape the conclusion that India is the root-cause of all the water related disputes in South Asia. In the light of above, a broad outline a rational water policy for South Asia has been evolved which is in congruence with the guidelines framed by the International Law Commission and the resolution passed at the United Nations General Assembly for sharing of international reparian waters. Author(s): Arun Kumar Singh D-5, II Floor, Amar Colony, Lajpat Nagar, IV, New Delhi, India. |
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Last Updated on Tuesday, 28 April 2009 12:49 |
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