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Journal articles on the topic 'Surface and ground water'

Author: Grafiati

Published: 2 June 2025

Last updated: 31 July 2025

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1

Kumar, Santan, Prabhash Kumar, and Surabhi Ranjan. "Ground and Surface Water Polluted in Manpur Block." International Journal of Trend in Scientific Research and Development Volume-2, Issue-2 (2018): 673–77. http://dx.doi.org/10.31142/ijtsrd9488.

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2

Heviánková, Silvie, Marian Marschalko, Jitka Chromíková, Miroslav Kyncl, and Michal Korabík. "Artificial Ground Water Recharge with Surface Water." IOP Conference Series: Earth and Environmental Science 44 (October 2016): 022036. http://dx.doi.org/10.1088/1755-1315/44/2/022036.

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3

itha, Kav, B. S. Polisgowdar, and Rubeena Tarranum. "Characterization of Surface Water and Ground Water Reservoirs." International Journal of Current Microbiology and Applied Sciences 9, no. 6 (2020): 4070–79. http://dx.doi.org/10.20546/ijcmas.2020.906.476.

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4

Chin, David A., and Xing Qi. "Ground Water under Direct Influence of Surface Water." Journal of Environmental Engineering 126, no. 6 (2000): 501–8. http://dx.doi.org/10.1061/(asce)0733-9372(2000)126:6(501).

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5

Daniel, John A., and James A. Staricka. "FROZEN SOIL IMPACT ON GROUND WATER-SURFACE WATER INTERACTION." Journal of the American Water Resources Association 36, no. 1 (2000): 151–60. http://dx.doi.org/10.1111/j.1752-1688.2000.tb04256.x.

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6

Adsule, A. A., and Dr G. S. Kulkarni. "Comparative Analysis of Ground Water and Surface Water of Kolhapur based on various Physico-Chemical Parameters." International Journal of Trend in Scientific Research and Development Volume-2, Issue-4 (2018): 301–4. http://dx.doi.org/10.31142/ijtsrd12899.

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7

Santan, Kumar, Kumar Prabhash, and Ranjan Surabhi. "Ground and Surface Water Polluted in Manpur Block." International Journal of Trend in Scientific Research and Development 2, no. 2 (2018): 673–77. https://doi.org/10.31142/ijtsrd9488.

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Human activities are considered to be contamination. Every persons wants clean water for drinking, bathing and other domestic uses, but not everybody appreciates the fact that our own actions are often the worst enemy in achieving that goal. Ground water is one of the most misused and misunderstood resources. Because ground water and its movement, and consequently also its pollution, is hidden from view beneath the land surface, the seriousness of ground water pollution problems has not been recognized until recently. The sources of manpur block ground water pollution are many and varied becau

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8

Salam, SMA, MA Mollah, A. Tasnuva, and MR Zaman. "Physicochemical Evaluation of Ground and Surface Water of Mohanpur Upazila of Rajshahi District." Journal of Environmental Science and Natural Resources 5, no. 2 (2013): 275–80. http://dx.doi.org/10.3329/jesnr.v5i2.14830.

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Surface and ground water samples of Mohanpur Upazila of Rajshahi district have been analyzed in order to check its quality especially for drinking, fish culture, irrigation and industrial purposes. The water supplies were analyzed for pH, temperature, electrical conductivity, chloride, hardness, alkalinity, manganese (Mn), lead (Pb), cadmium (Cd) and arsenic (As). All water samples were tasteless at the time of collection. pH values for surface water were 7.72-8.61 and those of ground water were 6.87-710; Total hardness for surface water was 112-181 ppm and ground water was 224-400 ppm as CaCO

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9

Mandlik, Prof D. N. "Increasing Ground Water Level by Penetrating Surface Runoff." International Journal for Research in Applied Science and Engineering Technology 9, no. VII (2021): 1194–97. http://dx.doi.org/10.22214/ijraset.2021.36511.

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System proposed in this paper is the planned filtrating penetration system to harvest the surface runoff like storm water into our designed unit in order to increase the natural level and replenishment of ground water resources. Ground water recharge is increasing in popularity as ground water resources are being depleted due to excess of water extraction of water from boreholes in the urban areas. Although the primary objective of this technology is to preserve or increase ground water resources, this kind of artificial recharge has been used for many other beneficial purposes. These include

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10

Rossi, P., N. Dörfliger, K. Kennedy, I. Müller, and M. Aragno. "Bacteriophages as surface and ground water tracers." Hydrology and Earth System Sciences 2, no. 1 (1998): 101–10. http://dx.doi.org/10.5194/hess-2-101-1998.

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Abstract. Bacteriophages are increasingly used as tracers for quantitative analysis in both hydrology and hydrogeology. The biological particles are neither toxic nor pathogenic for other living organisms as they penetrate only a specific bacterial host. They have many advantages over classical fluorescent tracers and offer the additional possibility of multi-point injection for tracer tests. Several years of research make them suitable for quantitative transport analysis and flow boundary delineation in both surface and ground waters, including karst, fractured and porous media aquifers. This

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11

Hsieh, Ping-Cheng, and Susan Bolton. "Laminar Surface Water Flow over Vegetated Ground." Journal of Hydraulic Engineering 133, no. 3 (2007): 335–41. http://dx.doi.org/10.1061/(asce)0733-9429(2007)133:3(335).

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12

Lin, Henry. "Surface and Ground Water, Weathering, and Soils." Journal of Environmental Quality 35, no. 5 (2006): 1967–68. http://dx.doi.org/10.2134/jeq2006.0618br.

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13

Satvinder Singh, M P Kaushal, and Satwinder Singh. "Augmenting Ground Water Recharge Through Surface Drains." Journal of Agricultural Engineering (India) 43, no. 2 (2006): 37–40. http://dx.doi.org/10.52151/jae2006432.1173.

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An existing mathematical model correlating runoff with recharge rate in a drain was used to determine the recharge rate through a surface drain. Two flow conditions were considered namely, free flow and detained flow. Detained flow conditions were made through a series of checks along the drain. Thirty years of rainfall values in the monsoon period was given as input to the model to yield runoff Recharge in the Raipur Link drain, Distt. Ludhiana. Punjab occurring due to runoff was determined. On an average, recharge caused by the runoff in the drain was 3% of the rainfall when the flow was det

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14

Nishioka, Mito, Megumi Yamashita, and Hirotaka Saito. "Influence of Radiative Components and Meteorological Conditions on Simulation of Slope-Specific Heat Balance." Journal of Environmental and Engineering Geophysics 28, no. 2 (2023): 75–90. http://dx.doi.org/10.32389/jeeg22-011.

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Fields have uneven surfaces, such as ridges, and the shortwave radiation of fields differs depending on the orientation of the slope of the unevenness, resulting in variations in the distribution of moisture on the ground surface. Therefore, it is necessary to estimate the heat and water balances spatially, taking into account the variation of the moisture distribution on the ground surface. Previously, one-dimensional simulations have been used to estimate the heat and water balance of non-sloping surfaces. To estimate the heat and water balance spatially while taking into account ground surf

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15

Ejaz, Muhammad Shafqat, and Richard C. Peralta. "Maximizing conjunctive use of surface and ground water under surface water quality constraints." Advances in Water Resources 18, no. 2 (1995): 67–75. http://dx.doi.org/10.1016/0309-1708(95)00004-3.

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16

Zorapapel, George(Bebe)T, and Mladen Vucetic. "The Effects of Seismic Pore Water Pressure on Ground Surface Motion." Earthquake Spectra 10, no. 2 (1994): 403–38. http://dx.doi.org/10.1193/1.1585780.

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The effects of the gradual buildup of seismic pore water pressures and associated degradation of stiffness on the ground surface motion are examined for shallow saturated liquefiable deposits. Ground surface displacements and accelerations, the Fourier Transforms of the acceleration-time histories and layer gain factors are analyzed. The analysis is based on the ground surface and sub-surface accelerations and pore water pressures recorded at sites that either fully liquefied or built up considerable pore water pressures during strong earthquakes. The analysis shows that: (i) the seismic pore

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17

Abdullateef Abdullahi Ibrahim, Muhammad Abdullahi Ibrahim, and Ali Gambo Yusuf. "Implications of industrial effluents on surface water and ground water." World Journal of Advanced Research and Reviews 09, no. 03 (2021): 330–36. http://dx.doi.org/10.30574/wjarr.2021.9.3.0110.

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The industrial discharge carries significant level of contaminants to the surface water and ground water. Whereas the quality of freshwater is very vital because is highly use by human for drinking, bathing, agriculture and other needs. The presence of contaminants from industries within the water may reduce the yield of crops and the growth of plants; it is also harmful to the aquatic living organisms, it alters the surface water and ground water quality. Industrial pollution is one of the major factors causing degradation of the environment, affecting the water we use, the air we breathe and

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18

Abdullateef, Abdullahi Ibrahim, Abdullahi Ibrahim Muhammad, and Gambo Yusuf Ali. "Implications of industrial effluents on surface water and ground water." World Journal of Advanced Research and Reviews 9, no. 3 (2021): 330–36. https://doi.org/10.5281/zenodo.4661787.

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The industrial discharge carries significant level of contaminants to the surface water and ground water. Whereas the quality of freshwater is very vital because is highly use by human for drinking, bathing, agriculture and other needs. The presence of contaminants from industries within the water may reduce the yield of crops and the growth of plants; it is also harmful to the aquatic living organisms, it alters the surface water and ground water quality. Industrial pollution is one of the major factors causing degradation of the environment, affecting the water we use, the air we breathe and

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19

Hendricks, Susan P., and David S. White. "Seasonal biogeochemical patterns in surface water, subsurface hyporheic, and riparian ground water in a temperate stream ecosystem." Archiv für Hydrobiologie 134, no. 4 (1995): 459–90. http://dx.doi.org/10.1127/archiv-hydrobiol/134/1995/459.

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20

Verberk, J. Q. J. C., J. Post, W. G. J. van der Meer, and J. C. van Dijk. "Direct capillary nanofiltration for ground water and surface water treatment." Water Supply 2, no. 5-6 (2002): 277–83. http://dx.doi.org/10.2166/ws.2002.0180.

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Capillary nanofiltration is a new concept in membrane filtration. This technique combines the advantages of the good water quality obtained from nanofiltration membranes with the easy hydraulic cleaning of capillary membranes. Direct capillary nanofiltration can be used to treat ground water or surface water without pre-treatment. At the Delft University of Technology several MSc-thesis projects have been carried out on this subject. This paper will describe some results of these studies. A model based on a mass balance to predict the flux of a capillary nanofiltration installation treating gr

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21

Woocay, Arturo, and John Walton. "Multivariate Analyses of Water Chemistry: Surface and Ground Water Interactions." Ground Water 46, no. 3 (2008): 437–49. http://dx.doi.org/10.1111/j.1745-6584.2007.00404.x.

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22

Hughes, Joseph D., and Jie Liu. "MIKE SHE: Software for Integrated Surface Water/Ground Water Modeling." Ground Water 46, no. 6 (2008): 797–802. http://dx.doi.org/10.1111/j.1745-6584.2008.00500.x.

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23

Oxtobee, Jaime P. A., and Kent S. Novakowski. "Ground Water/Surface Water Interaction in a Fractured Rock Aquifer." Ground Water 41, no. 5 (2003): 667–81. http://dx.doi.org/10.1111/j.1745-6584.2003.tb02405.x.

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24

REZAEI KALVANI, S., A. SHARAAI, L. MANAF, and A. HAMIDIAN. "ASSESSING GROUND AND SURFACE WATER SCARCITY INDICES USING GROUND AND SURFACE WATER FOOTPRINTS IN THE TEHRAN PROVINCE OF IRAN." Applied Ecology and Environmental Research 17, no. 2 (2019): 4985–97. http://dx.doi.org/10.15666/aeer/1702_49854997.

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25

Giri, Vedanti Arunkumar. "Artificial Ground Water Recharge Techniques." International Journal for Research in Applied Science and Engineering Technology 11, no. 7 (2023): 432–35. http://dx.doi.org/10.22214/ijraset.2023.54612.

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bstract: Artificial groundwater recharge aims at increasing the groundwater storage by modifying the natural movement of surface water with the help of suitable structures. It is a well-planned human endeavour to increase the amount of groundwater available through structures designed to increase the natural recharge or percolation of surface water into the water table, resulting in an improvement in the amount of groundwater available for withdrawal. The main objective of this technology is to conserve and augment groundwater resources in various parts of India, which includes maintaining or

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26

Chai, Mingtang, Nan Li, Furong Liu, Yu Gao, Yanhu Mu, and Wei Ma. "A Calculation Model for Ground Surface Temperature in High-Altitude Regions of the Qinghai-Tibet Plateau, China." Remote Sensing 14, no. 20 (2022): 5219. http://dx.doi.org/10.3390/rs14205219.

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As a major parameter in the energy balance of the ground surface, temperature represents the level of exchange of energy and moisture between the ground and air. The Qinghai-Tibet Plateau (QTP) has the permafrost region with the highest altitude and the largest area in low–middle latitude of the world. The variation in ground surface temperature has an impact on the existence and development of the permafrost. Therefore, the analysis of the ground surface temperature in the QTP is significant to reflect the energy exchange in permafrost regions. This paper collected solar radiation data and ca

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27

Harwell, Jeffrey H., David A. Sabatini, and R. C. Knox. "Surfactants for ground water remediation." Colloids and Surfaces A: Physicochemical and Engineering Aspects 151, no. 1-2 (1999): 255–68. http://dx.doi.org/10.1016/s0927-7757(98)00785-7.

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28

Yi, Jae-Eung. "Optimal Conjunctive Use of Surface and Ground Water." Journal of Korea Water Resources Association 35, no. 4 (2002): 367–74. http://dx.doi.org/10.3741/jkwra.2002.35.4.367.

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29

Basagaoglu, Hakan, and Miguel A. Marino. "Joint Management of Surface and Ground Water Supplies." Ground Water 37, no. 2 (1999): 214–22. http://dx.doi.org/10.1111/j.1745-6584.1999.tb00976.x.

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30

Mathewson, Christopher C. "Surface coal mining effects on ground water recharge." Journal of Hydrology 132, no. 1-4 (1992): 379–80. http://dx.doi.org/10.1016/0022-1694(92)90187-z.

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31

Mishra, R. K. "Fresh Water availability and It’s Global challenge." Journal of Marine Science and Research 2, no. 1 (2023): 01–03. http://dx.doi.org/10.58489/2836-5933/004.

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Water is prime natural resources fulfilling our needs in a precisious assets. We must acts to preserve and utilize every drop of water. Water resources can be assessed on the basis of surface and subsurface water bodies. Climate change impact on ground Water the impact of climate change on ground water has been studied much less than the impact on surface waters. Ground water reacts to climate change mainly due to change in ground water recharge, but also change in river level in response to increase in mean Temperature, precipitation ,variability and sea level as mean precipitations. Changing

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32

Lei, Bingbing, Bin Wang, Mingli Zhang, Zhixiong Zhou, Guang Li, and Guodong Yue. "Thermal-Moisture Dynamics at Different Underlying Surfaces in Permafrost Regions of the Central Tibetan Plateau by considering the Effect of Rainfall." Geofluids 2022 (July 28, 2022): 1–16. http://dx.doi.org/10.1155/2022/2230372.

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The Qinghai-Tibetan Plateau (QTP) has undergone an increase in rainfall and a drastic alteration in the moisture-heat regime in active layers and engineering. To investigate the water and heat responses of natural ground and engineering to rainfall, the differences in energy on the ground surface and the thermal-moisture dynamics of different permafrost underlying surfaces were discussed. Based on the meteorological data in 2013 observed at the Beiluhe observation station, three types of underlying surfaces (i.e., natural ground, asphalt pavement, and gravel pavement) were selected to compare

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33

Datta, J. K., S. Layek, A. Banerjee, N. K. Mondal, and S. Gupta. "Physico-chemical Characterization of Water Quality of Eutrophied Surface Water Body and Ground Water around the Field Crop Research Station, Burdwan, West Bengal." Asian Journal of Water, Environment and Pollution 7, no. 3 (2010): 69–75. http://dx.doi.org/10.3233/ajw-2010-7_3_08.

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A study on water quality of eutrophied surface water body of Kalna farm as well as ground water quality of the area was done to investigate the level of pollution and contamination that have occurred in these two sources of fresh water systems. Several physicochemical parameters viz., pH, temperature, TDS, turbidity, nitrate nitrogen, phosphate, sodium and potassium content were measured in groundwater samples. For surface water analysis, DO, BOD and COD were mediated to evaluate the pollution load of the surface water bodies surrounding the Kalna farm. Results indicate that all the surface wa

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34

Kulakov, V. V., R. S. Shtengelov, and D. V. Matveenko. "Interaction of ground and surface water in Khabarovsk water node area." Earth sciences and subsoil use 44, no. 2 (2021): 151–58. http://dx.doi.org/10.21285/2686-9993-2021-44-2-151-158.

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This research presents the results of long-term monitoring of groundwater levels within the Khabarovsk water node in the Amur and Tunguska interfluve on the area of the Middle Amur artesian basin in the aquifer of Pliocene-Lower Quaternary alluvial deposits. Observations have been carried out on 9 groups of wells of external monitoring and 5 groups of wells of internal monitoring at the Tunguska reservoir, with a depth of 3 observation wells in the group from 15 to 50 m. The interaction parameters of groundwater and the Pemzenskaya channel have been specified for the period from 2012 to 2020.

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35

Verstraeten, I. M., J. D. Carr, G. V. Steele, E. M. Thurman, K. C. Bastian, and D. F. Dormedy. "Surface Water‐Ground Water Interaction: Herbicide Transport into Municipal Collector Wells." Journal of Environmental Quality 28, no. 5 (1999): 1396–405. http://dx.doi.org/10.2134/jeq1999.00472425002800050002x.

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36

Zaadnoordijk, Willem Jan. "Simulating Piecewise-Linear Surface Water and Ground Water Interactions with MODFLOW." Ground Water 47, no. 5 (2009): 723–26. http://dx.doi.org/10.1111/j.1745-6584.2009.00582.x.

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37

Anisah Haromain, Safira, Emma Yuliani, Ussy Andawayanti, Tsuyoshi Imai, and Firda Samaniyatul Aliyah. "Interaction between Ground Water and Surface Water in Porong River, Sidoarjo." Jurnal Teknik Pengairan 15, no. 1 (2024): 22–36. http://dx.doi.org/10.21776/ub.pengairan.2024.015.01.3.

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38

PiPujol, M. D., and P. Buurman. "Analyzing ground-water gley and surface-water (pseudogley) effects in paleosols." Quaternary International 51-52 (January 1998): 77–79. http://dx.doi.org/10.1016/s1040-6182(98)90230-0.

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39

Yan, Jiansheng, and Keith R. Smith. "SIMULATION OF INTEGRATED SURFACE WATER AND GROUND WATER SYSTEMS - MODEL FORMULATION." Journal of the American Water Resources Association 30, no. 5 (1994): 879–90. http://dx.doi.org/10.1111/j.1752-1688.1994.tb03336.x.

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40

Ryan, Keith W., Donald M. Dwight, and Douglas A. Hlousek. "RECIRCULATING WELLS: GROUND WATER REMEDIATION AND PROTECTION OF SURFACE WATER RESOURCES." Journal of the American Water Resources Association 36, no. 1 (2000): 191–201. http://dx.doi.org/10.1111/j.1752-1688.2000.tb04259.x.

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41

Ezugwu, C. N., and S. Apeh. "Ground Water and Surface Water as One Resource: Connectivity and Interaction." IOSR Journal of Mechanical and Civil Engineering 14, no. 03 (2017): 54–59. http://dx.doi.org/10.9790/1684-1403075459.

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42

Winter, Thomas C. "Ground water and surface water: the linkage tightens, but challenges remain." Hydrological Processes 15, no. 18 (2001): 3605–6. http://dx.doi.org/10.1002/hyp.504.

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43

Toktaganov, T. Sh, A. O. Aidarkhanov, M. R. Aktayev, B. A. Kokezhanov, S. S. Pronin, and A. O. Iskenov. "OPTIMIZING MONITORING OBSESRVATIONS OF WATER IN RADIATION HAZARDOUS AREAS OF STS BY MEANS OF ISOTOPE HYDROLOGY TECHNIQUE." NNC RK Bulletin, no. 4 (December 30, 2018): 44–48. http://dx.doi.org/10.52676/1729-7885-2018-4-44-48.

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The article addresses determinations of features of ground water formed at places of radionuclide contaminations. It is found that the major source of ground water recharge is winter atmospheric precipitation. It is also revealed that ground water discharge into surface water occurs in August. This data is confirmed by measured results of stable isotopes as well as my measured level of ground water occurring in the bed of the Shagan river. During this period at places of ground water discharge there is a maximum concentration of man-made radionuclides in surface water of the Shagan river and K

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44

Gyawu-Asante, F. N., S. Aikins, and R. B. Voegborlo. "Effects of surface gold mining on surface and groundwater bodies in Bibiani, Ghana." Journal of Science and Technology (Ghana) 37, no. 1 (2017): 9–24. http://dx.doi.org/10.4314/just.v37i1.2.

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A study of the water sources from Bibiani and its environs was conducted between November, 2009 and April, 2010 to determine whether contamination (of water sources) from (these parameters) physical, chemical and trace metal in Bibiani is as a result of mining or geochemicaland biochemical processes within the environment. This was done by collecting water samples from two streams, two rivers, three boreholes (BHs) and three hand dug wells (HDWs). These were analysed in the laboratory. Levels of Arsenic (As), Iron (Fe), Manganese (Mn), pH, TotalDissolved Solids (TDS), Electrical Conductivity (

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45

Erg, K., E. Reinsalu, and I. Valgma. "GEOTECHNICAL PROCESSES AND SOIL-WATER MOVEMENT WITH TRANSPORT OF POLLUTANTS IN THE ESTONIAN OIL SHALE MINING AREA." Environment. Technology. Resources. Proceedings of the International Scientific and Practical Conference 1 (June 26, 2006): 79. http://dx.doi.org/10.17770/etr2003vol1.1984.

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One of the most important industries of Northeast Estonia is oil shale mining. Ground movements caused by mining reach the ground surface easily due to shallow location of workings. A new, artificial topography is formed on undermined areas, where the ground surface depressions are alternating with rising grounds. When the Quaternary cover contains loamy sediments, the surface water will accumulate in the depressions. The response of usable lands on undermined areas depends on the degree of changes in the relief and water regime. The accumulation of solid residues by oil shale mines and proces

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46

Kamsinarani, Kamsinarani, Masyahoro Masyahoro, and Alimudin Laapo. "Estimasi Fishing Ground berdasarkan sebaran Suhu Permukaan Laut dan Klorofil-a di Perairan Teluk Tolo." Mitra Sains 9, no. 1 (2021): 62–70. http://dx.doi.org/10.22487/ms26866579.2021.v9.i1.pp62-70.

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One of the major problem for fishermen of Tolo Bay water in optimizing the utilization of the fish resources is the difficulty in determining potential fishing grounds. The fishing area is very much determined by the distribution of oceanographic parameters, in particular the distribution of sea surface temperature and chlorophyll-a concentration. The aim of the reaserch is to estimate the fishing ground using integrated sea surface temperature and chlorophyll-a distribution image data from Aqua-Modis Level 3 Satellite and Seades 7.2. The Reseacrh was conducted using GIS-based Remote Sensing M

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47

Jiang, Zhen Wei, and Qi Yao Wang. "Study on the Formation and Repeated Opening Mechanism of Ground Fissures under the Role of Surface Water." Advanced Materials Research 243-249 (May 2011): 3238–43. http://dx.doi.org/10.4028/www.scientific.net/amr.243-249.3238.

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The role of surface water is also the main reason for the formation and development of ground fissures. Five mechanisms were obtained on the formation of ground fissures under the role of surface water in the loess region through theoretical analysis, i.e., fissuring mechanism induced by loess collapsible deformation; that induced by dissolution and suffosion; that induced by water-loss shrinkage; that induced by hydraulic pressure; that induced by humidification and softening. As the role of surface water had certain phased and periodic characteristics, repeated fissuring mechanism of ground

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48

S. Rajagopal and V. Rajagopalan. "Water Quality Index and Microbial Population Assessment for Ground Water." Journal of Environmental Nanotechnology 7, no. 3 (2018): 60–62. http://dx.doi.org/10.13074/jent.2018.09.183323.

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Pollution of water sources have become a common problem these days, be it ground water source or surface water sources. The most important and major usage of ground water is for irrigation unfortunately groundwater is susceptible to pollutants that may enter into the subsurface ground water by runoff. Presence of microbes in drinking water is now common problems as majority of the ground water sources are being substantially polluted. the physico chemical and microbial properties of water was studied and was found that the treated water sample showed a better water quality rating than the raw

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49

Ed-Idoko, J. O., J. O. Apochi, J. Ndukwe, et al. "Impact of Improper Waste Disposal on Surface and Ground Water." Journal of Agriculture and Ecology Research International 25, no. 6 (2024): 72–90. http://dx.doi.org/10.9734/jaeri/2024/v25i6641.

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Abstract:

Pollution in water occurs when harmful substance (often chemicals or biological) contaminate streams, river, lakes, oceans or other bodies of water, degrading water quality and rendering it unhealthy to humans, animal and the environment. The widespread problem of water pollution is jeopardizing our health. Water pathogens, in form of disease-causing bacteria and viruses from human and animal waste, are a major reason of illness from contaminated drinking water. Owing to the improper treatment facilities, waste is often discharged into the surface and ground water sources. Water bacteria can b

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Lawson, M., C. J. Ballentine, D. A. Polya, et al. "The geochemical and isotopic composition of ground waters in West Bengal: tracing ground-surface water interaction and its role in arsenic release." Mineralogical Magazine 72, no. 1 (2008): 441–44. http://dx.doi.org/10.1180/minmag.2008.072.1.441.

Full text

Abstract:

AbstractIn many areas of south and south-eastern Asia, concentrations of As in ground water have been found to exceed the WHO maximum concentration limit of 10 μg/l. This is adversely affecting the health of millions of people and has grave current and future health implications. It has recently been suggested that extensive abstraction of ground water in these areas may accelerate the release of As to ground water. This study uses geochemical and isotopic data to assess this hypothesis. The area investigated in this study is in the Chakdaha block of the Nadia District, West Bengal. The ground

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