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Journal articles on the topic 'Ganga'

Author: Grafiati
Published: 4 June 2021
Last updated: 13 June 2025

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1

Dasgupta, Subhoranjan. "Epar Ganga Opar Ganga - A Creative Statement on Displacement and Violence." Indian Historical Review 32, no. 2 (2005): 218–31. http://dx.doi.org/10.1177/037698360503200212.

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2

Markešić, Ivan. "Ivan Cvitković: Ganga – pjesma o životu u Hercegovini (Sociologijske marginalije o gangi)." Drustvena istrazivanja 27, no. 3 (2018): 563–65. http://dx.doi.org/10.5559/di.27.3.09.

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3

Bhargava, Devendra Swaroop. "Nature and the Ganga." Environmental Conservation 14, no. 4 (1987): 307–18. http://dx.doi.org/10.1017/s0376892900016829.

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The Ganga's unique and numerous virtues appear to be based on myths, but the reasons for its importance are traceable to scientific premises. The Ganga, symbolizing Indian culture and civilization, is regarded by the Hindus as the holiest amongst the rivers, and it is the Indo-Gangetic plain's most significant river owing to its mighty basin and course, and extraordinarily high self-purifying powers. The Ganga originates from Gangori in the Uttrakhand Himalayan glacier as an upland stream, emerges as a river of the plains at Rishikesh, and, after traversing almost the entirety of India from West to East, finally merges into the Bay of Bengal.
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4

Das, Subhajyoti. "Cleaning of the Ganga." Journal of the Geological Society of India 78, no. 2 (2011): 124–30. http://dx.doi.org/10.1007/s12594-011-0073-9.

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5

Dwivedi, Sanjay, Seema Mishra, and Rudra Deo Tripathi. "Ganga water pollution: A potential health threat to inhabitants of Ganga basin." Environment International 117 (August 2018): 327–38. http://dx.doi.org/10.1016/j.envint.2018.05.015.

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6

Chaturvedi, M. C. "The ganga-brahmaputra-barak basin." Sadhana 8, no. 1 (1985): 73–92. http://dx.doi.org/10.1007/bf02811272.

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7

Sahu, Sudarsan, N. J. Raju, and Dipankar Saha. "Active tectonics and geomorphology in the Sone-Ganga alluvial tract in mid-Ganga Basin, India." Quaternary International 227, no. 2 (2010): 116–26. http://dx.doi.org/10.1016/j.quaint.2010.05.023.

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8

Sharma, Maneesh, Heinz Tobschall, and Indra Singh. "Environmental impact assessment in the Moradabad industrial area (rivers Ramganga-Ganga interfluve), Ganga Plain, India." Environmental Geology 43, no. 8 (2003): 957–67. http://dx.doi.org/10.1007/s00254-002-0718-5.

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9

Jordan Woodward. "Harmony with Books and the Ganga." World Literature Today 89, no. 3-4 (2015): 128. http://dx.doi.org/10.7588/worllitetoda.89.3-4.0128.

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10

Alley, Kelly D. "On the banks of the Ganga." Annals of Tourism Research 19, no. 1 (1992): 125–27. http://dx.doi.org/10.1016/0160-7383(92)90112-3.

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11

Rao, Radhakrishna. "Turning to turtles to clean Ganga." Nature 343, no. 6259 (1990): 585. http://dx.doi.org/10.1038/343585d0.

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12

Iyer, Ramaswamy R. "The Indo—Bangladesh Ganga Waters Dispute." South Asian Survey 4, no. 1 (1997): 129–44. http://dx.doi.org/10.1177/097152319700400111.

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13

Thiyagarajan Babu, Thiyagarajan Babu. "Noble Ganga Tears-Sweat Bomb Theory." IOSR Journal of Nursing and health Science 1, no. 3 (2013): 52–54. http://dx.doi.org/10.9790/1959-0135254.

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14

Amarasekara, Nalini. "Environmental consequences of Menik Ganga diversion." International Journal of Water Resources Development 8, no. 4 (1992): 286–91. http://dx.doi.org/10.1080/07900629208722566.

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15

Elmsheuser, Johannes, Frederic Brochu, Greig Cowan, et al. "Distributed analysis in ATLAS using GANGA." Journal of Physics: Conference Series 219, no. 7 (2010): 072002. http://dx.doi.org/10.1088/1742-6596/219/7/072002.

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16

Maier, Andrew, Frederic Brochu, Greg Cowan, et al. "User analysis of LHCbdata with Ganga." Journal of Physics: Conference Series 219, no. 7 (2010): 072008. http://dx.doi.org/10.1088/1742-6596/219/7/072008.

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17

Jhunjhunwala, Bharat, and Ranjana Waghralkar. "Observational case studies of the effect of phage laden Ganga water on psoriasis." IP Indian Journal of Clinical and Experimental Dermatology 7, no. 3 (2021): 186–90. http://dx.doi.org/10.18231/j.ijced.2021.037.

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Water of Ganga river is reported to have more than 200 isolates of phages. This study has used the naturally available cocktail of phages in the Ganga water as a treatment for chronic Psoriasis. In the conventional Phage Therapy (PT) phages that are active against specific bacteria are first identified; then isolated, multiplied and administered to the patient. We have made a novel innovation of administering the naturally available cocktail of phages in the water of the Ganga river without first identifying the target bacteria and isolating specific phages that may be active against them. In doing so, we enable the large numbers of phages to self-identify the bacteria that are present and act against them. This approach shortcuts the tortuous process of conventional PT. Further, the phages act against a number of bacteria simultaneously and provide good results in psoriasis which has multiple causes.Patients who took Ganga water for only 2 weeks showed benefit but the benefit did not sustain after stoppage of the treatment and the disease relapsed to the pre-treatment levels. The same patients showed sustained benefit after they took Ganga water for four weeks. Conclusion is that Ganga water can be used for therapeutic purposes as long as the treatment is continued for at least four weeks. The study underscores the need to establish more robust protocol for treatment of dermatological and possibly other diseases with the cocktail of phages available in the waters of the Ganga river.
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18

Hasan, Nabi, Rais Ahmad Khan, and Jafar Iqbal. "River Ganga repository: An initiative towards the collection and dissemination of knowledge on the River Ganga." International Journal of Information Dissemination and Technology 7, no. 4 (2017): 238. http://dx.doi.org/10.5958/2249-5576.2017.00031.0.

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19

Khan, Taqveem Ali. "Groundwater Quality Evaluation Using Multivariate Methods, in Parts of Ganga Sot Sub-Basin, Ganga Basin, India." Journal of Water Resource and Protection 07, no. 09 (2015): 769–80. http://dx.doi.org/10.4236/jwarp.2015.79063.

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20

Singh, S., K. Prakash, and U. K. Shukla. "Spatiotemporal Migration of the River Ganga in Middle Ganga Plane: Application of Remote Sensing and GIS Technique." Journal of the Indian Society of Remote Sensing 48, no. 11 (2020): 1495–507. http://dx.doi.org/10.1007/s12524-020-01170-z.

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21

Jha, Murari Kumar. "Migration, Settlement, and State Formation in the Ganga Plain: A Historical Geographic Perspective." Journal of the Economic and Social History of the Orient 57, no. 4 (2014): 587–627. http://dx.doi.org/10.1163/15685209-12341359.

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By a consideration of geography and environment, this essay raises questions about migration, settlement, and state formation in the Ganga plain from the first millenniumbceto the early second millenniumce. It asks why Indo-Aryan speakers continued to migrate from north-western parts of South Asia towards the Ganga plain during the first millenniumbceand precisely what route they followed. To understand better these largely misunderstood historical problems related to migration and settlement, the essay casts doubt on the utility of geographers’ tripartite division of the Ganga plain, proposing instead a division based on aridity and rainfall. Such a division helps explain why the transitional zone between the drier and the more humid areas of the Ganga plain became the linchpin of migratory movements, state formation, and urban development since at least the middle of the first millenniumbce.
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22

Patty, Wilhelmina. "KARAKTERISTIK TIPE DASAR DAN PEMANFAATAN PERAIRAN DI SEKITAR PULAU GANGGA, KABUPATEN MINUT." JURNAL PERIKANAN DAN KELAUTAN TROPIS 6, no. 2 (2010): 108. http://dx.doi.org/10.35800/jpkt.6.2.2010.171.

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Coastal resources and space in the coastal around Gangga island, has been used for fishing activities and marine tourism. The purpose of this study to map the profile of bottom waters and to identify patterns sublitoral basic surface waters. The survey was conducted by using the acoustic method of sounding, followed by sediment sampling as well as shooting on the surface of the bottom waters. The result of observation indicates that the basic conditions of slope waters around the island of Ganga slope varies from flat to very steep slopes. Waters of the western Gangga island smaller flat slope found in coastal landform ranging from mangroves, coral reefs and seagrass. Bottom waters to the east of Gangga island to steep slope, with the basic pattern dominated by coral reefs and sand.
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23

Ramakrishnan, P. S. "The Sacred Ganga River‐based Cultural Landscape." Museum International 55, no. 2 (2003): 7–17. http://dx.doi.org/10.1046/j.1350-0775.2003.00420.x.

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24

PATEL, J. A., and A. B. VORA. "Salinity Induced Changes inZea maysL. (Ganga-2)." Journal of Experimental Botany 36, no. 1 (1985): 49–54. http://dx.doi.org/10.1093/jxb/36.1.49.

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25

Maier, A. "Ganga— a job management and optimising tool." Journal of Physics: Conference Series 119, no. 7 (2008): 072021. http://dx.doi.org/10.1088/1742-6596/119/7/072021.

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26

Modak, D. P., K. P. Singh, S. Ahmed, and P. K. Ray. "Trace metal ions in Ganga water system." Chemosphere 21, no. 1-2 (1990): 275–87. http://dx.doi.org/10.1016/0045-6535(90)90400-n.

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27

Chaturvedi, M. C., Peter Rogers, and Shyang-Lai Kung. "The coordinating model of the ganga basin." Sadhana 8, no. 1 (1985): 93–121. http://dx.doi.org/10.1007/bf02811273.

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28

Khatun, Hasnahara, and Dr Arshad jamal. "Geochemicals Heavy Metal Pollution of River Ganga - Causes and Impacts." International Journal of Trend in Scientific Research and Development Volume-2, Issue-2 (2018): 1035–38. http://dx.doi.org/10.31142/ijtsrd9576.

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29

Singh, S., K. Prakash, and U. K. Shukla. "Decadal scale geomorphic changes and tributary confluences within the Ganga River valley in Varanasi region, Ganga Plain, India." Quaternary International 507 (February 2019): 124–33. http://dx.doi.org/10.1016/j.quaint.2018.05.022.

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30

Sahu, Sudarsan, and Dipankar Saha. "Geomorphologic, stratigraphic and sedimentologic evidences of tectonic activity in Sone–Ganga alluvial tract in Middle Ganga Plain, India." Journal of Earth System Science 123, no. 6 (2014): 1335–47. http://dx.doi.org/10.1007/s12040-014-0470-8.

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31

Ala Eldin, M. E. H., M. Sami Ahmed, V. V. S. Gurunadha Rao, and R. L. Dhar. "Aquifer modelling of the Ganga-Mahawa sub-basin, a part of the Central Ganga Plain, Uttar Pradesh, India." Hydrological Processes 14, no. 2 (2000): 297–315. http://dx.doi.org/10.1002/(sici)1099-1085(20000215)14:2<297::aid-hyp927>3.0.co;2-u.

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32

Narwal, S. S., D. S. Dahiya, G. Singh, and D. S. Malik. "Response of maize cultivars to sowing in the winter." Journal of Agricultural Science 109, no. 2 (1987): 303–7. http://dx.doi.org/10.1017/s0021859600080722.

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SummaryIn a 2-year field study, all the maize cultivars tried (Partap-1 Ageti-76, Ganga-5 and DHM-103) produced similar length of ears and equivalent grain yields. However, Partap-1 and Ganga-5 produced greater 100-kernel weight and greater grain yield per ear but fewer ears per hectare than Ageti-76 and DHM-103. The yield attributes and grain yields of maize sown on 19 December, 29 December and 8 January were identical and were superior to those of the 19 January sowing. Maize sown on 19 December, 29 December and 8 January exhibited longer ears, more ears and fully developed kernels and thereby produced greater grain yields than the 18 January sowing.During 1983–4, in the 19 December and 29 December sowings all the cultivars gave identical grain yields. In the 8 January sowing Partap-1 and Ageti-76 produced similar yields and proved better than Ganga-5 and DHM-103. In the 18 January sowing Ageti-76, Ganga-5 and DHM-103 yielded more than Partap-1.
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33

Singh, Sandeep, Munendra Singh, A. K. Choudhary, Anju Saxena, I. B. Singh, and A. K. Jain. "Sr isotopic signature of the Ganga Alluvial Plain and its implication to Sr flux of the Ganga River System." International Journal of Earth Sciences 99, no. 8 (2009): 1991–97. http://dx.doi.org/10.1007/s00531-009-0479-4.

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34

Chaudhary, Meenakshi, and Tony R. Walker. "River Ganga pollution: Causes and failed management plans (correspondence on Dwivedi et al. 2018. Ganga water pollution: A potential health threat to inhabitants of Ganga basin. Environment International 117, 327–338)." Environment International 126 (May 2019): 202–6. http://dx.doi.org/10.1016/j.envint.2019.02.033.

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35

Singh, Gurnam, and Naresh Kumar Agarwal. "Fishing methods in upper Ganga River system of Central Himalaya, India." Journal of Fisheries 2, no. 3 (2014): 195. http://dx.doi.org/10.17017/jfish.v2i3.2014.43.

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Present study on fishing methods in the upper Ganga River system was conducted during the period 2010-2012. Upper Ganga river system consists of two major rivers basins viz. Alaknanda and Bhagirathi rivers and number of their 1st and 2nd order tributaries which flows through Garhwal region (Central Himalaya). This large network of fluvial water resources harbours rich Ichthyofaunal diversity. The varied potential of fish resources from these water bodies permits the utilization of wide array of fishing methods. Most of the fishing methods of the Garhwal region are primitive, based on indigenous traditional knowledge and well suited to turbulent nature of the streams. In present study eighteen fishing methods and gears have been documented from the upper Ganga River system. Study observed season, habitat and species specificity of the fishing methods. The utilization of crude and unscientific fishing methods is frequent in the streams of remote areas resulting into decline in fish resource. All the fishing methods employed in upper Ganga River system are classified into four types. The classification is based on their utilisation up to the level which will allow the sustainable harvesting and proper management of valuable fish resources.
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36

Chowdhury, Mahua Roy, Sangita Mitra, and Saswati Sen. "On the Behaviour, abundance, habitat use and potential threats of the Gangetic Dolphin Platanista gangetica in southern West Bengal, India." Journal of Threatened Taxa 8, no. 9 (2016): 9131. http://dx.doi.org/10.11609/jott.1752.8.9.9131-9137.

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The Ganga River Dolphin Platanista gangetica Roxburgh, 1801 is a globally endangered cetacean found in the River system of Ganga, Brahmaputra and Meghna in Bangladesh and India. A survey and research were conducted from 2012–2014 to explore the behaviour, abundance, habitat use and potential threats of the Dolphin in the lower, middle and upper stretches of the river Ganga and its tributaries in southern West Bengal. The study recorded different types of surfacing patterns with respect to their age class as well as on diurnal activity pattern of the individual. The adults and sub-adults were found to have different types of surfacing during different hours of the day. The morning and afternoon were observed to be feeding hours of the Dolphin. Multiple potential threats were encountered during the present study such as destructive fishing gears, dumping of solid and municipal waste, industrial effluents, agricultural run-off, construction of water structures, water extraction and reduction of river depth attributed to siltation. These factors contributed to the present study of the river dolphins in the Ganga, which are localised at certain pockets in good number.
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37

Ćaleta, Joško. "The Art of Ganga Singing: Cultural Tradition of the Dinaric Area." Musicological Annual 55, no. 1 (2019): 211–18. http://dx.doi.org/10.4312/mz.55.1.211-218.

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Ganga, currently the most popular traditional vocal genre of the Dinaric area (stretching across Croatia and Bosnia and Herzegovina), is one of the last examples of the archaic style of music making, entirely different from traditional styles and genres based on the heritage of Western European music, such as “klapa” singing. This style of traditional music making serves as an important identification marker of Dinaric communities in Southeastern Europe, both past and present. The author of the proposed book, the Sarajevan ethnomusicologist Ankica Petrović, remains the greatest proponent of the ganga music phenomenon in scholarly circles outside former Yugoslavia. Ganga, currently the most popular traditional vocal genre of the Dinaric area (stretching across Croatia and Bosnia and Herzegovina), is one of the last examples of the archaic style of music making, entirely different from traditional styles and genres based on the heritage of Western European music, such as “klapa” singing. This style of traditional music making serves as an important identification marker of Dinaric communities in Southeastern Europe, both past and present. The author of the proposed book, the Sarajevan ethnomusicologist Ankica Petrović, remains the greatest proponent of the ganga music phenomenon in scholarly circles outside former Yugoslavia.
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38

Sarkar, Ranjan, and Debasis Roy. "A Study on the Discharge Rate of the Ganga at Farakka." Paripex - Indian Journal Of Research 3, no. 5 (2012): 213–14. http://dx.doi.org/10.15373/22501991/may2014/66.

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39

Shukla, U. K., I. B. Singh, M. Sharma, and S. Sharma. "A model of alluvial megafan sedimentation: Ganga Megafan." Sedimentary Geology 144, no. 3-4 (2001): 243–62. http://dx.doi.org/10.1016/s0037-0738(01)00060-4.

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40

Srivastava, V. K. "Indian Rivers Pollution—Critical Analysis: Ganga Action Plan." Indian Chemical Engineer 52, no. 2 (2010): 155–56. http://dx.doi.org/10.1080/00194506.2010.497284.

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41

Bhargava, Devendra Swaroop. "Why the Ganga (Ganges) Could Not be Cleaned." Environmental Conservation 19, no. 2 (1992): 170–72. http://dx.doi.org/10.1017/s0376892900030666.

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42

Trivedi, R. C. "Water quality of the Ganga River – An overview." Aquatic Ecosystem Health & Management 13, no. 4 (2010): 347–51. http://dx.doi.org/10.1080/14634988.2010.528740.

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43

Chaube, Umesh C. "Water conflict resolution in the Ganga‐Brahmaputra basin." International Journal of Water Resources Development 6, no. 2 (1990): 79–85. http://dx.doi.org/10.1080/07900629008722456.

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44

Currie, R., J. Elmsheuser, R. Fay, et al. "Recent developments in user-job management with Ganga." Journal of Physics: Conference Series 664, no. 6 (2015): 062010. http://dx.doi.org/10.1088/1742-6596/664/6/062010.

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45

Vanderster, D. C., J. Elmsheuser, D. Liko, et al. "A PanDA backend for the ganga analysis interface." Journal of Physics: Conference Series 219, no. 7 (2010): 072056. http://dx.doi.org/10.1088/1742-6596/219/7/072056.

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46

Jain, Jyotindra. "Ganga Devi: Tradition and expression in Madhubani painting." Third Text 3, no. 6 (1989): 43–50. http://dx.doi.org/10.1080/09528828908576213.

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47

Dzhunov, I. A., M. J. Kenyon, J. Moscicki, et al. "Key developments of the Ganga task-management framework." Journal of Physics: Conference Series 396, no. 3 (2012): 032061. http://dx.doi.org/10.1088/1742-6596/396/3/032061.

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48

Antoniev, I., Z. Deng, J. Ebke, et al. "BESIII and SuperB: distributed job management with Ganga." Journal of Physics: Conference Series 396, no. 3 (2012): 032120. http://dx.doi.org/10.1088/1742-6596/396/3/032120.

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49

Purushothaman, P., and G. J. Chakrapani. "Heavy Metals Fractionation in Ganga River Sediments, India." Environmental Monitoring and Assessment 132, no. 1-3 (2007): 475–89. http://dx.doi.org/10.1007/s10661-006-9550-9.

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50

Srivastava, Shuchi, Pavitra Tandon, Renu Singh, and K. N. Uttam. "Elemental Investigation of River Ganga Water by LIBS." National Academy Science Letters 36, no. 1 (2013): 57–60. http://dx.doi.org/10.1007/s40009-012-0107-x.

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