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Artykuły w czasopismach na temat "Murshidabad District"
Rumi, Emili. "Muslim Education in Murshidabad, a Bengal District during 1704-1947: A Review". IRA-International Journal of Management & Social Sciences (ISSN 2455-2267) 11, nr 3 (18.07.2018): 128. http://dx.doi.org/10.21013/jmss.v11.n3.p3.
Pełny tekst źródłaSANAULLAH, MD. "Bidi Industry in Murshidabad District in Historical Context". INTERNATIONAL JOURNAL OF HUMANITIES, ENGINEERING, SCIENCE AND MANAGEMENT 4, nr 1 (30.06.2023): 68–79. http://dx.doi.org/10.59364/ijhesm.v4i1.222.
Pełny tekst źródłaAfsar Ali, MD. "A Study on the Attitude of the Hindu and Christian Secondary School Teachers of Malda and Murshidabad Districts, West Bengal, India towards Yoga Education in Schools in Relation to their Mental Health". Asian Review of Social Sciences 9, nr 1 (5.05.2020): 14–22. http://dx.doi.org/10.51983/arss-2020.9.1.1612.
Pełny tekst źródłaAfsar Ali, Mohamed. "A Study on the Attitude of the Hindu and Christian Secondary School Teachers of Malda and Murshidabad Districts, West Bengal, India towards Yoga Education in Schools in Relation to their Mental Health". Asian Review of Social Sciences 10, nr 1 (15.05.2021): 39–47. http://dx.doi.org/10.51983/arss-2021.10.1.2680.
Pełny tekst źródłaRadcliffe-Smith, A., i D. N. Guha Bakshi. "Flora of Murshidabad District, West Bengal, India". Kew Bulletin 40, nr 4 (1985): 870. http://dx.doi.org/10.2307/4109879.
Pełny tekst źródłaMondal, Biraj Kanti, Satiprasad Sahoo, Rima Das, Prabuddh Kumar Mishra, Kamal Abdelrahman, Aditi Acharya, Ming-An Lee, Anuj Tiwari i Mohammed S. Fnais. "Assessing Groundwater Dynamics and Potentiality in the Lower Ganga Plain, India". Water 14, nr 14 (10.07.2022): 2180. http://dx.doi.org/10.3390/w14142180.
Pełny tekst źródłaMollah, Dr Kamruzzaman. "A Case Study on Factors Leading to Late Coming at Tungi Swami Swarupananda High School and its Remedial Measures". International Journal of Research Publication and Reviews 03, nr 12 (2022): 1410–21. http://dx.doi.org/10.55248/gengpi.2022.31240.
Pełny tekst źródłaHalder, Ananta, Lusika Datta i Paramita Santra. "Regional Disparity in Educational Development in Murshidabad District, West Bengal". RESEARCH REVIEW International Journal of Multidisciplinary 6, nr 1 (17.01.2021): 140–47. http://dx.doi.org/10.31305/rrijm.2021.v06.i01.028.
Pełny tekst źródłaPanda, Surajit, i Jatisankar Bandyopadhyay. "Morphodynamic Changes of Bhagirathi River at Murshidabad District Using Geoinformatics". Journal of Geographic Information System 03, nr 01 (2011): 85–97. http://dx.doi.org/10.4236/jgis.2011.31006.
Pełny tekst źródłaHaldar, Dinesh. "Two New Cladosporium Species from Murshidabad District, West Bengal, India". International Journal of Current Research and Review 11, nr 5 (2019): 10–13. http://dx.doi.org/10.31782/ijcrr.2019.1013.
Pełny tekst źródłaRozprawy doktorskie na temat "Murshidabad District"
Neal, Andrew W. "Hydrogeochemical and mineralogical evaluation of groundwater arsenic contamination in Murshidabad district, West Bengal, India". Thesis, Kansas State University, 2010. http://hdl.handle.net/2097/7007.
Pełny tekst źródłaDepartment of Geology
Saugata Datta
More than 75 million people in the Bengal Delta of eastern India and Bangladesh are exposed to drinking water with dangerously high arsenic (As) concentrations; the worst case of environmental poisoning in human history. Despite recognition of dangers posed to chronic exposure to drinking water with elevated As, its biogeochemical cycle is inadequately constrained in groundwater flow systems due to its complex redox chemistry and microbially-mediated transformations. Arsenic concentrations in Bengal Delta sediments are comparable to global averages, but its highly heterogeneous spatial distribution (on scales of meters to kilometers) in sediments and groundwaters is poorly understood. Though many research efforts have targeted understanding this heterogeneity in Bangladesh, less work has been done in eastern India. Murshidabad (23°56.355‘N, 88°16.156‘E), an eastern district in West Bengal, India, where groundwaters are highly As-affected (~4000 μg/l), was chosen as our study area. Research objectives were: (1) characterize sediment cores (mineralogically, geochemically) and groundwaters (hydrochemically, isotopically) in areas with contrasting As concentrations—west (low-As) and east (high-As) of river Bhagirathi, a major distributary of Ganges flowing through the heart of Murshidabad; (2) describe and understand the extent of spatial variability, laterally and vertically, of dissolved As concentrations in shallow (< 60 m) aquifers, comparing sediment core chemistry to water chemistry; (3) identify source(s) of aquifer recharge and (4) role(s) of inorganic carbon within the aquifer to understand the bioavailability and mobilization of As from sediments to groundwaters. Mineralogical differences between high-As (grey) and low-As (orange-brown) sediments, were the presence of greater amounts of micas, Fe- and Mg-rich clays, amphiboles, carbonates, and apatite in high-As sediments; these were virtually absent from low-As sediments. In high-As areas, As was associated with amorphous and poorly-crystalline Fe-oxyhydroxide phases and labile (specifically-sorbed) phases, especially where Fe(II):Fe[subscript]T was high in the sediments. High-As groundwaters had high As(III):As[subscript]T, iron, bicarbonate, phosphate, and ammonium, and low concentrations of chloride and sulfate. Dry season precipitation was probably the main source of aquifer recharge; lighter values of [superscript]13C in dissolved inorganic carbon resulted from oxidation of natural organic matter. This study points to an idea that both microbially-mediated oxidation-reduction and competitive ion-exchange processes occurring in shallow aquifers of Murshidabad drive As mobilization and sequestration by aquifer sediments.
Sasidharan, Sankar Manalilkada. "Geochemical significance of arsenic and manganese toxicity in groundwaters from Murshidabad district, West Bengal, India". Thesis, Kansas State University, 2013. http://hdl.handle.net/2097/16275.
Pełny tekst źródłaDepartment of Geology
Saugata Datta
Mass poisoning of arsenic (As) has affected roughly 60 million people in the Bengal Basin (Bangladesh and West Bengal, India) and 43 million people alone in West Bengal. Elevated levels of Manganese (Mn) is another alarming issue in the groundwaters of this region (MCLs: As<10µg/L and Mn< 0.4mg/L). Four locations in Murshidabad district (south-central part of Bengal Basin) were chosen for this current study. Among the 4 locations, two of them showed high concentration of As (>50 - 4622µg/L; 2009 survey) and they are Beldanga: 23° 56'N& 88°15'E and Hariharpara: 24°3.68'N & 88° 21.63'E. On the other hand: Nabagram (24°12.08'N & 88°13.29'E) and Kandi (23°58.6'N & 88°6.68'E) demonstrated less dissolved As (<10µg/L) in groundwaters. Study areas were located to the west (Nabagram, Kandi) and east (Beldanga, Hariharpara) of the river Bhagirathi, a tributary of the river Ganges, flowing N-S through the district of Murshidabad. Eastern side of the river is occupied by grey colored Holocene sediments and western side has more oxidized orangish-brown Pleistocene sediments. Comparative study of major water quality parameters between these sites revealed high As (10-1263µg/L) and low Mn (0.1-1.3mg/L) in the areas like Beldanga, Hariharpara while low As (0-15µg/L) and higher Mn (0.2-4.2mg/L) in Nabagram and Kandi. The pH range for high and low As areas were 4.5-7.8 and 5.1-8.2 respectively. Phosphates showed values <0.04-2.21mg/L in high As areas and <0.08-2.52mg/L in low areas whereas Cl- values were higher within low As areas (29-200mg/L) and lower within high As areas (3.9-78.4mg/L). Fe(t) and Fe2+ values at high and low As areas were 0-13.5mg/L, 0.01-0.11mg/L and 0-1.4mg/L, 0.04-0.06mg/L respectively. δ18O and δD results revealed that monsoonal precipitation is the major recharge source in this area with some input from the surficial waterbodies as ponds in shallower depths within high As areas. The total As extracted from core sediments in these areas do not show much difference: total As in high and low As areas ranges from 6.4-18 mg/kg. Sequential extraction results revealed that majority of the sediment bound As is present in residual phases (>40%). DOC in groundwaters in high and low As areas were 1.5-3.2 and 0.5-1.3mg/L respectively and they had positive correlation with As within the depth profiles. Dissolved organic matter (DOM) characterization studies indicated that microbial proteins (Tyrosine and Tryptophan) are the major components in the groundwaters in the low As region, whereas high As area groundwaters tend to have higher content of humic DOM (A and C). Cl/Br molar ratio of high As wells were low compared to the low As wells. Current study revealed the importance of organic matters (and not the mineralogy of the sediments) both in sediments and groundwaters in controlling the release of As from sediment, at least in the shallow parts of Bengal delta aquifer and microbial mediated reductive dissolution of FeOOH in the presence of organic matter is the major mechanisms by which sediment bound As (<50m depth) is released into the groundwater. The darker organic matter rich sediments (OM both sediment bound and anthropogenically derived) existing at the depth range 20m-50m with reducing environment persisting in both high and low As areas are possible reasons for elevated levels of As in this region.
Rahman, Khalilur. "Democratic decentralisation and empowerment: a study of women of Murshidabad District in West Bengal (1978-1998)". Thesis, University of North Bengal, 2001. http://hdl.handle.net/123456789/147.
Pełny tekst źródłaRoy, Krishna. "Secularism and Indian politics : study of political attitudes and participation of muslims in the district of Murshidabad (1978-2012)". Thesis, University of North Bengal, 2018. http://hdl.handle.net/123456789/2815.
Pełny tekst źródłaAhammed, Abdul Kader. "Changing pattern of rural leadership : a study of Murshidabad and Cooch behar Districts". Thesis, University of North Bengal, 2008. http://hdl.handle.net/123456789/170.
Pełny tekst źródłaKsiążki na temat "Murshidabad District"
Indian freedom movement and Murshidabad District, 1905-1947. Kolkata: K.P. Bagchi & Co., 2008.
Znajdź pełny tekst źródłaBagchi, Jasodhara. Child labour in beedi industry, Murshidabad District in West Bengal. Calcutta: School of Women's Studies, Jadavpur University, 1996.
Znajdź pełny tekst źródłaHistory of Murshidabad District: With Biographies of Some of Its Noted Families. Creative Media Partners, LLC, 2022.
Znajdź pełny tekst źródłaWalsh, J. H. Tull. History of Murshidabad District: With Biographies of Some of Its Noted Families. Creative Media Partners, LLC, 2018.
Znajdź pełny tekst źródła1st, Roy ©. Krishna. Murshidabad : a Bengal District in Transition: Attitude and Participation of the Political Leaders of the District. INSC International Publisher (IIP), 2021.
Znajdź pełny tekst źródłaCzęści książek na temat "Murshidabad District"
Sultana, Bulbul Nargis, i Nasrin Banu. "Livelihood, Food Security, and Sustainability in Murshidabad District". W Agriculture, Environment and Sustainable Development, 251–70. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-031-10406-0_15.
Pełny tekst źródłaPatra, Poly, i Gouri Sankar Bhunia. "Spatial Clustering of P. falciparum Malaria Epidemiology in Murshidabad District". W Advances in Geographic Information Science, 339–52. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-75197-5_15.
Pełny tekst źródłaMollah, Swati. "Causes of Flood Hazard in Murshidabad District of West Bengal: Victims’ Perceptions". W Springer Geography, 99–113. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-26443-1_7.
Pełny tekst źródłaMukherjee, Sucheta. "An Assessment of Human Impact on Bhagirathi River in Murshidabad District: From Reverence to Responsibility". W Fluvial Systems in the Anthropocene, 87–103. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-031-11181-5_6.
Pełny tekst źródłaMandal, Anukul Chandra, i Gouri Sankar Bhunia. "Spatio-Temporal Variation of Morphological Characteristics in Bhagirathi River—Case Study in Murshidabad District, West Bengal (India)". W Geography of the Physical Environment, 179–91. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-030-79634-1_8.
Pełny tekst źródłaChatterjee, Rhitwik. "Spatiotemporal Variation in Physico-chemical Properties of Groundwater Within Arsenic-Affected Shallow Alluvial Aquifers of Murshidabad District, West Bengal, Eastern India". W Ground Water Contamination in India, 33–82. Cham: Springer Nature Switzerland, 2024. http://dx.doi.org/10.1007/978-3-031-49092-7_4.
Pełny tekst źródłaAhmed, S., A. Basu, D. Mandal, I. Saha i M. Biswas. "Investigation of biochemical properties of soil and groundwater in arsenic affected blocks of Murshidabad district and isolation of potential arsenic resistant bacteria". W Arsenic in the Environment: Bridging Science to Practice for Sustainable Development As2021, 71–72. London: CRC Press, 2024. http://dx.doi.org/10.1201/9781003317395-29.
Pełny tekst źródłaAhmed, S., A. Basu, D. Mandal, I. Saha i M. Biswas. "Exploration of biochemical properties of soil and groundwater in arsenic affected blocks of Murshidabad district and isolation of potential arsenic resistant bacteria". W Environmental Arsenic in a Changing World, 281–82. CRC Press, 2019. http://dx.doi.org/10.1201/9781351046633-111.
Pełny tekst źródłaSinha, Madhabendra, Sudhansu Sekhar Mahapatra, Abhijit Dutta i Partha Pratim Sengupta. "Microfinance and Women Empowerment: An Empirical Analysis". W Research Anthology on Microfinance Services and Roles in Social Progress, 1–13. IGI Global, 2022. http://dx.doi.org/10.4018/978-1-6684-7552-2.ch001.
Pełny tekst źródłaSinha, Madhabendra, Sudhansu Sekhar Mahapatra, Abhijit Dutta i Partha Pratim Sengupta. "Microfinance and Women Empowerment: An Empirical Analysis". W Advances in Finance, Accounting, and Economics, 52–64. IGI Global, 2019. http://dx.doi.org/10.4018/978-1-5225-5240-6.ch003.
Pełny tekst źródłaStreszczenia konferencji na temat "Murshidabad District"
Ahmed, Shamsuzzaman. "MORPHODYNAMIC CHANGES INDUCED HUMAN DISPLACEMENT AND ITS CONSEQUENCES OF BHAGIRATHI RIVER AT INDO-BANGLADESH BORDER DISTRICT MALDA AND MURSHIDABAD USING GEOINFORMATICS". W GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-295132.
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