Your search found 4 records
1 Chatterji, J.; Das, P. K.; Chakravarty, S.; Singh, H.; Agarwal, R. P. 1999. Scaling-up soil and water conservation efforts in Chotanagpur Plateau, Eastern India. In Hinchcliff, F.; Thompson, J.; Pretty, J.; Guijt, I.; Shah, P. (Eds.). Fertile ground: The impacts of participatory watershed management. London, UK: IT Publications. pp.259-272.
Soil conservation ; Water conservation ; Watersheds ; Social participation ; Non-governmental organizations / India / Chotanagpur Plateau
(Location: IWMI-HQ Call no: 333.91 G000 HIN Record No: H024870)

2 Karmakar, D. 2001. Jaldhar model: Capturing the raindrop – The Jaldhar model, wherein a portion of the land is turned into a water collection pit, has increased the soil moisture over 2,000 hectares of the Chotanagpur Plateau. In Agarwal, A.; Narain, S.; Khurana, I. (Eds.), Making water everybody’s business: Practice and policy of water harvesting. New Delhi, India: Centre for Science and Environment. pp.118-121.
Water harvesting ; Rain ; Models ; Rice ; Paddy fields ; Runoff ; Bunds / India / Chotanagpur Plateau
(Location: IWMI-HQ Call no: 333.91 G635 AGA Record No: H030618)

3 Pangare, V. 2003. 5% Pit technology technical report, Purulia, West Bengal, India. Poverty-Focused Smallholder Water Management: an IWMI research project supported by DFID. Final report document 6 of 9. Colombo, Sri Lanka: International Water Management Institute (IWMI). 18p.
Water conservation ; Rainwater ; Rainfed farming ; Rice ; Cultivation ; Water harvesting ; Water storage ; Models / India / West Bengal / Purulia / Chotanagpur plateau
(Location: IWMI HQ Call no: IWMI Record No: H043995)
https://publications.iwmi.org/pdf/H043995.pdf
(1.25 MB)

4 Gautam, S. K.; Maharana, C.; Sharma, D.; Singh, A. K.; Tripathi, J. K.; Singh, S. K. 2015. Evaluation of groundwater quality in the Chotanagpur plateau region of the Subarnarekha River Basin, Jharkhand State, India. Sustainability of Water Quality and Ecology, 6:57-74. [doi: https://doi.org/10.1016/j.swaqe.2015.06.001]
Groundwater ; Water quality ; Assessment ; Irrigation water ; Drinking water ; Water pollution ; Heavy metals ; Contamination ; Alkaline earth metals ; Sodium ; Magnesium ; Ions ; Salinity ; Chemicophysical properties ; Permeability ; Spatial variation ; Monsoon climate ; Hydrogeology ; Geochemistry ; River basins / India / Jharkhand / Chotanagpur Plateau / Subarnarekha River Basin
(Location: IWMI HQ Call no: e-copy only Record No: H047960)
https://vlibrary.iwmi.org/pdf/H047960.pdf
(3.16 MB)
Suitability study of groundwater for domestic and irrigation purposes was carried out in the middle Subarnarekha river basin, Jharkhand. Collected samples were analysed for physicochemical parameters such as conductivity, total dissolved solids (TDS), pH, and heavy metals. After the physicochemical analysis groundwater samples were categorised for simplicity, accordingly, it shows that 52.6% samples fall in Ca-Cl2, 33.3% in Ca-HCO3, 10.5% in Ca-SO4, and 1.7% samples in Mg-HCO3 and rest were Na-Cl type. Interpretation of hydro-geochemical data suggests that leaching of ions followed by weathering and anthropogenic impact (mainly mining and agricultural activities) control the chemistry of groundwater in the study area. The TDS concentration at Govindpur site varies from 2677 mg L1 in the pre-monsoon to 2545 mg L1 in the post-monsoon season that is higher than the BIS (2004-05) maximum permissible limit (2000 mg L1 ). The elevated concentration of NO3 was identified at Govindpur, Hatia Bridge, Kandra, Musabani, Saraikela, Mango and Tatanagar. The higher NO3 concentration was due to the action of leaching and anthropogenic activities. At most of sampling locations, the concentration of Cd, Pb, and Ni were found higher than the prescribed limits defined by BIS and WHO. Groundwater suitability for drinking purpose was also evaluated by the synthetic pollution index (SPI), it suggests that 74%, 95%, and 21% samples fall in seriously polluted category during pre-monsoon, monsoon, and post-monsoon season, respectively. The calculated values of SAR, Na%, RSC, PI, and MH have shown that except at few locations, most of groundwater samples are suitable for irrigation purposes.

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