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Purandara, B. K.
- Textural and Mineralogical Studies of the Beach Sands from Fort Cochin to Chellanam, Kerala
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Authors
Affiliations
1 School of Marine Sciences, Cochin University of Science and Technology, Cochin 682016, IN
1 School of Marine Sciences, Cochin University of Science and Technology, Cochin 682016, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 30, No 6 (1987), Pagination: 524-531Abstract
In general most of the beach sediments from the area under study are medium sand-sized, unimodal, moderately sorted, nearly symmetrical and mesokurtic in terms of their grain-size distribution. The standard deviation shows minor variations from September to December. The heavy minerals commonly found in these sediments in the order of decreasing abundance are hornblende, opaques, hypersthene, garnet, mica, sillimanite, augite and diopside. The percentage of quartz in the light mineral fraction varies from 57% to 99%. The provenance of these beach sands is believed to be the rocks of the Western Ghats - charnockite and gneissic terrain.- Estimation of Water Yield Under Various Climate Scenarios at a River Basin Scale in the Manimala River, Kerala, India
Abstract Views :143 |
PDF Views:138
Authors
Affiliations
1 Regional Centre, National Institute of Hydrology, Hanuman Nagar, Belagavi, Karnataka, IN
1 Regional Centre, National Institute of Hydrology, Hanuman Nagar, Belagavi, Karnataka, IN
Source
International Journal of Earth Sciences and Engineering, Vol 10, No 1 (2017), Pagination: 126-130Abstract
In the present study, a distributed hydrological model namely soil water analysis tool (SWAT) has been employed for Manimala River Basin in Kerala, India. The entire basin has been divided into 7 major sub-basin to predict the water balance components and their variability under changing climatic conditions. The calibration of the model using the observed data indicated the model parameters such as SOL_AWC, ESCO, GW_REVAP and CN are the sensitive parameters. The estimates of water balance component at basin and sub-basin level show that irrespective of land covers, the runoff generation is as high as 47% (runoff coefficient Q/P) and groundwater recharge is 36%. The estimate of ET is comparatively low.Keywords
Water Yield, Climate Change, GCM, SWAT, Manimala.- Assessment of Groundwater in Ghataprabha Sub-Basin Using Visual MODFLOW Flex
Abstract Views :234 |
PDF Views:158
Authors
Affiliations
1 Department of Water and Land Management, VTU, Belagavi, Karnataka, IN
2 National Institute of Hydrology, Hard Rock Regional Centre, Belagavi, Karnataka, IN
1 Department of Water and Land Management, VTU, Belagavi, Karnataka, IN
2 National Institute of Hydrology, Hard Rock Regional Centre, Belagavi, Karnataka, IN