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Bhattacharjee, S.
- Shallow Marine Siliciclastic Sedimentation in the Middle Proterozoic Gandikota Formation, Cuddapah Basin, Andhra Pradesh
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Authors
Affiliations
1 Geological Survey of India, Project: Cuddapah Basin, Operations: Andhra Pradesh, Bandlaguda, Hyderabad 500 068, IN
1 Geological Survey of India, Project: Cuddapah Basin, Operations: Andhra Pradesh, Bandlaguda, Hyderabad 500 068, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 55, No 1 (2000), Pagination: 65-76Abstract
The Gandikota Formation consists of 40 - 45 m thick shale - siltstone - quartzite (lower member) and 140 - 190 m thick quartzite and siltstone (upper member). Vertical profile of the lower member represents a coarsening up sequence of prograding shoreline setting. As many as eight qualtzite sheets of 15 to 25 m thickness each, constitue the upper member. The herringbone, tabular and trough cross stratified quartzite, and ripple bedded quartzite and siltstone constitute major sedimentary lithofacies in the upper member quartzite sheets. Palaeocurrent mean was towards NW and NNE. A shallow marine environment with poorly contined tidal channels is envisioned for the deposition of the upper member quartzite sheets.Keywords
Sedimentology, Gandikota Formation, Middle Prolelozoic, Cuddapah Basin, Andhra Pradesh.
- Petrological and PGE Mineralization Study of the Channagiri Mafic-Ultramafic Complex, Shimoga Supracrustal Belt, Karnataka
Abstract Views :198 |
PDF Views:146
Authors
S. Balakrishnan
1,
R. Madusudanan
2,
S. Bhattacharjee
3,
S. T. Narahari
3,
R. Ananthanarayana
3,
T. C. Devaraju
4
Affiliations
1 Geological Survey of India, Bangalore - 560 078, IN
2 Geological Survey of India, Bangalore - 560078, IN
3 Petrology Division, GSI, Hyderabad - 500 078, IN
4 'Rajamangala', Saptapur, Haliyal Road, Dharwad - 580001, IN
1 Geological Survey of India, Bangalore - 560 078, IN
2 Geological Survey of India, Bangalore - 560078, IN
3 Petrology Division, GSI, Hyderabad - 500 078, IN
4 'Rajamangala', Saptapur, Haliyal Road, Dharwad - 580001, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 71, No 5 (2008), Pagination: 746-748Abstract
No Abstract.Full Text
- Palaeocurrents and Depositional Setting in the Banganapalle Formation, Kurnool Sub-Basin, Cuddapah Basin, Andhra Pradesh
Abstract Views :153 |
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Authors
Affiliations
1 Geological Survey of India, Operations, Andhra Pradesh, Project: Cuddapah Basin, Bandlaguda, Hyderabad 500068, IN
1 Geological Survey of India, Operations, Andhra Pradesh, Project: Cuddapah Basin, Bandlaguda, Hyderabad 500068, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 53, No 2 (1999), Pagination: 255-259Abstract
Palaeocurrents of the diamondiferous Banganapalle Formation show convergence towards Nandyal depression in the Kurnool Sub-basin. Localised depocentres, separated by E-W trending ridges, are identified near Kurnool, Paniam, Uppalapadu and Proddatur. These ridges pass through Gani, Banganapalle and Gandikota and have influenced sediment dispersal pattern in the Banganapalle Formation. Provenance for the Banganapalle Formation was mainly the intrabasinal tract occupied by lower Cuddapah sediments, igneous intrusives and the basement located to the west. Deposition commenced in an alluvial environment followed by intertidal setting.Keywords
Sedimentology, Palaeocurrents, Banganapalle Formation, Diamond, Kurnool Sub-Basin, Cuddapah Basin, Andhra Pradesh.- Occurrence of Gold in Guntipaui-Atkur Area, Gadwal Schist Belt, Mahbubnagar District, A.P.
Abstract Views :195 |
PDF Views:157
Authors
Affiliations
1 Geological Survey of India, Hyderabad-500 068, IN
1 Geological Survey of India, Hyderabad-500 068, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 49, No 6 (1997), Pagination: 721-722Abstract
Examination of soil and bed rock samples of pegmatites and metabasalts has helped in identifying an auriferous zone in Guntipalli-Atkur area. The samples analysed anomalous gold values ranging from 0.025 to 4.25 ppm.Full Text
- Screening of Certain Chilli Germplasm against Yellow Mite, Polyphagotarsonemus latus (Banks)
Abstract Views :181 |
PDF Views:0
Authors
Affiliations
1 Department of Entomology, Assam Agricultural University, Jorhat (Assam), IN
1 Department of Entomology, Assam Agricultural University, Jorhat (Assam), IN
Source
International Journal of Plant Protection, Vol 10, No 2 (2017), Pagination: 320-323Abstract
An experiment was conducted during the year 2012 and 2013 to screen out 30 chilli germplasm against yellow mite, Polyphagotarsonemus latus (Banks). Out of 30 chill germplasms, 7 germplasmsviz., 13/09, 10/09, 7/09, CH/09/8A3, 11/CHIVAR-6, 10/CHIVAR-6, 10/CHIVAR-3 were found to be resistant as they were found free of mite infestation and leaf curl symptoms. Entries LCA-334, ASC-06-1, KA-2, BH10/04, VR-338, CHIVAR-5, CHIVAR-7, 11/CHIVAR-7, G-8B, G-5B, G-3, G-1, 17/09, 5/A/09, BH10/04 and Mem jolokia were found to be moderately resistant with a damage score of 0.2 to 1.4 showing about 25 per cent leaf curling. The entries 15/02, G-2 and CHIVAR-4 showed a damage score of 2.4, 2.7 and 2.29 and per cent leaf curling of 44.23, 46.53 and 29.28, respectively and were recorded as moderately susceptible. Whereas 11/CHIVAR-1 recorded the highest damage with damage score 3.6, showing 90.48 per cent leaf curling followed by Bhut jolokia and Pusa Juwala which were found to be highly susceptible showing around 82.2 to 89.7 per cent leaf curling with damage score 3.5 and 3.4, respectively.Keywords
Screening, Polyphagotarsonemus latus, Chilli Germplasm.References
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- Borah, D.C. (1987). Bioecology of Polyphagotarsonemus latus (Banks) (Acari; Tarsonemidae) and Scirtothrips dorsalis Hood (Thysanoptera: Thripidae) infesting chilli and their natural enemies. Ph.D. Thesis, University of Agricultural Sciences, Dharwad, KARNATAKA (INDIA).
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- Peter, K.V., Nybe, E.V. and Shylaja, M.R. (2005). Spices production and export from India, Scenario through Five Decades. Advances in Spices Research, pp. 43-50.
- Puttarudriah, M. (1959). Short review on the chilli leaf curl complex and the spray programme for its control. Mysore.J.Agric. Sci., 34 : 93-95.
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- Sharma, S. S. Kalra, V.K. Partap, P. S. and Sharma, N. K. (2009). Screening of chilli germplasm against yellow mite and its management. Indian J. Hort., 66(2) : 204-207.
- Singhal, V. (2003). Chillies in Indian Agriculture, Indian Economic Data Research Centre, In: Mayapuri, New Delhi, India, pp. 565-570.
- Estimating Stream Piracy in the Lower Ganga Plain of a Quaternary Geological Site in West Bengal, India Applying Sedimentological Bank Facies, Log and Geospatial Techniques
Abstract Views :205 |
PDF Views:66
Authors
Affiliations
1 Department of Geography, Sidho-Kanho-Birsha University, Ranchi Road, P.O. Purulia Sainik School 723 104, IN
2 Department of Geography, Jogesh Chandra Chaudhuri College (Calcutta University), 30, Prince Anwar Shah Road, Kolkata 700 033, IN
3 Department of Geography, University of Gour Banga, Mokdumpur, Malda 732 103, IN
1 Department of Geography, Sidho-Kanho-Birsha University, Ranchi Road, P.O. Purulia Sainik School 723 104, IN
2 Department of Geography, Jogesh Chandra Chaudhuri College (Calcutta University), 30, Prince Anwar Shah Road, Kolkata 700 033, IN
3 Department of Geography, University of Gour Banga, Mokdumpur, Malda 732 103, IN
Source
Current Science, Vol 117, No 4 (2019), Pagination: 662-671Abstract
River Bhagirathi is a distributary channel of River Ganga, and Babla is one of its right-bank tributaries in the Ganga delta plain. The Bhagirathi flows in a meandering pattern through the New Quaternary alluvium plain, whereas the Babla flows through the Old Quaternary deposits of yellowish-brown sand, silt and clay. As the Bhagirathi is a distributary of River Ganga, it brings in million tonnes of sediments annually. Mid-channel bar formation, bar dynamics and non-cohesive nature of bank materials promote bank failure and rapid shifting of the channels in the Newer Quaternary sites. As the Bhagirathi migrates towards River Babla, the interfluve zone is being progressively engulfed by the course of the former. To estimate the stream piracy or capture, bank materials, internal organization of mid-channel bar, flow parameters (velocity, channel depth, discharge, etc.) have been taken into consideration. This study documents changes in channel morphology and hydrological parameters, dynamic morphology and hydrological regime of the fluvial system from 1852 to 2017. It predicts the actual time when the Bhagirathi will capture River Babla near village Natungram. The study also discusses why in recent years the rate of lateral migration has increased for a particular portion on the right bank of River Bhagirathi near Natungram.Keywords
Bank Materials, Geospatial Technique, Interfluves, Quaternary Sites, Stream Piracy.Full Text
References
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- Turbulent Fluid Flow and Heat Transfer through a Horizontal Rectangular Diffuser with the Use of Single and Double Baffles
Abstract Views :118 |
PDF Views:2
Authors
Affiliations
1 Department of Computer Science and Engineering, Jadavpur University, Kolkata-700 032, IN
2 Department of Mechanical Engineering, Heritage Institute of Technology, Kolkata-700107, IN
3 Deputy Director of Industrial Training, West Bengal, In-Charge of Govt. ITI Howrah Homes Technical Education, Training and Skill Development Department, Govt. of West Bengal, IN
4 Department of Mechanical Engineering, Jadavpur University, Kolkata-700032, IN
1 Department of Computer Science and Engineering, Jadavpur University, Kolkata-700 032, IN
2 Department of Mechanical Engineering, Heritage Institute of Technology, Kolkata-700107, IN
3 Deputy Director of Industrial Training, West Bengal, In-Charge of Govt. ITI Howrah Homes Technical Education, Training and Skill Development Department, Govt. of West Bengal, IN
4 Department of Mechanical Engineering, Jadavpur University, Kolkata-700032, IN
Source
Journal of the Association of Engineers, India, Vol 91, No 1-4 (2021), Pagination: 15-24Abstract
Scientists and engineers give much attention for convective fluid flow around the baffles because of its wide application in different types of heat exchangers used in industries. Analysis of the velocity profiles of the turbulent flow and convection flow parameters have been studied for a horizontal rectangular asymmetric diffuser, the bottom wall of which is being heated. Single and double baffles of equal height are used in the experiments. The experimental study has been carried out at Reynolds numbers of 3.594x104 3.986x104 and 5.371x104 with base plate temperatures of 323K and 343K respectively. Skin friction coefficient along the walls has been calculated. The variation of local Nusselt number along the upper wall is observed carefully. The effort is made to establish some new empirical relationships between Coefficient of skin friction and Nusselt number with Reynolds number The size of recirculation bubble is also calculated.Keywords
Turbulence, Baffles, Rectangular Diffuser, Skin Friction Coefficient, Reynolds Number.References
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- Razak, A. A., Yaakob, Y. and Ramli, M. N., Computational Simulation of Turbulence Heat Transfer in Multiple Rectangular Ducts, World Academy of Science, Engineering and Technology, Vol. 53, pp.242-246, 2009.
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