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Relevant bibliographies by topics / Upper Mahananda Basin

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Academic literature on the topic 'Upper Mahananda Basin'

Author: Grafiati

Published: 18 May 2024

Last updated: 31 July 2025

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Journal articles on the topic "Upper Mahananda Basin"

1

Thokdar, Tanmay, and Snehasish Saha. "A micro scale study of Mahananda river bank erosion and temporal Land use land cover scenario with special reference to natural forest in the foothills of Darjeeling Himalaya, West Bengal, India." RESEARCH REVIEW International Journal of Multidisciplinary 8, no. 10 (2023): 103–18. http://dx.doi.org/10.31305/rrijm.2023.v08.n10.012.

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Bank erosion is an inevitable vestige of past to evident fluvial dynamics in relation to its discharge and velocities and work-load in view of its load washed or unwashed. The central idea is best suited to study the case of River Mahananda alias Mahanadi within the Upper Mahananda River basin area having similar kind of attestation of facts. The present study needed extraction of satellite imageries of Landsat from USGS sites associated with its processing and ultimately to frame out the temporal scenes through NDVI technique to visualize if the forest cover is at all influenced by bank erosi

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2

OJASVI, P. R., and R. K. PANDA. "LONG- TERM TRENDS AND PERIODICITIES IN THE DAILY RAINFALL SEQUENCES OVER UPPER MAHANADI BASIN." MAUSAM 49, no. 2 (2021): 259–62. http://dx.doi.org/10.54302/mausam.v49i2.3627.

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3

Khalkho, Dhiraj, M. P. Tripathi, S. Patel, and Love Kumar. "Distributed parameter modelling for sediment yield estimation from Hamp watershed in upper Mahanadi basin." Journal of Soil and Water Conservation 20, no. 1 (2021): 22–34. http://dx.doi.org/10.5958/2455-7145.2021.00005.9.

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Panigrahy, B. K., and B. C. Raymahashay. "River water quality in weathered limestone: A case study in upper Mahanadi basin, India." Journal of Earth System Science 114, no. 5 (2005): 533–43. http://dx.doi.org/10.1007/bf02702029.

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5

Saxena, Anju, Kamal Jeet Singh, and Shreerup Goswami. "Advent and decline of the genus Glossopteris Brongniart in the Talcher Coalfield, Mahanadi Basin, Odisha, India." Journal of Palaeosciences 63, no. (1-2) (2014): 157–68. http://dx.doi.org/10.54991/jop.2014.329.

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The paper deals with the distribution of the genus Glossopteris and its fructifications in different Lower Gondwana formations of Talcher Coalfield of Odisha State. We demonstrate how this taxon appeared in this basin in the earliest Permian Talchir Formation and evolved and diversified through the Karharbari, Barakar, Barren Measures and lower part of Kamthi formations and ultimately vanished in the early Triassic in the upper part of Kamthi Formation. Amongst fifty-one species of the genus Glossopteris recorded in all, one species each has been found in the Talchir and upper part of Kamthi f

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Rajput, Preeti, and Manish Kumar Sinha. "Geospatial evaluation of drought resilience in sub-basins of Mahanadi river in India." Water Supply 20, no. 7 (2020): 2826–44. http://dx.doi.org/10.2166/ws.2020.178.

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Abstract Development is said to be sustainable in respect of drought if the effect has been absorbed by the existing system. Occurrence of drought depends on physiographical, climatic factors and optimum utilization of available resources of the river basin. This study aims to evaluate the vulnerability and resilience of river basin systems for the identification of priority areas under drought susceptibility for three different river basins, namely Arpa, Kharun and Upper Seonath of Mahanadi river in central India, as a pilot area for this study. The study represents an approach to evaluate th

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Jana, B. N., and A. K. Ghosh. "A megaspore assemblage from the Athgarh Formation and its bearing on the age of the formation." Journal of Palaeosciences 46, no. (1-2) (1997): 149–55. http://dx.doi.org/10.54991/jop.1997.1333.

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Megaspores have been recorded from the Athgarh Formation of Mahanadi Basin. The megaspore assemblage comprises species of Banksisporites, Bacurnleres, Erlansonisporites, Minerisporites, Saccarisporites, Paxillitriletes, and seed structures referable to Spermatites. The megaspore assemblage has a preponderance of the genera Paxillitriletes and Minerisporites in association with other Early Cretaceous forms, and thus supports the age arrived at on the basis of megafloral data. Spore/pollen investigations had earlier revealed an age ranging between Upper Jurassic to Lower Cretaceous.

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Gautam, Saurabh, Madhumita Das, and Bhaskar Behera. "Palynostratigraphy and palaeoenvironment of the Permian sediments in Mand Coalfield, Mahanadi Basin, Chhattisgarh, India." Journal of Palaeosciences 67, no. (1-2) (2018): 185–200. http://dx.doi.org/10.54991/jop.2018.57.

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Palynological investigation of 483.00 m deep subsurface Permian sediments of borehole MSK–1, in Sithra–Kurekela Block of Mand Coalfield, revealed four distinct palynoassemblage zones. These palynoassemblages belong to Lower and Upper Barakar (Early Permian), Barren Measures and Raniganj (Late Permian) palynofloras of Indian Gondwana. The oldest Palynoassemblage–I, (Scheuringipollenites barakarensis) recorded between 483.60–309.00 m depths, shows dominance of non–striate bisaccate pollen grains chiefly ― Scheuringipollenites followed by Faunipollenites in association with Indotriradites, Dentat

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9

DHAR, O. N., and S. S. NANDARGI. "Monsoon onset and reservoir build up- A case Study for Hirakud." MAUSAM 43, no. 3 (2021): 315–20. http://dx.doi.org/10.54302/mausam.v43i3.3462.

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Onset of monsoon for each year of the period from 1961 to 1986 over the Upper Mahanadi basin has been studied taking into consideration the sharp increase in water levels of the Hirakud reservoir. This study has shown that .there are positive and negative time-lags in the arrival of monsoon run off into the reservoir. It has been seen that positive time lags are due to antecedent condition of the basin before the onset of monsoon while negative time-lag appears to be due to pre-monsoon thunderstorm activity which causes reservoir levels to increase before the onset of monsoon. Attempt has been

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Mishra, Siba Prasad, Abhisek Mishra, and Sonali Padhi. "Geo-informatics of Sedimentation in Indravati Reservoir, Odisha, India." Journal of Scientific Research and Reports 31, no. 1 (2025): 732–54. https://doi.org/10.9734/jsrr/2025/v31i12818.

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The Indravati Basin, in S-W Odisha, with catchment of 38306 Sq. Km. houses the complex Upper Indravati Project (UIP) comprising of four dams, eight dykes, a power house (600MW) and caters irrigation to 227.62 Th. ha in severely drought prone Kalahandi district in Odisha has commenced operation from 1999. Two Link Channels is constructed to interlink the Godavari- the Mahanadi basin. The power House tailrace water is diverted for irrigation to 128,000 hectares via Hati barrage. To solve the necessity of electricity and water for irrigation it is necessary to evaluate sediment entry to the reser

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Dissertations / Theses on the topic "Upper Mahananda Basin"

1

Sarkar, Subir. "A Geo- environmental Appraisal of The Upper Mahananda Basin of The Darjeeling Himalaya West Bengal." Thesis, University of North Bengal, 1989. http://hdl.handle.net/123456789/2333.

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Pompi, Sarkar. "Bank erosion and associated problems in upper mahananda basin in Darjeeling district, West Bengal." Thesis, University of North Bengal, 2021. http://ir.nbu.ac.in/handle/123456789/4664.

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Book chapters on the topic "Upper Mahananda Basin"

1

Mishra, Antaryami, Ajay Kumar Mishra, and Prava Kiran Dash. "Soil Genesis Classification and Land Use of Some Soils in the Upper Mahanadi Basin." In Mahanadi River. Springer Nature Singapore, 2025. https://doi.org/10.1007/978-981-96-1048-8_4.

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Bhoi, Kirtisuta, Saismruti Mohapatra, Prakash Chandra Swain, and Anil Kumar Kar. "Analysis and Forecasting of Meteorological Drought in Upper Mahanadi River Basin Using SPI and ARIMA in R." In Lecture Notes in Civil Engineering. Springer Nature Singapore, 2025. https://doi.org/10.1007/978-981-97-9180-4_1.

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