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Journal articles on the topic 'Upper Mahananda Basin'

Author: Grafiati
Published: 18 May 2024
Last updated: 31 July 2025

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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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4

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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6

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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7

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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8

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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10

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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11

Mishra, Vipin Kumar, Dhiraj Khalkho, Vinay Kumar Pandey, and Shruti Verma. "Decadal Change in Land Use and Land Cover Dynamics: A Comprehensive Assessment of the Kharun Catchment." Journal of Scientific Research and Reports 30, no. 12 (2024): 630–39. https://doi.org/10.9734/jsrr/2024/v30i122707.

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Land Use and Land Cover (LULC) changes exert profound influences on environmental and resource dynamics, particularly in developing regions experiencing rapid urbanization and agricultural expansion. This study investigates LULC changes over a 30-year period (1992–2022) in the Kharun catchment, part of the upper Mahanadi basin in Chhattisgarh, India. Encompassing 4,143.17 km² across six districts, the catchment plays a critical role in supporting agricultural and urban activities. Landsat imagery from 1992, 2002, 2012, and 2022 was analyzed using supervised classification with Remote Sensing (
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12

Singh, Kamal Jeet, Anju Saxena, and Shreerup Goswami. "Palaeobiodiversity of the Lower Gondwana rocks in the Korba Coalfield, Chhattisgarh, India and observations on the genus Gangamopteris McCoy." Journal of Palaeosciences 61, no. (1-2) (2012): 145–63. http://dx.doi.org/10.54991/jop.2012.356.

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The Korba Coalfield occupies the south-central part of Son-Mahanadi Master basin and is situated in the Korba and Bilaspur districts of Chhattisgarh State. With five open cast mines (Gevra, Dipika, Manikpur, Kusmunda and Laxman) spreading over 530 sq. kms, this coalfield is the biggest coal producing unit in India, however it was never explored for megafloral studies. Extensive investigations were recently conducted in this coalfield to discover the fossiliferous beds in the Lower Gondwana deposits and as a result a large number of plant fossils were recovered from these collieries and their e
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13

Chakraborty, Kunal, and Snehasish Saha. "Assessment of bank erosion and its impact on land use and land cover dynamics of Mahananda River basin (Upper) in the Sub-Himalayan North Bengal, India." SN Applied Sciences 4, no. 1 (2021). http://dx.doi.org/10.1007/s42452-021-04904-x.

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AbstractBank erosion is the predominant character of River Mahananda in the Sub-Himalayan North Bengal. The present study aims to identify the bank erosion mechanism as well as the impact of river bank erosion on land use and land cover (LULC) dynamics of the study area. Survey of India (SOI) topographical map 78 B/5 (1975) and satellite imageries for the temporal year of 1991 and 2019 from USGS have been used for the study. For the assessment of bank erosion process Bank erosion hazard index (BEHI) model has been adopted here. The channel migration has been delineated by the superimposition o
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14

Kumar, Raj, and D. Twinkle. "Magnetic structure of the uppermost mantle of the Eastern Continental Margin of India and Bay of Bengal inferred from Curie depths estimated by analyzing shipborne magnetic data using Bayesian inversion." Geophysical Journal International, July 24, 2025. https://doi.org/10.1093/gji/ggaf280.

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Summary The Eastern Continental Margin of India (ECMI) is a classic passive margin formed during the Mesozoic breakup of the supercontinent Gondwanaland. Since its formation, the margin has undergone complex post-rift thermal subsidence, magmatic activity, and interactions with adjacent tectonic plates. Extensive shipborne magnetic data have been acquired over the years, providing substantial coverage of the area. However, knowledge about the regional thermal structure and magnetic nature of the upper mantle of the ECMI and adjacent deep offshore Bay of Bengal is not understood uniformly throu
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15

Kumar, M. Dinesh, and Nitin Bassi. "The Climate Challenge in Managing Water: Evidence Based on Projections in the Mahanadi River Basin, India." Frontiers in Water 3 (June 21, 2021). http://dx.doi.org/10.3389/frwa.2021.662560.

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This study analyzes the long-term changes in the rainfall and surface hydrology of the upper and middle sub-basins of Mahanadi, an inter-state river basin in eastern India that experiences climate-induced hydrological extremes, and draws implications for the sustainability of irrigation and drinking water supplies. The likely impacts of rainfall changes on surface flow were also modeled. A Water Evaluation and Planning (WEAP) model was set up (beginning June 2009 and ending May 2050) to analyze the future water balance of the basin for the expected changes in socio-economic conditions. The mod
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16

Rabindra, K. Panda, and Singh Gurjeet. "Analysis of Trend and Variability of Rainfall in the Mid-Mahanadi River Basin of Eastern India." April 15, 2016. https://doi.org/10.5281/zenodo.1125001.

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The major objective of this study was to analyze the trend and variability of rainfall in the middle Mahandi river basin located in eastern India. The trend of variation of extreme rainfall events has predominant effect on agricultural water management and extreme hydrological events such as floods and droughts. Mahanadi river basin is one of the major river basins of India having an area of 1,41,589 km<sup>2</sup> and divided into three regions: Upper, middle and delta region. The middle region of Mahanadi river basin has an area of 48,700 km<sup>2</sup> and it is mostly dominated by agricult
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17

Pichuka, Subbarao, and Rajib Maity. "Spatio-temporal downscaling of projected precipitation in the 21st century: indication of a wetter monsoon over the Upper Mahanadi Basin, India." Hydrological Sciences Journal, October 24, 2016, 1–16. http://dx.doi.org/10.1080/02626667.2016.1241882.

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