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Academic literature on the topic 'Godavari River'

Author: Grafiati

Published: 6 September 2023

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Journal articles on the topic "Godavari River"

1

Tamrakar, Naresh Kazi, and Ramita Bajracharya. "Basinal and planform characteristics of the Kodku and the Godavari Rivers, Kathmandu, Central Nepal." Bulletin of the Department of Geology 15 (January 21, 2013): 15–22. http://dx.doi.org/10.3126/bdg.v15i0.7414.

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The rivers of the Kathmandu Basin are vulnerable to flash floods and disturbances caused by anthropogenic as well as climatic changes. Two southern tributaries of the Bagmati River: the Kodku and the Godavari Rivers, have been considered for their (i) watershed-scale geomorphic parameters such as relative relief, drainage texture and stream order, (ii) stretchscale planform parameters such as sinuosity (K), meander belt width (Wblt), meander wavelength (Lm) and radius of curvature (Rc), and (ii) longitudinal profiles and slopes. Both Kodku and the Godavari Rivers are elongate basins with wide ranges of the watershed-scale parameters. The Godavari River is longer, larger and more sinuous compared to the Kodku River. The development of the patterns of the fifth order main stem stretches of both rivers with respect to the stream slopes, and asymmetric patterns of the meander loops indicate anomalous growth of the river stretches. DOI: http://dx.doi.org/10.3126/bdg.v15i0.7414 Bulletin of the Department of Geology, Vol. 15, 2012, pp. 15-22

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Kharat, Sanjeevan J., and Sanjay D. Pagar. "Determination of Phosphate in Water Samples of Nashik District (Maharashtra State, India) Rivers by UV-Visible Spectroscopy." E-Journal of Chemistry 6, s1 (2009): S515—S521. http://dx.doi.org/10.1155/2009/913609.

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The major rivers of Nashik District (Maharashtra State, India) are Godavari, Kadawa, Girna, Punad and Mosam. The major water pollutant of Nashik District Rivers is Phosphate. The amount of phosphate has been determined by the molybdenum blue phosphorous method in conjugation with UV-Visible Spectrophotometer. The data has been analyzed by least square method. The more phosphate polluted river in Nashik district is Godavari. The least phosphate polluted river in Nashik District is Punad.

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3

Bhalla, Resham, Waykar B.B, and Balwinder Sekhon. "Water quality assessment of Godavari river water at Nashik." Environment Conservation Journal 13, no. 3 (December 20, 2012): 43–48. http://dx.doi.org/10.36953/ecj.2012.130308.

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Rivers are vital and vulnerable freshwater systems that are critical for the sustenance of aquatic life and also the main resource for domestic, industrial and agricultural purpose. Godavari is one of the sacred river rises near the Trimbakeshwar in the district of Nasik in the Indian state of Maharashtra. The river is approximately 1,465 km long and has a total catchment area of 31 mha. It flows in the eastward direction through the states of Maharashtra and joins the Bay of Bengal in Andhra Pradesh. Godavari river is under the serious threat as a result of the growing urbanization and industrialization and river water is used for irrigation, drinking and domestic purpose. Therefore the water quality of Godavari river was assessed by determining physico-chemical parameters like pH, temperature, conductivity, Total Dissolved Solids, Total Hardness, Dissolved oxygen, Biological oxygen demand, Chemical oxygen demand, Phosphates, Sulphates and heavy metals like Na, K, Fe, Pb at three locations S1, S2 and S3 during winter, summer and monsoon seasons in the year Nov. 2008 to Oct. 2010. The standard deviation and coefficient correlation of physico-chemical parameters was also calculated. The variations observed in physico-chemical parameters of Godavari river water during the study period may be due to increased influx of sewage, domestic and agricultural wastes which may vary from simple nutrients to toxic and hazardous substances thus making the river water unfit for drinking and domestic purpose.

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4

Kirkels, Frédérique M. S. A., Huub M. Zwart, Muhammed O. Usman, Suning Hou, Camilo Ponton, Liviu Giosan, Timothy I. Eglinton, and Francien Peterse. "From soil to sea: sources and transport of organic carbon traced by tetraether lipids in the monsoonal Godavari River, India." Biogeosciences 19, no. 17 (September 1, 2022): 3979–4010. http://dx.doi.org/10.5194/bg-19-3979-2022.

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Abstract. Monsoonal rivers play an important role in the land-to-sea transport of soil-derived organic carbon (OC). However, spatial and temporal variation in the concentration, composition, and fate of this OC in these rivers remains poorly understood. We investigate soil-to-sea transport of soil OC by the Godavari River in India using glycerol dialkyl glycerol tetraether (GDGT) lipids in soils, river suspended particulate matter (SPM), and riverbed sediments, as well as in a marine sediment core from the Bay of Bengal. The abundance and composition of GDGTs in SPM and sediments in the Godavari River differs between the dry and wet season. In the dry season, SPM and riverbed sediments from the whole basin contain more 6-methyl branched GDGTs (brGDGTs) than the soils. In the upper basin, where mobilisation and transport of soils is limited due to deficient rainfall and damming, contributions of 6-methyl brGDGTs in SPM and riverbed sediments are relatively high year-round, suggesting that they have an aquatic source. Aquatic brGDGT production coincides with elevated values of the isoprenoid GDGT-0 / crenarchaeol ratio in SPM and riverbed sediments from the upper basin, indicating low-oxygen conditions. In the wet season, brGDGT distributions in SPM from the lower basin closely resemble those in soils, mostly from the north and east tributaries, corresponding to precipitation patterns. The brGDGT composition in SPM and sediments from the delta suggests that soil OC is only effectively transported to the Bay of Bengal in the wet season, when the river plume extends beyond the river mouth. The sediment geochemistry indicates that also the mineral particles exported by the Godavari River primarily originate from the lower basin, similar to the brGDGTs, suggesting that they are transported together. However, river depth profiles in the downstream Godavari reveal no hydrodynamic sorting effect on brGDGTs in either season, indicating that brGDGTs are not closely associated with mineral particles. The similarity of brGDGT distributions in bulk and fine-grained sediments (≤ 63 µm) further confirms the absence of selective transport mechanisms. Nevertheless, the composition of brGDGTs in a Holocene, marine sediment core near the river mouth appears substantially different from that in the modern Godavari basin, suggesting that terrestrial-derived brGDGTs are rapidly lost upon discharge into the Bay of Bengal and/or overprinted by marine in situ production. The large change in brGDGT distributions at the river–sea transition implies that this zone is key in the transfer of soil OC, as well as that of the environmental signal carried by brGDGTs from the river basin.

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5

Satish. S. Patil, Satish S. Patil, and Ishwar B. Ghorade. "Zooplankton Diversity from Godavari River Water (Maharashtra)." Indian Journal of Applied Research 3, no. 5 (October 1, 2011): 337–38. http://dx.doi.org/10.15373/2249555x/may2013/100.

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6

Navasakthi, Shibani, Anuvesh Pandey, Rahul Dandautiya, Murtaza Hasan, Mohammad Amir Khan, Kahkashan Perveen, Shamshad Alam, Rajni Garg, and Obaid Qamar. "Assessment of Spatial and Temporal Variation in Water Quality for the Godavari River." Water 15, no. 17 (August 28, 2023): 3076. http://dx.doi.org/10.3390/w15173076.

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With increasing population and industrialization, the water quality of freshwater sources like rivers, lakes, and ponds is becoming increasingly degraded. Most of the rivers in India are becoming polluted, including the Godavari. With the construction of dams, new industries and unsustainable agricultural practices in the Godavari basin, the water characteristics are degrading spatially and temporally. The present study emphasizes the analysis of water quality parameters like temperature, pH, Dissolved Oxygen (DO), conductivity, Biological Oxygen Demand (BOD), nitrate, and faecal coliform concentration in the Godavari basin. This was achieved by analysis of data taken from the Central Pollution Control Board, India (CPCB) for 21 stations around the Godavari basin over a span of five years from 2015 to 2019. The Pearson Correlation coefficient for the water quality parameters was assessed to study the relationship among the parameters. Variation in the water quality parameter is observed from the graphs for each station for respective years. It was found that conductivity and DO, temperature and pH and DO and faecal coliform are negatively correlated. It was also observed that DO has a negative correlation with pH, BOD and faecal coliform, indicating the utilization of dissolved oxygen at higher rates due to increasing degradation of organic matter by aerobic microorganisms in the river. One-way ANOVA was applied to find out significant temporal variations and it was observed that temperature, pH, and faecal coliform level had significantly changed the overdue course of time (F(4, 115) = 2.451, p < 0.05). The obtained results from the analysis indicate that the selected water quality parameters have varied significantly spatially, whereas temporally, according to the ANOVA coefficient, only temperature, pH and faecal coliform had shown significant differences during the selected timeframe. Hence, the present study highlighted the deteriorating water quality of the Godavari River over time.

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Jain, Namrata, and P. Srinivasa Reddy. "Studies on Heavy Metal Contamination and Physico-chemical Properties of Godavari River Water at Rajahmundry, Andhra Pradesh." Oriental Journal Of Chemistry 38, no. 3 (June 30, 2022): 785–89. http://dx.doi.org/10.13005/ojc/380333.

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The present study is aimed to examine the water quality of the Godavari River at Rajahmundry. Water samples from Kotillingala Revu, Kovur Godavari river bridge, Saraswati Ghat, Dowleswaram, Pushkar Ghat were collected and analysed for pH, electrical conductivity, total hardness, TDS, DO, BOD, COD, nitrates. The concentration of six heavy metals were analysed quantitatively using atomic absorption spectrophotometer.

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8

Karki, Swarup Singh, and Naresh Kazi Tamrakar. "Fluvial morphology and dynamics of the Godavari Khola, southeast Kathmandu, Central Nepal." Bulletin of the Department of Geology 19 (December 1, 2016): 15–28. http://dx.doi.org/10.3126/bdg.v19i0.19990.

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The Godavari Khola flowing from the south to the north contributes the Hanumante Khola, which is one of important tributaries of the Bagmati River, flowing from the eastern part of the Kathmandu Basin. Recently, the Godavari Khola has been suffering from human encroachments due to rapid urbanization. Studying nature and dynamics of the stream are important works if the stream has to be made less affected and well managed. The present study aims to establish fluvial morphology and stability status of the Godavari Khola. For these purposes, the watershed was analysed for morphometric parameters and planform fluvial morphology, and thirteen representative segments were surveyed from upstream to downstream of the Godavari Khola for recording and analysing sediment properties, stream cross-sections and profiles, and hydraulic parameters, river dynamics and stability.The Godavari River is a fifth order stream, the two upstream segments of which are bedrock channels, and the rest of the segments are alluvial channels. The segments are classified into six kinds such as C4-, C5-, B3-, B4-, E4- and F4-type streams. The upstream segments are of B4-, B3- and ‘F4’-types which show entrenched, steep, gravel to cobble grade streams. The downstream segments are of C4-, C5-, E4- and F4-types showing non-entrenched to low entrenched streams with gentle slopes, high sinuosity and gravel to sand grade bed materials. The stability status of the Godavari Khola shows that the stream segments 1, 2, 11 and 13 lie in the degrading condition whereas the remaining nine segments lie in the aggrading condition. Because of the huge width/depth ratio in majority of the downstream channels, bank erosion is relatively prone in the downstream segments of the Godavari Khola, whereas bed incision is prone in segments 11 and 13.Bulletin of the Department of Geology, Vol. 19, 2016, pp. 15–28

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9

Somisetty, Anusha, Akshay Pachore, Renji Remesan, and Rohini Kumar. "Multi-Model Assessment of Streamflow Simulations under Climate and Anthropogenic Changes Exemplified in Two Indian River Basins." Water 14, no. 2 (January 11, 2022): 194. http://dx.doi.org/10.3390/w14020194.

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This study aims to evaluate the climate- and human-induced impacts on two contrasting river basins in India, specifically, the Ganges and the Godavari. Monthly discharge simulations from global hydrological models (GHMs), run with and without human influence using CMIP5 projections under the framework of the Inter-Sectoral Impact Model Intercomparison Project, are utilized to address the scientific questions related to the quantification of the future impacts of climate change and the historical impacts of human activities on these river basins. The five state-of-the-art GHMs were considered and subsequently used to evaluate the human and climate change impacts on river discharges (seasonal mean discharge and extreme flows) during the pre-monsoon, monsoon, and post-monsoon seasons under the RCP2.6 and RCP8.5 emission scenarios. Results showed that human impacts during the baseline period on long-term seasonal discharge in the Ganges and Godavari River basins for the pre-monsoon season are around 40% and 23%, respectively, and these impacts are stronger than the future climate change impact in the pre-monsoon season for the Ganges basin, whereas, for the Godavari basin, the same pattern is observed with some exceptions. The human impact in the course of the historical period on the pre-monsoon flows of both the Ganges and the Godavari are more significant than on the monsoon and post-monsoon flows. In the near future (2010–39) time slice, the impact of climate change on the streamflow of the Ganges is highest for the post-monsoon season (13.4%) under RCP 8.5 as compared to other seasons. For Godavari, in the near-future period, this impact is highest for the pre-monsoon season (18.2%) under RCP 2.6. Climate-induced changes in both of the basins during both the monsoon and post-monsoon seasons is observed to have a higher impact on future flows than direct human impact-induced changes to flow during the current period. High flows (31.4% and 19.9%) and low flows (51.2% and 36.8%) gain greater influence due to anthropogenic actions in the time of the pre-monsoon season compared to other times of year for the Ganges and Godavari basins, respectively. High flows for the Ganges during the near future time slice are most affected in the monsoon season (15.8%) under RCP 8.5 and, in the case of the Godavari, in the pre-monsoon season (18.4%) under the RCP 2.6 scenario. Low flows of the Ganges during the near-future period are most affected during the monsoon season (22.3%) and for the Godavari, low flows are affected most for the post-monsoon season (22.1%) under RCP 2.6. Uncertainty in the streamflow estimates is more pronounced for the Godavari basin compared to the Ganges basin. The findings of this study enhance our understanding of the natural and human-influenced flow regimes in these river basins, which helps the formation of future strategies, especially for inter-state and transboundary river management.

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10

Kolhe, Dr Bharati G., Shinde S. M. Shinde S. M, and Rane M. S. Rane M. S. "Composition and Biodiversity of Rotifer Population in Godavari River." Indian Journal of Applied Research 4, no. 6 (October 1, 2011): 554–56. http://dx.doi.org/10.15373/2249555x/june2014/172.

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Books on the topic "Godavari River"

1

Central Inland Capture Fisheries Research Institute (Barrackpore, India), ed. River Godavari, environment and fishery. Barrackpore: Central Inland Capture Fisheries Research Institute, Indian Council of Agriclutural Research, 2000.

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2

When Godavari comes: People's history of a river : journeys in the zone of the dispossessed. Delhi: Aakar Books, 2014.

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3

Abbasi, S. A. Environmental impact of water resources projects: With special reference to Krishna, Mahanadi, and Godavari river basins. New Delhi: Discovery Pub. House, 1991.

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4

Singh, Hardeep. Towards developing a perspective for water governance: Hydrology, water supply, and use in Maneru basin of river Godavari. Hyderabad: Research Unit for Livelihoods and Natural Resources, 2011.

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5

Rao, Subba. On the Banks of River Godavari. Xlibris, 2016.

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6

Ganti, Satyanarayana. My Journey from Godavari in Rajahmundry to River Mississippi in Greenville, USA. Author Reputation Press, LLC, 2022.

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Ganti, Satyanarayana. My Journey from Godavari in Rajahmundry to River Mississippi in Greenville, USA. Author Reputation Press, LLC, 2022.

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8

Butterflies, amphibians & reptiles of Godavari river basin, Andhra Pradesh: A pictorial field guide. Hyderabad: Singareni Collieries Company Limited, 2011.

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Book chapters on the topic "Godavari River"

1

Babar, Md, and R. D. Kaplay. "Godavari River: Geomorphology and Socio-economic Characteristics." In Springer Hydrogeology, 319–37. Singapore: Springer Singapore, 2018. http://dx.doi.org/10.1007/978-981-10-2984-4_26.

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2

Aher, Madhura, and S. M. Yadav. "Trend Analysis of Water Flow and Suspended Sediment Flow of Lower Godavari Basin, India." In River Hydraulics, 261–75. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-81768-8_22.

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Padder, Aajaz Ahmad, and Priyank J. Sharma. "Trends in Extreme Streamflow Indices in the Godavari River Basin." In Climate Change Impact on Water Resources, 127–40. Singapore: Springer Nature Singapore, 2023. http://dx.doi.org/10.1007/978-981-19-8524-9_11.

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Srinivasa Rao, G. V. R., M. Rajesh Kumar, T. P. Sreejani, and P. V. R. Sravya. "Multivariate Statistical Analysis of River Water Quality—A Study on River Godavari in Andhra Pradesh." In Water Resources and Environmental Engineering II, 69–77. Singapore: Springer Singapore, 2018. http://dx.doi.org/10.1007/978-981-13-2038-5_7.

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Shaikh, P. R., Girish Deore, A. D. Pathare, D. V. Pathare, and R. S. Pawar. "Assessment of Godavari River Water Quality of Nanded City, Maharashtra, India." In Techno-Societal 2020, 1117–29. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-69925-3_106.

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Shaikh, P. R., Girish Deore, A. D. Pathare, D. V. Pathare, and R. S. Pawar. "Assessment of Godavari River Water Quality of Nanded City, Maharashtra, India." In Techno-Societal 2020, 947–61. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-69921-5_95.

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Manohar Reddy, V., and Litan Kumar Ray. "Development of Machine Learning Based Flood Prediction Model for Godavari River Basin." In Disaster Resilience and Green Growth, 363–83. Singapore: Springer Nature Singapore, 2022. http://dx.doi.org/10.1007/978-981-19-7100-6_20.

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8

Kiran, S., Anwesna Poudyal, Samer Pradhan, and Monalisha Gautom. "Application of ArcGIS and HEC-RAS in Assessing Sedimentation in Godavari River Reach." In Lecture Notes in Civil Engineering, 157–67. Singapore: Springer Singapore, 2022. http://dx.doi.org/10.1007/978-981-16-7397-9_11.

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9

Pichuka, Subbarao, Srikanth Bhoopathi, and Siva Sai Syam Nandikanti. "Application of TVDM in Modeling the Observed Precipitation Over Godavari River Basin, India." In Climate Change Impact on Water Resources, 29–38. Singapore: Springer Nature Singapore, 2023. http://dx.doi.org/10.1007/978-981-19-8524-9_3.

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10

Lakeshri, Chaitanya, and Kaustubh Salvi. "Hydrologic Modeling with Transfer Function Based Approach: A Comparative Study over Godavari River Basin." In Learning and Analytics in Intelligent Systems, 115–22. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-24314-2_16.

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Conference papers on the topic "Godavari River"

1

Goud, Ravi Kumar, Ajay Kumar V., T. Rakesh Reddy, B. Vinod, and S. Shravani. "Effect of metal oxide nanoparticles on Godavari river water treatment." In PROCEEDINGS OF THE INTERNATIONAL SEMINAR ON METALLURGY AND MATERIALS (ISMM2017): Metallurgy and Advanced Material Technology for Sustainable Development. Author(s), 2018. http://dx.doi.org/10.1063/1.5038682.

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Sebastian, Maneesha, and Manasa Ranjan Behera. "Surge Height and Current Estimation Along K-G Basin." In ASME 2018 37th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2018. http://dx.doi.org/10.1115/omae2018-77945.

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Numerical investigation on storm surge characteristics would benefit the planners and designers of coastal structures and offshore platforms along the Krishna-Godavari (K-G) basin. The adjoining coastline has a wide range of geomorphological features and varying geometries due to the sediment deposition from the two major rivers, Krishna and Godavari. Two severe cyclonic storms (SCS) Laila (2010) and Helen (2013) that approached the basin from two different directions and made landfalls closer to each other were analyzed for determining the storm surge heights and currents along the K-G river basin. The maximum water elevations and maximum currents during the storm event and evolution of storm surge heights at different locations were studied. It could be concluded from the study that when a SCS event approaches K-G basin, in addition to the tide and wave effect, a maximum storm surge height and current of 1 m and 1.2 m/s can be expected along the coast, respectively. Similarly, the surge and current in the offshore regions were found to be 0.3 m and 0.8 m/s, respectively. These values may be considered while deriving design parameters for the offshore installations. The critical regions in the basin were identified where high surge heights and currents are expected.

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Das, Jew, and N. V. Umamahesh. "Multisite Downscaling of Monsoon Precipitation over the Godavari River Basin under the RCP 4.5 Scenario." In World Environmental and Water Resources Congress 2015. Reston, VA: American Society of Civil Engineers, 2015. http://dx.doi.org/10.1061/9780784479162.105.

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Hishamunda, Valens, and Chakrabarti Ramananda. "Temporal Variation in Major Ion Concentrations and 87Sr/86Sr of Headwaters of the Godavari River Draining Basalt, India." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.1033.

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