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Journal articles on the topic 'Mahi River'

Author: Grafiati

Published: 5 June 2025

Last updated: 1 August 2025

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1

Amita, O. Sankhwal, D. Shah Shruti, J. Gavali Deepa, and N. Dudani Sumesh. "Riparian Flora of Mahi River, Gujarat." Biolife 3, no. 4 (2022): 820–26. https://doi.org/10.5281/zenodo.7306479.

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<strong>ABSTRACT</strong> The rivers are important channels of materials and energy, which are constantly reeling under the impacts of human influences that often lead to problems in biodiversity conservation and ecosystem functions. The Mahi River in Gujarat is a west-flowing perennial river holding lot of ecological and religious importance. Hence, this study was carried out to document the floristic diversity in selected villages of Vadodara district falling in the riparian zone of the river. Total 328 species of flowering plants belonging to 230 genera and 73 different families was recorde

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2

Barodawala, S. F., P. K. Patel, and C. D. Patel. "The Possible Causes of Variation in Water Quality of Mahi River, Gujarat, India." Journal Geological Society of India 39, no. 6 (1992): 467–73. http://dx.doi.org/10.17491/jgsi/1992/390603.

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Abstract The damming of the Mahi has retarded the natural cleansing processes of the river, making it incapable of flushing away effluents. This problem is further compounded by the large-scale tidal ingress in the Mahi, which impedes the already sluggish flow of the water, thereby concentrating the pollutants in the downstream portion. This is critical, since nearly half of Baroda city's drinking water is obtained from French-wells dug in the Mahi river bed at Vasad which is under the influence of the tidal ingress.

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3

Pandya, Pranav J., and Kauresh D. Vachhrajani. "Birds of Mahi River estuary, Gujarat, India." Journal of Threatened Taxa 2, no. 6 (2010): 994–1000. http://dx.doi.org/10.11609/jott.o2316.994-1000.

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4

Pawar, Uttam, Pramodkumar Hire, Ranjan Sarukkalige, and Upaka Rathnayake. "Hydro-Meteorological Characteristics of the 1973 Catastrophic Flood in the Mahi Basin, India." Water 15, no. 9 (2023): 1648. http://dx.doi.org/10.3390/w15091648.

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The September 1973 flood in the Mahi Basin was one of the most catastrophic and widespread in the 20th century. However, the hydro-meteorological characteristics of the 1973 flood were not studied. Therefore, an attempt has been made to analyze the meteorological and hydrological processes that led to the 1973 flood. Accordingly, daily rainfall data, river discharge, and cross-section data were obtained for the analysis. The 1973 flood was associated with very heavy rainfall resulting from two successive low-pressure systems (LPS) from 26 to 31 August 1973 and 2 to 5 September 1973. The rainfa

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5

Raj, Rachna, D. M. Maurya, and L. S. Chamyal. "Tectonic Geomorphology of the Mahi River Basin, Western India." Journal Geological Society of India 54, no. 4 (1999): 387–98. http://dx.doi.org/10.17491/jgsi/1999/540406.

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Abstract Neotectonic activity along pre-Quaternary tectonic trends has played a major role in the evolution of Mahi drainage basin. The Mahi basin is controlled by NE-SW and WNW-ESE Aravalli trend in the uplands and by NNW-SSE Tertiary basement faults in the distal part. Lineament analysis shows three structural trends in the area which are related to major regional tectonic trends. Stream orientations indicate that the NNE-SSW and NNW-SSE trends represent lineaments which were active during the youngest tectonic phase. The NE-SW and WNW-ESE trends are slightly older. The evolution of overall

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Malik, J. N., Aniruddha S. Khadkikar, and S. S. Merh. "Allogenic Control on Late Quaternary Continental Sedimentation in the Mahi River Basin, Western India." Journal Geological Society of India 53, no. 3 (1999): 299–314. http://dx.doi.org/10.17491/jgsi/1999/530303.

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Abstract The late Quaternary continental succession exposed along the cliff-like banks (15-35 m) of the Mahi river basin comprises sediments of fluvial and aeolian origin and provides an opportunity to assess palaeoclimatic changes in western India. Seven different facies are recognized in the exposed sediment succession. The trough cross-stratified conglomerates (Gt) formed due to downstream migration of trains of sinuous-crested dunes in shallow channels, whereas the formation of planar cross-stratified gravels (Gp) is attributed to downstream accretion of the avalanching front of a mid-chan

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7

Banyal, Harinder Singh, and Sanjeev Kumar. "Studies on fish diversity of the Mahi River, Rajasthan State." Records of the Zoological Survey of India 119, no. 1 (2018): 1–8. https://doi.org/10.26515/rzsi/v119/i1/2019/141307.

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Banyal, Harinder Singh, Kumar, Sanjeev (2019): Studies on fish diversity of the Mahi River, Rajasthan State. Records of the Zoological Survey of India 119 (1): 1-8, DOI: 10.26515/rzsi/v119/i1/2019/141307

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8

Ram, Balak. "RIVERS OF RAJASTHAN: A CARTOGRAPHIC PRESENTATION AND ASSESSMENT OF THEIR CONDITION." Journal of Global Resources 9, no. 01 (2023): 37–48. http://dx.doi.org/10.46587/jgr.2023.v09i01.004.

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Abstract: Based on the interpretation of all the Survey of India topographical sheets of Rajasthan on 1:50,000 scale and Google Earth Images, basin wise a total of 455 rivers are identified and mapped and flow charts are prepared. Basin wise water resources development & planning documents are consulted to find out their characteristics, problems and potentials. Chambal, Mahi and Luni basins have good network of rivers. A large number of small rivers/nallah originating from low hills and uplands, are lost in sandy/alluvial plains. Overall unwarranted human activities are sole responsible f

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9

Chaudhary, Kinjalben Vinubhai, and Ashokkumar V. Babaria. "Study of Key Parameters of Soil of Vatrak Riverbed of Kheda District Gujarat and Its Impact on Floristic Diversity." RESEARCH REVIEW International Journal of Multidisciplinary 10, no. 4 (2025): 254–65. https://doi.org/10.31305/rrijm.2025.v10.n4.028.

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The Vatrak river is a tributary of the Sabarmati River. It flows for around 243 km in state of Gujarat. Origin of Vatrak river is in hills of Dungarpur, Rajasthan. It enters into Gujarat near village Moydi which is located in Meghraj Taluka of Aravali district. Vatrak flows parallel to Mahi River for 29 km in Rajasthan before entering Gujarat. Direction of the Vatrak river is South-west. It is joined by Mazum river on the border of Kheda District. Vatrak is joined by river Shedhi and Meshwo near Kheda Town. Vatrak finally merge with Sabarmati River at Vautha near Dholka. Maximum length of Vatr

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10

Sridhar, Alpa. "Mid–late Holocene hydrological changes in the Mahi River, arid western India." Geomorphology 88, no. 3-4 (2007): 285–97. http://dx.doi.org/10.1016/j.geomorph.2006.12.001.

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11

Patel, Ankit, T. Thomas, R. M. Singh, Vijay Shankar Yadav, Deepak Kumar, and Archana Kaushal. "Assessment of Climatic Variables for the Mahi River Basin in Western India." International Journal of Environment and Climate Change 15, no. 4 (2025): 287–303. https://doi.org/10.9734/ijecc/2025/v15i44810.

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One of the major problems that humanity is currently facing is climate change, whose effects can be seen everywhere in the world. Climate change is a result of both natural and manmade factors. These alterations have been more pronounced since the start of the industrial revolution, which resulted in significant emissions of greenhouse gases into the atmosphere, obstructing the outflow of longwave radiation and causing an increase in global warming. An attempt has been made to investigate the variability in rainfall, mean temperature, potential evapotranspiration and aridity index in the conte

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Patel, Ankit, Deepak Kumar, V. S. Yadav, Pavan Kumar Harode, and Archana Kaushal. "Comparison of Aridity Indices in Mahi River Basin under Climate Change Scenarios." Journal of Experimental Agriculture International 47, no. 4 (2025): 234–57. https://doi.org/10.9734/jeai/2025/v47i43373.

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Climate change represents one of the most pressing global challenges of the 21st century, driven by a combination of natural climatic variability and intensified by anthropogenic activities. Since the advent of the Industrial Revolution, the accelerated emission of greenhouse gases (GHGs) particularly carbon dioxide (CO₂), methane (CH₄), and nitrous oxide (N₂O) has significantly contributed to global warming by enhancing the greenhouse effect, wherein long-wave terrestrial radiation is increasingly trapped within the Earth's atmosphere. The combined effects of these processes are increasingly

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13

J.I., Nirmal Kumar, Shamiyan R. Khan, Rita N. Kumar, and P. R. Sajish. "Assessment of Hydrochemical Characters Variations in Relation to Phytoplankton during Pre-monsoon at J-point of Mahi Estuary, Gujarat, India." Our Nature 11, no. 2 (2014): 85–95. http://dx.doi.org/10.3126/on.v11i2.9533.

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Variations of hydro-chemical characters were recorded at three sites of Mahi estuary, near J-point (Lat. 22º10.3′N and Long. 72º44.28′E) during the pre-monsoon period. The concentration of the nutrients was relatively high due to the elevated atmospheric temperature, evapo-transpiration of water, slow saline intrusion as well as low inflow of surface water from Mahi River. On the contrary, dissolved oxygen (DO) was at its minimum level during this investigated period. The trophic status of all the three study stations was determined in terms of DO, phosphate, nitrate and sulphate in relation t

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14

JAIN, MAYANK, NIGEL H. WOODCOCK, and SAMPAT K. TANDON. "Neotectonics of western India: evidence from deformed Quaternary fluvial sequences, Mahi River, Gujarat." Journal of the Geological Society 155, no. 6 (1998): 897–901. http://dx.doi.org/10.1144/gsjgs.155.6.0897.

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15

Tripathy, Biplab, and Tanmoy Mondal. "Socioeconomic Challenges faced by Basin’s People in India." Think India 22, no. 2 (2019): 296–304. http://dx.doi.org/10.26643/think-india.v22i2.8730.

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India is a subcontinent, there huge no of people lived in river basin area. In India there more or less 80% of people directly or indirectly depend on River. Ganga, Brahamputra in North and North East and Mahanadi, Govabori, Krishna, Kaveri, Narmoda, Tapti, Mahi in South are the major river basin in India. There each year due to flood and high tide lots of people are suffered in river basin region in India. These problems destroy the socio economic peace and hope of the people in river basin. There peoples are continuously suffered by lots of difficulties in sort or in long term basis. Few bas

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16

Sharma, Pankaj, and Dolly Kumar. "Odonata diversity in and around Vadodara, Gujarat, India." ENTOMON 45, no. 1 (2020): 43–52. http://dx.doi.org/10.33307/entomon.v45i1.502.

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Investigation on the diversity of Odonates revealed a total of 38 species belonging to two suborders, six families, and 24 genera in and around Vadodara, in Gujarat, which included 15 species of Zygoptera (damselfly) and 23 species of Anisoptera (dragonfly). Out of the 38 species, 10 species are new records for the Vadodara. Most number of species was found in water reservoirs as compared to urban ponds and area around Mahi River. Furthermore, it was observed that areas around the rivers were adversely affected because of nearby sand mining. Amongst damselflies and dragonflies the population o

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17

Saxena, R. K., and Tudor Rickards. "Innovation and the Dynamics of Economic Growth: The Case of the Mahi River Project." Creativity and Innovation Management 6, no. 4 (1997): 206–17. http://dx.doi.org/10.1111/1467-8691.00071.

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18

Jain, M., S. K. Tandon, and S. C. Bhatt. "Late Quaternary stratigraphic development in the lower Luni, Mahi and Sabarmati river basins, western India." Journal of Earth System Science 113, no. 3 (2004): 453–71. http://dx.doi.org/10.1007/bf02716736.

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19

Bhati, Dinesh Singh, Swatantra Kumar Dubey, and Devesh Sharma. "Application of Satellite-Based and Observed Precipitation Datasets for Hydrological Simulation in the Upper Mahi River Basin of Rajasthan, India." Sustainability 13, no. 14 (2021): 7560. http://dx.doi.org/10.3390/su13147560.

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Hydrological modeling is an important tool used for basin management and studying the impacts of extreme events in a river basin. In streamflow simulations, precipitation plays an essential role in hydrological models. Meteorological satellite precipitation measurement techniques provide highly accurate rainfall information with high spatial and temporal resolution. In this analysis, the tropical rainfall monitoring mission (TRMM) 3B42 V7 precipitation products were employed for simulating streamflow by using the soil water assessment tool (SWAT) model. With India Metrological Department and T

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20

Raj, Rachna, D. M. Maurya, and L. S. Chamyal. "Tectonic Control on Distribution and Evolution of Ravines in the Lower Mahi Valley, Gujarat." Journal Geological Society of India 53, no. 6 (1999): 669–74. http://dx.doi.org/10.17491/jgsi/1999/530604.

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Abstract All along the Lower Mahi Valley, ravines form an important geomorphic unit. These have developed extensively in the Late Pleistocene continental sediments delimited by flat alluvial plains on one side and river channel on the other. The ravines are confined to all the three pediment, alluvial and estuarine zones. The intensity of these is more on the left bank compared to the right and suggest a differential uplift of the horst block dong basement faults. Morphologically, the ravines are divisible into two types: sharp crested, steep, deeply entrenched and gently sloping, with shallow

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21

Srivastava, P. K., S. Mukherjee, M. Gupta, and S. K. Singh. "Characterizing Monsoonal Variation on Water Quality Index of River Mahi in India using Geographical Information System." Water Quality, Exposure and Health 2, no. 3-4 (2011): 193–203. http://dx.doi.org/10.1007/s12403-011-0038-7.

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22

Sharma, Anupam, Abhay Kumar Singh, and Kamlesh Kumar. "Environmental geochemistry and quality assessment of surface and subsurface water of Mahi River basin, western India." Environmental Earth Sciences 65, no. 4 (2011): 1231–50. http://dx.doi.org/10.1007/s12665-011-1371-7.

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23

Sridhar, Alpa. "A mid–late Holocene flood record from the alluvial reach of the Mahi River, Western India." CATENA 70, no. 3 (2007): 330–39. http://dx.doi.org/10.1016/j.catena.2006.10.012.

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24

Modi, Dharmesh. "Monitoring Landform Dynamics of Mahi River Estuary at Gulf of Cambay, Gujarat Using RS-GIS Techniques." International Journal for Research in Applied Science and Engineering Technology 13, no. 5 (2025): 5488–95. https://doi.org/10.22214/ijraset.2025.71533.

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Abstract: The Gulf of Cambay (GoC), the extension of the Arabian Sea, is the valuable asset and is importantfor the economic progress of the state and the nation.This study is focused on estuary of Mahi River and its tributary at Gulf of Cambay (GoC).The studiesshows arising complications of mix nature in a regiondue to several reasons.To detect and assess the decadal landform changes for the 1978-2017 time frame and Level I & II Classification System for Coastal Land Use Mapping for the geology and geomorphological features were considered. Satellite data were used in ArcGIS environment t

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Sonia, Kusum Chauhan, and Jai Bharat Singh. "Impact of Irrigation on Cropping Pattern in Mahi River Dam Catchment Area in Banswara District (Rajasthan)." Anthology The Research 8, no. 10 (2024): E 84—E90. https://doi.org/10.5281/zenodo.11001877.

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This paper has been published in Peer-reviewed International Journal "Anthology The Research"                URL : https://www.socialresearchfoundation.com/new/publish-journal.php?editID=8837 Publisher : Social Research Foundation, Kanpur (SRF International)                  Abstract :  The cropping pattern refers to the proportion of land under cultivation of various crops at different points of time. This indicates the time and a

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Vaishali Rajwadi, Ganapat Bavaliya, and Bharat Maitreya. "Riparian Angiospermic vegetation of Gujarat: A review." World Journal of Advanced Research and Reviews 25, no. 3 (2025): 119–25. https://doi.org/10.30574/wjarr.2025.25.3.0597.

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Rivers are considered the cornerstone of human civilization all throughout the world. Humans are inextricably linked to the riverine ecology, as seen by the presence of villages, cities, industrial facilities, and irrigated agriculture along the riverbank. The term “riparian ecosystem” refers to vegetation communities that have been created along the banks of rivers or streams, which are interfaces between terrestrial and aquatic ecosystems. Species-rich environments and higher biomass production rates are characteristics of riparian vegetation zones, which are distinguished from other nearby

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Chaudhary, Kinjalben Vinubhai. "Study of Key Parameters of Water of Vatrak Riverbed of Kheda District Gujarat and Its Impact on Floristic Diversity." RESEARCH HUB International Multidisciplinary Research Journal 12, no. 5 (2025): 13–19. https://doi.org/10.53573/rhimrj.2025.v12n5.002.

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The Vatrak river is a tributary of the Sabarmati River. It flows for around 243 km in state of Gujarat. Origin of Vatrak river is in hills of Dungarpur, Rajasthan. It enters into Gujarat near village Moydi which is located in Meghraj Taluka of Aravali district. Vatrak flows parallel to Mahi River for 29 km in Rajasthan before entering Gujarat. Direction of the Vatrak river is South-west. It is joined by Mazum river on the border of Kheda District. Vatrak is joined by river Shedhi and Meshwo near Kheda Town. Vatrak finally merge with Sabarmati River at Vautha near Dholka. Maximum length of Vatr

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28

Nigam, Utkarsh, Vinodkumar M. Patel, Dhruvesh P. Patel, and Ghanshyam Vadodaria. "HEC-HMS based mathematical model for Sabarmati and Sahi river basin and land cover analysis using Q-GIS." Journal of Information and Optimization Sciences 46, no. 2 (2025): 317–28. https://doi.org/10.47974/jios-1916.

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Mathematical models are quite commonly used powerful tool in the hydrology for predicting and managing the water in various environments. Applications of rainfall runoff mathematical modeling highlights its unique contributions to different fields. In the present study hydrological rainfall runoff modelling has been performed for two major river basinsi.e. Sabarmati river basin and Mahi river basin.Standard frequency distribution methods Gumbel’s method and lognormal method has been deployed in IDF analysis. For this the mathematical HEC-HMS based model development and analysis has been extens

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Shah, Abhi, D. M. Maurya, and G. Archana. "Microbial diversity assessment within continuous subsurface sediment core of estuarine region of Mahi river basin, Western India." Canadian Journal of Biotechnology 1, Special Issue (2017): 118. http://dx.doi.org/10.24870/cjb.2017-a104.

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Sharma, Aditya, Devesh Sharma, and S. K. Panda. "Assessment of spatiotemporal trend of precipitation indices and meteorological drought characteristics in the Mahi River basin, India." Journal of Hydrology 605 (February 2022): 127314. http://dx.doi.org/10.1016/j.jhydrol.2021.127314.

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Das, Sofia P., Subrat K. Swain, Lakshman Sahoo, Joy Krushna Jena, and Paramananda Das. "Single Genetic Stock Revealed by Microsatellite Markers Among Wild Populations of Cirrhinus mrigala from Peninsular India." Turkish Journal of Fisheries and Aquatic Sciences 21, no. 09 (2021): 425–33. http://dx.doi.org/10.4194/1303-2712-v21_9_01.

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Cirrhinus mrigala (mrigal) is one of the Indian major carps widely cultured in the whole Indian subcontinent. Population genetic structure of this species from Peninsular Rivers of India is lacking. Among DNA markers, microsatellites are excellent tools to evaluate genetic variation of populations. In this study, genetic variation of six peninsular riverine mrigal populations was evaluated using seventeen microsatellite loci. In analyzing 288 samples, the number of alleles ranged from 4 to 27; observed heterozygosity from 0.595 to 1.00, expected heterozygosity from 0.586 to 0.959 and inbreedin

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Patel, Krunal, Rajmal Jain, Ajay N. Patel, and Manik H. Kalubarme. "Shoreline change monitoring for coastal zone management using multi-temporal Landsat data in Mahi River estuary, Gujarat State." Applied Geomatics 13, no. 3 (2021): 333–47. http://dx.doi.org/10.1007/s12518-021-00353-8.

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Khadkikar, A. S., L. S. Chamyal, J. N. Malik, D. M. Maurya, and S. S. Merh. "Arid-Humid Cycles in Mainland Gujarat over the Past 300 Ka: Evidence from the Mahi River Basin, India." Journal Geological Society of India 47, no. 3 (1996): 383–88. http://dx.doi.org/10.17491/jgsi/1996/470311.

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34

Gatti, Emma. "Drough and flood in Holocenic Western India: a study on phytolith and paleosequences of the Mahi river, Gujarat." Quaternary International 279-280 (November 2012): 161. http://dx.doi.org/10.1016/j.quaint.2012.08.190.

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35

Parmar, Urvashiben, and Murari Lal Gaur. "Judging spatio-temporal variability of key river water quality vis-à-vis land use changes in Mahi Basin." Journal of Soil and Water Conservation 21, no. 4 (2022): 385–93. http://dx.doi.org/10.5958/2455-7145.2022.00049.2.

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Gaurav Singh, M.J. Kaledhonkar, A.K. Singh, et al. "Sapota (Achras zapota) based bio-engineering measures for slope stabilization and sustainable productive utilization in Mahi ravines, Gujarat." Indian Journal of Soil Conservation 53, no. 1 (2025): 36–43. https://doi.org/10.53550/ijsc.v53.i1.186.

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A long-term field experiment (2010-2022) was conducted on 14% sloped ravine lands along the Mahi River in Gujarat to evaluate agroforestry systems integrated with bio-engineering techniques for runoff conservation, soil loss reduction, and productivity enhancement. Five treatments were tested on 72 × 24 m plots: (i) cowpea + castor on bench terraces (CCBT), (ii) sapota + cowpea + castor on bench terraces (SCCBT), (iii) sapota on bench terraces (SBT), (iv) sapota with staggered trenches on slope (SSTS) and (v) sapota on untreated slope (SS - control). Bench terraces were subdivided to reduce sl

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Shah, Abhi P., Shazi Farooqui, D. M. Maurya, Anupam Sharma, and G. Archana. "Linkage of Microbial Parameters with Sediment Physicochemical Properties in Subsurface Fluvial Sediment Deposits of the Mahi River Basin, Western India." Indian Journal of Microbiology 62, no. 2 (2022): 257–65. http://dx.doi.org/10.1007/s12088-021-00998-4.

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38

Farooqui, Shazi, Abhi P. Shah, D. M. Maurya, G. Archna, S. Nawaz Ali, and Anupam Sharma. "Texture, mineralogy and geochemistry of late Quaternary sediments of the Mahi River basin, western India: Implications to climate and tectonics." Applied Geochemistry 134 (November 2021): 105088. http://dx.doi.org/10.1016/j.apgeochem.2021.105088.

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Sridhar, Alpa, L. S. Chamyal, Falguni Bhattacharjee, and A. K. Singhvi. "Early Holocene fluvial activity from the sedimentology and palaeohydrology of gravel terrace in the semi arid Mahi River Basin, India." Journal of Asian Earth Sciences 66 (April 2013): 240–48. http://dx.doi.org/10.1016/j.jseaes.2013.01.017.

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40

Ramakrishnan, D., A. Bandyopadhyay, and K. N. Kusuma. "SCS-CN and GIS-based approach for identifying potential water harvesting sites in the Kali Watershed, Mahi River Basin, India." Journal of Earth System Science 118, no. 4 (2009): 355–68. http://dx.doi.org/10.1007/s12040-009-0034-5.

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Pokar, Krunal, Vasantkumar Rabari, Rishiraj Duggal, et al. "The estuarine plastics menace: Insights into prevalence, characterization and polymeric risk assessment of microplastics in the Mahi River Estuary, Gujarat, India." Marine Pollution Bulletin 208 (November 2024): 116936. http://dx.doi.org/10.1016/j.marpolbul.2024.116936.

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42

Gupta, Ronak, Ketan Tatu, Lamb Christian, and R.D. Kamboj. "ASSESSMENT OF WATER QUALITY PARAMETERS FOR ESTUARINE AND RIVERINE ZONES OF MAHI RIVER, GUJARAT DURING PRE-MONSOON AND POST-MONSOON SEASON." INTERNATIONAL JOURNAL OF HIGHER EDUCATION AND RESEARCH 9, no. 1 (2019): 193–213. https://doi.org/10.5281/zenodo.14363771.

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AnvariFar, Hossein, Alireza Khyabani, Hamid Farahmand, Saber Vatandoust, Hassan AnvariFar, and Shrinivas Jahageerdar. "Detection of morphometric differentiation between isolated up- and downstream populations of Siah Mahi (Capoeta capoeta gracilis) (Pisces: Cyprinidae) in the Tajan River (Iran)." Hydrobiologia 673, no. 1 (2011): 41–52. http://dx.doi.org/10.1007/s10750-011-0748-7.

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Subrahmany, Gangavarapu, G. Archana, and L. S. Chamyal. "Soil Microbial Activity and its Relation to Soil Indigenous Properties in Semi-arid Alluvial and Estuarine Soils of Mahi River Basin, Western India." International Journal of Soil Science 6, no. 4 (2011): 224–37. http://dx.doi.org/10.3923/ijss.2011.224.237.

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Vachhrajani, Kauresh, and Pranav Pandya. "Spatial Distribution and Substratum Preference of the Brachyuran Crab, Macrophthalmus Depressus (Decapoda, Ocypodidae) along the Lower Estuarine Mudflat of Mahi River, Gujarat, India." Crustaceana 83, no. 9 (2010): 1055–67. http://dx.doi.org/10.1163/001121610x521235.

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Solanki, Reshma, Kartik Upadhyay, and Raju Vyas. "Accidental stranding, rescue and release of Indo-Pacific Humpback Dolphin (Sousa chinensis) from a natural pool of the Mahi River, Vadodara District, Gujarat, India." Journal of the Marine Biological Association of India 60, no. 1 (2018): 97–101. http://dx.doi.org/10.6024/jmbai.2018.60.1.2009-15.

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Samaee, S. M., R. A. Patzner, and N. Mansour. "Morphological differentiation within the population of Siah Mahi,Capoeta capoeta gracilis, (Cyprinidae, Teleostei) in a river of the south Caspian Sea basin: a pilot study." Journal of Applied Ichthyology 25, no. 5 (2009): 583–90. http://dx.doi.org/10.1111/j.1439-0426.2009.01256.x.

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Sharma, Aditya, Devesh Sharma, S． K. Panda, and Anish Kumar. "Sensitivity analysis of different parameterization schemes of the Weather Research and Forecasting (WRF) model to simulate heavy rainfall events over the Mahi River Basin, India." Agricultural and Forest Meteorology 346 (March 2024): 109885. http://dx.doi.org/10.1016/j.agrformet.2023.109885.

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Akpo, M. A., A. Saidou, I. Balogoun, I. Yabi, and L. B. Bio Bigou. "Evaluation De La Performance Des Pratiques De Gestion De La Fertilite Des Sols Dans Le Bassin De La Riviere Okpara Au Benin." European Scientific Journal, ESJ 12, no. 33 (2016): 370. http://dx.doi.org/10.19044/esj.2016.v12n33p370.

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Abstract:

A good management of agricultural land based on scientific knowledge and farmer indigenuous knowledge is necessary to ensure sustainable agricultural production. Our research aims to evaluate the performance of farmers' strategies and improved soil fertility management practices in improving level of crop yields in the basin of the Okpara River in Benin. Surveys using semi-structured questionnaire were conducted from October 11 to November 30, 2015 on a sample of 1048 farmers belonging to socio-cultural groups Tchabè, Mahi, Ditamari, Lokpa, Bariba and Fulani. Informations collected concerned f

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Srivastava, P. K., S. Mukherjee, M. Gupta, and S. K. Singh. "Characterizing Monsoonal Variation on Water Quality Index of River Mahi in India Using Geographical Information System. Water Quality Exposure and Health, 2(3–4):193–203 (2011)." Water Quality, Exposure and Health 4, no. 1 (2012): 23–24. http://dx.doi.org/10.1007/s12403-012-0062-2.

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