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Relevant bibliographies by topics / Benue River

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Journal articles

Academic literature on the topic 'Benue River'

Author: Grafiati

Published: 4 June 2021

Last updated: 1 February 2022

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Journal articles on the topic "Benue River"

1

Odunuga, S., O. Adegun, S. A. Raji, and S. Udofia. "Changes in flood risk in Lower Niger–Benue catchments." Proceedings of the International Association of Hydrological Sciences 370 (June 11, 2015): 97–102. http://dx.doi.org/10.5194/piahs-370-97-2015.

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Abstract. Floods are devastating natural disasters with a significant impact on human life and the surrounding environment. This paper analyses historical and recent flood (2012 extreme) peak flow at strategic locations, land use activities and Floodplain Vulnerability Index analyses of the Niger–Benue River Floodplain. The 2012 peak flow at Jederbode on the Niger River was about 50% above the long term average. At Jebba (Niger), the 2012 peak flow of 1567 m3 s−1 was also far higher than the long term mean annual peak flow of 1159 m3 s−1. The 2012 peak flow at Lokoja was also about 50 % above

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2

Babagana, Saleh Mustapha, and Satendra Sharma. "GEOPHYSICAL CHARACTERIZATION OF AQUIFER SYSTEMS USING VERTICAL ELECTRICAL SOUNDING METHOD IN DEMSA, NORTHEAST NIGERIA." International Journal of Research -GRANTHAALAYAH 8, no. 11 (2020): 175–84. http://dx.doi.org/10.29121/granthaalayah.v8.i11.2020.2379.

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Electrical resistivity method using vertical electrical sounding (VES) technique and Schlumberger array was employed with the aim of delineating limits and types of aquifer system(s), and stratigraphic composition of the Demsa area, a confluence of Benue River in Northeast Nigeria. The result revealed that the hydrogeology of the area may be controlled by fractures (secondary porosity) developed in sedimentary units. Two aquifers, namely the upper alluvial aquifer and the confined deeper aquifer systems exist in the study area. The two aquifers occur at depths of 20.5 – 41 m, and 43.8 – 78.9 m

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3

Ibrahim, Ezekiel Gube, Nathaniel Yakubu, and Eneji Ishaq. "Determination of Heavy Metals from River Benue around the Makurdi Metropolis." International Journal of Trend in Scientific Research and Development Volume-1, Issue-5 (2017): 917–221. http://dx.doi.org/10.31142/ijtsrd2357.

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4

Pandey, R., and G. Amarnath. "The potential of satellite radar altimetry in flood forecasting: concept and implementation for the Niger-Benue river basin." Proceedings of the International Association of Hydrological Sciences 370 (June 11, 2015): 223–27. http://dx.doi.org/10.5194/piahs-370-223-2015.

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Abstract. Flood forecasting in the downstream part of any hydrological basin is extremely difficult due to the lack of basin-wide hydrological information in near real-time and the absence of a data-sharing treaty among the transboundary nations. The accuracy of forecasts emerging from a hydrological model could be compromised without prior knowledge of the day-to-day flow regulation at different locations upstream of the Niger and Benue rivers. Only satellite altimeter monitoring allows us to identify the actual river levels upstream that reflect the human intervention at that location. This

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5

Faraclas, Demuth. "Cross River as a model for the evolution of Benue-Congo nominal class concord systems." Studies in African Linguistics 17, no. 1 (1986): 40–54. http://dx.doi.org/10.32473/sal.v17i1.107495.

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Cross River languages exhibit nominal class/concord systems which typify almost every possible stage of simplification of the proto-Benue-Congo system, from full retention in some Upper Cross and Bendi languages to near complete elimination in the Ogoni group. The synchronic facts from Cross River shed light on some of the psycholinguistic processes involved in class/concord systems acquisition and retention as well as some of the sociolinguistic processes involved in the modification or loss of such systems. Taken together, the nominal class/concord systems of the Cross River languages corres

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6

., Otache, Y. Martins, I. E. Ahaneku, and M. A. Sadeeq. "Parametric Linear Stochastic Modelling of Benue River flow Process." Open Journal of Marine Science 01, no. 03 (2011): 73–81. http://dx.doi.org/10.4236/ojms.2011.13008.

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7

Wright, David K., Scott MacEachern, Jungyu Choi, Jeong-Heon Choi, Carol Lang, and Jean-Marie Datouang Djoussou. "Iron Age Landscapes of the Benue River Valley, Cameroon." Journal of Field Archaeology 42, no. 5 (2017): 394–407. http://dx.doi.org/10.1080/00934690.2017.1358017.

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8

Berns, Marla C., and Richard Fardon. "Central Nigeria Unmasked: Arts of the Benue River Valley." African Arts 44, no. 3 (2011): 16–37. http://dx.doi.org/10.1162/afar.2011.44.3.16.

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9

Nwauwa, A. O. "Integrating Arochukwu into the Regional Chronological Structure." History in Africa 18 (1991): 297–310. http://dx.doi.org/10.2307/3172068.

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The Niger-Benue Valley regional chronology is expanding. This is satisfying. Dates from the early city states and chiefdoms in the lower Cross river valley have been suggested and integrated into the larger regional chronological structure. Arochukwu was one such chiefdom. Utilizing the available genealogies from within Arochukwu and its satellite settlements, and guided by the existing methodology of chronology, I have calculated what I believe to be fairly reliable dates which locate the foundation of the chiefdom, ca. 1690/1720. These dates have been interrelated with the importation of the

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10

Adeleye, Adeniyi Olarewaju, Amoo Afeez Oladeji, Bate Garba Barde, Sadiq Ismaila Shina, and Ugba Samuel. "Physicochemical and bacteriological assessment of ricemill wastewater discharged into river Benue, Nigeria." Biological Environment and Pollution 1, no. 1 (2021): 1–10. http://dx.doi.org/10.31763/bioenvipo.v1i1.381.

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Rapid industrialization affects the environment in different ways through indiscriminate disposal of large amount of wastewater into the surrounding water bodies thereby causing serious problems to the environment. This study was conducted to assess the suitability of the ricemill wastewater being discharged into River Benue. Wastewater was sampled from point of discharge (sampling point A) and 20 meters away from the final entry into river Benue (sampling point B). Standardized methods were employed to analyze biochemical oxygen demand (BOD), chemical oxygen demand (COD), total dissolved soli

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