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š¼šØšØššØšØš¢šš£š© š¤š š©šš šš§š¤š©ššš©šš«š š¾šš„šššš©š® š¤š šššš¤šÆš šš¤š£š š¤š«šš§ š¼š¦šŖšššš§ šš®šØš©šš¢šØ ššØšš£š šššš¤š£ššš§š® ššš¤šš”ššš©š§šššš” ššš§šš¢šš©šš§šØ: š¼ š¾ššØš šš©šŖšš® šš ššš”š©šŖš£šš¤ š¼š§šš šš¤š§š©š šššØš©, ššššš§šš
DOI: https://doi.org/10.30564/jees.v2i2.1633
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An assessment of the protective capacity of the vadose zone overlying the aquifer systems in the Kaltungo area was carried out to determine its influence on groundwater quality. Applying the schlumberger array with a maximum electrode spread AB/2 = 100m through VES, thirty water well points were surveyed using Omega terrameter (PIOSO1) resistivity meter. The field data was first subjected to manual interpretation through curve marching and then digitized modeled curves using computer software. The interpreted data revealed that the area is characterized by eleven different curve types representing three to five geo electrical layers. In order to assess the protective capacity of the vadoze zone over the aquifer systems, the longitudinal conductance (S) and transverse resistance (T) (secondary geoelectric parameters) were computed from the primary data using the Dar Zarouk formula. The values of S obtained range from 0.0018 to 0.4056 ohms with a mean value of 0.0135 ohms while the values of T range from 0.55 ohms to 1195.68 ohms with a mean value of 39.84 ohms. The values of S and T obtained reveal that 90% of probed points has poor protective capacity, 10 % has moderate protective capacity and 83 % has high transmissivity, 17 % has intermediate transmissivity. The T and S values are skewed towards poorly protective capacity thus making groundwater in the area highly vulnerable to contamination from the surface. To achieve good groundwater quality in the area, proper completion of newly constructed wells should install protective casing through the entire vadose zone.
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šš¤š§š„šš¤š”š¤ššš šššØš„š¤š£šØš š¤š š ššš«šš§ š¾ššš£š£šš” š©š¤ ššš£š ššš£šš£š šš£ ššš«šš§ šš®šš, ššš©šŖš š¾š¤šŖš£š©š®, ššš£š®š
DOI: https://doi.org/10.30564/jees.v2i2.1935
Abstract
Over 40 billion tons of sand is mined worldwide every year which is estimated to be higher than the natural replacement rates. In Kenya, the rate of sand mining is raising concerns over its environmental effects since it is not regulated. This paper presents findings on the geomorphic effects of sand mining in the ephemeral River Tyaa channel in Kitui County. The study adopts the concept of feedback response mechanism of a natural geomorphic system. Through purposive sampling River Tyaa was selected for the study, where rampant sand mining was reportedly taking place. Random sampling on the five sand mining sites identified came up with a representative site namely Kanginga on which systematic sampling was applied while collecting data at both the active and control sites. Data on channel width, depth and slope angles was obtained through physical measurements while data on quantity of sand mined was obtained from Mwingi Sand Mining Cooperative. Multiple logistic regression analysis was used to analyse data whereby the model compared active and control sites. Test results indicated that sand mining had significantly increased river channel’s width (O.R. =1.531), depth (O.R. =1.527) and slope angles (O.R. =1.634) at active mining sites compared to control sites as deduced from the respective Odds Ratios. It concluded that sand mining had altered channel’s morphology resulting to adverse environmental effects such as loss of riparian vegetation and channel incision. It recommended curbing of illegal sand mining through licencing operators and reducing quantity of sand mined by closing some mines. Furthers, it recommended monitoring through regular Environmental Impact Assessment (E.I.A) and Audit (E.A) to inform protection of the river system from degrading.
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šš£šš”šŖšš£šš š¤š ššš¢š„šš§šš©šŖš§š šš£š ššš”šš©šš«š ššŖš¢šššš©š® š¤š£ š¼šš§ šš¤š”š”šŖš©šš¤š£ šš£ š¼ššššØ š¼šššš, šš©ššš¤š„šš
DOI: https://doi.org/10.30564/jees.v2i2.2286
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In this paper we access the effects of two atmospheric variables (temperature and relative humidity) on two important pollutants in the atmosphere (Nitrogen oxides (NOx) and carbon monoxide (CO)) by using one year (2016) data of Addis Ababa. Temperature has impact on atmospheric mixing and cause for the reduction of NOx as temperature increases. There are positive correlation between temperature and CO concentration from January to April with (R2 = 0.69), negative correlation from May to August with (R2 = 0.92) and no correlation for the remaining months. NOx and CO have moderate positive and negative correlation with relative humidity during the months January-April (R2 = 0.294 for NOx and R2 = 0291 for CO) and in the months May-August are R2 = 0.97 and R2 = 0.15 for NOx and CO respectively. But there are no clear correlation between the NOx and CO with relative humidity from September-December. NOx concentrations during wet season was almost about twice that of the dry season, but no such difference was observed in the case of CO. The seasonal average air temperature in wet season is relatively lower than dry season. NOx exhibited positive and CO negative seasonal correlations with relative humidity.
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ššš šš£š«šš§š¤š£š¢šš£š©šš” šš¢š„ššš© š¤š šš”ššØš©šš šššØš©š
DOI: https://doi.org/10.30564/jees.v2i2.2340
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ššŖšØš©ššš£šššš”šš©š® š¼šØšØššØšØš¢šš£š© š¤š š©šš šš§š¤šŖš£šš¬šš©šš§ ššŖšš”šš©š® šš£ š©šš ššš¤š®š§ššØš¤š”š š½š”š¤šš , š½šš§šššŖš¢ šæššØš©š§ššš©, šššØš© š½šš£ššš” š©š¤ š¼ššššš«š ššŖš§šš” ššš©šš§ ššššŖš§šš©š®
DOI: https://doi.org/10.30564/jees.v2i2.2479
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š¼ššššš«šš£š ššŖšØš©ššš£ššš”š ššØš šš£š ššš£šššš¢šš£š© š¤š ššš©šš§ šššØš¤šŖš§šššØ šš¤š§ šš§š§šššš©šš¤š£ šš£ ššššš§šš
DOI: https://doi.org/10.30564/jees.v2i2.2505Abstract
Water resource is available in Nigeria to meet water demand for domestic, agricultural and industrial use. If well enhanced and protected from various source of pollution. However, less information is available on suitability of water resources for irrigation use in Nigeria. This article reviews literature of the past with regards to influence of geogenic and anthropogenic activities on water resource for irrigation purpose in Nigeria and also to explain the current state of suitability of water resource for irrigation studies in Nigeria and gaps in studies. It also summarizes future ways on water resource management and preventive measure for water resource pollution for irrigation use. Related articles were downloaded from Google scholar in water-related issues. This paper tends to review previous article on water resource in Nigeria, and its suitability for irrigation. The primary aim of this paper is to produce a synoptic overview of the water resources in Nigeria and its suitability for irrigation use. From paper reviewed it was observed that 89 % of water resources was considered suitable for irrigation.
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ššš©ššš£š šš£š šš®šš§š¤ššš£ šš©š¤š§ššš šš£ ššš©šš” šš§ššš£šš šš§šš¢šš¬š¤š§š šØ: š¼ ššš£š ššš«ššš¬
DOI: https://doi.org/10.30564/jees.v2i2.2642Abstract
The need for a net zero carbon emission future is imperative for environmental sustainability hence, intensive carbon fuels would need to be replaced with less carbon emitting energy sources such as natural gas till clean energy source such as hydrogen becomes commercialized. As a result, this mini review discusses the use of metal organic framework (MOF) for adsorption of methane and hydrogen in specially designed tanks for improved performance so as to increase their applicability. Herein, adsorption (delivery) capacity of selected high performing MOFs for methane and hydrogen storage were highlighted in reference to the targets set by United States Department of Energy’s Advanced Research Projects Agency-Energy (ARPA-E) and Fuel Cells Technology Office. In this regard, specific design and chemistry of MOFs for improved methane and hydrogen adsorption were highlighted accordingly. In addition, an overview of computational and molecular studies of hypothetical MOFs was done - the various approaches used and their proficiency for construction of specific of crystalline structures and topologies were herewith discussed.
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