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Amalu Titus Oko Ugwu Igwe Izuchukwu Ehugbo Uchenna Okeh Benedette Duluora Emmanuel 《GeoJournal》2021,86(4):1691-1703
GeoJournal - The tourism industry has been touted to have huge significant impact on the social and economic growth of local people across the world. This study is carried out to examine the role... 相似文献
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The quest for improved water supply to cater for the ever increasing population has given rise to the assessment of water quality and resource potentials in Aba-Urban and its environments. The area, which lies within the Niger Delta Basin is underlain by the Benin Formation that is highly aquiferous. Samples of sands and water were subjected to sedimentological and hydrochemical analysis, respectively. Result reveals that the aquifer is thick (over 100 m) and unconfined. The computed aquifer parameters indicate high yielding clean-sands with hydraulic conductivity values ranging from 1.13 × 10–4 to 5.70 × 10–3 m/s. The specific discharge is about 14.2 m/year while the average linear groundwater velocity is calculated to be 53.46 m/year. Hydrochemical investigations carried out on water samples from Aba River and the groundwater system revealed low dissolved geochemical constituents. Although, there is a slight increase from the north to the southern part along the flow path. In general, the groundwater is relatively enriched in Ca, Mg?HCO-3ions and is predominantly of bicarbonate constituents. However, in some places Cl? ions dominate over HCO-3ions. This is common where the water has come in contact with domestic sewage. This kind of contamination is also accompanied by elevated concentration of NO-3ions. Generally, the groundwater in most cases meets the standard for human consumption and is a better alternative to surface water. Consequently an increase exploitation of the prolific Benin aquifer through more hygienic and safe methods will surely be the best way of improving the domestic water supply situation in Aba City. 相似文献
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Oluwasinaayomi Faith Kasim Olayide Josiah Omirin Daniel Izuchukwu Okoro 《GeoJournal》2018,83(1):137-151
Cohabitation, as a form of sexual relationship, is becoming popular among tertiary students in developing countries. This is largely due to emergence of sexual liberalization that projects premarital sex as acceptable societal norm. The paper analyses the spatial pattern of cohabitation in communities abutting tertiary institutions in Ibadan, Nigeria. Snowball sampling technique was used to identify cohabiters at Agbowo and Apete and the Coordinates of their residence were taken using Global Positioning System. Nearest Neighbour Analysis (NNA) was adopted for spatial analysis. Spatial pattern of cohabitation at Agbowo (NNA value 1.072615) shows a random pattern. The pattern at Apete (NNA value 0.802374) displays a cluster pattern. Finding identifies, ownership, use and types of building; inadequate on-campus accommodation; peer pressure and poverty as cohabitation causal factors influencing the observed spatial patterns. Therefore, parents and guardians should adopt high-investment strategy in safeguarding the welfare and wellbeing of their wards. 相似文献
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Stratigraphic and structural interpretative studies have been carried out within the paralic sequence of Agbada Formation in the Niger Delta Basin. The method of study involved integrating sequence stratigraphic techniques with well logs, biostratigraphy, and 3D regional seismic data obtained from several producing fields in the Coastal Swamp depobelt of the onshore Niger Delta Basin. This was targeted at establishing regional sequence stratigraphic and structural framework from well log correlation and seismic mapping so as to better define hydrocarbon leads. Well log correlation using stratigraphic bounding surfaces such as maximum flooding surfaces (MFSs) and sequence boundaries (SBs) indicates that the stratigraphic package was deposited within the Middle to Late Miocene (8.5 to 12.1 Ma) age. Recognized depositional sequences revealed differential thickening and thinning of the associated system tracts (lowstand system tract (LST), transgressive system tract (TST), and highstand system tract) (HST)). This observed stratal behavior has been attributed to the influence of syndepositional tectonic structures that characterize the Coastal Swamp depobelt, which lies within the extensional zone. Flattening of MFSs at various ages indicates observable basinward shift of the depositional center. The genetic units of LST and HST serve as good hydrocarbon reservoir whereas HST and TST constitutes mainly the source and seal packages rocks in the area. Structural interpretation revealed the occurrence of simple/faulted rollover anticline, collapsed crest, regional hanging wall and footwall, horst block, and subdetachment fault structural styles that constitute the key hydrocarbon entrapment mechanisms. Structural top maps show fault-dependent closures which dominate the extensional zone, which could form possible hydrocarbon leads and prospects that should be targeted during exploration studies for development. 相似文献
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