AKPEN STATE BENUE - AN OVERVIEW

Akpen state Benue - An Overview

Akpen state Benue - An Overview

Blog Article



In a great number of hydrologic challenges, involving a well or pumping district in close proximity to or in which drinking water‐stages are slipping, the current principle is for that reason not strictly applicable. This paper investigates partly the nature and outcomes of the mathematical idea that considers the movement of floor‐water before equilibrium is achieved and, for a consequence, includes time like a variable.

Within this review the annual rainfall details of forty yrs (1978-2017) for South-South, Nigeria was collected from the archive of NiMet. A few procedures were used for the analysis; statistical differences among two the equivalent-size time scales, coefficient of variability along with the anomaly strategy. The craze analysis working with t-exam, Sen's estimator slope and Mann Kendall were also performed if you want to find out the craze within the rainfall variables. The outcome present that the variances amongst The 2 implies of the equivalent-duration time scales exposed variability of 7.00mm. Similarly, the CV of rainfall was 0.

The approach Within this study was manufactured to the background that though there are numerous components that account for flooding, rainfall attribute or designs keep on being the main driver of flooding while in the tropics. Therefore, rainfall development Assessment was carried out within the Makurdi drainage basin making use of rainfall information from 1980 to 2014 to determine the flood bearing potentials from the rainfall. Evaluation of variance (ANOVA), 3 yr going signify, basic linear regression, rainfall anomaly index and Pearson Second correlation ended up utilized for the Examination. The regression line equation (y= three.414 + 1105), displays that Makurdi drainage basin has had rise in rainfall. The end result through the rainfall anomaly index demonstrates that Makurdi drainage basin was characterised by larger extent of very moist circumstances in 1984, 1998 and 1999.



Paul's as well as the Romanche oceanic change faults. Some twenty m.y. of renovate fault motion could have elapsed prior to West Africa was entirely divided by oceanic crust from northern Brazil. The South Atlantic, Benue trough, as well as the Gulf of Guinea shaped an unstable RRF triple junction, which can have brought on internal strain while in the African plate. It may well also have resulted in possible dilation of your Gulf of Guinea remodel faults which, along with the quick intervening ridge segments, served to localize the Cretaceous volcanicity thought to be to blame for the not too long ago identified North Brazilian Ridge.

Geoelectric survey using Vertical Electrical Sounding (VES) was performed in elements of Ikot Abasi Community Authorities Akpen state Benue Area, Akwa Ibom state, Nigeria. Within this area there isn't a borehole which has been drilled till now, the key targets of this research should be to certainly be a tutorial for the suitable placement of borehole in order to avoid wild cat drilling and also in order to avoid salt intrusions utilizing the VES ... [Present comprehensive summary] geophysical approaches. Schlumberger electrode configuration was used in obtaining the information. Four to 5 geoelectric levels were delineated from the interpreted results.

Determinations of these two constants are almost always associated with quantitative scientific tests of floor‐h2o troubles.

Everyday rainfall facts of 31 decades was employed for the examine. The daily rainfall knowledge was subjected to quite a few analyses. The result attained indicated that there's a downward pattern while in the rainfall amount of money gained in Abuja during the last 31 several years. Also, a gradual decadal drop in rainfall was observed using the SPI to check the 3 decades below assessment.

NIJOTECH enables open up obtain for distribution on the released article content in almost any media As long as total (not portion) of content articles are dispersed.



Any time a very well is pumped or in any other case discharged, water‐levels in its neighborhood are reduced. Until this lowering happens instantaneously it represents a lack of storage, either through the un‐watering of the part of the previously saturated sediments if the aquifer is nonartesian or by launch of saved drinking water from the compaction of your aquifer due to the lowered tension When the aquifer is artesian. The mathematical concept of ground‐water hydraulics has become centered, seemingly completely, over a postulate that equilibrium has been attained and thus that water‐amounts are not slipping.

static water degree and aquifer depth have been manufactured to point out these parameter variations during the review region.

This analyze analyses Makurdi rainfall facts from 1955 to 2015, for the objective of detecting the rainfall variability, trends, and examining its implications on flood incidence. Facts on daily rainfall and flood occurrences ended up gathered from appropriate authorities companies. Rainfall traits were analyzed working with Mann–Kendall, Spearman’s rank correlation and Student’s t assessments, both of those giving Virtually identical results for the three procedures. Rainfall variability was analyzed utilizing standardized precipitation index (SPI).

Provision of submit design support (PCS) expert services to state water authorities in Nigeria: constraints and the way in which ahead

In this research, We now have coupled surface area geophysical strategy with pumping check success to deliver a cost effective and productive choice in aquifer parameter estimation. Vertical Electrical Sounding (VES) was completed at forty web-sites in the study location with the identification of the vertical variation in subsurface lithology and for the characterization of your aquifer process in the research location. The interpretation on the VES knowledge discovered three to five geoelectric units with the depth to aquifer varying from 7 to 108m and the resistivity from the saturated layer varying between 42.



Report this page