Hydraulic characteristics of the Maastrichtian sedimentary rocks of the southeastern Bida Basin, central Nigeria

A set of outcrop samples from the Lokoja and Patti Formations of the southe rn Bida Basin (Nigeria) was examined for grain size distribution, sedimenta ry and hydraulic characteristics. Most of the samples are well-sorted with an uniformity coefficient (U) ranging between 1.3 and 6.3. The mean effecti ve grain diameter (d(10)) is in the order of 0.11 mm, the mean value of d(9 0) was determined as 0.66 mm (both geometric mean) and the median grain siz e (d(50)) as 0.23 mm. Based on these values, the sedimentary sequence can b e described as 'fine to medium sized sand', having minor amounts of either silt, or coarse sand and some gravel. The total porosity of the samples was determined by laboratory methods to be in the range of 9-29%. The hydrauli c conductivity (K) was determined according to Hazen and Beyer, and by Shep herd's formula, the last resulting in a geometric mean of 3.3 m d(-1) or 3. 3 darcy. The results are used to estimate local groundwater potential. The entire pore space (potential groundwater reservoir) for the area under stud y is estimated to be in the order of 290-430 km(3). Because of higher hydra ulic conductivities, it is recommended that the Lokoja Formation is concent rated on as a target for groundwater exploration. (C) 2000 Elsevier Science Limited. All rights reserved.