Isotope and geochemical characterization of surface and subsurface waters in the semi-arid Sokoto Basin, Nigeria

  • Adelana S
  • Olasehinde P
  • Vrbka P
N/ACitations
Citations of this article
30Readers
Mendeley users who have this article in their library.
Get full text

Abstract

Stable isotopes and geochemical studies have been applied in the investigation of groundwater resources in Sokoto Basin, northwestern Nigeria. Generally, the characteristic hydrochemical classification in the study area is calcium-alkali-bicarbonate. Surface waters are characterized by alkali-calcium-bicarbonate while groundwater is of Ca-Mg-HCO 3. The plot of δ 18 O versus δ 2 H shows that five isotopic groups can be distinguished. Group I-III is of groundwater origin while group IV and V represent surface water. A combination of the hydrochemical and isotope data (14 C, 13 C and 3 H) reveals the Sokoto basin aquifers generally contains good quality groundwater of Holocene age (100 to 10,000 years BP).

Cite

CITATION STYLE

APA

Adelana, S., Olasehinde, P., & Vrbka, P. (2004). Isotope and geochemical characterization of surface and subsurface waters in the semi-arid Sokoto Basin, Nigeria. African Journal of Science and Technology, 4(2). https://doi.org/10.4314/ajst.v4i2.15298

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free