Premium
Solute concentrations in the lower niger river and the source rock contribution
Author(s) -
Martins O.
Publication year - 1988
Publication title -
hydrological processes
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.222
H-Index - 161
eISSN - 1099-1085
pISSN - 0885-6087
DOI - 10.1002/hyp.3360020103
Subject(s) - tributary , total dissolved solids , albite , rainwater harvesting , chloride , weathering , environmental chemistry , water quality , hydrology (agriculture) , feldspar , biotite , geology , environmental science , mineralogy , chemistry , geochemistry , environmental engineering , paleontology , ecology , quartz , cartography , geotechnical engineering , organic chemistry , biology , geography
Abstract Water quality analyses for the Niger River for the 1980/81 hydrological year are presented. The samples were collected from the main river at Lokoja, and from two main tributaries, the Kaduna and the Benue Rivers. Different water types were distinguished by the concentrations of major ions. The type Ca > Na > Mg > K ‐ HCO 3 > SO 4 > Cl was represented at all stations during at least part of the year. Chloride was found to dominate the sulphate ion in the Kaduna and Niger, while the Benue maintained a higher concentration of sulphate relative to chloride all year round. Distinct patterns of seasonal variation in the ion concentrations were observed, particularly for the samples collected at Lokoja. Low ion concentrations were prominent during periods of high discharge, while low flow periods coincided with high dissolved ion concentrations. The contribution of rainwater to the total dissolved solids in the river waters was assessed indirectly using rainwater chemistry data from the Gulf of Guinea. The estimated rainwater contribution to the Lower Niger amounts to 5.15 mg 1 −1 . Geochemical weathering calculations involving reactions of the four major minerals of granitic rocks ‐ anorthite, biotite, albite, and K‐feldspar ‐ with carbon dioxide and water, can account for the average water composition of the Lower Niger. The proportion of the ionic components was also related to the occurrence of the respective element in the minerals.