Previous Page  11 / 13 Next Page
Information
Show Menu
Previous Page 11 / 13 Next Page
Page Background

Page 69

conferenceseries

.com

Volume 7

Journal of Geology & Geophysics

ISSN: 2381-8719

Soil Science 2018

October 22-23, 2018

October 22-23, 2018 | Berlin, Germany

2

nd

Annual Congress on

Soil and Water Sciences

Preliminary investigation into groundwater suitability for domestic use in the Matoks catchment,

Limpopo Province, South Africa

Lawrence Diko Makia

University of Venda, RSA

Statement of the Problem:

The Matoks area, comprising Mphakane, Dikgading, Sekonye, Springs, Mamotshana, Makgato

and Sekalegolo villages, under the jurisdiction of the Molemole Local Municipality have been collectively described as a water

scarce community. To address current and future water demands of these communities, there is a dire need to evaluate the

groundwater resource potentials in the area.

Methodology & Theoretical Orientation:

In this study, groundwater physico-chemical parameters (pH, conductivity, TDS,

alkalinity and hardness) and chemical constituents (HCO3, NO3, NH4, Cl, F, Mg, Ca, Na, and K) from 11 boreholes drilled

within crystalline aquifers in the area were analysed. Hill-Piper and the simplified Durov diagrams were used to appraise

chemical characteristics of groundwater.

Findings:

Results for the physico-chemical parameters ranged as follows; pH (6.8-8.81), conductivity (67.8-413.2 mS/cm),

TDS (439.4-2685.8 mg/L), alkalinity (176-410 mg/L as HCO3), and total hardness (81.15-630.84 mg/L as CaCO3), with

concentration of major ions in the order; CO3>NO3>Cl>F>NH4 and Ca>Na>Mg> K. Groundwater was classified into four

hydrogeochemical facies: Ca2+- Mg2+- HCO3 – (Type I); Na+- K+ - Ca2+- HCO3– (Type II); Na+- K+- Cl- - SO42- (Type

III) and Ca2+ - Mg2+-Cl-- SO42- (Type IV). About 36.4% of the samples trend towards Type III (saline) whereas 63.6% tend

towards Type II (alkaline).

Conclusion & Significance:

The results suggests significant mixing of the water types, primarily through ion exchange

reactions. Based on World Health Organization and the South African standards, water quality from 7 of the 11 boreholes was

classified as good, 3 poor and one unacceptable for domestic use. Several recommendations are advanced to mitigate adverse

health risk as well as improve water quality.

dikom73@gmail.com

J Geol Geophys 2018, Volume 7

DOI: 10.4172/2381-8719-C2-021