MARIKI CHE 312
Page 1: Introduction to Groundwater Quality Issues
Importance of Water Sources
Human civilization and development rely on the availability of quality water.
Main sources of this water include surface water (lakes, rivers, dams) and groundwater.
Groundwater is essential for drinking, irrigation, and industrial use, particularly in arid and semi-arid regions.
Groundwater Contamination
The quality of groundwater is influenced by human and natural activities along water flow paths.
Contamination sources include:
Solid waste and wastewater disposal.
Inadequate water supply infrastructure in developing countries, leading to reliance on groundwater due to perceived purity.
Groundwater quality can be negatively impacted by both anthropogenic and natural factors.
Natural Contaminants
Soils and rocks contribute composite elements and compounds to groundwater.
Interaction between water and soil/rocks can introduce toxic metals and other contaminants.
Anthropogenic Contaminants
Activities such as industrial, domestic, and agricultural can introduce nutrients, heavy metals, and organic pollutants into groundwater.
Use of agrochemicals can further exacerbate contamination levels; for example, phosphorus fertilizers may contain heavy metals like Cd and As.
Health Risks Associated with Contaminated Groundwater
Elevated levels of heavy metals pose significant health risks, even at low concentrations, affecting essential biological functions.
Toxic metals in water can affect human, plant, and animal health through direct ingestion or secondary routes (like irrigation).
High concentrations of metals like Al, Cd, As, Pb, and others have been reported in recent studies, indicating severe pollution risks and necessitating investigation.
Page 2: Study Area Overview and Objectives
Study Area Description
Research conducted along the slopes of Mount Meru in Tanzania, specifically in Akeri, Kikwe Wards, and Usa River Township.
Geographic coordinates: Latitude 3°00.00 - 3°40.00 S, Longitude 36°00.00 - 37°.55.00' E.
Ecosystem features:
Various water sources including rivers, springs, and groundwater.
Rainfall ranges from 500 mm to over 1200 mm per year, which sustains these water systems.
The district is divided into three zones based on altitude and climate:
Highland/Upper Zone: 1440m to 1800m above sea level, 1000mm+ rainfall, agricultural focus on coffee, banana, and Irish potatoes.
Middle Zone: 1000m to 1350m, 500 to 1000mm rainfall, agriculture and livestock.
Lower Zone: 800m to 1000m, rainfall 300 to 500mm, reliant on irrigation for crops like rice and maize.
Objective of the Study
Evaluate levels of heavy metals (Al, As, Cd, Cu, Fe, Mn, Pb) in groundwater near populated areas on Mount Meru slopes to determine water quality and contamination patterns.
Aim to establish a better understanding of groundwater health risks due to potential toxic metal exposure.
Page 3: Methodology
Data Collection Techniques
Reconnaissance Survey:
Identification and mapping of groundwater sources (boreholes, springs, shallow wells) between January and February 2013.
Data collected included depth and water levels.
Sample Collection and Analysis:
50 groundwater samples collected weekly during dry (August - October 2013) and wet (March-April 2014) seasons.
Collection techniques varied based on water source, ensuring fresh samples were analyzed duly treated for contaminants.
Analytical Procedures
Water samples analyzed for heavy metal content using Inductively Coupled Plasma Optical Emission Spectrophotometer (ICP-OES) methods.
On-site measurements for pH, temperature, electrical conductivity, etc., followed standard protocol using appropriate analytical instruments.
Page 4: Groundwater Quality Variation
Concentration Variation of Metals
Groundwater quality was found to vary based on sampling points, water source types, and seasonal changes.
Aluminum (Al):
Concentrations highest in spring water compared to boreholes and shallow wells.
Dry season ranged between 0.04-3.72 mg/l and wet season below detection to 3.14 mg/l.
Borehole Water:
Lowest Al concentrations compared to other sources, with a range of 0.07-0.34 mg/l (dry) and 0.02-0.66 mg/l (wet).
Shallow Wells:
Higher than boreholes but lower than springs; dry season: 0.05-1.28 mg/l; wet season: 0.04-0.71 mg/l.
Significant Findings
Concentrations of Al exceeded WHO drinking water recommendations, suggesting a health hazard in certain samples.
ANOVA revealed significant differences in Al concentrations among different sources with noteworthy higher levels in wet season spring samples.
Page 5: Summary of Toxic Metals Analysis
Sample Results Overview
Copper (Cu):
Highest in boreholes (mean of 0.02 mg/l) during the dry season, below detection in wet season across sources, variance dependent on rainfall.
Iron (Fe):
Notable concentrations in springs compared to other sources, variability across dry and wet seasons.
Significant p-values in ANOVA indicate noteworthy seasonal variations of Fe concentrations.
Manganese (Mn):
Variations observed are minimal across sources and seasons, but significant enough to merit attention following WHO guidelines.
Arsenic (As) and Lead (Pb):
Noted significantly high levels in various wells during the dry season, especially dangerous due to potential sources like agricultural runoff.
Seasonal measurements showed lower levels during the wet season, indicating rainwater's dilution effect.