Knowing The Microbiological and Chemical Quality Of Borehole Water! (Is All Groundwater Safe To Drink?)

Groundwater from non-polluted areas is generally safe for domestic purposes - to drink, prepare food, wash clothes, bath and water the garden. 


But how can we be sure that the chemical, microbiological and physical properties of water are acceptable for domestic users? In this article, we will look at the need to analyse groundwater samples to determine its quality.

Microbiological Quality: Micro-organisms are filtered out and die off as the water travels through the ground. Very often, because it travels slowly the water in a deep unconfined aquifer or a confined aquifer has been there for many years and is free of harmful organisms.

Shallow, unconfined aquifers are not much safer than surface water sources because the water has had very little filtration or storage time before it is collected for drinking. 

Campylobacter, Escherichia coli (E. coli), Cryptosporidium, Giardia and viruses have all been found in groundwater supplies. These microbes are carried into the aquifer from the surface. 

The vulnerability of aquifers to microbial contamination is increased by:

1. Shallow aquifer depth.
2. Microbial contamination in the surface water catchment.
3. Water flowing quickly through the aquifer via particularly porous material or fractured rock.
4. The absence of a confining layer. 

2.3 Chemical Quality: The chemical quality of groundwater is influenced by the quality of the water entering the aquifer as well as by the minerals in the ground. Minerals in the soil and rocks dissolve into the water as time passes. 

In limestone country, for example, the water can become very ‘hard’ as the lime dissolves. In some regions, arsenic is present in volcanic rocks and can be found in groundwater taken from particular aquifers.
Knowing The Microbiological and Chemical Quality Of Borehole Water! (Is All Groundwater Safe To Drink?)

Often, because a deep aquifer is devoid of oxygen, the form of the chemicals will change as they pass through it. As a result, it is common for groundwater to contain ammonia, sulphides and the soluble forms of many metals such as manganese and iron. These and other compounds can cause problems with the taste, smell or colour of the water. A number of common chemical contaminants that are a particular issue in groundwater are described in Table 1 below.

Common Contaminants in Groundwater:


1. Arsenic and Boron: Arsenic and boron often occur at potentially harmful levels in groundwater, particularly in geothermal and hydrothermal areas. The concentration of arsenic can vary significantly in shallower bores between summer and winter. 

2. Calcium and Magnesium: High calcium and magnesium concentrations can cause water to be ‘hard’, which can lead to problems of scale formation on hot surfaces and difficulty in getting soap to lather. This often happens in areas where limestone is part of the land formation. 

3. Fluoride: Fluoride has not been commonly found at levels that are of concern to health in New Zealand. However, if fluoride is being dosed, the concentration in the source water should be taken into account when deciding the dose rate. 

4. Iron and manganese: Iron in drinking-water in high enough concentrations can cause an unpleasant metallic taste and a rusty colour, which can stain fixtures and clothing. Manganese can also affect the taste of the water and has potential health effects when present in the water at higher levels. When oxidised, manganese can be deposited in pipes. It also causes staining of laundry. Iron and manganese are often found together in groundwater. The conditions that lead to the presence of iron and manganese can be localised and may change over time. 

High nitrate concentrations can occur in drinking-water sources due to contamination from farming, septic tank systems and solid waste disposal. A high nitrate concentration can be toxic to bottle-fed infants. 

5. Pesticides: In some boreholes, pesticides may be present. Testing should be undertaken if it is suspected that pesticides may be present, particularly in shallow unconfined aquifers. 

6. Radioactive Elements: Groundwater can contain naturally occurring radioactive elements, such as radon. Water from new underground sources must be tested for radon before they are connected to a reticulated drinking-water supply. 

7. Salinity: Some aquifers are naturally saline (salty). Bores located near the coast maybe affected by seawater flowing into the aquifer if excessive water abstraction causes seawater to be drawn into the aquifer to replace the freshwater. 


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Five Facts About Borehole Drilling That You Need To Take Note Of:
1. Know Your Borehole Casings:The Preferred Borehole Casing In Zimbabwe Is Class 9 and 10 (Pressure Classes.)This is because Class 9 and Class 10 Casings are more collapse resistant. The strength of a Casing is often described as collapse resistance.

2. Borehole Drilling Depth: The exact depth, of where the water is located, cannot be established by the drilling contractor nor the Water Surveyor (Borehole Siter).

3. The Is No 100% Guarantee On Water: It is important to note that it is never a 100% guarantee that any hole will yield water, the amount and water quality can also not be guaranteed by the drilling contractor and water surveyor.

4. Borehole Siting or Water Surveying Is Important: Making use of a hydrologist or traditional water diviner will increase your chances of having a successful borehole that will yield a sufficient amount of water.

5. Know The Risks: The risk of the borehole drilling lies with the property owner. The client will still be liable for the drilling costs irrespective of a borehole yielding water or not.

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