Cover Page
  The Hydrologic Cycle
  Meteroric Water
  Ground Water
  Surface Water
Hardness
Ion Exchange Softeners
Iron
Iron Removal
Manganese
Manganese Removal
Hydrogen Sulfide
Hydrogen Sulfide Removal
Chlorides and Sulfates
Sodium
Fluorides
Turbidity
Removal of Turbidity
What is meant by pH?
Alkalinity
Removal of Alkalinity
Acidic Water
Removal of Acidity
Objectionable Tastes and Odors
Nitrates
Bacterial Contamination
Forms of Lower Plant Life in Water
Forms of Lower Animal Life in Water
Decontamination by Chlorination
Decontamination by Reverse Osmosis

 

 

Surface Water

We classify lakes, rivers, reservoirs and ponds, for example, as surface water. These bodies receive water directly from precipitation and from surface run-off. They also derive a portion of their supplies from underground springs connected with ground water sources.

While surface water, as a rule, has the advantage of lower mineral content, there are certain disadvantages to be considered: 

  1. The presence of much contaminated matter making water unfit for human consumption until properly treated.

  2. Industrial and municipal pollution of many supplies.

  3. Surface run-off bringing mud and decayed vegetation into the water.

  4. Possibility of animal and human wastes in the water.

  5. In many cases good environments for algae and bacteria.

Regardless of the mineral and organic make-up of a water source, both deep wells and large lakes make available water that is more or less consistent quality from season to season. In contrast, many small bodies of water, shallow wells and springs often reflect seasonal and even daily variations in their mineral content.

 

 

Copyright of Island Well Drillers Limited 2001


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