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Science of Water : Concepts and Applications

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<strong>Water</strong> Treatment 319<br />

Total residual<br />

Dem<strong>and</strong><br />

Chloramines<br />

formed<br />

FIGURE 9.9 Breakpoint chlorination curve.<br />

Breakpoint Chlorination<br />

To produce a free chlorine residual, enough chlorine must be added to the water to produce what is<br />

referred to as breakpoint chlorination (i.e., the point at which near complete oxidation <strong>of</strong> nitrogen<br />

compounds is reached; any residual beyond breakpoint is mostly free chlorine [see Figure 9.9]).<br />

When chlorine is added to natural waters, the chlorine begins combining with <strong>and</strong> oxidizing the<br />

chemicals in the water before it begins disinfecting. Although residual chlorine will be detectable<br />

in the water, the chlorine will be in the combined form with a weak disinfecting power. As we see<br />

in Figure 9.9, adding more chlorine to the water at this point actually decreases the chlorine residual<br />

as the additional chlorine destroys the combined chlorine compounds. At this stage, water may<br />

have a strong swimming pool or medicinal taste <strong>and</strong> odor. To avoid this taste <strong>and</strong> odor, add still<br />

more chlorine to produce a free residual chlorine. Free chlorine has the highest disinfecting power.<br />

The point at which most <strong>of</strong> the combined chlorine compounds have been destroyed <strong>and</strong> the free<br />

chlorine starts to form is the breakpoint.<br />

The chlorine breakpoint <strong>of</strong> water can only be determined by experimentation. This simple<br />

experiment requires 20 1000-mL beakers <strong>and</strong> a solution <strong>of</strong> chlorine. Place the raw water in the<br />

beakers <strong>and</strong> dose with progressively larger amounts <strong>of</strong> chlorine. For instance, you might start with<br />

0 in the fi rst beaker, then 0.5 mg/L <strong>and</strong> 1.0 mg/L, <strong>and</strong> so on. After a period <strong>of</strong> time, say 20 min, test<br />

each beaker for total chlorine residual <strong>and</strong> plot the results.<br />

Breakpoint Chlorination Curve *<br />

When the curve starts, no residual exists, even though there was a dosage. This is called the initial<br />

dem<strong>and</strong> <strong>and</strong> is microorganisms <strong>and</strong> interfering agents using the result <strong>of</strong> the chlorine.<br />

After the initial dem<strong>and</strong>, the curve slopes upward. Chlorine combining to form chloramines<br />

produces this part <strong>of</strong> the curve. All <strong>of</strong> the residual measured on this part <strong>of</strong> the curve is combined<br />

residual.<br />

At some point, the curve begins to drop back toward zero. This portion <strong>of</strong> the curve results from<br />

a reduction in combined residual, which occurs because enough chlorine has been added to destroy<br />

(oxidize) the nitrogen compounds used to form combined residuals.<br />

The breakpoint is the point where the downward slope <strong>of</strong> the curve breaks upward. At this<br />

point, all <strong>of</strong> the nitrogen compounds that could be destroyed have been destroyed.<br />

* Refer to Figure 9.9 for the following explanation.<br />

Chloramines<br />

destroyed<br />

Chlorine added to water<br />

Free residual<br />

formed<br />

Combined chlorine residual<br />

Free<br />

available<br />

chlorine<br />

residual

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