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Science of Water : Concepts and Applications

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110 The <strong>Science</strong> <strong>of</strong> <strong>Water</strong>: <strong>Concepts</strong> <strong>and</strong> <strong>Applications</strong><br />

FIGURE 4.1 pH <strong>of</strong> selected liquids.<br />

pH<br />

pH is a measure <strong>of</strong> the hydrogen ion (H + ) concentration. Solutions range from very acidic (having<br />

a high concentration <strong>of</strong> H + ions) to very basic (having a high concentration <strong>of</strong> OH − ions). The pH<br />

scale ranges from 0 to 14, with 7 being the neutral value (see Figure 4.1). The pH <strong>of</strong> water is important<br />

to the chemical reactions that take place within water, <strong>and</strong> pH values that are too high or low<br />

can inhibit the growth <strong>of</strong> microorganisms.<br />

High pH values are considered basic <strong>and</strong> low pH values are considered acidic. Stated another<br />

way, low pH values indicate a high level <strong>of</strong> H + concentration, while high pH values indicate a low<br />

H + concentration. Because <strong>of</strong> this inverse logarithmic relationship, there is a tenfold difference in<br />

H + concentration.<br />

Natural water varies in pH depending on its source. Pure water has a neutral pH, with an equal<br />

number H + <strong>and</strong> OH − . Adding an acid to water causes additional positive ions to be released so that<br />

the H + ion concentration goes up <strong>and</strong> the pH value goes down.<br />

HCl ↔ H + + Cl −<br />

To control coagulation <strong>and</strong> corrosion by water, the waterworks operator must test for the hydrogen<br />

ion concentration to determine the water’s pH. In a test for coagulation, as more alum (acid)<br />

is added, the pH value lowers. If more lime (alkali) is added, the pH value rises. This relationship<br />

should be remembered—if a good fl oc is formed, the pH should then be determined <strong>and</strong> maintained<br />

at that pH value until the raw water changes.<br />

Pollution can change water’s pH, which in turn can harm animals <strong>and</strong> plants living in the water.<br />

For instance, water coming out <strong>of</strong> an ab<strong>and</strong>oned coal mine can have a pH <strong>of</strong> 2, which is very acidic<br />

<strong>and</strong> would defi nitely affect any fi sh crazy enough to try to live in it. By using the logarithm scale,<br />

this mine-drainage water would be 100,000 times more acidic than neutral water—so stay out <strong>of</strong><br />

ab<strong>and</strong>oned mines.<br />

√ Important Point: Seawater is slightly more basic (the pH value is higher) than most natural<br />

fresh water. Neutral water (such as distilled water) has a pH <strong>of</strong> 7, which is in the middle <strong>of</strong> being<br />

acidic <strong>and</strong> alkaline. Seawater happens to be slightly alkaline (basic), with a pH <strong>of</strong> about 8. Most<br />

natural water has a pH range <strong>of</strong> 6–8, although acid rain can have a pH as low as 4.<br />

COMMON WATER MEASUREMENTS<br />

Neutral<br />

Acidic Basic<br />

0 1 2 3 4 5 6 7 8 9 10 11 12 13 14<br />

1 M Gastric Oranges Urine Blood Sea Household 1 M<br />

HCl juices Tomatoes Pure water ammonia NaOH<br />

water<br />

<strong>Water</strong> practitioners/regulators such as waterworks operators <strong>and</strong> USEPA along with their scientifi c<br />

counterparts at the U.S. Geological Survey (USGS) have been measuring water for decades. Millions<br />

<strong>of</strong> measurements <strong>and</strong> analyses have been made. Some measurements are taken almost every

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