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<br />001220 <br /> <br />IX.l <br /> <br />IX. CHEMICAL, PHYSICAL, AND BIOLOGICAL QUALITr <br /> <br />General considerations <br /> <br />. <br /> <br />In regard to its quality--chemical, physical, or biological--no <br />water body should be assumed to be uniform or unchanging with time. <br />In fact, lack of uniformity and continual change with time are the <br />rule and not the exception. <br /> <br />Thus, the analysis of a single water sample can show no more than <br />the chemiCal, physical, or biological character of the water body at one <br />point in space and at one moment in time. It may tell little about the <br />water-quality situation, or even may be misleading, unless it is supple- <br />mented by full information as to nature of the water environment, as to <br />changes taking place in that environment, and as to the manner in which <br />the sample was taken. Such Wormation is quite as meaningful, and may <br />be even more so, as assurance that methods of analysis were competent <br />and accurate. <br /> <br />Water quality varies greatly through the several phases of the <br />hydrologic cycle. In nature, water approaches maximum purity in its <br />vapor phase, immediately as it is rejuvenated by evaporation from an <br />ancestral water body such as one of the oceans, a lake, or a stream. <br />Shortly after the vapor phase, water quality begins to change in accord <br />with the physical and chemical characteristics of the environment. In <br />the atmospheric environment, noticeable but generally.minor changes <br />occur in the content of the solutes from both natural and artificial <br />sources; also, in the basic chemical makeup of the water, as in the <br />ratio of hydrogen to tritium. After it encounters the surface of the <br />earth, water undergoes major change in its chemical and physical <br />characteristics. Thus, when water falls into an ocean as rain or snow, <br />its dissolved-solids content soon equals the average salt content found <br />in the oceans. Precipitation on land results in slower but diverse <br />changes in water quality. Erosion of soil particles can cause 'Water to <br />become very turbid as it moves across the land surface. Also, many <br />COl1llllon minerals enter into solution whether the wate;r is on the land <br />surface or in the ground; solubility, chemical reactivity, and temperature <br />control the resulting concentration of the salts. Bacterial growth and <br />other biological activity vary significantly with changes in the physical <br />and chemical characteristics of the environment. In turn, this activity <br />affects the physical and chemical quality of the water through changes <br />which include concentration of dissolved gases and solids, pH, temperature,. <br />color, taste, and odor. Biological growth also may make the water toxic <br />to other life forms. <br /> <br />