Document BRyEYbLYpR4DpM8dXKRBo863o

1066 CHAPTER 42 1958 Guide which will combine with the sulphate and chloride ions, is called permanent or non carbonate hardness. Inhibitor. A chemical substance added to an environment to reduce corrosion. Ion. An electrically charged atom or group of atoms. Passivity. The tendency of a metal to become abnormally inactive in a certain environment. pH. The logarithm of the reciprocal of the hydrogen ion concentration of a solu tion. The pH value denotes the degree of acidity or alkalinity of a solution. The value of a neutral solution, such as pure water, is 7. Values below 7 are increasingly acid, while values above 7 are.increasingly alkaline: ; .; Polarization. An effect produced on. the electrode of an, electrolytic cell by products formed by the passage of current through the cell. Hydrogen is the product generally formed, although other corrosion products may also cause polarization. Polarization reduces corrosive activity by offering a resistance to current flow and developing an opposing electromotive force. Scale. Scale1 is a deposit formed from solution directly in place .upon a confining surface. It is a deposit which will retain its physical shape when mechanical means Table 1. Mineral Analyses Typifying Composition of Waters Available and Used Industrially in the USA SUBSTANCR Unit Location oe Abea*'1* U) (2) (3) (4) (5) (6) (7) (8) ' (9) SiOt Fe Ca Mg Na K 2 6 12 37 10 9 22 14 000 1 0 002 6 5 36 62 92 96 3 155 400 1 2 8 18 34 27 2 '46 1-300 2 6 7 44 8 183 215 , 78 11.000 111 1 18 10 3 1 ' 400 HCO 14 13 119 202 339 334 549 210 : 150 SO 10 2 22 135 84 . 121 11. 389 2,700 Cl 2 10 13 13 10 280 22. 117 19,000 NO* 1 0 2 13 0. ! 1 3 CaCO* Non-Carbonate Hardness................. CaSO 31 12 5 66 165 426 434 983 564 948 35,000 11 98 165 287 274 8 172 125 7 18 40 58 54 0 295 5,900 * All Values are parte per million of the unit cited to nearest whole number (see Reference 5). ( b Numbers indicate location or area as follows: (1) Catskill supply--New York City (6) Well Water--Maywood, 'Illinois-- (2) Swamp Water (Colored) Black Creek, Middleburg, Florida (3) Niagara River (Filtered) Niagara Falls, New York (4) Missouri River (Untreated) Average 2090 ft (7) Well Water--Smithfield. Va'--330'ft. (8) Well Water--Rosewell, N. Mexico (5) Well Waters--Public Supply--Dayton, Ohio--30-60 ft. (9) Ocean Wateri-Average are used to remove it from the surface on which it is deposited. Seale, which may or may not adhere to the underlying surface, is usually crystalline and dense,, fre quently laminated, and occasionally columnar in structure. Sludge. Sludge1 is a water-formed sedimentary deposit. It usually does not cohere sufficiently to retain its physical shape when mechanical means are used to remove it from the surface upon which it deposits. Sludge is not always found at the place where it is formed. It may be hard and adherent, and baked to the surface on which it has been deposited.1 Water-Formed Deposits. A water-formed deposit1 is any accumulation of in soluble material derived from water or formed by the reaction of water upon sur faces in contact with water. Deposits formed from or by water in all of its phases may be further classified as scale, sludge, corrosion products, or biological deposits. CLASSIFICATION AND CHARACTERISTICS OF WATER Due to the many conditions of water encountered in industry,4 it is fre quently necessary to obtain expert advice and a prescribed treatment to make the water suitable for use in a given process. The heating and air Corrosion and Water Formed Deposits, Causes and Prevention 1067 conditioning engineer is concerned chiefly with two broad classifications of water: (1) those waters containing various amounts of mineral impurities and (2) condensates that are relatively free from mineral impurities but contain various amounts of dissolved gases such as carbon dioxide, oxygen, and sulphur dioxide, that tend to make them corrosive. Dissolved gases are the main factors affecting condensate corrosiveness, but they may also be present in water containing mineral impurities to an extent that will make the water corrosive. Mineralized Waters All the waters found in streams, wells, lakes, and the ocean are min eralized. The same is true of all municipal supplies even though they may have been treated. For a given area, ground waters are likely to be more highly mineralized than are surface waters. Conversely, surface waters are more likely to be contaminated with municipal sewage and trade wastes. Virtually all mineralized waters also contain biological organisms. Mineralogical Characteristics. The character and amount of extraneous inorganic materials--including deleterious gases--dissolved and sus- Tabi.e 2. Conversion Factors for Water Analyses To Convert Into Multiply by Grains per U. S. gallon................................... Grains per Imperial gallon ............................ Grams per liter....................................... Mg per liter...................................................... ppm ppm ppm ppm m17 i 1000 i pended therein, describe the mineralogical characteristics of any water. Revealing such information is the function of a mineralogical chemical analysis. The analyses in Table 1 disclose the composition of the public water supplies used by about 45 percent of the total population of the cities, in the United States, having more than 20,000 inhabitants.6 All values recorded are in terms of parts per million.* This is the approved standard terminology for reporting the results of mineral analyses.6 Values reported in the other terms commonly used may be converted into the standard form by using the factors listed in Table 2. Data for dissolved gases or pH values have been omitted in Table 1 because even waters of the same mineral contents may vary widely in these respects. Unpolluted natural waters usually have pH values within h r?n. to 8' depending upon their free CO, contents. Polluted waters, which include those derived from wells or swamps in marshy ground, may nave pH values well below 5. Biological Characteristics. The slime-forming organisms are mostly ower plants, grouped by botanists into the phylum thallophyta. This group is distinguished by the absence of leaves, roots, or stems from the fosses, ferns, and seed plants which comprise the three other phyla of the plant kingdom. thallophyta (see Table 3) are divided into algae, which can synchpe chlorophyll for the production of sugar, and the fungi which lack orophyll, and must therefore secure already synthesized carbohydrates. rial m*Mion are hereinafter abbreviated ppm. A part per million signifies a unit weight of mateion umt weights of the solution.