Document Jr4QNMdLLyYJD971LeGZLveLa

218 CHAPTER 10 . 1958 Guide#; ' Na tion line represents the limiting concentrations of water vapor which cani/` exist as vapor at various temperatures. rl A common condition inside buildings, 70 F and 40 percent relative*' humidity, is represented by point A. This is a condition of partial satura- '. tion; i.e., less than 100 percent relative humidity. The vapor pressure ?, of the water present in the air, although not shown on the chart, can be calcu- lated readily from the vapor pressure at saturation and the relative hu- A | midity, since., relative humidity is very nearly equal to the ratio of the:';: actual vapor pressure to the saturation pressure at the. existing temper-*'. ature. The increasing relative humidity accompanying cooling from thei condition represented by A on the chart to point B can readily be followed.?^ At B, however, at 44.6 F, the relative humidity becomes 100 percent, and I the air-vapor mixture is said to be saturated. The temperature at whichj'; ' |1;this particular air-vapor mixture, upon cooling, becomes saturated is. its 'C; ..<r . m' m 0F-; rnf:. Fio. 1. Two Typical Heating and Cooling Processes in Air within Buildings?- Shown on A.S.H.A.E. Psychrometric Chart : - .. i%i' dew-point temperature. Upon further cooling, to 35 F, the original amount^ of water vapor can no longer be retained and is reduced, in this case,'tog the condition represented by C, from 0:0633 lb per lb dpi air to 0.0427g: lb per lb dry air. The process ABC is typical of that which an air-vaporjf mixture experiences when it comes in contact with a cool window surfaces Cooling from B to C results in visible condensation on the glass surface. the point C were below 32 F, the condensation would be in the form.o frost. Once the temperature drops below the dew point, or frost point if low 32 F, the vapor pressure at the condensing surface is also reduced,^, thereby establishing a gradient of vapor pressure from the room air to window surface. This gradient will operate, in conjunction with thfe convective action within the room, to move water vapor continuous# to the window surface to be condensed, so long as the concentration^op water vapor in the room is maintained. A common winter process is that shown by DE, showing air at 20,J| saturated, being heated to 70 F with a resulting large decrease in relatij~ humidity. This explains, in part, the greatly reduced relative humidity Moisture in Building Construction 219 experienced in houses in extreme cold weather, when cold outside air enters the house and is heated. WATER IN BUILDING MATERIALS The surfaces of most common materials have an affinity for water molecules. Molecular forces of attraction will hold water molecules to the surface, but decrease very rapidly with increase in distance of molecu lar proportions. The film thickness and therefore the amount of water held in equilibrium with the surrounding atmosphere is roughly propor tional to relative humidity. Surface films of water molecules, at low humidities, may be only one molecule thick; at moderate humidities poly-molecular films may be established, while at humidities very close to 100 percent, the films become so thick, relatively, that small pores may become filled and larger capillaries may be partially filled. At satura tion conditions all voids in tbe material may be completely filled.. Some materials such as silica gel, alumina and most natural fibrous materials present very large effective surfaces to the water molecules, so that the amount of water held on the effective surface in these materials may be relatively large, even at moderate humidities. These are said to be hygroscopic. Other materials, such as most metals, not penetrated by the water molecules, present relatively small surfaces and so may take only minute quantities of water, except when wetted directly by liquid. Substances having a great affinity for water, and their use.as dehumidifying agents, are described in Chapter 37. Data on the moisture contents of various common materials in equilibrium with the atmosphere at various relative humidities are given in Table 2 of Chapter 46, and equilibrium moisture content is further discussed in Chapter 47 on Industrial Drying Systems. Significant dimensional changes take place in many materials used in buildings, with change in moisture content. Those which take place in wood, of the order of 0.1, 2, and 4 percent in the longitudinal, radial and tangential directions, respectively, on a change from air dry at 12 to 15 Per?nJ' moisture content to oven dry are perhaps the best known. Most wood-fiber products, including papers, will exhibit moisture expansion consistent with the basic wood properties to a degree dependent on the ber orientation and arrangement. Data on wood are available in publica10ns on wood technology. Almost all plant and animal fibers experience ppremable moisture changes with changing relative humidity and undergo stantial dimensional changes of the same order as those in wood. Less g nerally recognized are the dimensional changes which can occur in onry materials as a result of changes in moisture content, of b a e'*^er an essential or a contributory factor in almost all cases as th^TM0^11 building materials resulting from chemical changes such bv fro stee' ' Physical changes such as the spalling of masonry control ^Ctl0n' or. biological processes such as the rotting of wood. The afip ,ot water in building constructions may be necessary to ensure Cond S6mCe ^r0m ^he materials involved. wettimT^118^1?1' wa^er vapor, although not the only means by which ticuiarl may be brought about, is nevertheless a most insidious one par- most likel'n tresPec*; freeze-thaw breakdown, since from its nature it is be rjsj. Qr f 0 .ccur at points of low temperature at which there may later reezing while the material remains in a saturated condition.