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Principles of naval engineering - Historic Naval Ships Association

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Chapter 8 -INTRODUCTION TO THERMODYNAMICSare poor absorbers. In general, good reflectorsare poor radiators and poor absorbers.In considering thermal radiation, the concept<strong>of</strong> black body radiation is frequently a usefulconstruct. A black body is conceived <strong>of</strong> as anideal or theoretical body which, being perfectlyblack, is a perfect radiator, a perfect absorber,and a perfect nonreflector <strong>of</strong> radiant energy.The thermal radiation emitted by such a perfectblack body is proportional to T^— that is, to theabsolute temperature raised to the fourth power.Because <strong>of</strong> the fourth power relationship, doublingthe absolute temperature increases theradiation 16 times, tripling the absolute temperatureincreases the radiation 81 times, andso forth. The thermal radiation emitted by realbodies is also proportional to the fourth power <strong>of</strong>the absolute temperature, although the totalradiation emitted by a real body depends alsoupon the surface <strong>of</strong> the body. Consideration <strong>of</strong>the relationship between the thermal radiation<strong>of</strong> a body and the fourth power <strong>of</strong> the absolutetemperature <strong>of</strong> that body explains why the problem<strong>of</strong> thermal insulation against radiationlosses increases so enormously as the temperatureincreases.CONVECTION.— Although convection is <strong>of</strong>tenloosely classified as a mode <strong>of</strong> heat transfer, itis more accurately regarded as the mechanicaltransportation <strong>of</strong> a mass <strong>of</strong> fluid (liquid or gas)from one place to another. In the process <strong>of</strong> thistransportation, all the thermal energy storedwithin the fluid remains in stored form unless itis transferred by radiation or by conduction.Since convection does not involve thermal energyin transition, we cannot in the most fundamentalsense regard it as a mode<strong>of</strong> heat transfer.Convection is the transportation or the move -ment <strong>of</strong> some portions within amass <strong>of</strong> fluid. Asthis movement occurs, the moving portions <strong>of</strong>the fluid transport their contained thermalenergy to other parts <strong>of</strong> the fluid. The effect <strong>of</strong>convection is thus to mix the various portions <strong>of</strong>the fluid. The part that was at the bottom <strong>of</strong>the container may move to the top or the partthat was at one side may move to the other side.As this mixing takes place, heat transfer occursby conduction and radiation from one part <strong>of</strong> thefluid to another and between the fluid and itssurroundings. In other words, convection transportsportions <strong>of</strong> the fluid from one place to another,mixes the fluid, and thus provides anopportunity for heat transfer to occur. Butconvection does not, in and <strong>of</strong> itself, "transfer"thermal energy.Convection serves a vital purpose in bringingthe different parts <strong>of</strong> a fluid into closecontact with each other so that heat transfer canoccur. Without convection, there would be littleheat transfer from, to, or within fluids, sincemost fluids are very poor at transferring heatexcept when they are in motion.Two kinds <strong>of</strong> convection may be distinguished.Natural convection occurs when there are differencesin the density <strong>of</strong> different parts <strong>of</strong> thefluid. The differences in density are usuallycaused by unequal temperatures within the mass<strong>of</strong> fluid. As the air over a hot radiator is heated,for example, it becomes less dense and thereforebegins to rise. Cooler, heavier air is drawnin to replace the heated air that has moved upward,and convection currents are thus set up.Another example <strong>of</strong> natural convection, and onethat may be quite readily observed, may befound in a pan <strong>of</strong> water that is being heated ona stove. As the water near the bottom <strong>of</strong> the panis heated first, it becomes less dense and movesupward. This displaces the cooler, heavier waterand forces it downward; as the cooler water isheated in turn, it rises and displaces the waternear the top. By the time the water has almostreached the boiling point, a considerable amount<strong>of</strong> motion can be observed in the water.Forced convection occurs when some mechanicaldevice such as a pump or a fan producesmovement <strong>of</strong> a fluid. Many examples <strong>of</strong> forcedconvection may be observed in the shipboard<strong>engineering</strong> plant: feed pumps transporting waterto the boilers, fuel oil pumps moving fuel oilthrough heaters and meters, lubricating oilpumps forcing lubricating oil through coolers,and forced draft blowers pushing air throughboiler double casings, to name but a few.The mathematical treatment <strong>of</strong> convectionis extremely complex, largely because theamount <strong>of</strong> heat gained or lost through the convectionprocess depends upon so many differentfactors. Empirically determined convection coefficientswhich take account <strong>of</strong> these manyfactors are available for most kinds <strong>of</strong> <strong>engineering</strong>equipment.Sensible Heat and Latent HeatThe terms sensible heat and latent heat are<strong>of</strong>ten used to indicate the effect that the transfer<strong>of</strong> heat has upon a substance. The flow <strong>of</strong>167

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