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Page Title: CHAPTER 3 PRESSURIZATION AND AIR-CONDITIONING SYSTEMS
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Aviation Structural Mechanic E2 - How airplanes are built and how to maintain them
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ENVIRONMENTAL CONTROL  SYSTEMS

CHAPTER  3 PRESSURIZATION   AND AIR-CONDITIONING   SYSTEMS Terminal Objective: Upon completion of this chapter, you will be able to recognize  the  operational  and  component  differences  between  air  cycle  and refrigerant  cycle  air-conditioning  systems  (ACS). Transferring   a   human   being   from   his natural environment on the earth’s surface to the environment existing at 40,000 feet places him in surroundings in which he cannot survive without artificial aids. Even at half that altitude, breathing becomes very rapid; and above 25,000 feet un- consciousness occurs, quickly followed by death. A brief study of the earth’s atmosphere tells us why  this  condition  exists. STRUCTURE  OF THE ATMOSPHERE Learning Objective: Recognize the affect high altitude flight could have on flight personnel  because  of  decreased  atmos- pheric  pressure. The  envelope  of  atmosphere  surrounding  the earth is a gaseous mixture consisting chiefly of nitrogen and oxygen. There are traces of other gases, but they have no significance as far as body functions are concerned. Chemical analysis has shown  that  the  proportions  of  nitrogen  and oxygen  are  constant  throughout  the  thickness  of the atmosphere, up through 200,000 feet or more. ATMOSPHERIC PRESSURE Although  the  chemical  content  of  the atmosphere remains fairly constant, the density (mass per unit volume) of the atmosphere varies with altitude. At 18,000 feet the density is about one-half of the density at sea level, and at 36,000 feet it is only about one-fourth of the density at sea level. The atmospheric pressure also varies with  the  altitude.  The  pressure  exerted  by  the atmosphere may be compared to the pressure of a  column  of  water.  If  holes  are  made  in  the container of the column, the force with which the water  spurts  out  of  the  upper  holes  will  be considerably less than that at the bottom of the column. Similarly, the pressure exerted by the atmosphere is much greater near the surface of the  earth  than  it  is  at  high  altitudes.  For example, the pressure of the atmosphere at sea level is 14.7 psi, while the pressure at 40,000 feet above sea level is 2.72 psi, and at 60,000 feet is 1 psi. As an aircraft ascends to higher altitude, the resulting decrease in atmospheric pressure may affect flight personnel in several ways. The most noticeable effect is in breathing. Breathing is a mechanical process that depends heavily  on  atmospheric  pressure.  When  a  person inhales,  he  automatically  raises  his  ribs  and depresses  his  diaphragm  so  that  the  chest  cavity is enlarged. This reduces the air pressure within the  cavity  below  that  of  the  atmosphere  outside. Air  is  thus  pushed  into  the  lungs.  When  he exhales, he reduces the chest cavity, increasing the pressure within it. This pushes the air out of the lungs. When  low  atmospheric  pressures  are  en- countered,  the  lungs  are  not  filled  so  completely when inhaling. With lower density, a person gets fewer molecules of air in each breath. If he gets fewer molecules of air in each breath, he also gets fewer molecules of oxygen, and no person can live unless he gets a sufficient amount of oxygen. This  problem  may  be  solved  up  to  certain altitudes by the proper use of oxygen equipment; however, at extremely high altitudes (above 35,000 feet), the atmospheric pressure is so low that the pressure of the blood and other liquids in the body are no longer balanced. The human body then tends to burst. In some cases, blood vessels near 3-1

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