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Theory of Engine Operation - Delmar Learning

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the piston as it is pushed downward to turn the crankshaft. This is an example <strong>of</strong> how engine efficiency<br />

is decreased. Friction may occur in solids, liquids, and gases. The airflow over a vehicle<br />

causes friction. The manufacturers carefully engineer their vehicles to be aerodynamic. This means<br />

that the resistance to motion from friction between the vehicle and the air is minimized. This is<br />

carefully calculated and measured as the coefficient <strong>of</strong> draft (Cd). Unfortunately, there are conditions<br />

and vehicles that can lose up to half <strong>of</strong> their mechanical energy to aerodynamic drag.<br />

Behavior <strong>of</strong> Liquids and Gases<br />

Molecular Energy<br />

Electrons are in constant motion around the nucleus <strong>of</strong> atoms or molecules. Kinetic energy is always<br />

occurring. The kinetic energy <strong>of</strong> liquids, gases, and solids changes in response to temperature.<br />

When temperature decreases, so does kinetic energy. As temperature increases, so does kinetic<br />

energy. Solids have the slowest reaction to temperature, while gases have the quickest response to<br />

changes in temperature. We know this theory already through our discussion <strong>of</strong> combustion. As<br />

temperature increases within the combustion chamber, the gases rapidly expand and the increasing<br />

kinetic energy is used to create thermal energy that is converted into mechanical energy.<br />

Temperature<br />

The volume <strong>of</strong> liquids, gases, and solids increases with temperature. It is the increased volume <strong>of</strong><br />

gases on top <strong>of</strong> the pistons that produces the force to push the piston downward. When filling<br />

engine fluids, such as tire air pressure and coolant, we must be aware <strong>of</strong> the effects <strong>of</strong> temperature<br />

on volume. It is easy to overfill a coolant reservoir if the coolant is at ambient temperature<br />

and you top the fluid <strong>of</strong>f to the maximum level. As the fluid heats up, it may expand beyond the<br />

capacity <strong>of</strong> the reservoir and develop enough pressure to blow the cap’s pressure relief valve.<br />

Pressure and Compressibility<br />

Pressure is always applied equally to all surfaces <strong>of</strong> a container. If there is a leak in the container,<br />

the pressure will leak out and equalize with the atmospheric pressure. Gases and liquids both<br />

flow, so they are classified as fluids. But there are distinct and significant differences between the<br />

characteristics <strong>of</strong> gases and liquids. Gases can be compressed; the molecules squeeze tighter<br />

together and form greater pressure. You can easily fill a tire with excess pressure. Luckily, you can<br />

further compress the gases in a combustion chamber to produce more power. Liquids, on the<br />

other hand, cannot be compressed. A liquid fills a chamber, and you cannot add more liquid; you<br />

can only increase pressure. Brake and clutch hydraulic systems work with liquids. When you<br />

depress the clutch or brake pedals, you move the liquid, under pressure to exert force on a piston.<br />

This force produces mechanical work from the brake caliper piston or the clutch hydraulic<br />

lever. If there is a leak in the system, air can enter. Air is a gas and is compressible. Air in a<br />

hydraulic system will cause a lack <strong>of</strong> pressure and force.<br />

Pressure and Vacuum<br />

Air is a gas with weight and mass. It is layered high above the surface <strong>of</strong> the earth and exerts a<br />

pressure on the earth’s surface. This pressure is called atmospheric pressure. A column <strong>of</strong> air<br />

extending from the earth’s surface at seal level to the outer edge <strong>of</strong> the earth’s atmosphere weighs<br />

14.7 pounds. We say that atmospheric pressure is 14.7 pounds at sea level. This pressure changes<br />

as we climb in altitude. If we are 14,000 feet above sea level in the mountains, that column <strong>of</strong> air<br />

no longer weighs 14.7 lbs; atmospheric pressure decreases. Also, as temperature increases, the<br />

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