We discussed equilibrium reactions before, especially in the stoichiometry section. We mentioned
chemical equilibria, between reactants and products. We also
mentioned solubility equilibria in the precipitation section. Now let's
introduce some other types of equilibrium. Suppose we put a
partially-filled balloon on each end of a tube with a
piston. Initially the piston is clamped in place. If we remove the
clamp so the piston can move, it will move until the pressure on
each side is equal. At this point, the balloons will probably also
be the same size (unless they are different size balloons), because
they are stretched out by equal inside pressure. The moving piston adjusts the volume
on each side until the pressures are equal, and then the system
reaches mechanical equilibrium, because the piston won't move any
more. Pressure is the property that tells us whether systems will be
at mechanical equilibrium; if we clamp the piston and put on a new
balloon, if it's at the same pressure as the other balloons then the
piston won't move when the clamp is removed.
We measure temperature using a thermometer. In science we use 2 scales to measure temperature, the Celsius or centigrade scale, on which water freezes at 0 °C and boils at 100 °C; and the Kelvin scale, on which water freezes at 273.15 K and boils at 373.15 K. The Celsius scale is probably what you are used to from regular life (although I am used to the Fahrenheit scale), and it is convenient because it focuses on water, which is very important for our lives. The Kelvin scale is good for science and thermodynamics especially, because 0 K is the lowest possible temperature. We'll study exactly what that means later.