In isothermal the temperature is constant whereas in adiabatic the temperature falls or rises rapidly.Consider the case for expansion where in adiabatic the temperature drops. If you consider PV/T=constant then for same pressure we can show that as temp decreases the volume also decreases. During expansion for isothermal the temp does not change so volume is higher than adiabatic.
Example:
Isothermal P=8 Pa, V=x , T=2K
Adiabatic P=8 Pa, V=y, T=1K (as it drops)
Using PV/T=constant we can find that y is less than x.
of the release of latent heat
A D-T graph for non-uniform motion would appear as a curve rather than a straight line. This is because the distance covered by the object is changing at varying rates over time, causing the curve in the graph to represent this non-uniformity. The steeper the curve, the faster the object is accelerating or decelerating.
A steeper inclined plane pushes up more on an object than a flatter one. This is because the steeper the inclined plane, the more of the object's weight is directed perpendicular to the plane's surface, resulting in a greater normal force pushing up on the object.
An inclined plane with a steeper angle will push up more than one with a gentle slope. The steeper the incline, the more force is required to push an object up the incline due to the increased component of weight acting against the motion.
A ball rolls faster on a steeper ramp because gravity has a greater component pulling the ball downhill, increasing its acceleration. On a less steep ramp, the gravitational force component is smaller, resulting in slower acceleration and lower speed for the ball.
Reason being vaguely adiabatic process is more rapid - process is done so fast that no energy is allowed to enter or exit the system. So P-v variations will be high
Flatter lines have a _____ slope than that of steeper lines
Yes.A mountain is generally steeper than a hill because it is taller.
30% is steeper than 15% slope.
The bed of a youthful valley will be steeper than the remainder of the watercourse, and the valley walls will be steeper than the remainder of the watercourse.
The saturated adiabatic lapse rate is lower than the dry adiabatic lapse rate because during the process of condensation, heat is released into the atmosphere, which partially offsets the cooling effect of rising air. This release of heat makes the cooling rate of saturated air less than that of dry air as it ascends through the atmosphere.
-- Any number less than -5 is a steeper line sloping down. -- Any number greater than +5 is a steeper line sloping up.
The adiabatic lapse rate is lower when it's cloudy because clouds trap heat near the Earth's surface, slowing the rate at which temperature decreases with increasing altitude. This is known as the moist adiabatic lapse rate, which is typically lower than the dry adiabatic lapse rate that applies in clear, dry conditions.
why some long-run average cost curves are steeper on the downward side than others.
Stability prevails when the environmental lapse rate is less than the adiabatic lapse rate. This means that the temperature of the surrounding air decreases at a slower rate with altitude compared to the dry or moist adiabatic lapse rates, resulting in a more stable atmosphere.
heating curve is hotter than the cooling curve
less than the wet adiabatic rate.