build-up p pressure 生成压力
DELTA P Differential Pressure 压差
Lo P Low pressure 低压下限
earth pressure p 土压力
ultrahigh-pressure metamorphic p-t-t path 超高压变作用p
NO PRESSURE P-CAL 无压力输出
That's a liquid, at some pressure p.
这是液体,出于一定压强下的。
PA Some partial pressure, p sub A, temperature T.
在温度T下的分压为。
Normally I couldn't do that Vdp because this term would have p dV plus V dp, but we've specified the pressure is constant, so the dp part is zero.
一般情况下我不能这么写,因为这一项会包含pdV和,但是我们已经假定压强为常数,所以包含dp的部分等于零。
pV=RT dT here because the pressure is constant, dV=RdT/p so dV is equal to R over p dT.
因为对1摩尔气体有,于是。
Because what we've done is we forced p, pressure here, to be equal to the external pressure.
因为这里我们让内部的压强,等于外部的压强。
It's not constant pressure, because we have a delta p going on. It's not constant volume either.
也不是恒容,这个限制,是这个实验的限制。
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