00:01
In order to find kd, we will be using this equation.
00:05
P is equivalent to 2 pi times m times r times t, all raise to the 1 half, multiplied by kt, pardon me, kd times theta, divided by na times s star, multiplied by 1 minus theta, then we'll multiply this value by the exponential of negative delta h divided by rt.
00:31
M is our molecular weight, kd is the rate of disorption, s is our surface coverage, p is pressure, t is temperature, and delta h is our enthalpy of absorption, and i've denoted theta as our additional surface coverage.
00:53
Now when we want to find kd, we have to plug in everything that we know.
00:59
So first we'll get 2 times 10 to the negative 5th, pascal's, our pressure, is equivalent to 2 pi times 28 grams per mole, multiplied by our r constant, 8 .314, multiplied by our temperature, 298 kelvin, and then we'll raise this entire quantity in brackets to the one -half power.
01:22
Then we'll multiply that by kd, that's the quantity that we do not know, multiplied by our surface coverage, 0 .5...