MathewsMD said:
ΔH = ΔE + ΔPV but since P is constant ΔH = ΔE + PΔV
ΔE = q + w = q - PΔV (at constant pressure)
So ΔH = q - PΔV + PΔV = q
So isn't ΔU = ΔH in this case, if pressure is constant?
No. That doesn't follow from your own algebra.
Just wondering, if you have a bomb calorimeter and volume is kept constant, how can we say pressure is constant before and after? Do we just wait for the product(s) to settle and hopefully return to the original pressure and then calculate enthalpy changes at that time?
No. The bomb calorimeter at constant volume does not measure what we define as "heat of reaction." However, if the reaction takes place involving ideal gases, we can calculate what the heat of reaction would be.
Sorry, I'm just having trouble understanding this concept. If you are at the melting point of water (273.15K) you have to lose enough energy to turn ALL of the liquid water to ice, correct?
Yes.
So despite being at a temperature a little higher (ex. 280K) there would still be ice present, but it would be in low quantities, right?
At 280, you can't have ice and water present simultaneously
in equilibrium. Even under non-equilibrium conditions, if part of the water were at 280, the water at the interface with the ice would be at 273 (the water temperature would vary with spatial position in the system), and all the ice would be at 273 (or below).[/quote]
At equilibrium, below 273, water can't exist as a liquid. In some non-equilibrium cases, it can be cooled below 273, but the system is thermodynamically unstable, and the slightest disturbance will cause the water to solidify (provided the heat of solidification is removed).
I'm confused in understanding how both the products and reactants are to be measured at 298.15K and 1atm if the other exists in only trace amounts in those conditions...wouldn't there be negligible ice in these conditions as the formation of liquid water is favoured?
The terms products and reactants usually refer to chemical reactions. If you are referring to a phase change like this, you really can't have water at 298 change to ice at 298. Ice at 298 is a hypothetical state that can be assigned an enthalpy by extrapolating the behavior of ice from below 273. So this can still be a reference state for ice mathmatically, but the change in enthalpy from 273 to 298 will always automatically cancel out from any practical calculations.
Also, since ΔH = mcΔT, if T is not constant, then ΔT ≠ 0 and thus ΔH (in this case) is not a standard enthalpy, right?
There is no such thing as a change in enthalpy ΔH being a standard enthalpy. Here's how it works: The enthalpy of the material in some standard state is specified to have a certain value (there's a method of establishing preciesely what this value is relative to the pure atomic species making up the formula for the material, which are assigned enthalpies of zero). You can then evaluate the enthalpy of the material in some other state by evaluating the change in the enthalpy from the standard state, and then adding it to the enthalpy of the standard state.