Thanks Bob and Rich,
Appreciate the correction. I spoke with another ground instructor on this and it confused the heck out of him too, which is probably what got me on my high horse.
I thought he did a good job of explaining when he said High (Density Altitude) and Low (Density Altitude) on the whiteboard. We had both concurred on the subject of air "density" when in fact as Richard pointed out its not really the density of molocules rather the MASS of the molocules, an important point that I was definitely missing.
And Bob you are right, it was inappropriate to discredit CASA for that one (OK they get a break this time
as it is indeed an International term (hence my take on using the words "other regulatory authorities) and used in Science. Apologies if my slant was to agressive, I was simply trying to crush a walnut with a hammer to see what was inside
PS: Thanks for your help too Pannier, I just found a great bit of information (ok it was only Wikipedia) on air density after the above posts and it was very interesting in its brief consideration of a new variable - VAPOUR PRESSURE! (different from STATIC, DYNAMIC or EXAM pressure
but as Bob rightly said "The subject of Aerodynamics could well occupy years of study at the Tertiary Level".
Wikiquote below: (quite interesting)
The addition of water vapor to air (making the air humid) reduces the density of the air, which may at first appear contrary to logic.
This occurs because the molecular mass of water (18 g/mol) is less than the molecular mass of dry air (around 29 g/mol). For any gas, at a given temperature and pressure, the number of molecules present is constant for a particular volume (see Avogadro's Law). So when water molecules (vapor) are added to a given volume of air, the dry air molecules must decrease by the same number, to keep the pressure or temperature from increasing. Hence the mass per unit volume of the gas (its density) decreases.
The density of humid air may be calculated as a mixture of ideal gases. In this case, the partial pressure of water vapor is known as the vapor pressure. Using this method, error in the density calculation is less than 0.2% in the range of −10 °C to 50 °C