That was quick... my dual location has already been figured out! (cf Steamy Tea - good to see some Cornish representation...).
As regards house placement... if you know Goonvrea you might well know the house.
But the last comment is the important one ...
I've always considered GSHPs as a better option because of the physics of heat transfer... ie water is around 20x better at moving heat from a surface than air. Plus, I have the space for a slinky loop that I can install myself. Plus I'm assuming our climate and ground heatflow is better suited than other areas in the UK because of our "southerly" latitude and minor temperatures swings. But, and there's a big but... GSHPs are sooo much more expensive.
Also I'm intrigued by an older thread that I found from SteamyTea, TerryE and JSHarris. (I commend JSHarris for his code and suggest he can bore me anytime with such work). His wall temperature profile that shows how stable the interior temperatures are whilst the exterior wangs about betwen 10 and zero.
Anyhow let me try to set out a cogent message that relates my interest in the consensus on AHSP vs GSHP and also the concept of seasonal heat storage, thermal inertia and thermal penetration.
I'm keen to understand some of the fascinating comments made within this thread. In particular from StormyTea, TerryE and JSHarris.
When I click on the youtube link I get a message describing this as private and I need to sign in on Youtube, which I try to avoid... is there any other way to get this?
I'm assuming the lack of thermal penetration is because fourier's law (-k.dT/dx) tells us that heat flow will be much greater up than down? But what if the heat source is under an insulator?
I bet every non-technical person now mentions the guy in Grand Designs, with his heat storage system. I suspect his design is a very special case.
From my back of a fag-packet calculations I was thinking that the problem with storage is just size. EG. If you had a house with footprint of radius r, the notional heat island under the house would have a volume of half 4/3. pi. r^3. If this hemisphere touches the water table where the water just whisks away your heat and never goes above 12C. You'd chop your volume at the base ... a bit like an upside down egg.
Assuming for this exercise that it doesn't ... a half 4/3. pi. r^3 would give a volume of around 1000 m3, for r=8. Multiply that by heat capacity of say 800 J/kg.k and density of 1500 kg/m3 and delta T of say 5 degree on average gives c. 1800 kwh of heat storage. (Is this right?)
If so, this aint much when you consider a stone/cob home will need about 15,000 kwh a year to stay warm. My 1800 kWh estimate for storage doesn't really factor in how much heat buggers off out the bottom of the storage volume and leaks out the sides. The only utility I could see with trying to inject summer heat under your house to create a heat store, would be for relatively short time scales - say between sunny periods and cloudy periods... and even that doesn't account for whether you could realistically get much of the heat back...
Hmmmm.... I'm convincing myself of the futility of heat storage: you can't put enough heat in to store on the time-scale that you want, and even if you did, you might only get a small proportion of it back.
Comments welcome on whether the issue with storage is just size and also the ASHP vs GSHP angle.
Regards
Stephen