Green Building Bible, Fourth Edition |
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These two books are the perfect starting place to help you get to grips with one of the most vitally important aspects of our society - our homes and living environment. PLEASE NOTE: A download link for Volume 1 will be sent to you by email and Volume 2 will be sent to you by post as a book. |
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GSHP systems rely on the fact that, under normal geothermal gradients of about 0.5oF/100 ft (30 oC/km) (Grant et al., 1982), the earth temperature is roughly constant in a zone extending from about 20 ft (6.1 m) deep to about 150 ft (45.7 m) deep (Hart and Couvillion, 1986). This constant temperature interval within the earth is the result of a complex interaction of heat fluxes from above (the sun and the atmosphere) and from
below (the earth interior). As a result, the temperature of this interval within the earth is
approximately equal to the average annual air temperature (Hart and Couvillion, 1986).
Above this zone (less than about 20 feet (6.1 m) deep), the earth temperature is a damped
version of the air temperature at the earth’s surface. Below this zone (greater than about
150 ft (45.7 m) deep), the earth temperature begins to rise according to the natural
geothermal gradient.
Below the so-called ‘neutral zone’ (some −20 m depth in Canada), the temperature field is governed by non-diurnal and non-seasonal changes. Temperatures below this depth are linked to surface climatic forcing and deep terrestrial heat flow. The energy supply for a heat exchanger can be tapped from the vertical geothermal heat flux, the horizontal conduction of heat, advective transport with groundwater (if present), and heat exchange between the ground surface and the atmosphere.
Posted By: tony99.95% solar generally with about 0.05% or less radioactive decay heat from the core
Another factor related to thermal conductivity is the presence of overburden such as sand, clay and moraine. Such materials typically have thermal conductivities that are far lower than most rock types (Midttømme 1997), thereby acting as low-conductivity thermal blankets that will increase the subsurface temperature.
Posted By: SeretTo my mind, if a layer of thermally insulating overburden willincreasesubsurface temperature, then at least 50% of the heat must be coming from somewhere other than overhead.
Posted By: Ed Davies
It would indicate thatsomeheat is coming from below but I don't see any reason why it has to be 50%. Even a quite small percentage of heat from below will raise the temperature somewhat.
Posted By: SeretBecause an insulating layer will inhibit heat flow in both directions. If more than 50% of the energy was coming from above the layer it would cause the temperature below it to fall, not rise.