the Thermal stream in velikobritanii. Results

you are: the Thermal stream in velikobritanii

Values of a thermal stream can be calculated directly by means of an one-dimensional parity

q=TO dT/dz,

Where q - a thermal stream, To - factor of heat conductivity and dT/dz - a temperature gradient.

Factors of heat conductivity and prevalence of breeds of various types vary over a wide range, therefore it would be wrong to multiply average factor of heat conductivity on a chink by an average temperature gradient. More reliable method consists in calculation of a thermal stream for each site litologicheskogo a cut separately and the subsequent calculation of its average value. Advantage of this way is also that he allows to reveal any sharp changes konduktivnogo the thermal stream, caused addition or heat outflow at presence vodonosnyh horizons.

The Resulted topographical amendments are found by method Dzheffrisa. At the smoothed relief these amendments on the depths exceeding 100 m, are insignificant. Such situation is characteristic almost for all chinks where the topographical amendment is not resulted.

For calculation of influence of last freezing and changes of temperature of a surface during postglacial time evolution of superficial temperature was approximated by a number of step functions. The amendments received thus only when they were entered by authors of original works. To compare the values received in deep chinks (we will tell, is deeper 150, climatic amendments are better for excluding.