Two-dimensional anomalies of heat conductivity. Illegitimacy consequences

you are: Two-dimensional anomalies of heat conductivity

However and after that corrections sometimes remain distinctions in the values of a vertical thermal stream measured on different depths in the same chink. In their some cases try to connect or with influence of the non-stationary phenomena, such, as change of a climate or surface washout, or with local nekonduktivnym teploperenosom at movement of subsoil waters; it is underlined, that these divergences can be and result of an incorrect estimation of factor of heat conductivity of the layers crossed by a chink.

In this article we analyze possible consequences of illegitimacy mentioned above an assumption about one-dimensionality, proving, that the thermal stream can refract at borders of some usual geological structures; we show, that this refraction also (and it is not less frequent) can cause local variations of a vertical thermal stream.