the Thermal stream in danii. Discussion and conclusions

you are: the Thermal stream in danii

Presence powerful and, from the point of view of values of factor of heat conductivity, obviously, homogeneous complex of adjournment of limestones and a chalk in the Danish subpool allows to calculate values of a thermal stream with sufficient accuracy at use of not so exact temperatures of the oil in face oil and gas boreholes. In the Danish subpool of northern Jutland where sedimentary breeds of the big capacity lie down, the thermal stream is estimated on the average by values 60-65 мВт/м2, and at the account of the climatic amendment - nearby 75 мВт/м2. These values - the same order, as an estimation of a thermal stream of the North Sea to the West from the Danish region.

The Values calculated for area Gryondals-eng which are received in boundary area of a hollow near to the Fennoskandsky board, approximately on 20 мВт/м2 more low. Even if not to give too great value to each separate number in regional estimations, it is all the same obvious, that this difference will be co-ordinated with prospective fall of a thermal stream towards a board.

Observable temperature variations can be caused substantially, thus, variations of a thermal stream and to a lesser degree variations of factor of heat conductivity.

It was Not revealed considerable thermal anomalies neither in temperature, nor in a thermal stream, except what are connected with hydrochloric structures.