the Thermal stream in danii. The simplified model

you are: the Thermal stream in danii

It is visible, that the simplified model And is better, than model In, corresponds to linear increase in temperature with depth. This fact, and also that here the estimation or only the first approach to an estimation of size of the climatic amendment to Denmark is necessary for us, have led us to a choice of model And for calculation of the corrected values of a thermal stream. Klimaticheski the indignant temperatures were calculated by means of the formulas given Karslo and Egerom for step and linear change where value of factor temperaturoprovodnosti was used, equal 10-6 m2/with. After introduction of the climatic amendment of value of a thermal stream raise on 12-13 мВт/м2. Model use In would give increase on 14-16 мВт/м2.

It is supposed, that the temperatures measured in a face of five boreholes in northern Jutland, are exact in limits ±3 To, and average factor of heat conductivity - in limits ±0,2 Vt / (м*К), that corresponds to accuracy of definition of a thermal stream yo12-14 мВт/м2. We consider, that the factor of heat conductivity established in area Gryondals-eng, is exact in limits ±0,3 Vt / (м*К), therefore accuracy of definition of a thermal stream there is equal ±6 мВт/м2 (q2) and ±8 мВт/м2 (q3). On this basis five values from northern Jutland are not considered essentially various. For these five points average values 62 мВт/м2 (q2) after corrective action on influence of hydrochloric structure and 75 мВт/м2 (qз) after introduction of the climatic amendment are accepted.