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Snashots of (a) the temperature, (b) the hydraulic head (h), (c) the hydraulic head differeecence (dh) between the calculated and isoterhmal (ΔT=0 °C) head and (d) the hydraulic head decrease (Δh<0 m) at t=4∙106 d and at ΔT=100 °C (Ra=2003). (b, c) The head maximum and the head difference is denoted by a black diamond and squere, respectively
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On the basis of earlier conceptions, water table variation was suggested as the main driving force of regional groundwater motion. Since that time it has been perceived, that furteher driving forces (e.g. density change by temperature differences, etc.) can induce groundwater flow. Foremost, Lapwood [1] proved analytically the onset of free thermal...
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