Fractured rocks play an important role in transport of natural resources through subsurface systems. In recent years, interest has grown in investigating heat transport by means of tracer tests, driven by the important current development of geothermal applications. Many field and laboratory tracer tests in fractured media show that fracture - matrix exchange is more significantfor heat than mass tracers, thus thermal breakthrough curves are strongly controlled by matrix thermal diffusivity. In this study, the behaviour of heat transport in a fractured network, at bench laboratory scale, has been investigated.

Experimental Study of Heat Transport in Fractured Network / Pastore, N.; Cherubini, C.; Giasi, C. I.; Allegretti, N. M.; Redondo, J. M.; Tarquis, M.. - In: ENERGY PROCEDIA. - ISSN 1876-6102. - STAMPA. - 76:(2015), pp. 273-281. ( European Geosciences Union General Assembly 2015 - Division Energy, Resources and Environment, (EGU) Austria Center Vienna, Vienna, AUSTRIA APR 12-17, 2015) [10.1016/j.egypro.2015.07.860].

Experimental Study of Heat Transport in Fractured Network

Cherubini, C.;
2015-01-01

Abstract

Fractured rocks play an important role in transport of natural resources through subsurface systems. In recent years, interest has grown in investigating heat transport by means of tracer tests, driven by the important current development of geothermal applications. Many field and laboratory tracer tests in fractured media show that fracture - matrix exchange is more significantfor heat than mass tracers, thus thermal breakthrough curves are strongly controlled by matrix thermal diffusivity. In this study, the behaviour of heat transport in a fractured network, at bench laboratory scale, has been investigated.
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11368/3059714
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