The Geothermal Convector (GTC) is an unconventional system that uses a two-
phase closed thermosyphon for heat extraction from a geothermal aquifer wit
hout fluid withdrawal. This paper reports on the experimental tests carried
out on a GTC prototype installed in a geothermal well on the island of Isc
hia. The GTC prototype comprises a tube bundle with a central feeding pipe
as the evaporator, and a conventional shell-and-tube type condenser with co
oling water flow inside the tubes. The evaporator and condenser are connect
ed using flexible ducts. The GTC is equipped with an annular convection pro
moter. This paper describes the prototype, the experimental plant and the t
ests carried out on the experimental apparatus, and reports the results, th
ereby illustrating the device performance. The experimental tests indicate
that there is a limit to the heat obtained by the GTC; this limit arises fr
om the thermal and fluid dynamic interaction between the well and the aquif
er. In particular, the heat flow is due to a short-circuit effect in the aq
uifer between cold and warm fluids, respectively, leaving and entering the
well. An estimate of this short-circuit effect for the Ischia aquifer is ob
tained from the two-dimensional (2D) thermal and flow fields determined usi
ng the Finite Element Method. (C) 1998 Elsevier Science Ltd. All rights res
erved.