Showing papers by "Marco Canepa published in 2001"

TL;DR: In this article, irreversible water-rock mass transfer accompanying the generation of the Bisagno valley groundwaters, starting from local rainwaters, was simulated through reaction path modeling in reaction progress mode, and the simulations assumed bulk dissolution of local stream sediments (i.e. without any constraint on their mineralogy and on the dissolution rates of primary solid phases) and precipitation of chalcedony, illite, a smectite solid mixture, a hydroxide solid mixture.