SPRINGS SEEN AND INTERPRETED IN THE CONTEXT OF GROUNDWATER FLOW-SYTEMS
In keeping with this past, the present paper seeks to explore the possibility of a further application of the concept. According to the proposed thesis, springs are but one member of a community of various groundwater discharge-features, the "virtual spring", which occur at the terminal ends of groundwater flow-systems. Because all the other discharge indicators also bear imprints of subsurface conditions existing within the boundaries of the systems’ flow-path volume, together, i.e., in synergy with the springs, they provide more information than springs could do alone.
Some possible results of interpreting “springs” in the context of groundwater flow-systems are exemplified by: explaining the types and concentrations of environmental isotopes in the Montecatini Terme thermal-springs, Italy; evaluating ecohydrological effects of planned land drainage, Grote-Nete basin, Belgium; advancing a new theory of hypogenic karst formation; understanding thermal-karst processes that may produce hydrocarbon reservoirs in carbonates, Hungary; solving the riddle of large differences in 238U, 226Ra and 222Rn contents in the waters of closely spaced springs, St. Placidus, Switzerland; and, mitigating the 200-year old danger posed by the Campo Vallemaggia landslide, Swiss Alps.