“…They have also been used to delineate catchment areas [ 6 ] and study groundwater trajectories and active conduit networks in karst aquifers and caves [ 7 , 8 ]. Furthermore, they have been used to evaluate pipe flow [ 9 ], investigate leaks from reservoirs [ 10 ], and examine the behavior of contaminants (e.g., pesticides) in surface water [ 11 , 12 ]. Recently, fluorescent dyes have been used as tracers to distinguish between drilling fluid and on-site groundwater in deep subsurface borehole drilling [ 3 , [13] , [14] , [15] , [16] , [17] , [18] ], and as non-adsorbable tracers to compare with the behavior of adsorbable tracers in borehole-based solute transport tests [ 19 , 20 ].…”