“…Dissolved noble gases have emerged as important geochemical indicators of both continental paleoclimate (Stute et al, 1995;Peeters et al, 2003;Hall et al, 2005) and mass transport in hydrological basins (Price et al, 2003;LaBolle et al, 2006), hydrocarbon reservoirs (Torgersen and Kennedy, 1999;Zhou et al, 2005), lacustrine sediments (Poreda et al, 2004;Brennwald et al, 2005), aquitards (Rü bel et al, 2002;Hendry et al, 2005), engineered clay barriers (Higashihara et al, 2005) and the oceans (Rodehacke et al, 2007). Despite this importance of noble gases in low-temperature geochemistry, remarkably few measurements of noble gas diffusion coefficients in liquid water have been reported.…”