... CATE simultaneously provides information not only about influx, but also about multiple other fluxes (efflux, net flux, and flux to the xylem), as well as kinetic constants of exchange, and subcellular compartmentation, of the traced ion. CATE has been used extensively to investigate a wide range of plant processes, including: ion fluxes and compartmentation across membranes for K + , NH 4 + , Na + , NO 3 -, and Cl - (Cram, 1968;Pallaghy and Scott, 1969;Macklon and Higinbotham, 1970;Pierce and Higinbotham, 1970;Pitman, 1971;Macklon, 1975;Behl and Jeschke, 1982;Jeschke, 1982;Mills et al., 1985;Lee and Clarkson, 1986;Siddiqi et al., 1991;Kronzucker et al., 1995a, b, c, d;Min et al., 1999;Britto et al., 2001Britto et al., , 2002Britto et al., , 2004Kronzucker et al., 2003b;Ritchie, 2006); salinity stress (Hajibagheri et al., 1988); stomatal function (MacRobbie, 1981(MacRobbie, , 1995; forest succession (Kronzucker et al., 1997(Kronzucker et al., , 2003a; metal tolerance (Lasat et al., 1998(Lasat et al., , 2000Zhu et al., 2000;Pedas et al., 2005); synergistic effects of mineral nutrition (Kronzucker et al., 1999); action of hormones (Hellwege and Hartung, 1997;Jovanovic et al., 2000); and compartmentation of herbicides (DiTomaso et al., 1993;Lasat et al., 1997). ...