To assess the extent of water flow through channels in the membranes of intact higher plant cells, the effects of HgCl 2 on hydraulic conductivity (L P ) of wheat (Triticum aestivum L.) root cells were investigated using a pressure probe. The L P of root cells was reduced by 75% in the presence of 100 M HgCl 2 . The K ؉ -channel blocker tetraethylammonium had no effect on the L P at concentrations that normally block K ؉ channels. HgCl 2 rapidly depolarized the membrane potential (V m ) of the root cells. The dose-response relationship of inhibition of L P and depolarization of V m were not significantly different, with half-maximal inhibition occurring at 4.6 and 7.8 M, respectively. The inhibition of L P and the depolarization of V m caused by HgCl 2 were partially reversed by -mercaptoethanol. The inhibition of L P by HgCl 2 was similar in magnitude to that caused by hypoxia, and the addition of HgCl 2 to hypoxia-treated cells did not result in further inhibition. We compared the L P of intact cells with that predicted from a model of cortical cells incorporating water flow across both the plasma membrane and the tonoplast using measured values of water permeability from isolated membranes, and found that HgCl 2 has other effects in addition to the direct inhibition of water channels.The cloning and functional expression of aquaporins from higher plants (Maurel et al., 1993(Maurel et al., , 1997a Daniels et al., 1994 Daniels et al., , 1996 Kammerloher et al., 1994;Yamada et al., 1997;Weig et al., 1997; Chaumont et al., 1998; Johansson et al., 1998) has indicated that water flow across intact higher plant membranes could be predominantly through aquaporins. The biophysical evidence for this in higher plants has lagged behind the molecular work, but recent studies have shown that biophysical characteristics of water transport are consistent with water flow occurring predominantly through channels in some membranes. This evidence includes the following: (a) the ratio of osmotic to diffusional water permeability is greater than unity (Niemietz and Tyerman, 1997); (b) the activation energy is low (Maurel et al., 1997b; Niemietz and Tyerman, 1997); and (c) water permeability is sensitive to sulfhydryl reagents, in particular HgCl 2 (Maurel et al., 1997b; Niemietz and Tyerman, 1997).In the membranes of intact giant charophyte cells, high diffusional water permeability, low activation energy, and inhibition by sulfhydryl reagents have been well established (Wayne and Tazawa, 1990;Henzler and Steudle, 1995;Steudle and Henzler, 1995;Tazawa et al., 1996; Schü tz and Tyerman, 1997). The frictional interactions between the transport of water and highly permeant molecules (Tyerman and Steudle, 1982;Steudle and Henzler, 1995; Hertel and Steudle, 1997) are also indicative of water movement through aqueous pores in the membranes of characean cells.Inhibition by mercurials of water flow through most (Maurel, 1997;Tyerman et al., 1999) but not all (Daniels et al., 1994) aquaporins has prompted experiments testing th...