“…The van't Hoff law says that in a dilute solution, the osmotic pressure in Pa, P os , is proportional to the A c c e p t e d M a n u s c r i p t 9 temperature in Kelvin, T, and the concentration of the solute in mole, c solute , and R is the ideal gas constant (R= 8.314 J⋅mol −1 ⋅K −1 ). To influence osmosis, the plant can thus modify the flux of ions (in particular potassium and chloride) (Blatt, 2000;Hedrich, 2012;Wang et al, 2017) and make changes in metabolism to alter osmotic compound concentrations (Argiolas et al, 2016) or modify the permeability of the membrane for water through aquaporin gating (Törnroth-Horsefield et al, 2006;Alleva et al, 2012;Maurel et al, 2015;Rodrigues et al, 2017). Brownian motion and diffusion of water and solute will, of course, take place in both chambers but the case against osmosis being driven by diffusion of solvent down a presumed water concentration gradient is nearly sealed, despite occasional counter-arguments leaking through (Nelson, 2017).…”