“…If the reference electrode exhibits constant potential independent of the solution composition, changes in E as a function of pH, ionic strength, electrolyte composition, and adsorbate concentration arise from reactions at the mineral/solution interface. Multiple planes of charge can be specified that dictate the total potential drop across this interface, including the space charge layer in the mineral surface, the Helmholtz layer, and the diffuse layer in solution (as opposed to just the latter two for insulators) (Garrett and Brattain, 1955;Morrison, 1980;Natarajan et al, 1998). As will be discussed below, for conditions where the voltage drops across two of the three layers are understood, the third can be directly determined.…”