Field classification of Vertosols and Sodosols in Australia involves the ca
lculation of an exchangeable sodium percentage (ESP) of the subsoil to esti
mate sodicity. ESP has historically been determined by laboratory measureme
nt of the cation exchange capacity (CEC) and exchangeable sodium. This ofte
n leads to a delay in field classification and mapping and missed extension
opportunities with landholders. Recently, ion-specific electrode field met
ers have been developed that allow the determination of the sodium ion conc
entration within a soil solution. If field tests and/or calculation can est
imate clay percentage and sodium concentration, there is potential for rapi
d field assessment of ESP. The field meter accurately predicted exchangeabl
e sodium (R-2=0.83). In addition CEC was related to clay percentage (R-2=0.
79). The estimated ESP calculated by the field tests compared favourably wi
th the actual ESP measurement (R-2=0.85).