Chloridometers are used to measure Cl– ions in plant tissues. This instrument titrates the Cl– with Ag+ released from a silver wire. It works as follows: Ag+ is released at a constant rate as current is passed between a pair of silver generator electrodes. Cl– in the sample solution precipitates with the generated Ag+ as AgCl. After all the Cl– in the sample has precipitated there is a steady increase in Ag+ in solution. This results in an increasing current through a pair of silver indicator electrodes. When an increase in an indicator current is detected, a relay is activated, and a timer is automatically stopped (the timer runs concurrently with Ag+ generation – amperometric indication). Since the rate of generation of Ag+ is constant, the amount of Cl– precipitated from the sample is proportional to the elapsed time. Therefore, solutions with higher quantities of Cl– take a longer time to reach the end-point, and Cl– is quantified by making a standard curve to relate time to known concentrations of Cl– in standard solutions.