A method of measuring the calcium oxalate scale forming propensity of a continuously flowing solution having a pH of from about 2 to about 3 comprising measuring the rate of deposition of calcium oxalate scale from the solution on to a quartz crystal microbalance having a top side comprising a working electrode in contact with the solution and a second, bottom side isolated from the solution, wherein the pH of the solution proximate to the microbalance is controlled electrochemically at from about 3.5 to about 9, wherein the working electrode is coated with or made of a conductive material on which the evolution of hydrogen gas does not interfere with the deposition of calcium oxalate onto the surface of the working electrode at the electrochemical polarization necessary to achieve a pH of 3.5-9 proximate to the microbalance and wherein the pH of the solution proximate to the surface of the microbalance is measured using a surface pH measuring module comprising a mesh electrode laid over a pH electrode wherein the mesh is made of the same material as the working electrode.