Abstract

Abstract Exchangeable acidity of soils has previously been measured by titration of soil extracts to a phenolphthalein endpoint at pH 8.3. The use of standard hydrogen and aluminium solutions indicates that this is inaccurate and a preferred technique, differential potentiometric titration is proposed.

Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call