Abstract
Abstract A study has been made of the effect of rapid pH change upon the absorption of zinc by six soils with diverse organic matter contents. At pH values more than one pH unit above the soil pH, organic matter and zinc in soil solution increased considerably. Addition of calcium caused reprecipitation of organic matter and zinc, suggesting that zinc at high pH is primarily absorbed on organic matter where it is selectively retained as an organic complex.
Sign-in/Register to access full text options 
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 callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
