Abstract
Soil-water diffusivity values of a sandy loam soil, measured by Bruce and Klute's and Gardner's methods, were compared with those calculated from the moisture-suction relationship. The measured values of diffusivity were significantly correlated with calculated values of diffusivity. Bruce and Klute's method overestimated diffusivity values at different moisture contents compared with those calculated from the moisture-suction relationship. Diffusivity values measured by Gardner's method and those calculated were almost identical.
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.
