Abstract
The inherent erodibility of twenty soils was indexed using Middleton's dispersion ratio and Anderson's surface-aggregation ratio. These indices were then used as dependent variables for several regression analyses. The milliequivalents per 100 grams of oven-dried soil for the four most plentiful soil cations (Ca, Mg, K, and Na) were determined and then used as independent variables in the regressions. The best fit to the data was found to be an equation of the type: Both the linear and the curvilinear terms were significant at the arbitrarily selected 5 per cent level.
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.
