| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 8894266 | Geoderma | 2018 | 10 Pages |
Abstract
- A high degree of multicollinearity existed between many of the physiochemical parameters
- Poorly-crystalline iron (Feo) and pH were consistently strong driver of net N mineralization rate.
- The influence of Feo and pH exceeded total C and climatic variables, but was less than total N.
- The inclusion of pedogenic iron fractions improved explained variance over models without iron.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Jordon Wade, Hannah Waterhouse, Leslie M. Roche, William R. Horwath,