| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4573973 | Geoderma | 2012 | 11 Pages |
Abstract
⺠In complex soils, δ13C methods cannot be used alone to assess the origin of carbonates. ⺠L104 and amount of impurities give information about carbonates formation environment. ⺠Micromorphology and N2 adsorption analysis allow observing pedogenic carbonates.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Marcella Catoni, Gloria Falsone, Eleonora Bonifacio,