Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
8873218 | Geoderma Regional | 2018 | 14 Pages |
Abstract
From soil sampling, clear differences in carbon stocks to 30â¯cm were observed when comparing the stocks measured at sites from both countries. In New Zealand, soil carbon stocks were estimated to be as high as 101â¯t/ha for the top 30â¯cm of soil. For the Australian sites which were all situated in the Hunter Valley region of NSW, the highest measured soil carbon stocks were 25â¯t/ha for the top 30â¯cm. The largest soil carbon variance was observed at the New Zealand hill country farm, where the landscape consists of alluvial terraces, complex broken valley sides and a summit plateau mantled with volcanic ash. In Australia, the presence of subsoil pedogenic carbonate (marl) contributed to high variance estimates relative to the other sites.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Brendan Malone, Carolyn Hedley, Pierre Roudier, Budiman Minasny, Edward Jones, Alex McBratney,