| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4436477 | Applied Geochemistry | 2011 | 4 Pages |
The contribution of individual grain size fractions (2000–500, 500–250, 250–63, 63–2 and < 2 μm) to bulk soil surface area and reactivity is discussed with reference to mineralogical and oxalate and dithionite extractions data. The 63–2 μm fraction contributed up to 56% and 67% of bulk soil volume and BET surface area, respectively. Consideration of these observations and the mineralogy of this fraction suggest that the 63–2 μm fraction may be the most influential for the release of elements via mineral dissolution in the bulk soil.
► Contribution of grain size fractions to bulk soil surface area and reactivity. ► Influence of amorphous and free Fe oxides phases on soil surface area. ► 63–2 μm fraction may be the most influential for soil elemental release rates.
