Abstract
Greenlandic glacial rock flour (GRF) is a potential source of extremely fine-grained silicate minerals for CO2 uptake via enhanced rock weathering. The chemical makeup of this material also indicates that it may be a good source of plant nutrients. GRF was applied at rates of 10 (GRF10) and 50 (GRF50) t ha−1 to a low-fertility sandy clay loam in Ghana to evaluate its impact on maize production relative to a control over five consecutive growing seasons. Other soil amendments, including N fertilizers, were uniformly applied across all treatments. GRF50 significantly increased grain and total dry matter yield (TDMY) across all five seasons. Seasonal increases in TDMY with GRF50 ranged from 28–87% relative to the control, and grain yield increases ranged from 28–77%. In total over the course of the five growing seasons, GRF50 produced an additional 12.9 t ha⁻1 of TDMY and 7.6 t ha⁻1 of grain relative to the control. GRF10 had a significant effect on TDMY and grain yield in the first two growing seasons, though the effect of GRF10 decreased over time and by the fifth growing season TDMY and grain yield were equivalent to the control. Nonetheless, the application of this lower amount of GRF still resulted in an additional 7.4 t ha⁻1 of TDMY and 4.5 t ha⁻1 of grain yield over the course of the experiment. These results suggest that the significant co-benefits of GRF as a fertilizer may incentivize the adoption of enhanced rock weathering in tropical, nutrient-poor environments and could increase food security in such regions.
| Original language | English |
|---|---|
| Pages (from-to) | 761-772 |
| Number of pages | 12 |
| Journal | Nutrient Cycling in Agroecosystems |
| Volume | 131 |
| Issue number | 3 |
| DOIs | |
| Publication status | Published - Dec 2025 |
Keywords
- CDR
- Enhanced rock weathering
- Glacial rock flour
- Rock dust
- Silicate minerals
- Soil remineralization