The Unrealized Potential — Soil Organic Carbon (SOC) layer quantifies the additional carbon that could accumulate in the top 30 cm of soil if the land were restored to native vegetation cover, expressed in tC/ha. Soil carbon accumulation occurs through increased organic matter inputs from root turnover, leaf litter, and microbial biomass under restored vegetation.
Unlike biomass carbon that can be gained relatively quickly through tree growth, soil carbon accumulation is a slow process spanning decades to centuries. However, SOC gains are more permanent — once built up, soil carbon persists longer than above-ground biomass carbon, which is vulnerable to fire, storms, and logging.
SOC unrealized potential is particularly high in:
Output unit: tC/ha (additional SOC achievable in top 30 cm)
| Code | Name | Provider | Type | Coverage | Resolution | Reference Year |
|---|---|---|---|---|---|---|
| Walker 2022 | Unrealized Potential (SOC) | Walker et al. / S3 | Raster (COG) | Global | ~300 m | 2016 |
COPERNICUS/S2_SR_HARMONIZED | Sentinel-2 L2A | ESA/Copernicus | Multispectral | Global | 10 m | 2017 — present |
GOOGLE/DYNAMICWORLD/V1 | Dynamic World | Google/WRI | Land cover | Global | 10 m | 2015 — present |
USGS/SRTMGL1_003 | SRTM DEM | NASA/USGS | Elevation | 60N-56S | 30 m | 2000 |
| Indicator | Unit | Range | Inverted |
|---|---|---|---|
carbon_stock_unrealized_potential_soc | tC/ha | [0, 5, 15, 40, 80, 150] | No |
| Level | Thresholds | Interpretation |
|---|---|---|
| E (Very Low) | < 5 tC/ha | Soil near natural SOC capacity |
| D (Low) | 5-15 tC/ha | Minor SOC gain possible through improved management |
| C (Moderate) | 15-40 tC/ha | Significant SOC buildup achievable |
| B (High) | 40-80 tC/ha | Heavily depleted soils with high restoration potential |
| A (Very High) | > 80 tC/ha | Severely degraded soils — maximum SOC recovery potential |
Il layer Potenziale Non Realizzato - SOC quantifica il carbonio aggiuntivo che potrebbe accumularsi nei primi 30 cm di suolo se il terreno fosse ripristinato alla copertura vegetale nativa, secondo Walker et al. (2022). L'accumulo di SOC avviene attraverso l'aumento degli apporti di materia organica da turnover radicale, lettiera e biomassa microbica. Il processo e lento (decenni-secoli) ma i guadagni sono piu permanenti del carbonio della biomassa. Il raster viene raffinato tramite Random Forest con NDVI, copertura del suolo ed elevazione. Suoli agricoli degradati e aree deforestate mostrano il potenziale SOC piu elevato. Output in tC/ha.