0-28
28-61
61-84
Zaragosa Series
| Soil Fertility | High |
|---|---|
| Soil pH | Neutral (6.5-7.5) |
| Organic Matter | Low |
| Phosphorus (P) | Moderate to high |
| Potassium (K) | Moderate |
| Nutrient Retention | High |
| Base Saturation | High |
| Salinity Hazard | None |
| Physical Soil Quality | |
|---|---|
| Relief | Level to nearly level |
| Water Retention | High |
| Drainage | Very poor |
| Permeability | Slow |
| Workability/Tilth | Hard |
| Stoniness | Few to common concretions |
| Rooting Depth | Deep (>1m) |
| Flooding | Seasonal |
| Erosion |
Surface Soil Type: Clay
Family name: Fine, smectitc (ca.), isohyperthermic, Vertic Epiaquept
Fine textured soil with moderate amount of clay 18 35 and isohyperthermic temperature regime 22C It is in the incipient development stage toward mature soil but has not fully developed its diagnostic horizons Inceptisol ept It is saturated with water for repeated periods of time aqu manifested by its grayish color with or without mottles This is a representative of the great group Epiaquepts that is dominated by clays that shrink and swell producing wide cracks and slickensides due to repeated wetting and drying vertic