Poorly-Drained Silty Gley
Silt Loam · Alluvial floodplain or depressional wetland deposit. Likely found in low-lying areas of temperate river valleys.

AI Disclaimer
This soil report was produced by AI from a single photo. Treat it as a starting point, not laboratory truth.
pH, drainage, fertility, and composition are visual estimates — send a sample to an accredited lab before any decision that would be painful to get wrong.
Crop and amendment tips are general guidance — local climate, microclimate, and gardening history always win over an AI's best guess.
pH
Slightly acidic to neutral (6.0–7.0). Anaerobic conditions often stabilize pH near neutral, though localized organic decomposition can lower it.
Drainage
Poorly Drained. The lack of bright red or yellow iron oxides indicates the profile is saturated for significant portions of the year.
Organic Matter
Moderate (3–5%). The dark value suggests accumulated carbon, though decomposition is slowed by anaerobic conditions.
Erosion Risk
Moderate water erosion risk. Silt-heavy soils are highly transportable by surface runoff if not protected by cover crops.
Overall Read
This is a challenging, heavy soil defined by its wetness. While naturally fertile, its physical limitations require specific plant selection or engineering (drainage) to be productive.
Texture
Fine and smooth; likely a powdery feel when dry and slippery/non-sticky when wet. Expected behavior in a ribbon test would be a weak ribbon less than 2.5cm due to high silt content.
Color Analysis
Dark bluish-gray (GLEY1 4/1). The grayish hue suggests gleying, a process occurring in waterlogged conditions where iron is reduced due to lack of oxygen.
Estimated Composition
60% Silt, 25% Clay, 10% Sand, 5% Organic Matter. Estimated with low confidence due to image blur.
Water Retention
High water retention. The fine particle size effectively holds moisture, but may lack plant-available oxygen when saturated.
Aeration
Poor Aeration. Evidence of gleying indicates chronic oxygen deficiency, which can lead to the production of methane or hydrogen sulfide.
Compaction Level
Moderately firm. Fine-textured saturated soils are highly susceptible to compaction from foot or wheel traffic.
Structure & Aggregation
Massive or Platy structure. Lack of visible granular aggregates suggests low pore space and potential for high density.
Fertility Indicators
Moderate Fertility. While mineral content is likely high, nutrient availability (especially Phosphorus) may be limited by wetness and low microbial activity.
Climate Suitability
Humid temperate or maritime climates. Requires management to handle excess water during spring thaw or heavy rain events.
Crops Worth Trying
Willows, Sedges, Elderberry, and water-tolerant grasses. For agriculture, Rice or moisture-tolerant forage like Timothy grass.
Plants To Avoid
Lavender, Rosemary, Succulents, and Mediterranean herbs which require 'dry feet' and high drainage.
Home Garden Use
Best suited for rain gardens or bog gardens. Not recommended for standard in-ground vegetable beds without significant drainage installation.
Agricultural Use
Suitable for seasonal grazing or specialized hydrophilic crops. Often requires tile drainage for traditional row-crop production.
Landscaping Use
Ideal for storm-water retention basins and naturalized riparian edging to prevent runoff into waterways.
Common Problems
Root rot (Phytophthora), lack of oxygen for root respiration, and delayed planting due to slow warming in spring.
Amendments Needed
Incorporate coarse organic matter (wood chips or straw) to improve macropores; apply garden lime only if a test confirms high acidity.
Try These At Home Tests
Perform a 'Smell Test': a sour or rotten egg smell confirms anaerobic conditions. A 'Jar Test' will likely show a thick layer of suspended silt.
Professional Lab Recommendation
Request a Comprehensive Soil Health test including bulk density and Cation Exchange Capacity (CEC) to manage nutrient loading. Costs typically $25-$50.
Fun Facts
Gleyed soils are often used by geologists to map ancient wetlands and historical flood patterns because the gray color persists long after the water recedes.