About Hydric Soils
What is a Hydric Soil?
"A hydric soil is a soil that formed under
conditions of saturation, flooding, or ponding long enough during the growing season to
develop anaerobic conditions in the upper part." (Federal Register, July 13, 1994) A
hydric soil is a soil that meets this definition.
What are Hydric Soil Criteria?
Hydric soil criteria are used to generate Hydric Soils
Lists based on estimated soil properties. There are four types of criterion:
- All Histosols except Folists
- Soils that have a seasonally high water table during the
growing season.
- Soils that are frequently ponded for long or very long
duration during the growing season.
- Soils that are frequently flooded for long or very long
duration during the growing season.
What are Hydric Soils Lists?
Hydric Soils Lists contain soils or soil map unit
components that have a probability of being hydric. The Hydric status of a soil is an
interpretation made by comparing its estimated soil properties with the Hydric Soil
Criteria. A soil that is identified as hydric on a list must be confirmed in the field as
meeting the Hydric Soil Definition through the use of hydric soil field indicators and/or
best professional judgment.
What are Hydric Soil Field Indicators?
Hydric Soil Field Indicators are soil profile features
used to identify and delineate hydric soils in the field. Presence and documentation of a
field indicator confirms that a soil meets the Hydric definition. These field indicators
are contained in the USDA-NRCS publication Field
Indicators of Hydric Soils.
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