Delineation
Program
Hydric Soils In Florida: Fact Sheet
- Definition: Hydric
soils are those soils that are saturated, flooded,
or ponded long enough during the growing season for
the development of anaerobic conditions in the
topsoil. The anaerobic conditions in a hydric soil
favor the growth and regeneration of hydrophytic
vegetation.
- Hydric soils include all of the
very poorly drained and some of the poorly drained soils.
- Generally, in sandy textured
soils, the hydric soil indicators must be within 6 inches of the
soil surface.
- Generally in loamy and clayey
textured soils, the hydric soil indicators must be within 12 inches
of the soil surface.
- The presence of just one hydric
soil indicator within the appropriate depth is enough evidence for a
soil to be called hydric. Hydric soils must be verified in the
field.
- The hydric soil indicators used in
Florida were developed by the Soil Conservation Service (now known
as the NRCS, Natural Resources Conservation Service) specifically
for Florida.
- A detailed description of the hydric soil indicators developed for Florida is provided in Soil
and Water Relationships of Florida's Ecological Communities, FL-SCS,
1992, second edition.
- Chapter 62-340, F.A.C.,
Delineation
of the Landward Extent of Wetlands and Surface Waters (1994)
cites the above publication for the description and use of hydric
soil indicators.
- According to the NRCS, 4 hydric
soil indicators indicate a water table at or above the soil surface.
These 4 indicators can also be used as hydrologic indicators for the
Florida Wetland Delineation (62-340.500(8)).
The indicators are:
- Muck
- Mucky Texture
- Gley Color
- Sulfidic Smell
- The following hydric soil
indicators identify soils with a high water table capable of
providing saturation to the soil surface for extended periods of
time.
| All Soils |
Sandy Soils |
Loamy and Clayey Soils |
| Stratified Layers |
Sandy Redox |
Depleted Matrix |
| Organic Bodies |
Stripped Matrix |
Marl |
|
Dark Surface |
Fe/Mn Masses |
|
Thin Dark Surface |
Umbric Surface |
|
Polyvalue Below Surface |
Thick Dark Surface |
|
|
Redox Dark Surface |
|
|
Depleted Dark Surface |
A complete list of soil map units (by county) that have hydric soils as a principle
component or as an inclusion is in Hydric Soils of Florida Handbook, 1995. Florida
Association of Environmental Soil Scientists (Direct all inquiries to
FAESS, P.O. Box
7025, Gainesville, FL. 32605, or call V.M. Carlisle (904-376-5079)