Classification of Wetlands and Deepwater Habitats of the United States
Appendix D
Criteria for Distinguishing Organic
Soils from Mineral Soils
The criteria for distinguishing organic soils from mineral soils
in the United States (U.S. Soil Conservation Service, Soil Survey
Staff 1975:13-14, 65) are quoted here so that those without ready
access to a copy of the Soil Taxonomy may employ this information
in the classification of wetlands:
For purposes of taxonomy, it is necessary, first, to define the
limits that distinguish mineral soil material from organic soil
material and, second, to define the minimum part of a soil that
should be mineral if the soil is to be classified as a mineral
soil.
Nearly all soils contain more than traces of both mineral and
organic components in some horizons, but most soils are
dominantly one or the other. The horizons that are less than
about 20 to 35 percent organic matter by weight have properties
that are more nearly those of mineral than of organic soils. Even
with this separation, the volume of organic matter at the upper
limit exceeds that of the mineral material in the fine-earth
fraction.
MINERAL SOIL MATERIAL
Mineral soil material either
- Is never saturated with water for more than a few days and
has <20 percent organic carbon by weight; or
- Is saturated with water for long periods or has been
artificially drained, and has
- Less than 18 percent organic carbon by weight if 60 percent
or more of the mineral fraction is clay;
- Less than 12 percent organic carbon by weight if the mineral
fraction has no clay; or
- A proportional content of organic cabon between 12 and 18
percent if the clay content of the mineral fraction is between
zero and 60 percent.
Soil material that has more organic carbon than the
amounts just given is considered to be organic material.
DISTINCTION BETWEEN MINERAL SOILS AND ORGANIC SOILS
Most soils are dominantly mineral material, but many
mineral soils have horizons of organic material. For simplicity in
writing definitions of taxa, a distinction between what is meant
by a mineral soil and an organic soil is useful. In a mineral
soil, the depth of each horizon is measured from the top of the
first horizon of mineral material. In an organic soil, the depth
of each horizon is measured from the base of the aerial parts of
the growing plants or, if there is no continuous plant cover from
the surface of the layer of organic materials. To apply the
definitions of many taxa, therefore, one must first decide whether
the soil is mineral or organic.
If a soil has both organic and mineral horizons, the relative
thickness of the organic and the mineral soil materials must be
considered. At some point one must decide that the mineral
horizons are more important. This point is arbitrary and depends
in part on the nature of the materials. A thick layer of sphagnum
has a very low bulk density and contains less organic matter than
a thinner layer of well-decomposed muck. It is much easier to measure
thickness of layers in the field than it is to determine tons of
organic matter per hectare. The definition of a mineral soil, therefore,
is based on thickness of the horizons or layers, but the limits of
thickness must vary with the kinds of materials. The definition that
follows is intended to classify as mineral soils those that have no
more organic material than the amount permitted in the histic epipedon,
which is defined later in this chapter.
To determine whether a soil is organic or mineral, the thickness
of horizons is measured from the surface of the soil whether that
is the surface of a mineral or an organic horizon. Thus, any 0
horizon at the surface is considered an organic horizon, if it
meets the requirements of organic soil material as defined later,
and its thickness is added to that of any other organic horizons
to determine the total thickness of organic soil materials.
DEFINITION OF MINERAL SOILS
Mineral soils, in this taxonomy, are soils that meet one of the
following requirements:
- Mineral soil material <2 mm in diameter (the fine-earth
fraction) makes up more than half the thickness of the upper 80
cm (31 in.);
- The depth to bedrock is <40 cm and the layer or layers of
mineral soil directly above the rock either are 10 cm or more
thick or have half or more of the thickness of the overlying
organic soil material; or
- The depth to bedrock is >40 cm, the mineral soil material
immediately above the bedrock is 10 cm or more thick, and either
- Organic soil material is <40 cm thick and is decomposed
(consisting of hemic or sapric materials as defined later) or
has a bulk density of 0.1 or more; or
- Organic soil material is <60 cm thick and either is
undecomposed sphagnum or moss fibers or has a bulk density that
is <0.1.
ORGANIC SOIL MATERIALS
Organic soil materials and organic soils
- Are saturated with water for long periods or are artificially
drained and, excluding live roots, (a) have 18 percent or more
organic carbon if the mineral fraction is 60 percent or more clay,
(b) have 12 percent or more organic carbon if the mineral fraction
has no clay, or (c) have a proportional content of organic carbon
between 12 and 18 percent if the clay content of the mineral
fraction is between zero and 60 percent; or
- Are never saturated with water for more than a few days and
have 20 percent or more organic carbon.
Item 1 in this definition covers materials that have been called
peats and mucks. Item 2 is intended to include what has been
called litter or 0 horizons. Not all organic soil materials
accumulate in or under water. Leaf litter may rest on a lithic
contact and support a forest. The only soil in this situation is
organic in the sense that the mineral fraction is
appreciably less than half the weight and is only a small
percentage of the volume of the soil.
DEFINITION OF ORGANIC SOILS
Organic soils (Histosols) are soils that
- Have organic soil materials that extend from the surface to one
of the following:
- A depth within 10 cm or less of a lithic or paralithic
contact, provided the thickness of the organic soil materials is
more than twice that of the mineral soil above the contact; or
- Any depth if the organic soil material rests on fragmental
material (gravel, stones, cobbles) and the interstices are filled
with organic materials, or rests on a lithic or paralithic
contact; or
- Have organic materials that have an upper boundary
within 40 cm of the surface and
- Have one of the following thicknesses:
- 60 cm or more if three-fourths or more of the volume is moss
fibers or the moist bulk density is <0.1 g per cubic centimeter
(6.25 lbs per cubic foot);
- 40 cm or more if
- The organic soil material is saturated with water for long
periods (>6 months) or is artificially drained; and
- The organic material consists of sapric or hemic materials
or consists of fibric materials that are less than three-fourths
moss fibers by volume and have a moist bulk density of 0.1 or
more; and
- Have organic soil materials that
- Do not have a mineral layer as much as 40 cm thick either at
the surface or whose upper boundary is within a depth of 40 cm
from the surface; and
- Do not have mineral layers, taken cumulatively, as thick as
40 cm within the upper 80 cm.
It is a general rule that a soil is classed as an organic soil
(Histosol) either if more than half of the upper 80 cm (32 in.)
[sic] of soil is organic or if organic soil material of any
thickness rests on rock or on fragmental material having
interstices filled with organic materials.
Soils that do not satisfy the criteria for classification as
organic soils are mineral soils.
Previous Section -- Appendix C
Return to Contents
Next Section -- Appendix E