Soil


Introduction
Soil is the only contact most plants and animals have with the earth.  The type of soil found in a region greatly influences plant growth, so it is most relevant to farmers and gardeners.  In addition, some soils are prone to erosion, which can affect the water quality of an area.  The depth, richness, and chemical composition of soil is also very important to native plants as well as to the assortment of small vertebrates and invertebrates which call the soil home.

The majority of soil is made up of weathered rock, so the type of bedrock influences the overlying soil to a large extent.  We have discussed geology and its effect on the chemical composition of Wortroot's soil in a previous section. 

In addition to weathered rock, soil contains decayed plants and animals which add organic matter to the soil.  In our forest habitats, decayed tree leaves make up the bulk of the soil's organic matter.  As a forest ages, more and more organic matter builds up, resulting in deeper, richer, and damper soil.  However, the type of overlying plant community also influences the growth of the soil layer.  Oak and beech leaves tend to decay slowly, so soil beneath these tree species is often poorer and thinner than would be expected due to the age of the forest.  Conifers, such as pines, typically have acidic leaves (needles) which change the chemical composition of the soil. 

Not all soils are created by the rocks and trees below and above them.  Some soils, known as alluvial soils, are carried from the surrounding hills and deposited in valley bottoms.  These soils often contain a mixture of different soil types and are unrelated to the rock found beneath them.  Alluvial soils tend to contain a large amount of organic matter, and thus can provide rich farmland. 


Wortroot Soil Map
The map below shows the soil types found at Wortroot. 

Soil map.


The black letters on the map refer to soil types, each of which is listed in the table below.

Map Symbol
Soil
Slope Range
Internal drainage
Parent Material
Color of subsoil
General productivity
Land class
A
Alluvial soils, undifferentiated
0-3
Medium to slow


Medium to moderately high
Fourth
Dse
Dunmore silty clay loam, eroded steep phase
30-60
Medium
Residual material from weathered limestone
Yellowish brown or faintly reddish brown
Medium
Fourth
Dst
Dunmore silty clay loam, eroded hilly phase
15-30
Medium
Residual material from weathered limestone
Yellowish brown or faintly reddish brown
Medium to moderately high
Third
Gs
Greendale silt loam
0-5
Medium
Local wash mainly from Elliber, Clarksville, Dandridge, Lodi, and Westmoreland soils
Brownish yellow, light brownish yellow, or yellow
Moderately high
Second
Hcr
Hagerstown silty clay loam, eroded phase
3-15
Medium
Residual material from weathered limestone
Reddish brown to brownish red
High
First
Ht
Hagerstown stony silt loam
3-15
Medium
Residual material from weathered limestone
Reddish brown to brownish red
Moderately high
Fourth
Htz
Hagerstown stony silt loam, steep phase
15-60
Medium
Residual material from weathered limestone
Reddish brown to brownish red
Medium
Fourth
Me
Melvin silt loam
0-3
Very slow
Alluvium from uplands underlain mainly by limestone
Gray, spotted with brown or rust brown
Medium
Fourth
RoL
Rolling stony land (limestone material)
3-30
Medium to slow


Medium to moderately high
Fourth
RsL
Rough stony land, limestone material
30-60+



Moderately low
Fifth
TLe
Teas-Litz silt loam, eroded steep phase
30-60
Medium
Residual material from weathered shale and some limestone and sandstone
Purplish brown, dark purplish brown, or purplish red (Teas); light brown or yellowish brown (Litz)
Moderately low
Fourth
TLr
Teas-Litz silt loam, eroded phase
15-30
Medium
Residual material from weathered shale and some limestone and sandstone
Purplish brown, dark purplish brown, or purplish red (Teas); light brown or yellowish brown (Litz)
Moderately low to low
Fourth
TLv
Teas-Litz silt loam, very steep phase
60+
Medium
Residual material from weathered shale and some limestone and sandstone
Purplish brown, dark purplish brown, or purplish red (Teas); light brown or yellowish brown (Litz)
Moderately low to low
Fifth


A few symbols can also be found on the map.  A diamond divided by a vertical line denotes a depression which is easy to cultivate across.  A circle denotes a spring, while a small "v" denotes a rock outcrop. 


Implications For Farming

Soil maps are most useful in determining which areas to use for agriculture.  Each soil type is classified, ranging from first class soils which are good for both crops and pasture, to fifth class soils which are poorly suited to any sort of agriculture.  Of the soils found at Wortroot, only Hcr (found on the southwest corner of the property) and Gs (found in a small patch along the road) are well suited for growing crops.  Dst soil, found along Beech Bluff, is rated as poor to fair for crops and poor to good for pasture.  The majority of the rest of the property is suited to pasture, with Middle Cave Ridge and Upper Cave Ridge unsuited to any form of agriculture. 


Erosion
Red letters on the map refer to erosion at the time the survey was completed (in 1951):
S = Moderate sheet erosion
SS = Severe sheet erosion
SG = Moderate sheet and gully erosion
GG = Severe gully erosion

Since that time, the forest has grown up in most regions and has stabilized the soils.  During this inventory, I did not notice erosion at the locations marked on the map.  However, I did see two patches of erosion on extremely steep hillsides - on northwest Middle Cave Ridge and on the west side of Upper Cave Ridge.  The erosion is currently minimal, but any type of disturbance to these areas, such as logging or road-building, would result in an erosion problem. 


Further Study

I did not inventory the small animals found in the soil layer.  In particular, millipedes reach a great diversity in our region and can be used as an indicator of soil depth and health.  A survey of these invertebrates at a later date would be a useful addition to our knowledge of the property. 


Source

United States Department of Agriculture.  1951.  Soil Survey: Scott County, Virginia. 




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Last updated 9/04.