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HomeMy WebLinkAboutSDP201600020 Study 2016-05-06 Soils Report
for
TEXAS ROADHOUSE
Tax Map ID: 06100-00-00-12300
Item Number: SDP201600020
Prepared: May 6, 2016
ALUMULE LOUISA
•
NILSON
Thomas Jefferson Soil & Water Conservation District
"To exercise leadership in promoting natural resource protection. "
706 Forest Street, Suite G
Charlottesville, Virginia 22903
Phone: (434) 975-0224
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Conservation Service National Cooperative Soil Survey Page 1 of 3
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Soil Map—Albemarle County,Virginia Texas Roadhouse
Map Unit Legend
Albemarle County,Virginia(VA003)
Map Unit Symbol Map Unit Name Acres in AOI Percent of AO1
27B Elioak loam,2 to 7 percent 10.3 42.6%
slopes
28C3 Elioak clay loam,7 to 15 percent 0.2 0.7%
slopes,severely eroded
34C Glenelg loam,7 to 15 percent 7.6 31.2%
slopes
34D Glenelg loam,15 to 25 percent 2.5 10.3%
slopes
50D Manor loam,15 to 25 percent 3.2 13.1%
slopes
95 Wehadkee silt loam 0.5 2.1%
Totals for Area of Interest 24.3 100.0%
USDA Natural Resources Web Soil Survey 5/6/2016
s Conservation Service National Cooperative Soil Survey Page 3 of 3
Dwellings and Small Commercial Buildings---Albemarle County,Virginia Texas Roadhouse
Dwellings and Small Commercial Buildings
Soil properties influence the development of building sites, including the selection
of the site,the design of the structure,construction,performance after construction,
and maintenance.This table shows the degree and kind of soil limitations that affect
dwellings and small commercial buildings.
The ratings in the table are both verbal and numerical. Rating class terms indicate
the extent to which the soils are limited by all of the soil features that affect building
site development. Not limited indicates that the soil has features that are very
favorable for the specified use. Good performance and very low maintenance can
be expected. Somewhat limited indicates that the soil has features that are
moderately favorable for the specified use. The limitations can be overcome or
minimized by special planning, design, or installation. Fair performance and
moderate maintenance can be expected. Very limited indicates that the soil has
one or more features that are unfavorable for the specified use. The limitations
generally cannot be overcome without major soil reclamation, special design, or
expensive installation procedures. Poor performance and high maintenance can
be expected.
Numerical ratings in the table indicate the severity of individual limitations. The
ratings are shown as decimal fractions ranging from 0.01 to 1.00. They indicate
gradations between the point at which a soil feature has the greatest negative
impact on the use (1.00) and the point at which the soil feature is not a limitation
(0.00).
Dwellings are single-family houses of three stories or less. For dwellings without
basements, the foundation is assumed to consist of spread footings of reinforced
concrete built on undisturbed soil at a depth of 2 feet or at the depth of maximum
frost penetration, whichever is deeper. For dwellings with basements, the
foundation is assumed to consist of spread footings of reinforced concrete built on
undisturbed soil at a depth of about 7 feet. The ratings for dwellings are based on
the soil properties that affect the capacity of the soil to support a load without
movement and on the properties that affect excavation and construction costs.The
properties that affect the load-supporting capacity include depth to a water table,
ponding, flooding, subsidence, linear extensibility(shrink-swell potential), and
compressibility. Compressibility is inferred from the Unified classification.The
properties that affect the ease and amount of excavation include depth to a water
table, ponding, flooding, slope, depth to bedrock or a cemented pan, hardness of
bedrock or a cemented pan, and the amount and size of rock fragments.
Small commercial buildings are structures that are less than three stories high and
do not have basements. The foundation is assumed to consist of spread footings
of reinforced concrete built on undisturbed soil at a depth of 2 feet or at the depth
of maximum frost penetration, whichever is deeper. The ratings are based on the
soil properties that affect the capacity of the soil to support a load without movement
and on the properties that affect excavation and construction costs.The properties
that affect the load-supporting capacity include depth to a water table, ponding,
flooding, subsidence, linear extensibility(shrink-swell potential), and
compressibility(which is inferred from the Unified classification).The properties that
affect the ease and amount of excavation include flooding, depth to a water table,
ponding, slope, depth to bedrock or a cemented pan, hardness of bedrock or a
cemented pan, and the amount and size of rock fragments.
USDA Natural Resources Web Soil Survey 5/6/2016
Conservation Service National Cooperative Soil Survey Page 1 of 3
Noise
Dwellings and Small Commercial Buildings--Albemarle County,Virginia Texas Roadhouse
Information in this table is intended for land use planning, for evaluating land use
alternatives, and for planning site investigations prior to design and construction.
The information, however, has limitations. For example, estimates and other data
generally apply only to that part of the soil between the surface and a depth of 5 to
7 feet. Because of the map scale, small areas of different soils may be included
within the mapped areas of a specific soil.
The information is not site specific and does not eliminate the need for onsite
investigation of the soils or for testing and analysis by personnel experienced in the
design and construction of engineering works.
Government ordinances and regulations that restrict certain land uses or impose
specific design criteria were not considered in preparing the information in this table.
Local ordinances and regulations should be considered in planning, in site
selection, and in design.
Report—Dwellings and Small Commercial Buildings
[Onsite investigation may be needed to validate the interpretations in this table and
to confirm the identity of the soil on a given site.The numbers in the value columns
range from 0.01 to 1.00. The larger the value, the greater the potential limitation.
The table shows only the top five limitations for any given soil. The soil may have
additional limitations]
Dwellings and Small Commercial Buildings-Albemarle County,Virginia
Map symbol and soil Pct.of Dwellings without basements Dwellings with basements Small commercial buildings
name map
unit Rating class and Value Rating class and Value Rating class and Value
limiting features limiting features limiting features
27B—Elioak loam,2 to
7 percent slopes
Elioak 80 Not limited Not limited Somewhat limited
Slope 0.13
28C3—Elioak clay
loam,7 to 15
percent slopes,
severely eroded
Eli oak 80 Somewhat limited Somewhat limited Very limited
Slope 0.37 Slope 0.37 Slope 1.00
34C—Glenelg loam,7
to 15 percent slopes
Glenelg 85 Somewhat limited Somewhat limited Very limited
Slope 0.37 Slope 0.37 Slope 1.00
---- ---- ---
34D—Glenelg loam,
15 to 25 percent
slopes
Glenelg 80 Very limited Very limited Very limited
Slope 1.00 Slope 1.00 Slope 1.00
USDA Natural Resources Web Soil Survey 5/6/2016
Conservation Service National Cooperative Soil Survey Page 2 of 3
• •
Dwellings and Small Commercial Buildings---Albemarle County,Virginia Texas Roadhouse
Dwellings and Small Commercial Buildings—Albemarle County,Virginia
Map symbol and soil Pct.of Dwellings without basements Dwellings with basements Small commercial buildings
name map
unit Rating class and Value Rating class and Value Rating class and Value
limiting features limiting features limiting features
50D—Manor loam,15
to 25 percent slopes
Manor 85 Very limited Very limited Very limited
Slope 1.00 Slope 1.00 Slope 1.00
95—Wehadkee silt
loam
Wehadkee 80 Very limited Very limited Very limited
Flooding 1.00 Flooding 1.00 Flooding 1.00
Depth to saturated 1.00 Depth to saturated 1.00 Depth to saturated 1.00
zone zone zone
Data Source Information
Soil Survey Area: Albemarle County, Virginia
Survey Area Data: Version 10, Dec 11, 2013
USDA Natural Resources Web Soil Survey 5/6/2016
Conservation Service National Cooperative Soil Survey Page 3 of 3
w.
Roads and Streets,Shallow Excavations,and Lawns and Landscaping---Albemarle County, Texas Roadhouse
Virginia
Roads and Streets, Shallow Excavations, and Lawns and
Landscaping
Soil properties influence the development of building sites, including the selection
of the site,the design of the structure,construction,performance after construction,
and maintenance.This table shows the degree and kind of soil limitations that affect
local roads and streets, shallow excavations, and lawns and landscaping.
The ratings in the table are both verbal and numerical. Rating class terms indicate
the extent to which the soils are limited by all of the soil features that affect building
site development. Not limited indicates that the soil has features that are very
favorable for the specified use. Good performance and very low maintenance can
be expected. Somewhat limited indicates that the soil has features that are
moderately favorable for the specified use. The limitations can be overcome or
minimized by special planning, design, or installation. Fair performance and
moderate maintenance can be expected. Very limited indicates that the soil has
one or more features that are unfavorable for the specified use. The limitations
generally cannot be overcome without major soil reclamation, special design, or
expensive installation procedures. Poor performance and high maintenance can
be expected.
Numerical ratings in the table indicate the severity of individual limitations. The
ratings are shown as decimal fractions ranging from 0.01 to 1.00. They indicate
gradations between the point at which a soil feature has the greatest negative
impact on the use (1.00) and the point at which the soil feature is not a limitation
(0.00).
Local roads and streets have an all-weather surface and carry automobile and light
truck traffic all year.They have a subgrade of cut or fill soil material;a base of gravel,
crushed rock, or soil material stabilized by lime or cement; and a surface of flexible
material(asphalt), rigid material (concrete), or gravel with a binder.The ratings are
based on the soil properties that affect the ease of excavation and grading and the
traffic-supporting capacity. The properties that affect the ease of excavation and
grading are depth to bedrock or a cemented pan, hardness of bedrock or a
cemented pan, depth to a water table, ponding, flooding, the amount of large
stones,and slope.The properties that affect the traffic-supporting capacity are soil
strength (as inferred from the AASHTO group index number), subsidence, linear
extensibility(shrink-swell potential), the potential for frost action, depth to a water
table, and ponding.
Shallow excavations are trenches or holes dug to a maximum depth of 5 or 6 feet
for graves, utility lines, open ditches, or other purposes. The ratings are based on
the soil properties that influence the ease of digging and the resistance to sloughing.
Depth to bedrock or a cemented pan, hardness of bedrock or a cemented pan,the
amount of large stones,and dense layers influence the ease of digging,filling, and
compacting. Depth to the seasonal high water table, flooding, and ponding may
restrict the period when excavations can be made. Slope influences the ease of
using machinery. Soil texture, depth to the water table, and linear extensibility
(shrink-swell potential) influence the resistance to sloughing.
L•SDA Natural Resources Web Soil Survey 5/6/2016
Conservation Service National Cooperative Soil Survey Page 1 of 4
NYISigP
Roads and Streets,Shallow Excavations,and Lawns and Landscaping---Albemarle County, Texas Roadhouse
Virginia
Lawns and landscaping require soils on which turf and ornamental trees and shrubs
can be established and maintained. Irrigation is not considered in the ratings. The
ratings are based on the soil properties that affect plant growth and trafficability
after vegetation is established.The properties that affect plant growth are reaction;
depth to a water table; ponding; depth to bedrock or a cemented pan;the available
water capacity in the upper 40 inches; the content of salts, sodium, or calcium
carbonate; and sulfidic materials.The properties that affect trafficability are
flooding,depth to a water table,ponding,slope,stoniness, and the amount of sand,
clay, or organic matter in the surface layer.
Information in this table is intended for land use planning, for evaluating land use
alternatives, and for planning site investigations prior to design and construction.
The information, however, has limitations. For example, estimates and other data
generally apply only to that part of the soil between the surface and a depth of 5 to
7 feet. Because of the map scale, small areas of different soils may be included
within the mapped areas of a specific soil.
The information is not site specific and does not eliminate the need for onsite
investigation of the soils or for testing and analysis by personnel experienced in the
design and construction of engineering works.
Government ordinances and regulations that restrict certain land uses or impose
specific design criteria were not considered in preparing the information in this table.
Local ordinances and regulations should be considered in planning, in site
selection, and in design.
Report—Roads and Streets, Shallow Excavations, and Lawns
and Landscaping
[Onsite investigation may be needed to validate the interpretations in this table and
to confirm the identity of the soil on a given site.The numbers in the value columns
range from 0.01 to 1.00. The larger the value, the greater the potential limitation.
The table shows only the top five limitations for any given soil.The soil may have
additional limitations]
Roads and Streets,Shallow Excavations,and Lawns and Landscaping Albemarle County,Virginia
Map symbol and soil Pct.of Local roads and streets Shallow excavations Lawns and landscaping
name map
unit Rating class and Value Rating class and Value Rating class and Value
limiting features limiting features limiting features
27B—Elioak loam,2 to
7 percent slopes
Eli oak 80 Very limited Somewhat limited Very limited
Low strength 1.00 Too clayey 0.13 Low exchange 1.00
capacity
Frost action 0.50 Dusty 0.08 Too clayey 0.50
Unstable excavation 0.01 Dusty 0.08
walls
USDA Natural Resources Web Soil Surrey 5/6/2016
Conservation Service National Cooperative Soil Survey Page 2 of 4
Roads and Streets,Shallow Excavations,and Lawns and Landscaping---Albemarle County, Texas Roadhouse
Virginia
Roads and Streets,Shallow Excavations,and Lawns and Landscaping-Albemarle County,Virginia
Map symbol and soil Pct.of Local roads end streets Shallow excavations Lawns and landscaping
name map
unit Rating class and Value Rating class and Value Rating class and Value
limiting features limiting features limiting features
28C3-Elioak clay
loam,7 to 15
percent slopes,
severely eroded
Elioak 80 Very limited Somewhat limited Very limited
Low strength 1.00 Slope 0.37 Low exchange 1.00
capacity
Frost action 0.50 Too clayey 0.13 Too clayey 0.50
Slope 0.37 Dusty 0.08 Slope 0.37
Unstable excavation 0.01 Dusty 0.08
walls
Droughty 0.01
34C-Glenelg loam,7-------- j _.---------- -----to 15 percent slopes
Glenelg 85 Very limited Somewhat limited Somewhat limited
Low strength 1.00 Slope 0.37 Low exchange 0.75
capacity
Frost action 0.50 Dusty 0.07 Slope 0.37
Slope 0.37 Unstable excavation 0.01 Dusty 0.07
walls
34D-Glenelg loam,
15 to 25 percent
slopes
Glenelg 80 Very limited Very limited Very limited
Slope 1.00 Slope 1.00 Slope 1.00
Low strength 1.00 Dusty 0.07 Low exchange 0.75
capacity
Frost action 0.50 Unstable excavation 0.01 Dusty 0.07
walls
50D-Manor loam,15
to 25 percent slopes �
Manor 85 Very limited Very limited Very limited
Slope 1.00 Slope 1.00 Slope 1.00
Frost action 0.50 Dusty 0.04 Low exchange 0.75
capacity
Unstable excavation 0.01 Dusty 0.04
walls
USDA Natural Resources Web Soil Survey 5/6/2016
Conservation Service National Cooperative Soil Survey Page 3 of 4
•
Roads and Streets,Shallow Excavations,and Lawns and Landscaping---Albemarle County, Texas Roadhouse
Virginia
Roads and Streets,Shallow Excavations,and Lawns and Landscaping Albemarle County,Virginia
Map symbol and soil Pct.of Local roads and streets Shallow excavations Lawns and landscaping
name map
unit Rating class and Value Rating class and Value Rating class and Value
limiting features limiting features limiting features
95—Wehadkee silt
loam
Wehadkee 80 Very limited Very limited Somewhat limited
Flooding 1.00 Depth to saturated 1.00 Depth to saturated 0.94
zone zone
Low strength 1.00 Flooding 0.60 Flooding 0.60
Depth to saturated 0.94 Dusty 0.08 Low exchange 0.50
zone capacity
Unstable excavation 0.01 Dusty 0.08
walls
Data Source Information
Soil Survey Area: Albemarle County,Virginia
Survey Area Data: Version 10, Dec 11, 2013
USDA Natural Resources Web Soil Survey 5/6/2016
-11126 Conservation Service National Cooperative Soil Survey Page 4 of 4
Soil Features---Albemarle County,Virginia Texas Roadhouse
Soil Features
This table gives estimates of various soil features. The estimates are used in land
use planning that involves engineering considerations.
A restrictive layer is a nearly continuous layer that has one or more physical,
chemical, or thermal properties that significantly impede the movement of water
and air through the soil or that restrict roots or otherwise provide an unfavorable
root environment. Examples are bedrock, cemented layers, dense layers, and
frozen layers.The table indicates the hardness and thickness of the restrictive layer,
both of which significantly affect the ease of excavation. Depth to top is the vertical
distance from the soil surface to the upper boundary of the restrictive layer.
Subsidence is the settlement of organic soils or of saturated mineral soils of very
low density. Subsidence generally results from either desiccation and shrinkage,
or oxidation of organic material,or both,following drainage.Subsidence takes place
gradually, usually over a period of several years. The table shows the expected
initial subsidence,which usually is a result of drainage,and total subsidence,which
results from a combination of factors.
Potential for frost action is the likelihood of upward or lateral expansion of the soil
caused by the formation of segregated ice lenses(frost heave)and the subsequent
collapse of the soil and loss of strength on thawing. Frost action occurs when
moisture moves into the freezing zone of the soil. Temperature, texture, density,
saturated hydraulic conductivity(Ksat), content of organic matter, and depth to the
water table are the most important factors considered in evaluating the potential for
frost action. It is assumed that the soil is not insulated by vegetation or snow and
is not artificially drained. Silty and highly structured, clayey soils that have a high
water table in winter are the most susceptible to frost action. Well drained, very
gravelly, or very sandy soils are the least susceptible. Frost heave and low soil
strength during thawing cause damage to pavements and other rigid structures.
Risk of corrosion pertains to potential soil-induced electrochemical or chemical
action that corrodes or weakens uncoated steel or concrete. The rate of corrosion
of uncoated steel is related to such factors as soil moisture, particle-size
distribution, acidity, and electrical conductivity of the soil. The rate of corrosion of
concrete is based mainly on the sulfate and sodium content, texture, moisture
content,and acidity of the soil.Special site examination and design may be needed
if the combination of factors results in a severe hazard of corrosion. The steel or
concrete in installations that intersect soil boundaries or soil layers is more
susceptible to corrosion than the steel or concrete in installations that are entirely
within one kind of soil or within one soil layer.
For uncoated steel, the risk of corrosion, expressed as low, moderate, or high, is
based on soil drainage class, total acidity, electrical resistivity near field capacity,
and electrical conductivity of the saturation extract.
For concrete, the risk of corrosion also is expressed as low, moderate, or high. It
is based on soil texture, acidity, and amount of sulfates in the saturation extract.
USDA Natural Resources Web Soil Survey 5/6/2016
"ria Conservation Service National Cooperative Soil Survey Page 1 of 3
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Soil Features---Albemarle County,Virginia Texas Roadhouse
Soil Features
This table gives estimates of various soil features. The estimates are used in land
use planning that involves engineering considerations.
A restrictive layer is a nearly continuous layer that has one or more physical,
chemical, or thermal properties that significantly impede the movement of water
and air through the soil or that restrict roots or otherwise provide an unfavorable
root environment. Examples are bedrock, cemented layers, dense layers, and
frozen layers.The table indicates the hardness and thickness of the restrictive layer,
both of which significantly affect the ease of excavation. Depth to top is the vertical
distance from the soil surface to the upper boundary of the restrictive layer.
Subsidence is the settlement of organic soils or of saturated mineral soils of very
low density. Subsidence generally results from either desiccation and shrinkage,
or oxidation of organic material,or both,following drainage.Subsidence takes place
gradually, usually over a period of several years.The table shows the expected
initial subsidence,which usually is a result of drainage,and total subsidence,which
results from a combination of factors.
Potential for frost action is the likelihood of upward or lateral expansion of the soil
caused by the formation of segregated ice lenses(frost heave)and the subsequent
collapse of the soil and loss of strength on thawing. Frost action occurs when
moisture moves into the freezing zone of the soil. Temperature, texture, density,
saturated hydraulic conductivity(Ksat), content of organic matter, and depth to the
water table are the most important factors considered in evaluating the potential for
frost action. It is assumed that the soil is not insulated by vegetation or snow and
is not artificially drained. Silty and highly structured, clayey soils that have a high
water table in winter are the most susceptible to frost action. Well drained, very
gravelly, or very sandy soils are the least susceptible. Frost heave and low soil
strength during thawing cause damage to pavements and other rigid structures.
Risk of corrosion pertains to potential soil-induced electrochemical or chemical
action that corrodes or weakens uncoated steel or concrete. The rate of corrosion
of uncoated steel is related to such factors as soil moisture, particle-size
distribution, acidity, and electrical conductivity of the soil. The rate of corrosion of
concrete is based mainly on the sulfate and sodium content, texture, moisture
content,and acidity of the soil.Special site examination and design may be needed
if the combination of factors results in a severe hazard of corrosion. The steel or
concrete in installations that intersect soil boundaries or soil layers is more
susceptible to corrosion than the steel or concrete in installations that are entirely
within one kind of soil or within one soil layer.
For uncoated steel, the risk of corrosion, expressed as low, moderate, or high, is
based on soil drainage class, total acidity, electrical resistivity near field capacity,
and electrical conductivity of the saturation extract.
For concrete, the risk of corrosion also is expressed as low, moderate, or high. It
is based on soil texture, acidity, and amount of sulfates in the saturation extract.
USDA Natural Resources Web Soil Survey 5/6/2016
Conservation Service National Cooperative Soil Survey Page 1 of 3
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