2013-09-18_PERMIT FILE - M2013064 ‎(9)‎

• Permit No: M2013064
• IBM Index Class Name: PERMIT FILE
• Doc Date: 9/18/2013
• Doc Name: New Application
• From: Varra Companies, Inc
• To: DRMS
• Media Type: D
• Archive: No

Custom Soil Resource Report
Soil Chemical Properties
This folder contains a collection of tabular reports that present soil chemical properties.
The reports (tables) include all selected map units and components for each map unit.
Soil chemical properties are measured or inferred from direct observations in the field
or laboratory. Examples of soil chemical properties include pH, cation exchange
capacity, calcium carbonate, gypsum, and electrical conductivity.
Chemical Soil Properties
This table shows estimates of some chemical characteristics and features that affect
soil behavior. These estimates are given for the layers of each soil in the survey area.
The estimates are based on field observations and on test data for these and similar
soils.
Depth to the upper and lower boundaries of each layer is indicated.
Cation - exchange capacity is the total amount of extractable cations that can be held
by the soil, expressed in terms of milliequivalents per 100 grams of soil at neutrality
(pH 7.0) or at some other stated pH value. Soils having a low cation- exchange capacity
hold fewer cations and may require more frequent applications of fertilizer than soils
having a high cation - exchange capacity. The ability to retain cations reduces the
hazard of ground -water pollution.
Effective cation - exchange capacity refers to the sum of extractable cations plus
aluminum expressed in terms of milliequivalents per 100 grams of soil. It is determined
for soils that have pH of less than 5.5.
Soil reaction is a measure of acidity or alkalinity. It is important in selecting crops and
other plants, in evaluating soil amendments for fertility and stabilization, and in
determining the risk of corrosion.
Calcium carbonate equivalent is the percent of carbonates, by weight, in the fraction
of the soil less than 2 millimeters in size. The availability of plant nutrients is influenced
by the amount of carbonates in the soil.
54
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•
68 — Ustic Torriorthents,
moderately steep
Ustic torriorthents
85
Very limited
Very limited
Slope
1.00
Filtering capacity
1.00
Slope
0.63
Seepage
100
Not rated
85 —Water
Water
86— Borrow Pits
95
Not rated
Borrow pits
100
Not rated
Not rated
Soil Chemical Properties
This folder contains a collection of tabular reports that present soil chemical properties.
The reports (tables) include all selected map units and components for each map unit.
Soil chemical properties are measured or inferred from direct observations in the field
or laboratory. Examples of soil chemical properties include pH, cation exchange
capacity, calcium carbonate, gypsum, and electrical conductivity.
Chemical Soil Properties
This table shows estimates of some chemical characteristics and features that affect
soil behavior. These estimates are given for the layers of each soil in the survey area.
The estimates are based on field observations and on test data for these and similar
soils.
Depth to the upper and lower boundaries of each layer is indicated.
Cation - exchange capacity is the total amount of extractable cations that can be held
by the soil, expressed in terms of milliequivalents per 100 grams of soil at neutrality
(pH 7.0) or at some other stated pH value. Soils having a low cation- exchange capacity
hold fewer cations and may require more frequent applications of fertilizer than soils
having a high cation - exchange capacity. The ability to retain cations reduces the
hazard of ground -water pollution.
Effective cation - exchange capacity refers to the sum of extractable cations plus
aluminum expressed in terms of milliequivalents per 100 grams of soil. It is determined
for soils that have pH of less than 5.5.
Soil reaction is a measure of acidity or alkalinity. It is important in selecting crops and
other plants, in evaluating soil amendments for fertility and stabilization, and in
determining the risk of corrosion.
Calcium carbonate equivalent is the percent of carbonates, by weight, in the fraction
of the soil less than 2 millimeters in size. The availability of plant nutrients is influenced
by the amount of carbonates in the soil.
54