· C = climatic characterization of windspeed and surface soil moisture expressed as a percentage.
(iii) I = the susceptibility of the soil to wind erosion.
Note: The factor values for the equations used in the soil-loss equations are those in effect as of January 1, 1990.
C. Calculating EI
The EI for a soil map unit is determined by dividing the potential erodibility for the soil map unit by the soil loss tolerance (T) value established for the soil in the FOTG as of January 1, 1990 [7 CFR Section 12.21(a)].
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Erosion Equation
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Calculation
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Sheet and Rill Erosion (USLE)
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R x K x LS = EI
T
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Wind Erosion (WEQ)
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C x I = EI
T
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Note: The Highly Erodible Map Unit List contained in the FOTG as of January 1, 1990, will be used for all EI calculations, including sodbuster determinations and reviews of previous determinations.
D. Highly Erodible Soil Map Units
A soil map unit with an EI of 8 or greater is considered to be highly erodible [7 CFR Section 12.21(b)].
E. Potentially Highly Erodible Map Units
Whenever a soil map unit description contains a range of a slope length and steepness characteristics that produce a range of LS values which result in RKLS/T quotients both above and below 8, the soil map unit will be entered on the list of highly erodible soil map units as “potentially highly erodible.” [7 CFR Section 12.21(c)]
511.1 Highly Erodible Soil Map Unit List
A. Highly Erodible Soil Map Unit List
The Highly Erodible Soil Map Unit List is a list of all soil map units (names and symbols) in an area. [7 CFR Section 12.20(b)] These soil map units are specifically categorized as being—
(i) Highly Erodible (HEL) from wind erosion
(ii) HEL or Potentially Highly Erodible (PHEL) from sheet and rill erosion.
Note: When a field determination includes PHEL soil map units, the HEL determination shall be verified through a field review to determine the correct LS factor value for that specific field in order to finalize the field HEL determination. [7 CFR Section 12.21(c)] If necessary, a new determination shall be issued when the field verification changes the original office HEL determination label.
B. HEL Soil Map Unit List Area
(1) The HEL Soil Map Unit List developed as of January 1, 1990, will be used for all HEL determinations.
(2) The HEL Soil Map Unit List shall be developed and maintained for any of the following:
(i) Each soil survey area
(ii) Each FOTG area
(iii) Other geographic areas as determined by the STC.
C. HEL Soil Map Units and Soil Map Unit Components
The percentage of HEL soil map unit components that are required to achieve predominance of a soil map unit will be established by the STC. Determine whether a soil map unit is considered highly erodible according to the following table.
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IF the soil map unit...
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AND...
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THEN...
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Is named for either—
· A single type of soil or
· A single miscellaneous area,
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Either the named—
· Soil is identified as highly erodible, or
· Miscellaneous area is identified as highly erodible,
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The entire soil map unit is considered highly erodible.
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Is named for two or more—
· Types of soils or
· Miscellaneous areas,
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A predominance of the named components are all highly erodible,
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Less than a predominance of the named components are highly erodible,
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The soil map unit is not considered highly erodible.
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Contains highly erodible soils only as inclusions.
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The soil map unit is not considered highly erodible.
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D. Filing HEL Soil Map Unit Lists
The HEL Soil Map Unit List shall be a part of Section II of the FOTG.
E. Tenure of HEL Soil Map Unit List
The HEL Soil Map Unit List that was in effect January 1, 1990, will remain unchanged for HEL determinations.
F. Areas with More Than One “R” or “C” Value
(1) A separate HEL soil map unit list will be developed for soil survey areas or counties having more than one “R” or “C” factor value.
(2) A map showing the boundaries of each individual C or R factor value area will be placed in Section I of the FOTG.
511.2 Developing HEL Soil Map Unit Lists Using an Existing Soil Survey
A. List of Soil Map Units
(1) A list of soil map units may be available as follows:
(i) FOTG
(ii) Published soil survey
(2) Determine if the list is up-to-date by comparing it against Section II of the FOTG on file in the NRCS office.
B. Needs for Erodibility Calculations
Determine erodibility calculations in each soil survey area or county for each soil map unit, including all components of a complex, association, or undifferentiated unit.
C. Procedure for Calculating Soil Map Unit Erodibility
When calculating erodibility for soil map units, use the following table for guidance.
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To DETERMINE...
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USE...
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The LS value required for a soil map unit to be highly erodible for areas subject to sheet and rill erosion.
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The following equation:
8T/RK = LS
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L and S on-site
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The procedures in the National Agronomy Manual
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L and S in the office
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The data in the FOTG
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(C*I)/T for WEQ
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D. Determining HEL Soil Map Units
A soil map unit is considered to be highly erodible when the following criteria apply:
(i) Sheet and rill erosion areas: The value for LS equals or exceeds 8T/RK for the shortest length and minimum percent slope.
(ii) Wind erosion areas: The value of CI/T equals or exceeds 8.
E. Determining PHEL Soil Map Units
(1) In sheet and rill erosion areas, a soil map unit is considered to be PHEL if the following criteria apply:
(i) The value for LS that is less than 8T/RK for the shortest length and minimum percent of slope.
(ii) The value for LS that exceeds 8T/RK for the longest length and maximum percent of slope.
(2) Any fields with PHEL soil map units will be verified on-site to determine whether they are HEL or non-highly erodible (NHEL), as shown in the following table:
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STEP
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ACTION
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1
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Make on-site L (slope length) and S (slope percent) measurements on several representative slopes for each PHEL soil delineation.
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2
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Use the procedures in the National Agronomy Manual when determining LS values.
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3
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Determine the predominance of HEL for a map unit by comparing the total area of the delineation to that area with an EI of 8 or greater.
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4
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Document all decisions with supporting data placed in the case file.
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511.3 Developing HEL Soil Map Unit Lists When a Completed Soil Survey is not Available
A. Soil Survey in Progress
(1) If a soil survey was in progress or has been started since January 1, 1990, determine if the soil mapping units added to the soil survey legend are highly erodible using the procedures set forth in NFSAM, Section 511.2.
(2) The factor values that are to be used for soil mapping units on new or modified soil survey legends are the factor values set forth in the FOTG that were in effect as of January 1, 1990.
B. Amending the HEL Soil Map Unit List
(1) If a map unit discussed in paragraph 511.3(A) is HEL, it shall be appended to the HEL Soil Map Unit List of the FOTG (as of January 1, 1990), with appropriate documentation and explanation to support the addition.
(2) The only HEL map units that will be appended to the HEL Soil Map Unit List are those that have been correlated since January 1, 1990, where the correlation has been completed according to the procedures in the National Soil Survey Handbook.
C. Approvals
Each HEL map unit appended to the HEL Map Unit List will be dated and approved by the State Soil Scientist.
D. Filing and Archiving HEL Soil Map Unit Lists
(1) The amended HEL Map Unit List will be filed in the appropriate FOTG. All previous copies of the HEL Map Unit List shall be filed as per instructions set forth in GM 120, Part 408.
(2) Mark the HEL Soil Map Unit List that has been replaced with the following: “Superseded by HEL Map Unit List dated [enter appropriate date].”
E. No Changes to Previously Included Soil Map Units
(1) Under no circumstances will the soil map units previously included on the January 1, 1990, HEL Map Unit List have their classification changed.
(2) Fields with previous HELC determinations will not be changed by any additions of soil map units to the HEL Soil Map Unit List.