[Federal Register Volume 61, Number 108 (Tuesday, June 4, 1996)]
[Rules and Regulations]
[Pages 27998-28000]
From the Federal Register Online via the Government Publishing Office [www.gpo.gov]
[FR Doc No: 96-13920]
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DEPARTMENT OF AGRICULTURE
Natural Resources Conservation Service
7 CFR Part 610
Technical Assistance
AGENCY: Natural Resources Conservation Service, USDA.
ACTION: Final rule.
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SUMMARY: Section 301(c) of the Federal Agriculture Improvement and
Reform Act of 1996 (FAIRA) requires the Secretary of Agriculture to
publish in the Federal Register, within 60 days of the enactment of
FAIRA, the universal soil loss equation (USLE) and wind erosion
equation (WEQ) used by the Department of Agriculture (the Department)
as of the date of publication. The Natural Resources Conservation
Service (NRCS) utilizes factors from the USLE, the revised universal
soil loss equation (RUSLE) and the WEQ in equations to predict soil
erosion due to water and wind. The Department was first required to use
the factors from the USLE and WEQ to make highly erodible land (HEL)
determinations under the Food Security Act (FSA) of 1985, Pub. L. 99-
198. The FSA defined HEL as land that has the potential for an
excessive annual rate of erosion in relation to the soil loss tolerance
level as determined by the Secretary through application of factors
from the USLE and WEQ.
This final rule sets forth the USLE and WEQ used by the Department
as of this date and the circumstances under the equations are used.
Since the first mandated use of the USLE in 1985, the technology used
to predict soil erosion due to water has been refined. The refinement
is reflected in a revised USLE (RUSLE) which will also be used under
the circumstances described in this rule.
EFFECTIVE DATE: This rule is effective June 3, 1996.
FOR FURTHER INFORMATION CONTACT: David L. Schertz, National Agronomist,
Natural Resources Conservation Service, P.O. Box 2890, Washington, D.C.
20013; Fax 202-720-2646 or Internet:dschertz@usda.gov.
SUPPLEMENTARY INFORMATION:
Rulemaking Analyses
EO 12291: Not major.
Regulatory Flexibility Act: No significant impact.
Paperwork Reduction Act: Does not apply.
National Environmental Policy Act: Not applicable.
Civil Rights Impact Analysis: Not applicable.
Federalism Assessment: Does not have sufficient federalism
implications to warrant an assessment.
Unfunded Mandate: Not applicable.
Background And Purpose
The Natural Resources Conservation Service (NRCS) of the United
States Department of Agriculture (the Department), utilizes the
universal soil loss equation (USLE), the revised universal soil loss
equation (RUSLE) and the wind erosion equation (WEQ) to predict soil
erosion due to water and wind. Section 301(c) of the Federal
Agriculture Improvement and Reform Act of 1996 (FAIRA), which was
enacted April 4, 1996, requires the Secretary of Agriculture to publish
in the Federal Register by June 3, 1996, the USLE and WEQ used by the
Department as of the date of publication. NRCS is publishing the
equations and the rules under which the USLE, RUSLE, and WEQ factors
are used for administering programs.
The equation for predicting soil loss due to erosion for both the
USLE and RUSLE is A=R x K x LS x C x P. The factors in the equation
have the following definitions:
1. A is the estimation of average annual soil loss in tons per acre
caused by sheet and rill erosion.
2. R is the rainfall erosivity factor.
3. K is the soil erodibility factor.
4. LS is the slope length and steepness factor.
5. C is the cover and management factor.
6. P is the support practice factor.
A paper published by K.G. Renard, et al., in the May-June, 1994
Journal of Soil and Water Conservation, volume 49(3), pages 213-220,
entitled, ``RUSLE revisited: Status, questions, answers, and the
future'', describes the revision. Primary differences between the USLE
and RUSLE include the following:
R Factor: RUSLE includes more R values for the Western United
States than the USLE. For the eastern United States, R values are
generally the same as those used in the USLE but includes some
revisions.
K Factor: Values used in RUSLE are similar to the USLE values but
are adjusted to account for changes, such as freezing and thawing, and
soil moisture. These adjustments are calculated at one-half month
intervals for use in RUSLE and are applicable in the northern and
southern plains, midwest, southern, and eastern United States.
LS Factor: USLE uses one LS table; RUSLE uses four LS tables, as
determined by the relationship of rill to interrill erosion. Although
both the USLE and RUSLE can account for the effects of complex slopes,
RUSLE simplifies this LS determination through the use of computer
technology.
C Factor: USLE provides estimates of soil changes for 4-5 crop
stage periods throughout the year. RUSLE provides estimates of cover
and soil changes on one-half month intervals, especially in relation to
canopy, surface residue, residue just under the surface, and the
effects of climate on residue decomposition, roughness, roots, and soil
consolidation.
P Factor: USLE uses P factors for contouring, contour
stripcropping, and terracing from table values established for field
slope ranges; and for terraces, the P factor is also based on channel
gradients. RUSLE uses P factors for farming across the slope and
includes new process-based routines to determine the effect of
stripcropping and buffer strips. Values for farming across the slope
are based on slope length and steepness, row grade, ridge height, storm
severity, soil infiltration, and the cover and roughness conditions.
The stripcropping P factor is based on the amount and location of soil
deposition.
The equation for predicting soil loss due to wind erosion is
E=f(IKCLV). The factors in the equation have the following definitions:
1. E is the estimation of average annual soil loss in tons per
acre.
2. f indicates the equation includes functional relationships that
are not straight-line mathematical calculations.
3. I is the soil erodibility index.
4. K is the ridge roughness factor.
5. C is the climatic factor. All climatic factor values are
expressed as a percentage of the value established at Garden City,
Kansas. Garden City, Kansas was the location of early research in the
WEQ and established the standard for climatic factors against which the
other locations are measured.
6. L is the unsheltered distance across an erodible field, measured
along the prevailing wind erosion direction.
7. V is the vegetative cover factor.
The Department was first statutorily required to use the factors
from the USLE and WEQ to make highly erodible land (HEL) determinations
under the Food Security Act (FSA) of 1985, Pub. L. 99-198. The
Department published the equations used to determine HEL during
promulgation of the regulations
[[Page 27999]]
implementing the HEL and wetland conservation provisions of the FSA, 7
CFR Part 12 (see Federal Register, Vol. 52, No. 180, page 35194,
September 17, 1987). Section 12.21 provides that land in a soil map
unit will be considered to be highly erodible if the quotient of either
the RKLS/T or the CI/T equals or exceeds 8. The factors, R, K, and LS
are from the USLE. The USLE factors are explained in the U.S.
Department of Agriculture Handbook 537. The factors C and I are from
the WEQ. The WEQ factors are explained in a paper by N.P. Woodruff and
F.H. Siddaway, 1965. The soil loss tolerance (T) value represents the
average annual rate of soil erosion that could occur without causing a
decline in long term productivity. The specific factors values which
are used for determining whether soil map units are considered to be
highly erodible are published in the local Field Office Technical Guide
(FOTG) which is maintained in each NRCS field office. The values
published as of January 1, 1990, in the FOTG are the basis for all HEL
determinations. The FOTG is available for review in each NRCS field
office. The values vary across the country to correspond to differences
in climate, soil types, and topography.
Since the publication of the USLE in 1985, additional research on
erosion processes has resulted in refined technology for determining
the factor values in the USLE. RUSLE represents a revision of the USLE
technology in how the factor values in the equation are determined.
RUSLE is explained in the U.S. Department of Agriculture Handbook 703,
``Predicting Soil Erosion by Water: A Guide to Conservation Planning
with the Revised Universal Soil Loss Equation (RUSLE).''
Since the passage of the FSA in 1985, USLE and WEQ have been used
to compile the highly erodible soils list and to make highly erodible
field determinations. USLE has been used to develop conservation plans
and revisions and to conduct status reviews. As new understanding is
gained through research on erosion processes, updates of erosion
prediction equations can occur. Changing the highly erodible soils list
and field determinations each time these technologies are updated would
be disruptive to farmers and impractical for long range planning.
Therefore, no changes to the existing highly erodible soils list or
field determinations will be made as a result of the implementation of
RUSLE. However, as technology is improved, such as with RUSLE, NRCS
will use it to develop new conservation plans, plan revisions, and to
conduct status reviews. NRCS will not require producers to meet more
restrictive levels of erosion reduction that might result from using
RUSLE instead of USLE while carrying out existing conservation plans.
Therefore, all existing conservation plans developed using USLE, that
have been implemented, will remain acceptable plans for purposes of the
HEL conservation provisions of the FSA.
List of Subjects in 7 CFR Part 610
Soil conservation, Technical assistance, Water resources.
For the reasons set forth above, 7 CFR Part 610 is amended as
follows:
PART 610--TECHNICAL ASSISTANCE
1. The authority for Part 610 is revised to read as follows:
Authority: 16 U.S.C. 590a-590f, 590q, 3801(a)(9).
Secs. 610.1-610.5. [Designated as Subpart A]
2. Sections 610.1 through 610.5 are designated as subpart A--
Conservation Operations.
3. Section 610.1 is revised to read as follows:
Sec. 610.1 Purpose.
This subpart sets forth Natural Resource Conservation Service
(NRCS) policies and procedures for furnishing technical assistance in
conservation operations.
4. Subpart B--Soil Erosion Prediction Equations containing
Secs. 610.11 through 610.14 is added to read as follows:
Subpart B--Soil Erosion Prediction Equations
Sec.
610.11 Purpose and scope.
610.12 Equations for predicting soil loss due to water erosion.
610.13 Equations for predicting soil loss due to wind erosion.
610.14 Use of USLE, RUSLE, and WEQ.
Subpart B--Soil Erosion Prediction Equations
Sec. 610.11 Purpose and scope.
This subpart sets forth the equations and rules for utilizing the
equations that are used by the Natural Resources Conservation Service
(NRCS) to predict soil erosion due to water and wind. Section 301 of
the Federal Agriculture Improvement and Reform Act of 1996 (FAIRA) and
the Food Security Act, as amended, 16 U.S.C. 3801-3813 specified that
the Secretary would publish the universal soil loss equation (USLE) and
wind erosion equation (WEQ) used by the Department within 60 days of
the enactment of FAIRA. This subpart sets forth the equations,
definition of factors, and provides the rules under which NRCS will
utilize the USLE, the revised universal soil loss equation (RUSLE), and
the WEQ.
Sec. 610.12 Equations for predicting soil loss due to water erosion.
(a) The equation for predicting soil loss due to erosion for both
the USLE and the RUSLE is A=R x K x LS x C x P. (For further
information about USLE see the U.S. Department of Agriculture Handbook
537, ``Predicting Rainfall Erosion Losses--A Guide to Conservation
Planning,'' dated 1978. Copies of this document are available from the
Natural Resources Conservation Service, P.O. Box 2890, Washington, DC
20013. For further information about RUSLE see the U.S. Department of
Agriculture Handbook 703, ``Predicting Soil Erosion by Water: A Guide
to Conservation Planning with the Revised Universal Soil Loss Equation
(RUSLE).'' Copies may be purchased from the National Technical
Information Service, 5285 Port Royal Road, Springfield, VA 22161.)
(b) The factors in the USLE equation are:
(1) A is the estimation of average annual soil loss in tons per
acre caused by sheet and rill erosion.
(2) R is the rainfall erosivity factor. Accounts for the energy and
intensity of rainstorms.
(3) K is the soil erodibility factor. Measures the susceptibility
of a soil to erode under a standard condition.
(4) LS is the slope length and steepness factor. Accounts for the
effect of length and steepness of slope on erosion.
(5) C is the cover and management factor. Estimates the soil loss
ratio for each of 4 or 5 crop stage periods throughout the year,
accounting for the combined effect of all the interrelated cover and
management variables.
(6) P is the support practice factor. Accounts for the effect of
conservation support practices, such as contouring, contour
stripcropping, and terraces on soil erosion.
(c) The factors in the RUSLE equation are defined as follows:
(1) A is the estimation of average annual soil loss in tons per
acre caused by sheet and rill erosion.
(2) R is the rainfall erosivity factor. Accounts for the energy and
intensity of rainstorms.
(3) K is the soil erodibility factor. Measures the susceptibility
of a soil to erode under a standard condition and adjusts it bi-monthly
for the effects of freezing and thawing, and soil moisture.
(4) LS is the slope length and steepness factor. Accounts for the
effect of length and steepness of slope on
[[Page 28000]]
erosion based on 4 tables reflecting the relationship of rill to
interrill erosion.
(5) C is the cover and management factor. Estimates the soil loss
ratio at one-half month intervals throughout the year, accounting for
the individual effects of prior land use, crop canopy, surface cover,
surface roughness, and soil moisture.
(6) P is the support practice factor. Accounts for the effect of
conservation support practices, such as cross-slope farming,
stripcropping, buffer strips, and terraces on soil erosion.
Sec. 610.13 Equations For Predicting Soil Loss Due To Wind Erosion.
(a) The equation for predicting soil loss due to wind in the Wind
Erosion Equation (WEQ) is E=f(IKCLV). (For further information on WEQ
see the paper by N.P. Woodruff and F.H. Siddaway, 1965. ``A Wind
Erosion Equation,'' Soil Science Society of America Proceedings, Vol.
29, No. 5, pages 602-608, which is available from the American Society
of Agronomy, Madison, Wisconsin. In addition, the use of the WEQ in
NRCS is explained in the Natural Resources Conservation Service (NRCS)
National Agronomy Manual, 190-V-NAM, second ed., Part 502, March, 1988,
which is available from the NRCS, P.O. Box 2890, Washington, DC 20013.)
(c) The factors in the WEQ equation are defined as follows:
(1) E is the estimation of the average annual soil loss in tons per
acre.
(2) f indicates the equation includes functional relationships that
are not straight-line mathematical calculations.
(3) I is the soil erodibility index. It is the potential for soil
loss from a wide, level, unsheltered, isolated field with a bare,
smooth, loose and uncrusted surface. Soil erodibility is based on soil
surface texture, calcium carbonate content, and percent day.
(4) K is the ridge roughness factor. It is a measure of the effect
of ridges formed by tillage and planting implements on wind erosion.
The ridge roughness is based on ridge spacing, height, and erosive wind
directions in relation to the ridge direction
(5) C is the climatic factor. It is a measure of the erosive
potential of the wind speed and surface moisture at a given location
compared with the same factors at Garden City, Kansas. The annual
climatic factor at Garden City is arbitrarily set at 100. All climatic
factor values are expressed as a percentage of that at Garden City.
(6) L is the unsheltered distance. It is the unsheltered distance
across an erodible field, measured along the prevailing wind erosion
direction. This distance is measured beginning at a stable border on
the upwind side and continuing downward to the nonerodible or stable
area, or to the downwind edge of the area being evaluated.
(7) V is the vegetative cover factor. It accounts for the kind,
amount, and orientation of growing plants or plant residue on the soil
surface.
Sec. 610.14 Use of USLE, RUSLE, and WEQ.
(a) All Highly Erodible Land (HEL) determinations are based on the
formulas set forth in 7 CFR Sec. 12.21 using some of the factors from
the USLE and WEQ and the factor values that were contained in the local
Field Office Technical Guide (FOTG) as of January 1, 1990. In addition,
this includes the soil loss tolerance values used in those formulas for
determining HEL. The soil loss tolerance value is used as one of the
criteria for planning soil conservation systems. These values are
available in the FOTG in the local field office of the Natural
Resources Conservation Service.
(b) RUSLE will be used to:
(1)(i) Evaluate the soil loss estimates of conservation systems
contained in the FOTG.
(ii) Evaluate the soil loss estimates of systems actually applied,
where those systems were applied differently than specified in the
conservation plan adopted by the producer or where a conservation plan
was not developed, in determining whether a producer has complied with
the HEL conservation provisions of the Food Security Act of 1985, as
amended, 16 U.S.C. Sec. 3801 et seq., set forth in 7 CFR Part 12; and
(2) Develop new or revised conservation plans.
Dated: May 30, 1996.
Paul W. Johnson,
Chief, Natural Resources Conservation Service.
[FR Doc. 96-13920 Filed 5-31-96; 11:33 am]
BILLING CODE 3410-16-M
