|
| |
NSSH Part 630
Benchmark Soils
Definition and Purpose
(630.00)
- Definition.
A benchmark soil is one of large extent within one or more major
land resource areas (MLRA), one that holds a key position in the
soil classification system, one for which there is a large amount of
data, one that has special importance to one or more significant
land uses, or one that is of significant ecological importance.
- Purpose.
Benchmark soils, while being important soils in their own right, are
also intended to serve as proxies for other similar soils. Their
purpose is to focus data collection and the investigative effort on
soils that have the greatest potential for extending collected data
and resultant interpretations to other soils. This purpose is
relevant both in making soil surveys and to soil survey customers in
their goal to extend findings of their research The cost of
investigation and the large number of combinations of soil uses and
management practices preclude laboratory and field studies of all
soils; therefore, studies of benchmark soils are an essential
component of developing nationwide soil databases and soil
interpretations. Data obtained by studying benchmark soils can be
used to help estimate important properties in similar soils.
Benchmark soils can also be used to test new interpretations or to
provide input to regional scale models. Knowledge of the properties
and behavior of benchmark soils contributes to the understanding and
interpretation of other soils with similar properties. This
knowledge is important to soil technology and the use of soil
surveys.
Lists of benchmark soils are useful in planning many kinds of soil
studies. The designation of “benchmark” facilitates the selection of
soils that meet research and other study objectives while also
allowing for maximum extension of study data. Benchmark soils can be
selected for their representativeness and included in studies of
single soils or a suite of soils, such as those representing a
gradient in temperature or moisture across a region. The list and
accompanying information about the soil’s classification, land uses,
land cover, and ecological significance are useful in the
development of cross-site studies or networks, such as soil
monitoring networks.
Example uses for benchmark soils:
- extending estimated soil property data to similar soils
- documenting soil properties for ecological site descriptions
- assessing conservation effects
- evaluating soil interpretations
- studying macro/micronutrient and trace elements
- monitoring change in soil quality and natural resource
condition
- measuring saturated hydraulic conductivity
- documenting attainable dynamic soil property values for
specific management systems
- verifying and testing soil erodibility factors
- collecting crop and range plant adaptation and yields
- assessing soil fertility
- locating sources for training materials and onsite training
activities
- modeling crop/soil/pesticide scenarios for surface water and
groundwater assessments
- modeling pedotransfer functions
- conducting cross-site research
Policy and Responsibilities (630.01)
- The MLRA
Soil Survey Office (MLRA SSO) is responsible for:
- through cooperation and consultation with the technical team
members, evaluating the benchmark soils in their area of
responsibility for adherence to the benchmark soils definition
and purpose,
- proposing changes to the benchmark soils status of soil
series through the MLRA
Soil Survey Area Management Team to the MLRA
Soil Survey Regional Office,
- identifying soil series that are considered similar to the
benchmark soils for the extrapolation and transfer of data,
- ensuring pedon descriptions are in NASIS pedon for benchmark
soil sampling sites,
- Including a focus on benchmark soils in long-range, project,
and investigation plans,
- developing an inventory of existing data for benchmark soils
within their area of responsibility. assessing the adequacy of
the data ,and developing plans to fill identified data gaps, and
- developing a narrative record for each benchmark soil within
their area of responsibility.
- The MLRA
Soil Survey Regional Office (MO) is responsible for:
- maintaining the benchmark status data element for soil
series in the soil classification database,
- assuring that benchmark soils are adequately addressed in
MLRA SSO long-range, project, and investigation plans,
- assuring the entire MLRA
is adequately represented by an
optimal number of benchmark soils by approving/denying
recommendations for changes to benchmark soil status,
- maintaining an inventory of existing data for benchmark
soils, as supplied by each MLRA SSO, for their region,
- consulting with appropriate members of MLRA
Management Teams with regard to requests for revisions to
benchmark status, and
- focusing long-range soil survey investigation plans on
benchmark soils and their characteristics.
- The state soil scientist is responsible for:
- reviewing proposed changes, as a member of a MLRA
Management Team, to the benchmark status of soil series, and
forwarding those that the management team concurs with to the MO
for approval,
- soliciting input from cooperators and interdisciplinary
specialists in the selection of benchmark soils, and
- ensuring that benchmark soils are considered in organizing
and planning research, special studies, and investigations.
- The National Soil Survey Center (NSSC) is responsible for:
- providing policy and guidance in the selection of benchmark
soils,
- providing customer support assuring that internet access and
query routines for benchmark soils are available and functioning
properly,
- communicating and consulting with the staff at the site
hosting the electronic files needed to deliver benchmark soil
information,
- through liaisons assigned to each MO and MLRA SSO, assisting
in the development of investigations plans,
- performing laboratory characterization, and
- maintaining the laboratory database.
- The National Geospatial Development Center is responsible for:
- developing Web-based geospatial analysis tools for use in
analyzing and revising benchmark soils by major land resource
area, and
- developing Web-based map display products.
Criteria for Selecting Benchmark Soils
(630.02)
- Criteria.
The soil series that are designated as benchmark soils within an MLRA
should collectively reflect the major diversity of soils within
the area. The criteria are:
- Extent. The soil series that are selected as benchmark soils
are commonly of large extent (>100,000 acres) in the Land
Resource Region (LRR), and of moderate or large extent (> 10,000
acres) in the Major Land Resource Area. Not all series of
moderate or large extent are benchmark soils. Generally, the
combined total extent of all benchmark soils should comprise
about 20 to 25 percent of the total soil area of the major land
resource area. When combining the extent of the benchmark soils
plus the extent of similar soils that they represent,
collectively they are representative of 60 to 80 percent or more
of all soils in the major land resource area. This kind of
representation ensures that any collected data are widely
applicable.
- Key taxonomic classes. Soils that are representative of key
positions in Soil Taxonomy within the MLRA
(such as commonly
occurring great groups, subgroups, or families) are considered
for benchmark soil designation. Research on these can be easily
applied to other soils in those classes. Typically no more than
one or two soils from the same family are designated as
benchmark soils within an MLRA. See item 4 below for a reason to
have more than one.
- Existing data. When similar soils are potential candidates
for benchmark soil designation, soil series for which there are
adequate amounts of data have preference over equally suitable
series for which there are less data. Data-completeness of
correlated pedon data must be evaluated concurrently with
analyses of series extent, taxonomic significance, or unique
importance. The national cooperative soil characterization database
(http://ssldata.nrcs.usda.gov/),
maintained by the National Soil Survey Center, includes
laboratory data for benchmark soils. In addition, soil survey
investigations reports identify benchmark soils. This will
optimize the identification of potential benchmark candidates.
Benchmark soils need to be well documented with complete
characterization data. Ideally, there should be 3 to 5 pedons
characterized. Each description must be accurately georeferenced.
The data should include physical characterization (e.g.
particle-size, bulk density, moisture characteristics, Atterberg
limits, etc), chemical characterization (e.g. pH, base status,
CEC, organic carbon, and calcium carbonate equivalent as
applicable, etc), and mineralogical characterization (e.g., clay
minerals, grain counts). Additional data such as cations
extracted by ammonium oxalate, cations extracted by dithionate
citrate, electrical conductivity, COLE, phosphate retention,
exchangeable sodium percentage, melanic index, or other
properties are important for some soils and should be considered
when evaluating the completeness of existing data. Since there
is not a single list of appropriate data for every soil, the
assigned liaison from the Soil Survey Laboratory, and where
applicable, the local university NCSS cooperator, should be
consulted to evaluate the adequacy of the existing data,
identify data needs, and develop plans to expand the data
available for benchmark soils in the region.
- Other considerations. The set of benchmark soils for a MLRA
should include representatives from the major parent materials
and landforms in the area. For example, coarse-loamy, mixed,
active, mesic Typic Hapludalfs may be common on both extensive
till plains and stream terraces in the MLRA. A single series
from this family might not be adequate to represent these
conditions if some key properties are significantly different
between the two settings.
Certain soils are especially important because of their use or
ecological importance in the landscape. If these soils are
essential to the understanding of landscape processes or
ecological functions within the MLRA, or interpretations for
unique land uses or land management practices, they may be
designated as benchmark soils, even if they are not extensive.
The number of soils meeting this criterion alone is small,
perhaps two or three per MLRA.
- General Guidance.
Using the criteria discussed above, select the fewest number of
soils required to adequately represent the soils in the MLRA. By
considering extent, taxonomic placement, ecological significance,
major parent materials and landforms, uniquely important soils, and
existing data, an optimal benchmark soil list can be developed.
Maintaining a Record of Benchmark Soil
Data Needs (630.03)
- Maintenance.
The benchmark status designation for soil series is recorded in the
Soil Classification Database (SC). This database is managed by the
assigned MO staffs. Soil surveys are dynamic; consequently the
adequacy of the current benchmark soils status needs to be evaluated
periodically as soil survey information is updated. While changes
can be made at any time, keep in mind that if changes are made too
frequently, the effectiveness in fulfilling the intended purpose of
the benchmark soils may be diminished. The benchmark soils
designation is recorded for soil series within MLRAs.
- Access to Benchmark Soil List.
Use the on-line Soil Series Classification (SC) or Official Soil
Series Descriptions (OSD) data access search routines to access and
sort benchmark soils. These files are on the soils Web site by
selecting View OSD by Query at
http://soils.usda.gov/technical/classification/osd/index.html or
by selecting Create Report by Query at
http://soils.usda.gov/technical/classification/scfile/index.html.
- Development of a Comprehensive Report.
Each MLRA soil survey office leader, in consultation with the
technical team members, the MLRA Management Team, and NCSS
cooperators as appropriate, develops a comprehensive report
summarizing the kinds of data and information currently available
and data needed to predict the behavior of soils in each major land
resource area. This report compares existing data and information on
benchmark soils with needs to determine the adequacy of information
for the major land resource area. This comparison helps plan for
studies of soil properties, qualities, and behavior.
- Narrative Record of Each Benchmark Soil.
Based on the comprehensive report, a narrative record of each
benchmark soil is provided to state soil scientists for
distribution. The record helps to facilitate long-range planning and
to encourage cooperative ventures with research institutions.
Discuss the kinds of special studies and soil properties needed.
Include literature references of research studies on the benchmark
soil. Refer to Exhibit 630-1 for an example of a narrative record.
Sample Narrative Record for Benchmark Soils
(Exhibit 630-1)
BETA SERIES -- a member of the fine-loamy, mixed, superactive, frigid
Typic Argiustolls family. It dominantly occurs in the Rolling Soft Shale
Plains, Major Land Resource Area (MLRA) 54, but it also extends into the
Southern Dark Brown Glaciated Plains, MLRA 53C. The Beta series is about
105,000 acres in extent. Most areas of Beta soils are in privately
managed grasslands used for grazing.
Beta soils are 100 to 150 centimeters deep to soft bedrock and formed
in materials derived and weathered from sandstone, siltstone, and shale
with a thin capping of glacial drift.
Other Series Represented: The Beta series is similar to the following
series in MLRA 54.
| Theta |
Fine-loamy, mixed, superactive, frigid Typic Argiustolls |
| Gamma |
Fine-loamy, mixed, active, frigid Typic Argiustolls |
| Delta |
Fine-silty, mixed, superactive, frigid Typic Argiustolls |
Data can potentially be used as a surrogate for these similar soils,
but care should be taken when extending data for one soil series to
another to ensure that the extension of data is reasonable for the
particular case under consideration. These series, along with the Beta
series, collectively are about 225,000 acres in extent.
The Beta series was selected as a benchmark soil primarily because it
is an important soil occupying upland positions that have been impacted
by glaciation in this otherwise unglaciated area. In addition, these
soils support some of the most productive grasslands in the area.
Information needs: In MLRA
54, knowledge of the properties, qualities, and behavior of the Beta
soils is useful in understanding: (1) the effect of changes in cropping
systems and management practices on dynamic soil properties, (2) the
penetration of roots and the movement of water into the soft bedrock,
(3) pesticide and nutrient fate and transport for surface water and
groundwater assessment, (4) the use of soils with soft bedrock for
septic tank absorption fields, (5) the Silty rangeland ecological site,
and (6) the use of soils with soft bedrock for building site
development. The bedrock underlying Beta soils contains deposits of
strippable coal, and the knowledge of soil properties, qualities, and
behavior is important for the development of effective soil reclamation
measures.
Data needs: The following dynamic properties and morphological
attributes are needed across the common crop management systems:
saturated hydraulic conductivity, soil bulk density, organic carbon,
surface roughness, consistence, structure, and macropore characteristics
(geometry, frequency, distribution, and continuity). The purpose is to
integrate the macropore characteristic with structure, particle-size
distribution, and mineralogy in order to develop a pedotransfer function
that predicts saturated hydraulic conductivity.
Laboratory data: NRCS NSSC Soil Characterization Database:
User Pedon ID
82STATEFIPS031005
84STATEFIPS021002
87STATEFIPS005001
91STATEFIPS007007
97STATEFIPS013011
ANYSTATE University pedon data
(List sources and contacts where information can be acquired)
< Back to Part 630 Contents
| |
|