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NORTH CAROLINA PLAT FIELD DATA COLLECTION
FREQUENTLY ASKED QUESTIONS – SERIES 1
- How far downstream can a pond
exist and still claim credit for the pond as a BMP in PLAT?
The rule to use when assessing the eligibility of any of the PLAT
BMPs is that the practice (pond, sediment basin, buffer,
water table control
structure) must either exist (or be plannend for) in the
area between the land where the nutrients are applied and a perennial
stream
(or an intermittent
stream with uninterrupted concentrated flow to a perennial
stream). By
definition, a perennial stream is one in which water flows
or stands all year long in a normal year. If a perennial
stream feeds the pond, then it cannot be included as a PLAT BMP.
- Can credit be claimed for BMPs that are “planned” in
the determination of the PLAT rating?
Generally, yes, because running PLAT is just a part of developing
a nutrient management plan. A major benefit of the PLAT approach is
that it can be used as a planning tool to identify needed BMPs that will
reduce potential P losses. When BMPs are claimed in PLAT, either
directly in the BMP section, or indirectly through the entry of a “planned” soil
loss estimate, these are documented on the PLAT results printout. If
the management or BMPs specified in PLAT do not exist at the time PLAT
is run, then a conservation plan for the field(s) must be developed and
include the identified practices. Similarly, if a soil erosion rate
is entered in PLAT that is less than the existing soil erosion rate for
the field, then erosion control practices must be included in the conservation
plan that support the soil erosion rate specified in PLAT. All such “planned” BMPs
credited in PLAT must be scheduled and installed during the first year
of the nutrient management plan.
The exception to the use of “planned” BMPs in PLAT is when
PLAT is run in response to the DENR requirement to run PLAT in preparation
for the next NPDES permitting. Because a full nutrient
management plan is not being developed at the same time,
then the PLAT
rating should be computed using existing conditions for
the field.
- The drainage spacing seems to make a
big difference in the resulting PLAT rating. How should
the drain spacing be computed to ensure an accurate PLAT
rating?
Dealing with artificially-drained fields can be confusing. This
confusion exists primarily because of the diversity of soils and drainage
classes that often exists within a single field. If the field is
composed of soils that are all poorly drained or the field is entirely
drained through artificial structures (open ditches, tile lines), then
the planner should designate “YES” on the drainage question
in PLAT, and the drain spacing and depth should be entered. For
regularly-spaced drains, enter the distance between drains (in feet). For
irregularly spaced drains, divide the area of the field
(in square feet) by the linear distance of drains (both
surface and subsurface)
to obtain
the drain spacing.
If only a portion of the field is poorly drained and requires artificial
drainage, then the planner must decide whether subdividing
the fields is appropriate. See the question and answer
below for guidance on determining when subdividing fields is
appropriate.
If the decision is to subdivide the field into two parts based
on drainage class, then each portion must have PLAT analyzed
separately. The
drain spacing for the poorly drained portion of the field is computed
using either of the procedures described above. For the portion
of the field not requiring artificial drainage, designate “NO” on
the drainage question in PLAT. If the decision is made not to subdivide
the field, then the planner should answer the entire drainage question
(YES/NO, drain spacing and depth) based ONLY on the drainage in the predominant
portion of the field – not the entire field.
In summary: the drainage spacing should be calculated based only
on the portion of the field that needs drainage.
- What about fields that have only a perimeter
ditch along one edge? How is drain spacing computed?
An open ditch may serve one or more purposes within a cropland
setting. It
may simply serve as an outlet for tile lines or other drainage structures,
and exist only to convey water drained from upslope or nearby sites. It
may also serve as an outlet for conveying surface runoff water away from
a site to prevent ponding. A common example of this would be a roadside
ditch that was installed to carry surface water from the roadway and adjacent
land. The third function is to provide subsurface drainage for water
moving laterally through the soil. From a drainage
standpoint, open ditches should only be considered in
PLAT when they
serve to provide
subsurface drainage.
In summary: if a single edge of the field ditch is the only artificial
drainage, then this field would in most cases be considered
undrained.
- We know that the option exists for planners
to subdivide fields for the purposes of running PLAT
and developing the nutrient management plan. What is the guidance
for determining when this should be done?
This question is one of the primary reasons that resource management
planning is a professional activity. Soil properties, drainage class,
land slope, drainage area and direction, and applicability of BMPs may
all vary WITHIN any single field. Recording all this variability
is not feasible. Thus, one of the first tasks of any resource planner
is to decide when the conditions within an individual field are so diverse
that the field should be subdivided for planning purposes, and when the “predominant” conditions
in a field can be used to represent the entire field. As
with RUSLE soil erosion computations, collecting soil
samples, pest
management planning, nutrient management planning, and
of course, PLAT analyses
all
require
professional judgment.
The planner should look at this in-field variability from two dimensions: “areal
extent” and “impact”. First, if the field is generally
homogeneous, but only a small portion of the field is “dissimilar”,
then generally it is advised to use the soil, drainage class, management,
BMPs, etc from the predominant portion of the field to represent the entire
field. Although there is no single “correct” threshold,
fields should generally not be subdivided when the “dissimilar” areas
represent less than 25 percent of the field.
The second dimension to consider is the “impact” from the
variability within the field. For example, if the erosion rate calculated
from the characteristics for half of the field is 4 tons/acre/year, and
the other half of the field is eroding at 5-6 tons/acres/year, it would
not be logical to subdivide the field into nutrient management subfields
for PLAT. The erosion rate should be averaged for the field. If
however, the second half was eroding at 12 tons/acre/year, then the field
should probably be subdivided because there would likely be a significant
impact on the resulting PLAT rating. By NOT subdividing,
the entire field would likely be rated as high or very
high, even though only
half the field would really have a potential for excessive
P
loss.
In general, the two best site characteristics to use in assessing
the need to subdivide fields are the variation in (1)
soil mapping units,
and (2) management and applicable BMPs within the field. A
planner might go through the following logic process:
Note: This is simply one way of logically considering
this decision. Whatever
approach is used should be logical and defensible.
It should also be remembered that subdividing fields can be used as
an optional planning tool to assist producers with high or very ratings
to identify environmentally sound areas for waste application. Even
if a decision was made to use the characteristics of the predominant
part of the field to represent the entire field, and the resulting rating
is
HIGH or VERY HIGH, the planner may still want to consider a subdivision. The
planner has the discretion to identify subfields that can realistically
be managed separately, and run PLAT on the subfields separately. This
may allow a producer in some cases to identify a significant portion
of a field that will result in a low or medium rating.
- The
buffers between our cropland fields and the surface water is often
not a regular width, and they vary in vegetation
type, and even overland flow concentration. How should be determine
buffer width and composition for PLAT purposes?
Generally buffer widths should be averaged for a field. Concentrated
flow through a buffer defeats the filtering effect of the buffer. When
a portion of a field drains through direct channel through the buffer,
that portion of the field may need to be subdivided into a subfield for
PLAT purposes. See the discussion and flowchart above on subdividing
fields.
PLAT allows users to enter the width of buffer by vegetation type. For
example, a common buffer in North Carolina would be a 20 ft vegetated
buffer of grass and 15 feet of trees/shrubs. These are entered
in PLAT as two separate buffers.
- Does a buffer have to be immediately
adjacent to a field to claim the buffer credit?
No. If the field drains through the buffer prior to reaching the
surface water, then it may be counted, regardless of distance from the
field. See question number 1. Planners should be cautious,
however, of concentrated flow through the buffer.
- When wetlands occur in buffers, should
these be considered a surface water, and ineligible for credit as
part of the buffer practice?
The answer is that it depends upon the type and location of the wetland.
Obviously, it is not realistic or desirable to map all the wetlands
in the buffer as part of the nutrient management planning process. The
essential question is where do excessive nutrients moving from the
field reach a perennial stream?
Planners should understand that PLAT provides no credit for a buffer
in reducing soluble or leaching P losses, so the function of the
buffer is for particulate P only -- primarily P attached to soil
particles in runoff. A recognized ecological function of a wetland where sufficient
vegetation is present is the trapping of sediment and attached material. Similarly,
in depressional wetlands within a buffer that have standing water through
a portion of the year, there should be a particle-trapping function similar
in concept to that identified for sediment basins. So simply meeting
the criteria for being a wetland (hydrology, hydric soils, hydrophytic
vegetation) should not in itself make a site ineligible to be considered
part of a buffer.
An exception to claiming this particulate P reduction credit for
wetlands within a buffer exists when the buffer includes a permanent
or seasonally
inundated wetland that is directly connected to a perennial stream. In
this situation, the edge of the wetland essentially becomes the edge of
the stream, at least for some period of the year. Since the buffer
width for PLAT purposes is measured from the edge of the field (on
which PLAT is being run) to a stream, this exception eliminates the
unintended identification of the stream itself as a buffer.
In summary, wetlands vary in nature from site to site. If the wetland
area of the buffer is seasonally inundated under standing water each year
(not just periodic storm event flooding) -- AND the inundated area includes
(is directly connected to) a perennial stream, then the buffer width should
only extend from the edge of the field to the estimated edge of the seasonally
inundated stream/wetland. If a buffer area contains a depressional
area that is inundated seasonally but NOT directly connected to a
perennial stream, then the buffer width may include this wetland.
Once again, this determination requires professional judgement by
the planner. The soils database does contain data by soil type on whether
it is seasonally flooded and duration information, etc. that could be
used in cases where it is questionable. The soils and topo maps
do also include the identification of perennial streams.
A word of caution: Planners need to be aware of misperceptions that
may be associated with this issue. Just as with any buffer,
the wetland would not be considered part of the waste application area
-- waste is not applied in the buffer. In addition, the use of
buffer BMPs in PLAT is not an authorization to over apply manure
to the extent
that direct runoff of the material occurs.
- The receiving slope is difficult to determine
on the flatter Coastal Plain settings. How should receiving slopes
be determined on these sites?
To determine the length of the receiving slope, simply identify the
lower end (toe) of the RUSLE slope. This is defined as either the
edge of the field or where deposition starts within the field. The
receiving slope is defined as the distance between this point (where
deposition starts) and the edge of the field.
In general, the rule of thumb is that if a receiving slope is really
difficult to identify when standing in the field, it probably (1)
does not exist, or (2) will make such a small difference in the sediment
delivery that it does not matter. (The sheet and rill erosion
on slopes less than 3 percent is generally low.) If a receiving slope
is not evident,
do not report one.
- Is there any guidance on the number and methodology for collecting
deep samples when these are required?
Yes. There is a SoilFacts information sheet available on the NCSU
nutrient management web page that contains guidance on the proper
procedures for collecting deep samples to prevent contamination.
The number of samples required depends, just as with an agronomic
sample, on the soil diversity within the field. Logistically, it is not
realistic to pull the same number of deep samples as the agronomic sample;
however, at least 5 samples per field should usually be collected. If
there are significant differences expected in the texture of the subsoil
material or nutrient application history within the field, it is advisable
to separate these samples rather than submitting a single composite deep
sample for the entire field. This provides flexibility in the
planning process to subdivide the field if needed.
- How long is the PLAT rating applicable? Does it have to
be re-run every year, or when the plan is amended, or when the plan
is revised?
A PLAT rating applies for the life of the nutrient management plan. USDA
nutrient management policy specifies that nutrient management plans must
be revised at least every five years, or earlier if revisions are needed
due to changes in the operation. PLAT only needs to be run when
the nutrient management plan is written or revised.
- What is the policy on the 4” versus the 8” sampling
depths for grassland and conservation tillage?
The soil sample to be used by PLAT should be the standard agronomic
sample depth for the crop as recommended by NCDACS and NCSU. This
is 8 inches for conventionally tilled crops, and 4 inches for pasture,
hayland, and no-tilled crops.
- If as a planner, you think the soils data mapped in a field
is not correct or that the field is predominately composed of an
inclusion(s) in the soil mapping unit, how should this be handled?
The soils data used by PLAT and the nutrient management plan should
always be based on the soil mapping unit identified on the official NRCS
soils map for the county, with the following exceptions:
If you think the soils data for the field being planned is not
correct, then you should contact your NRCS Area Resource Soil Scientist
to
request assistance. An on-site soils investigation may be warranted in some
cases. Except as indicated below, planners should always use
the mapping unit identified on the official NRCS soils map.
If the field being planned falls on a portion of a soil mapping
unit that is predominantly within a soil inclusion as listed and
described in the official NRCS Soil Series Description for the county,
then
you may document this determination in the “Add Comments” feature
of the PLAT print out. If this determination is made, it should
also apply in the resulting nutrient management plan, and be documented
accordingly. This option is intended to help overcome limitations
in the use of soils maps due to the original mapping scale. Abuse
of this option will result in bad things… very bad things.
If the soils in your county are currently being remapped and the
newly mapped series is not yet available within the PLAT soils
legend for
the county, contact your local soil scientist. Procedures will
be developed to accommodate these situations as quickly as possible.
- What data may be used to estimate the nutrient application rates
in PLAT?
PLAT requires the entry of the planned or estimated nutrient application
sources by type, amount, and application method. This data is
used to compute the potential source P transport off-site.
The material and amount specified in this section may come from
an existing nutrient management/waste utilization plan, historical
records,
or in cases where neither exists, the type and amount of material
that is tentatively planned to be applied to the site. The amount
specified in the final nutrient management plan may not exceed
the amount used
to generate the PLAT rating for the site.
The P content of the material entered into PLAT may be derived
from laboratory analysis, the default values that already exist
in PLAT,
or historical data. See the 590 NRCS Nutrient Management Standard
for the criteria for specifying the nutrient values for animal
waste to be
applied.
- Is there any opportunity to get some additional field training
on collecting the data to support PLAT?
Yes. Optional field training for agency staff, technical specialists,
and TSPs is currently being planned. NRCS and SWCD staff should
make requests for training through their NRCS Area Office. All
others may make requests for field training to Roger Hansard, 919-873-2133,
Roger.Hansard@nc.usda.gov.
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