QDMA Articles :
Soil Test Science
By: Robert N. Smith
The importance of testing your soil
before planting food plots has been stressed in many previous
articles in Quality Whitetails. The process is quick, inexpensive,
and makes a world of difference in the quality and productivity
of your plots.
Most serious food plot planters test their soil before planting.
However, once they receive the soil analysis back from the lab,
many are left scratching their heads trying to make sense of the
report and calculate appropriate lime and fertilizer requirements.
This article will detail how to read a soil sample and implement
the recommendations in the field.
Before outlining how to interpret a soil analysis, some background
information is needed. Plants can be thought of as nutrient transfer
agents to get nutrients from the soil into the deer. The condition
and quality of the soil affects how well plants can transfer nutrients.
Managing soil fertility impacts how well plants grow, and how
nutritious they are. In brief, collect six or more samples from
each plot to be planted and mix these in a plastic or glass container.
Then collect a single subsample from this mixture. The samples
should be collected diagonally across the plot to ensure all soil
variability is accounted for. Records should be kept for reference
when collecting future samples from the same plot.
Sampling depth is one of the most important aspects of soil testing.
Soil levels can vary greatly between three and six inches deep.
A core sampler which collects 4-inch samples is the most commonly-used
sampling tool, although a shovel or hand spade can do the job.
After each food plot has been representatively sampled, the sample
should be labeled with location and type(s) of seed or seed mix
to be planted. The samples are usually sent to a Cooperative Extension
Service, university, or private agronomic laboratory for analysis.
Some fertilizer companies offer free analysis to their customers,
while most other labs charge a nominal fee of $5 to $12 per sample.
It is important to remember that different plants have different
nutrient needs. This is especially important when planting mixes
containing both broadleaf plants like clover, and grasses like
wheat. With a little experience or professional advice, you will
soon learn which plants have the highest lime and fertilizer requirements.
Soil tests are performed on subsamples to estimate soil acidity
(pH) and the amount of available nutrients in soil. The results
are then summarized and printed. The difference between the available
nutrients and the amount needed by the plants for optimum production
is then recommended. Lime and fertilizer amendments are generally
grouped for food plots with similar soil test results.
SOME SIMPLE SOIL FERTILITY CONCEPTS
Some soils can retain and transfer nutrients better than others.
Lime and fertilizer applications are the most efficient in the
best soils, so selecting high quality sites for food plots is
important. Two important soil fertility characteristics are 1)
how much total nutrition the soil can hold and, 2) how much of
that nutrition is actually available. Soil nutrients may be lost
or made unavailable through leaching, plant uptake, browsing
(physical removal), volatilization, denitrification (loss of nitrogen),
acidification, microbial uptake, and erosion.
Soil scientists use the term "cation exchange capacity"
to explain how much transferable nutrition soils can sustain.
Organic matter and soil texture are two important determinants
of cation exchange capacity.
Decomposed organic material in the soil increases the soil¹s
ability to hold water and nutrients. Though it may be beneficial
in the long run, putting large amounts of fresh organic matter
(e.g., manure) on the soil can decrease the available nutrients,
especially nitrogen, in the short term as microbe populations
break down the complex carbon molecules. This short-term utilization
of available nutrients by decomposer organisms is
why organic gardeners compost material before adding it to the
soil.
Soil texture (size of particles) is important because it determines
the surface area available to hold soil water through surface
tension. Size also controls the sites that available nutrient
ions can be held onto the soil. Clays are the finest textured
particles, sands are the largest, and silts are intermediate.
To help envision the impact of particle size, think about sand
as double 00 buckshot (9 pellets in a standard 12 gauge shell)
and clay as number 8 shot with 238 pellets in a comparable load.
A cubic foot of sandy soil can have a surface area of 0.9 acre,
while soils with more silt and clay can have three acres or more
of surface area in a cubic foot. In brief, the greater the surface
area of the soil, the more nutrients and water it can hold. While
a soil such as clay may contain a large amount of nutrients, if
the nutrients are not available for plant uptake, neither plants
nor wildlife benefit. For nutrients to be available, there needs
to be 1) adequate soil moisture, 2) good soil tilth (fluffy but
firm), 3) a soil microbe population in balance with organic matter,
4 )suitable pore space and aeration, and most importantly, 5)
a proper pH for the crop being grown.
LIME
Soil acidity impacts nutrient availability. In an acidic soil
(low pH),nutrients are bound to soil particles making them unavailable
to the plants. If fertilizer is added to an unlimed acidic soil,
only a portion becomes available. The remainder, sometimes the
majority of the nitrogen and phosphorus, is bound to the acidic
soil particles. Lime is the agent that can change the nutrient
balance and free nutrients for plant uptake. As pH increases up
to the optimum range (generally between pH 6-7) for the crop,
nutrients become more available. In addition, since most soil
fungi and bacteria cannot tolerate acidic conditions, they do
not break down organic matter efficiently in an acidic soil. The
addition of lime allows these microbial populations to flourish
and release the tightly bound nutrients. The result is an indirect
fertilization. Two important characteristics of lime are the kind
of lime and the size of the lime particles. All agricultural liming
materials are compared to calcium carbonate to allow for comparison.
If magnesium is needed in the soil, then dolomite is the preferred
liming material.
With all other factors being equal, the finer the lime is ground,
the more rapidly it acts and the more thoroughly it is mixed into
the soil. Conversely, the more grinding done, the higher the cost
and the more rapidly its effects are lost. Lime particles larger
than half an inch are practically useless, while those smaller
than 0.06 of an inch are 100 percent effective. Most agricultural
limestone generally passes through a half-inch mesh screen with
25 to 50 percent passing through a 0.06-inch mesh screen.
Similar to many nutrients, lime can be leached from the soil.
This happens most rapidly in warm regions with abundant rainfall
and especially on sandy soil. Many premium forage plants, such
as alfalfa and some clovers,
require a pH of 6.0 or higher. If you are trying to grow one of
these plants, choose soils with a clay component and lime regularly.
While some food plots may only need liming every two or three
years, on some sites it is necessary to lime annually, especially
for the first few years after a new food plot is created. Lime
is also needed more frequently in areas where high amounts of
the ammonium form of nitrogen are added, where crops with high
calcium and magnesium needs are planted, and where maintenance
of a high pH is critical for crop production.
SOIL NUTRIENTS
Similar to the test for soil pH, tests for nutrients involve extractingthe
available nutrients from a known quantity of soil in a water mixture.
The nutrients most commonly tested for include phosphorus, potassium,
calcium, and magnesium. Micronutrients that may be tested for
include boron, zinc, copper, manganese, and iron. Tests for nitrogen
and sulfur are generally not conducted because the rate at which
they are released from soil organic matter or transferred into
gaseous form cannot be reliably predicted. In areas where soils
are highly deficient in sulfur or calcium, highly concentrated
fertilizers are not recommended because they rarely contain these
elements.
SOIL TEST INTERPRETATION AND USE
Soil test results are usually returned with one page for each
sample submitted. This page will contain a summary of the available
nutrients in the soil and may include a table and/or bar graphs
showing whether the sample has a low, adequate, or high availability
for each nutrient tested. The results will also contain a recommended
lime and fertilizer amendment to enhance the soil for the plant(s)
of interest. The amounts of nitrogen and sulfur recommended for
a specific crop are based on fertilizer trials in the region of
the state where the soil sample originated. Since nitrogen can
easily be lost, recommendations often call for a split application
- half at planting and half just before major plant growth. Micronutrients
are generally not added unless the soil test indicates there is
a deficiency. Specific tests for micronutrients are typically
done when plant deficiency symptoms (typically yellow or purple
coloration or irregular growth habits) indicate a problem.
Soil test results from all food plots should be divided into groups
needing similar amounts of amendments. Unless you only have a
small number of food plots, it usually is not cost effective to
treat each food plot with exactly what it needs, so a general
prescription is made for each group of similar food plots. These
soil test results will usually be grouped by some correlated characteristic,
like hills and bottoms or new food plots and old food plots. With
new food plots, it can take five to eight years of high annual
nutrient amendments to build up the available nutrients before
getting onto a maintenance application of lime and fertilizer.
Considering the topographic position, soil color, and soil texture
can help you logically group your plots. When developing a recommended
amendment for a group, it is important to keep the nutrients in
balance. Too much of one nutrient may interfere with availability
or uptake of other nutrients or leach into adjacent water. Adding
too much of some nutrients can result in plant death or lack of
germination. For example, over-application of animal waste high
in manganese can result in manganese toxicity and food plots that
don¹t reliably produce forage for several years.
The type of lime or fertilizer used usually depends on three factors:
1) the material¹s ability to provide the needed nutrient
changes in the soil, 2) material cost, and 3) transportation and
spreading difficulties and costs. For small or isolated food plots,
getting the material to the plot and spread is usually critical.
It is difficult or impossible to get commercial applicators to
take large equipment, sometimes even tractors, into some small
food plots. If transportation or spreading with small equipment
or by hand is involved, using concentrated materials that may
cost a little more per ton may be justified.
For practical purposes, the minimum amount of lime to spread is
two tons per acre since this will not "overlime" any
food plot that shows a need forlime through a soil test and it
optimizes the use of transport and spreading equipment. From an
economical standpoint, the best time to lime is just before or
after most farmers in your area have applied lime. Lime contractors
would much rather work on large agricultural fields than in small
scattered food plots, so it can help to offer them work while
their equipment is idle. For most nutrient efficiency, especially
alfalfa or other pH dependent plants, lime should be applied five
to six months prior to planting to allow it to have time to impact
soil chemistry. If the soil test calls for two tons of lime equivalent,
then you need two tons of calcitic limestone, 1.8 tons of dolomitic
limestone, or 3.3 tons of basic slag. This is calculated by taking
the tons needed and dividing by the percent CaCO3 equivalency
in decimal form (1.10 for dolomitic lime). For example two tons
divided by 1.1 CaCO3 equivalents equals 1.8 tons.
If the recommendation is to apply 80 pounds of nitrogen, 80 pounds
of phosphorus, and 80 pounds of potassium per acre, the nutrients
could be supplied in 800 pounds of 10-10-10, 615 pounds of 13-13-13,
or 400 pounds of 20-20-20. Obviously, if you are spreading this
by hand, then you may want to consider using 20-20-20, even if
it is more expensive. Calculating fertilizer rates is done by
dividing the recommended application rate by the fertilizer analysis
(number on the bag for that nutrient) multiplied by 100. For instance,
if using the fertilizer 0-0-60 (0 percent N, 0 percent P2O5, and
60 percent K2O), and the recommended application rate is 120 pounds
potassium (K2O) per acre, then the rate is:120 pounds K2O needed
divided by 60 pounds K20 times 100 which equals 200 pounds of
0-0-60 per acre. This calculation would be done for each nutrient
to be added, with slight over-application preferred.
When dividing food plots into groups for treatment and deciding
what materials to use in the food plot, it often pays to work
through this process with your local fertilizer applicator. It
is in their best interest to help you manage your soil fertility
since lime and fertilizer application is a recurring need. Cooperative
extension service agents or other knowledgeable professionals
also can provide recommendations.
Soil tests are not infallible, but the recommendations are generally
pretty good and far better than any "seat-of-the-pants guess."
Keeping copies of the soil test recommendations and watching the
success of the food plots after following the recommendations
can enhance your confidence in this important, but often overlooked,
tool.
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