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How to Interpret Yout Soil Test Results
October, 2017
Dr. Maria L. Silveira,
UF/IFAS RCREC, Ona
Soil testing is the best tool for monitoring soil fertility levels. However, interpretation of soil test results can be somewhat confusing. This document provides a brief explanation of the general guidelines for interpreting soil test results.
Field Sampling
The first
step in ensuring reliable soil test results is proper soil sample
collection. Soil results and interpretation are only reliable if the samples
are collected properly. In other words, the test results are only as good as
the sample taken. It is very important to submit soil samples to the
laboratory that truly represent the area of interest so that test results
are reliable and fertilizer recommendations can be made for the entire area.
This can be accomplished by submitting a composite sample. A minimum of 15
to 20 subsamples (approximately 6 inches deep) should be collected from each
field. Samples should be taken at random in a zigzag pattern over the entire
area. Areas that are managed or cropped differently should be sampled
separately. Similarly, areas that show clear problem signs (i.e., poor
forage production, disease) should also be sampled and analyzed separately.
Avoid sampling areas not typical of the total field such as near water,
feed, or shade.
Soil testing laboratories
offer a wide range of parameters. In general, most soil test reports include
the determination of pH, buffer pH, phosphorus, potassium, calcium, and
magnesium concentrations. Micronutrients (e.g., zinc, copper, iron, and
manganese), organic matter, and physical properties (e.g., percentage of
sand, silt, and clay) can also be determined. Since laboratories use
different test methods, it is very important that the soil testing
laboratory selected to conduct the soil test uses the procedures recommended
by University of Florida. In Florida, Mehlich-3 is
currently the standard soil test procedure to determine the concentration of
plant available nutrients. Lime recommendations are based on Adams-Evans
procedure. Using a testing procedure not applicable to Florida soils can
result in misleading soil testing interpretation and recommendations.
Although nutrient concentrations in the soil are not expected to vary
considerably from year to year, tracking soil test results over time can
provide useful information relative to the effect of liming, fertilization,
or past management decisions on the fertility status of the soil. Monitoring
changes in pH and level of a particular essential nutrient can also help
farmers to determine soil fertility approaches that sustain adequate crop
production.
Soil pH
Soil pH
is the most commonly measured soil property. It describes the relative
acidity or alkalinity of the soil and represents one of the most useful and
informative soil parameter because its relationship to many aspects of soil
fertility and plant growth.
The pH
scale ranges from 1 to 14, however most inorganic soils in Florida have a pH
around 4 to 6. The lower the pH values, the greater the acidity in the soil.
Soils with pH less than 5 are considered strongly acid, while values of 5 to
5.5 and 5.5 to 6.5 are considered moderately and lightly acid, respectively.
Soil pH range of 6.6 to 7.2 is considered neutral, 7.3 to 8.2 is slightly
alkaline and above 8.2 is moderately to strongly alkaline. The relatively
acidic nature of most Florida soils is due the parent material as well as
the environmental conditions (i.e., intensive rainfall) in which these soils
were formed. Agricultural practices such as the use of nitrogen fertilizers
and crop removal also contributes to increase soil acidity. Since pH is measured using a logarithmic
scale, a decrease of 1 unit of pH results in a 10-fold increase in acidity,
so small changes in pH values can have important implications.
Buffer pH
In Florida, the Adams-Evans test is used to determine the amount of lime required to adjust the soil pH to the target level.The Adams-Evans test measures the soil acidity in water and in a buffer solution (pH of 8) to determine soil lime requirement. The lower the pH of the buffer solution, the greater the amount of lime needed to raise the soil pH to the desirable level. Soils that contain more clay minerals and organic matter typically require greater amounts of lime to raise the pH.
Nutrient Concentrations
Routine
soil tests only measure only a portion of the total pool of nutrients in the
soil. They do not measure total amounts of nutrients in the soil. Rather,
most soil testing procedures are designed to mimic the root uptake of
nutrients in the soil.
One of
the major goal of testing the soil is to determine whether or not crops will respond to fertilization. Extensive research has
been done to determine the relationship between available nutrients,
fertilization application and yield responses. Of greater importance than
the actual nutrient concentration, is the classification of the degree of
nutrient sufficiency.The degree of nutrient sufficiency is reported as:low, medium, or high. In general, when soil test level is equal or
greater than medium, additional fertilization is not expected to result in
an anticipated yield response. Table 1 represents the current interpretation
of soil test results for agronomic crops in Florida.
Table 1. Current Mehlich-3 soil test interpretation for
agronomic crops in Florida (Mylavarapu et al., 2013).
Element | Low | Medium | High |
Part per million (ppm) | |||
Phosphorous (P) | ≤ 25 | 26-40 | > 41 |
Potassium (K) | ≤ 25 | 26-40 | > 41 |
Magnesium (Mg) | ≤ 10 | 11-23 | > 24 |
Cation Exchange Capaciy
Cation
exchange capacity or CEC refers to the capacity of the soil to hold positively charged ions, also
known as cations. Some laboratories calculate the CEC based on the summation
of cations (potassium, calcium, magnesium, sodium, and buffer pH) or on an
actual CEC determination procedure. Soils that contains more clay or organic
matter often exhibit higher CEC than coarse-textured soils.
Lime and Fertilizer Recommendations
Soil testing results provide
basic soil fertility information so management decisions can be implemented
to insure efficient and effective fertilization strategies for the required
forage production goals. However, caution should be exercised when
interpreting fertilizer recommendations generated by commercial laboratories
because they typically use different soil fertility approaches. For
instance, while University of Florida fertilizer recommendations are based
on crop nutrient requirement, fertilizer recommendations generated by
commercial labs (particularly out-of-state) may be target at building up
nutrients in the soil. However, given the environmental conditions in
Florida associated with the coarse-textured soils, most Florida soils have
limited ability to retain nutrients; therefore, for economic and
environmental reasons, the nutrient “build up” approach is not appropriate
for our conditions. In addition to the soil test results, economic issues
(e.g., fertilizer cost, hay prices) must also be considered when choosing
the most adequate fertilization strategy. Decisions regarding liming and
fertilizer sources should be based on cost, availability, soil
characteristics, and forage management.
From time to time, we come
across some issues associated with analytical error or improper soil
collection or handling that result in unusual soil test results. It is
important to identify these potential limitations. Drastic changes in soil
test results or zero values may indicate an unrepresentative soil sample or
a laboratory error. When in doubt, the best approach is to collect and
submit a new sample or contact the lab to repeat the analysis. If you need
further assistance, please consult with your local county agent or other
university personnel.