What
a Soil Test Tells You
A soil test is a "snapshot" of
the chemical status of your soil. The
test report shows the pH (degree of acidity), and the available amounts of various
plant nutrients that were present in your soil at the time of sampling. Some soil tests also report total organic
matter present in the soil. The soil test report is an index of the
chemical aspect of soil fertility, and therefore tells only part of the story. It is a valuable diagnostic tool, but it
cannot alone tell you the correct way
to manage your soil.
Three
Aspects of Soil Fertility
Physical
– good drainage, aeration, moisture-holding capacity, and ease of penetration
by plant roots. A crumbly, porous, deep soil provides all of these, is easy to
work, and is said to have good tilth,
or good physical structure.
Chemical
- adequate levels of all essential plant nutrients, favorable pH, favorable
nutrient balance, freedom from toxic excesses of any one element.
Biological
- diversity of beneficial soil organisms (bacteria, fungi, protozoa, nematodes,
tiny insect-like creatures, earthworms, etc.)
that digest organic residues (fallen
leaves, manure, crop residues, etc.)
into humus (the decomposed organic
matter that makes topsoil dark brown and enhances its capacity to hold water
and nutrients). This activity is called
the organic matter cycle, and it releases nutrients in plant-available
form. In addition, healthy and diverse
soil life promotes good tilth and protects plants against soil-borne pathogens.
The
Soil Life is the Engine of Soil Fertility
In nature, the organic matter cycle
provides all of the nutrients that support the natural vegetation. In agriculture, we remove some organic
matter and nutrients in harvest, and therefore we have to "feed" the
soil life to maintain fertility. This
is done with compost, cover crops, crop residues, organic mulches, and
sometimes purchased organic fertilizers.
In a well-balanced, fertile soil, that
is receiving adequate organic inputs each year, the organic matter cycle will
provide your crops with most or all of the nutrients they need: nitrogen (N), phosphorus (P), potassium (K),
calcium (Ca), magnesium (Mg) sulfur (S) and micronutrients such as boron (B),
copper (Cu), zinc (Zn), iron (Fe), manganese (Mn), molybdenum (Mo) sodium (Na)
and silicon (Si). However, in the real
world of gardening and farming, some mineral supplementation is often needed. This is where the soil test becomes useful.
Mineral
Amendments – which ones, and how much?
In addition to compost and other organic
matter, the soil often needs certain mineral supplements in order to reach
optimum fertility and crop yields. This
may occur because:
(1)
past farming practices have depleted some nutrients,
(2)
the soil is naturally low in certain nutrients, or
(3)
the soil is too acid or too alkaline for the crops you
are growing.
A soil test can help identify the
amendments and amounts your soil needs.
If the testing laboratory gives recommendations for organic gardens and
farms, this is most helpful. Otherwise,
you may have to "translate" conventional fertilizer recommendations
to organic amendments.
Taking
a Soil Sample
Getting a good representative sample is
very important for obtaining a meaningful soil test report. Collect a soil sample by taking cores 0-6
inches deep (0 to 8 inches for a garden with deep topsoil) from 12 to 25 points
evenly scattered through the field or area you are testing. If you do not have a coring tool, dig a hole
about 8 inches deep with a shovel, leaving a smooth nearly-vertical
surface. Use a trowel to take a small,
even slice of soil from 0-6 inches depth along this surface. Combine and thoroughly mix the 12 to 25
samples in a stoneware crock or clean plastic bucket (not metal, which can cause false readings for iron, aluminum or
zinc). Allow the combined sample to dry
for a day or two at room temperature (not
in direct sunlight). Then put a pint of air-dry soil into a
sample bag provided by the lab, or a ziplock plastic bag, and mail it to the
lab with your testing instructions, payment and a brief description of the
field.
If you are farming several fields, do a
soil test for each. Also, if you know
that two or more sections of a given field have different soil types, or widely
different cropping histories, take a sample for each section.
Reading
the Report
Usually, the lab will report each
nutrient in parts per million (ppm) or pounds per acre (lb/acre). NOTE: 1 ppm = about 2 lb/acre in the plow
layer (6 inches depth). These numbers
represent an approximation of the plant-available
nutrients present, not the total amount of each element in the soil. NOTE:
some labs report elemental P and K, and others report phosphate (P2O5)
and potash (K2O). 1 ppm P =
2.3 ppm P2O5; 1
ppm K = 1.2 ppm K2O.
Most labs will follow the number for
each nutrient with a letter code as follows:
VL = very low (critically
deficient); L = low (likely to
restrict crop yield); M = medium
(sufficient for most crops, may be limiting to heavy feeders); H = high (favorable); and VH = very high (ample, possibly
excessive). Any nutrients that are
rated VL or L on your soil test usually needs to be supplemented, whereas
nutrients rated VH may indicate a
need to cut back on inputs of those elements.
Direct measurements of soluble soil nitrogen (N) are often misleading, as
this element can fluctuate wildly between nearly undetectable and excessive
levels (that may leach to groundwater) within a single season. Therefore, many labs do not report N per se, but give an estimated nitrogen release (ENR) in lb/acre-year, based on the
soil's organic matter content, and texture.
If the ENR is 120 or more, the organic matter will provide most or all
the N needed by most crops.
The soil test will also give soil pH. A pH of 7.0 is neutral; 6.0 is mildly acid,
5.0 is strongly acid, and 4 is extremely acid, while numbers above 7 indicate
alkaline soil. Most crops prefer a pH
of 6.0 to 6.8, although they will thrive at anywhere from 5.5 to 7.5 if soil
life is healthy and balanced.
Strawberries and brambles do well at pH 5.5 to 6.0; and blueberries at
about 5.0.
A good soil test should include a
measurement of total soil organic matter (SOM), usually given in percent. This is a rough estimate of the vigor of the soil life and organic matter
cycle. Generally, good SOM levels for
tilled fields are 1.5 to 3% for sandy soils, 2.5 to 5% for loams, and 4 to 6%
for heavy, clayey soils. (These figures
are for “wet chemistry” methods for total OM; “loss on ignition” figures are
often 1.5 times as much.) The warmer
the climate, the lower the SOM, even if soil life is healthy and active. So
don’t let those northern gardeners give you an “organic matter inferiority
complex!” If your soil is dark brown, crumbly and well drained, and plants are
thriving, the soil probably has a healthy organic matter cycle. It is actually possible to have too much
SOM. At 7 to 10%, it may tie up
micronutrients, leach nitrate to the groundwater, or contain so much available P
and K that plant nutrition is unbalanced.
Some labs also report cation exchange capacity (CEC). This is an estimate of the soil's ability to
hold positively charged (cation)
nutrients in plant-available form, especially K, Ca, Mg and Na. The soil's CEC resides in its clay and humus
content; thus rich, clay-loam soils will have a high CEC, and dry sandy soils
will have a low CEC. Building soil
organic matter will somewhat enhance CEC.
Some farm consultants and soil test labs pay attention to the relative amounts of Ca, K and Mg held on
a soil’s CEC (base saturation ratio), and seek to adjust the cation
balance. For more on cation balancing,
see the VABF information sheets, Soil
Cation Nutrient Balancing – missing link or red herring?, and Does My Soil Need Cation Balancing?
How to Avoid Pitfalls in Reading Soil Tests
Some
soil labs do more accurate work than others; and some provide vital data (e.g.
SOM) that others do not. Different labs
use different procedures, so that lab A
may report 100 ppm P for a given soil, and lab B only 40 ppm. Each lab
also develops its own ranges for VL, L, M, H, and VH based on experience with
its particular methodology. Find a lab
that you trust, and stick with it.
Because soil is a dynamic, living
system, its pH and the levels of some nutrients can vary significantly during
the course of one season. Retest your
soil every two to three years - at the
same time of year and using the same lab - and notice the trends. Are SOM, pH and nutrient levels approaching
the optimum range? Are “low” nutrient
levels coming up, and “excessive” nutrient levels coming down?
Some soil labs are prepared mainly to
give recommendations for chemical fertilizers, and will often recommend more N,
P, K and lime than is actually needed, even on highly fertile soils. When this happens, you can learn how to
convert their recommendations to organic inputs, or to make your own
recommendations. Or, you could switch
to an organic- or sustainable-oriented soil testing lab.
Amendments
for Specific Nutrient Problems
Acidity
(pH below 6.0): Use agricultural limestone (not hydrated
lime – it is too harsh) to raise pH. If
the soil is rated L or M in calcium, but H or VH in magnesium, use high calcium lime. If magnesium is also L or M, use dolomitic limestone. Use 1,000 – 2,000lb/acre (23-45 lb/ 1,000
sq. ft) for moderate acidity on loamy to clayey soils. Sandy soils should be limed lightly, 500 – 1,000 lb/acre - and only
if pH drops to 5.5. Retest soil one to two years later to see if more lime is
needed.
Alkalinity
(pH 7.5 or above; rare in eastern US):
Use acidic organic mulch (tree leaves, pine straw, chipped brush), avoid
liming. For strong alkalinity or for
acid-loving fruits, use elemental sulfur
at 200 - 500 lb/acre (= 5-11 lb/1,000 sq ft).
Low
organic matter: Use generous
amounts of compost (5 to 20 tons/acre, or 250 to 900 lb/ 1,000 sq. ft) the
first couple of years. Grow cover crops
and use organic mulch. You may need an
organic N-P-K fertilizer to obtain satisfactory crop yields at first. Grow a legume green manure or apply composted manure to provide N. Foliar-feed with fish emulsion or seamix.
Phosphorus: If P is low, supplement with colloidal
phosphate or rock phosphate at 500 to 1,000 lb/acre (12 to 23 lb/ 1,000 sq.
ft), then apply some high quality compost and grow legume or buckwheat cover
crops to unlock the P. NOTE: avoid
liming at same time as rock phosphate is applied, since mild acidity (pH about
6.0) promotes P availability.
Optimal available P (P1 or "weak
Bray") is about 20 to 40 ppm; If available P soars above 100 ppm, it can
tie up micronutrients - cut back on manure use, as manure is high in P.
Potassium: If K is low, it can often be supplemented
with manure compost and/or hay mulch, both of which are rich in K. Potassium sulfate, greensand and sul-po-mag
are three mineral amendments that can add K if the soil is very low in this
nutrient. If K gets very high (over 350
ppm or over 8% base saturation) it can make the soil sticky, upset plant
nutrition or reduce vegetable quality.
Cut back on the use of hay mulch and manure compost until K is
reduced. If both P and K are sky-high
but SOM is low, the land probably has a history of intensive chemical
fertilizer use. Grow legume cover
crops, and use mulch or compost based on leaves or brush (low in P and K) to
replenish N and SOM without aggravating P and K excesses.
Calcium: If Ca is low but pH is optimal or high, use
gypsum at 300 to 500 lb/acre (7-11 lb/1,000 sq ft) once or twice a year until
soil tests indicate that Ca levels are medium to high.
Magnesium: if Mg is low but pH is optimal or high, use
sul-po-mag or Epsom salts at 200 to 300 lb/acre (5-7 lb/1,000 sqft), and retest
soil in a year to see if more is needed.
Sulfur: If S is well below optimum (10 ppm or
lower), use gypsum at 500 lb/acre, or sul-po-mag at 200-400 lb/acre.
Micronutrients: A low level of boron (B) should be corrected
with about 5 to 10 lb borax per acre (2-4 ounces/1,000
sq ft) - no more, as some crops are
sensitive to too much B. For other
micronutrients, moderately low levels can be amended with good compost, seaweed
meal or rock powders such as granite dust (check label for micronutrient
content). A critically low
micronutrient (VL on soil test, or diagnosed crop deficiency) can be
supplemented in sulfate or chelate form.
Mark Schonbeck
Recommended Reading
Building Soils for Better Crops, 2nd ed. Fred Magdoff & Harold van Es, 1999. This is an excellent manual of sustainable soil management,
written in user-friendly language, and covering all aspects of sustainable management
of nutrients and SOM, soil conservation and proper tillage. Available from Sustainable Agriculture
Publications, Hills Bldg, Rm. 10, U. Vermont, Burlington, VT 05405-0082, for $19.95 + 3.95 shipping.
How
can organic vegetable growers increase soil organic matter without overloading
the soil with nutrients?, by Brian Caldwell, Cornell Coop. Extn. In The
Natural Farmer, vol. 2, issue 44 (Spring 2000), page 8; excerpted in Virginia Biological Farmer, Aug-Sept
2000, page 7.
This work has received funding support
from the Southern Region Sustainable
Agriculture Research and Education (SARE) program, and the Organic Farming Research Foundation of
Santa Cruz, CA. It was conducted under
the auspices of the Virginia Association
for Biological Farming, P.O. Box 1666, Louisa, VA 23093