Soil is the outermost layer of our planet that all life depends upon. Five tons of topsoil
spread over an acre is as thin as a dime. It takes natural processes at least 500 years to
form 1 inch of topsoil. Over 70,000 types of soils have been identified in the United
States. Five to ten tons of animal life can live in an acre of healthy soil.
- Healthy Garden loam (Topsoil) is composed of sand, silt, clay, humus (at least 5%),
macro-nutrients, trace minerals, micro-nutrients, and microorganisms.
- Organic matter (i.e. compost) in the top 6 inches of the soil provides:
- growth-promoting hormones
- toxins and antibiotics
- mycorrhizae fungi
- nematode destroying fungi
- unlocks minerals
- nitrogen fixing microorganisms
- increase moisture holding capacity
- sticky substances that bind particles into aggregates
- increases air space, drainage and aeration
- acts as a buffer against chemicals and high/low soil pH
- releases nutrients over a long period of time
- maintains the soil base exchange capacity
- gives soil good tilth--easy to work and till, wet or dry
- helps recycle waste products and prevents erosion
- Compost is an excellent soil amendment that also acts as a slow release fertilizer
containing nitrogen, phosphorus, potassium, trace minerals, microelements, humic
acids, fulmic acids, and other needed nutrients (vitamins, enzymes, microorganisms,
etc.).
- Healthy soils contains the following microorganisms: bacteria, fungi, actinomycetes,
algae, protozoa, yeasts, nematodes, germs, and other tiny critters. Over 13,000 different
organisms have been identified that live in the soil.

Microorganisms feed on organic matter in the soil and form glue like material called
polysaccharides. These complex sugars are what binds or welds individual soil particles
together creating larger aggregates. This process gives soil its wonderful soft crumbly
texture and helps prevent erosion.
- "A healthy soil has a constantly changing, but always active population of microbes.
There are approximately 900,000,000 (nine hundred billion) of these lifeforms in every
one pound of soil." H. Garrett, Harmony With The Environment, Acres USA, June 1993
- Humus is the dark brown to black substance that is the secret key to healthy soil. It is
nearly insoluble and contains about 30% each of lignin, protein, and complex sugars. It
contains 3-5% Nitrogen and 55-60% Carbon. Humus is the source of food and energy
for microorganisms development and is the stage of decomposition that provides food
from the soil to plants in the form of slow release nitrogen, phosphorus and sulphur.
- Mulch is the best way to add organic material to your soil. Compost is the best mulch
for this purpose.
- There are 930 billion microorganisms in each one pound of soil under turf. There are
about 70 pounds of them living and working in each 1,000 square feet of root zone.
Many of these organisms are very short-lived, so the turnover is rapid. One Hundred
pounds of dead microorganisms will contain close to ten pounds of nitrogen, five
pounds of phosphate, 2 pounds of potassium, one half pound of calcium oxide, one half
pound of magnesium oxide, and one third pound of sulfate. With 70 pounds of these
creatures per 1000 square feet of root zone, the poundage adds up to enough per acre for
excellent crop production. Elliot C. Roberts, The Lawn Institute.
- Synthetic chemical fertilizers destroy soils. As soils are being destroyed, plants become
weaker and actually attract insects, diseases and weeds. When we spray fungicides,
insecticides and herbicides we accelerate the destruction of the soil. Humus (organic
matter) is literally burned out of the soil reducing (if not eliminating) the
microorganisms that take nitrogen from the air and make it available for plants. This
requires larger amounts of nitrogen based chemical fertilizer to get plants (crops) to
grow and the cycle continues. Additionally, soil structure is destroyed greatly
increasing erosion and the leachates in the

runoff pollutes streams, ponds, groundwater, etc.
- Organic matter also stores mineral nutrients such as calcium, magnesium, potassium and
many others. It keeps these valuable nutrients from washing out of the soil, and makes
them more available to the plant (Medina Magazine).

runoff pollutes streams, ponds, groundwater, etc.
- Organic matter also stores mineral nutrients such as calcium, magnesium, potassium and
many others. It keeps these valuable nutrients from washing out of the soil, and makes
them more available to the plant (Medina Magazine).
- According to Dr. E. Ingham, Soil Biologist, Oregon State University, a teaspoon of
healthy soil is teeming with:
- 100 million or so individual bacteria
- 50 to 150 meters of fungal threads
- 10,000 to 100,000 protozoa
- 5 to 500 beneficial nematodes
- Thiamin (vitamin B1, aneurin) is a naturally occurring compound present in soils, water,
plant and animal tissue, which is required for microbial and plant growth. Thiamin is
known to affect both root and plant growth. A reduction of organic matter in soils
reduces the CEC ratio which leads to reduced Fe (iron) and Al (aluminum) availability
on the surface of clay particles which may cause a reduction in thiamin absorption.
Organic matter also helps bind thiamin with increasing pH. The absorption of thiamin
is closely related to the stoichiometric exchange of the Ca++ (calcium ion) which suggest
that absorption of Thiamin occurs by an exchange mechanism. Soil Science Society of
America Journal, Nov./Dec. 1994, p.1829
- A healthy soil will have an abundant earthworm population which is busily at work
increasing the soils fertility.
- Soil pH is constantly changing. Large changes can occur naturally with 48 hours. Soil
compaction can raise the pH level even moisture can change the pH.
- A recent study found that soil compaction reduces crop yields and plants grown in
compacted soils had greatly increased insect damage. Journal of the American Society
for Horticultural Science, 120(6):956-963. 1995
- Soils with lots of organic matter hold minerals better. A recent study of agricultural
soils found that total soil sulfur decreased in all treatments where no organic material was
added. However, of the organic amendments 26-54% of the sulfur remained in the soil
with a half-life of 24-38 years. Soil Science Society of America Journal, p.174-178,
Vol. 60 #1, January-February 1996.
- Synthetic soils (generally light weight potting or bedding media) are often soil-less, this
means they looses water very quickly, they do not retain nutrients, do not support
beneficial microbes or other beneficial organisms such as earthworms. Hence a lot of
disease and insect problems are the result.
- In Texas it is estimated that we lose up to 4,000 pounds of humus per acre each year due
to natural soil breakdown in high temperatures. Neil Sperry's Gardens, Nov.-Dec. 1996.
Note 1: Along the Gulf Coast with higher moisture levels, humus lose is even greater.
Note 2: Freshly organic matter contains 1-2% humus or less. It is the action of microbes
and earthworms that convert organic matter into humus. Depending on the form of
organic matter, it could take 400 cubic yards per acre each year to replace what is lost.
- One of the biggest problems we have with our soils is the loss of trace and micro
nutrients (i.e. minerals). The growth and health of plants is limited by the least available
nutrient. As plants grow the minerals are used up to form plant tissue from stalks and
leaves to the fruits and vegetables we eat. If the minerals needed for good health are not
in the soil then they are not in our food (plant or animal) and our health suffers. To
restore soil health we must add back mineral dusts (lava, granite, basalt, etc.) to the soil.
The microbes will release the minerals for plants to use.
- Research has recently identified a physical property associated with good soil, the
Paramagnetic force as it is often incorrectly called. After studying soils from around
the world he has found that the healthiest soils with best plant growth and highest crop
yields have high paramagnetic values while poor soils have low values. How these low
level energy fields affect plant growth is not fully understood but the direct correlation
with plant growth is confirmed. Volcanic rocks (lave, granite, basalts, etc.) generally
have high paramagnetic values hence mineral dusts form these rocks have an additional
value. Paramagnetism - Rediscovering Nature's Secret Force of Growth, by Philip
Callahan, Ph.D., 1995.

Research from Europe has found than bacteria that lives in the guts of grazing animals
like cows and horses produce the vitamin B12 and extra B12 is excreted in the manure.
When manure is used as fertilizer at a rate of 10 grams per 1,000 grams of soil the plants
grown in manure fertilized soil had 2-3 times the B12 as plain soil plants. Plants have the
ability to absorb whole vitamins directly from the soil. Plant and Soil Journal.
- When Penn State University tested over 50 samples of alleged sterile potting mix in
sealed plastic bags they found all the bags had disease spores. A sterile mix is a
biological vacuum waiting to be filled.
- Researchers at the USDA's Soil Microbial Systems Lab have discovered a new protein
named glomalin, which is produced by fungi that helps glue soil particles together
making it easier for air and water to move through the soil. The improved circulation
also creates a healthier environment for plants and beneficial microorganisms. Tests
have shown that no-tilled corn plots were more stable and contained more glomalin than
tilled plots. Soils with the well stabilized structure were far less prone to erosion from
wind or water. BioCycle, December 1997.
- USDA scientists have found a fungal protein (glomalin from the Glomales fungi), that
binds soil particles together. They also found that there is less of this protein in tilled
soils than untilled soils. Studies of various soils have shown that glomalin glues soil
particles together into beneficial aggregates with some soils having up to 2% by weight
of this protein. These fungi are found around the world growing on root hairs of plants.
The American Gardener, March/April 1998

DEFINITIONS:
Clays: + smallest of soil particles, high nutrient and water retention capability, helps bond
larger soil particles together
- high % of clay can make soil difficult to work, shrink and swell with water
content, slippery when wet, hard when dry, poor aeration

Silts : + between clay and sand in size and properties, important in loam soils
- not important by themselves
Sands: + coarsest of all soil particles, well aerated, drains rapidly, ideal for root
growth
- moisture and nutrient retention are poor
Loams: (1) soil that contains equal amounts of clays, silt, and sand, plus some organic
matter, the ideal garden soil
(2) Example a 40 % sand, 40% silt, and 20% clay is considered a loam
Sandy loam: 10% clay, 65% sand, 25% silt
Silt loam: 60% silt, 20% clay, 20% sand
Clay soil: any soil over 55% clay
Coarse sand:often called sharp sand or builders sand.
small gravel:often called bird gravel or pea gravel
SIMPLE SOIL TESTS
1: Take a sample of soil 8-12 inches deep and place into a jar 75% full of water, and shake
vigorously for 10-15 minutes and all soil chunks are dissolved. Let jar set for several days
(until water clear) and you will see different layers of gravel then sand silt and clay. The
thickness of each layer related to total thickness gives the amount of each.
2: Get a handful of soil and wet it a little with water. Squeeze your hand into a fist and
then release. All but the most sandy soil will form a ball or clump with distinct finger marks, if
you can make a rope with the ball then a good mix of sand silt and clay, if you can flatten the rope into a ribbon without breaking it has a high clay content
3: Rub a small amount of soil between thumb and forefinger:
- If it feels gritty then the soil is sandy.
- If it feels like moist flour or talcum powder the its silty.
- if it feels slippery and moldable or sticky then it contains a lot of clay.
4: Sieve analysis (by weight or volume), take a soil sample and dry in a oven at low heat,
or in the sun, then pass through sieves and measure the amount of soil in each size category.
USEFUL REFERENCES:
A non-technical overview of soils:
Start With The Soil, Grace Gershuny, Rodale Press, Emmaus, Pennsylvania, Copyright 1993,
ISBN 0-87596-567-9.
The Dirt Doctor's Guide to Organic Gardening, J. Howard Garrett,, University of Texas Press,
Copyright 1995, 0-292-72780-1.
The Rodale Book Of COMPOSTING, Deborah L. Martin and Grace Gershuny, Editors
Rodale Press, Emmaus, Pennsylvania, Copyright 1992, ISBN 0-87857-990-7.
A semi-technical overview of soils:
An Acres U.S.A. Primer, by Walters and Fenzau, published by Acres U.S.A., Copyright 1992,
ISBN: 0-911311-37-8
A technical introduction to soils:
Introduction To Soil Physics, by Daniel Hillel, published by Academic Press, Inc., Copyright
1982, ISBN: 0-12-348520-7

Paramagnetism - Rediscovering Nature's Secret Force of Growth, by Philip Callahan, Ph.D.,
published by Acres U.S.A. Press, Copyright 1995, ISBN: 0-911311-49-1
ORGANIC Soil Conditioning, William R. Jackson, PhD, Copyright 1993, Jackson Research
Center, ISBN 0-9635741-0-8
SOIL TESTING LABORATORIES:
Texas Plant and Soil Lab (from Acres, USA)
Route 7, Box 213Y
Edinburg, TX 78539
Peaceful Valley Farm Supply (from Organic Gardening Magazine)
P.O. Box 2209
Grass Valley, CA 95945 (916) 272-4769
Timberleaf (from The Dirt Doctor's Guide To Organic Gardening)
5569 State Street
Albany, OH 45710
Tiberleaf Soil Testing Services (from Organic Gardening Magazine)
26489 Ynez Rd., Suite C-197
Temecula, CA 92591 (909) 677-7510
Wallace Laboratories (from Organic Gardening Magazine)
365 Coral Circle
El Segundo, CA 90245 (310) 615-0116
Extension Soil, Water, and Forage Testing Laboratory
Texas A&M University- Soil and Crop Sciences
College Station, Texas 77843-2474 (409) 845-4816


Terry Bell - manager, or Gene Bickerstaff
Soil and Plant Laboratory (from Composting Council)
352 Mathew Street
Santa Clara, CA 95050 (408) 727-5125 (James West)
Soil Control Lab (from Composting Council)
42 Hanger Way
Watsonville, CA 95076 (408) 724-5422 (Frank Shields)