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Soil
Structure
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Most of
us are not used to thinking of the tilth of
the soil, but it is essential to any gardener.
If soil has a healthy structure, the likelihood
of erosion, compaction, run-off, flooding, and
leaching are low; its drainage, aeration, and
water retention are good; and its fertility
is enhanced. Think of your soil as a seven-layer
bean dip. There are different consistencies
to each layer, and some we like better than
others. The differences in the respective layers
of soil are actually particles of broken-down
rock, called minerals, in different levels of
degradation. Over time, these minerals have
settled on the earth's surface in layers and
have been influenced by wind, water, vegetation,
and man.
Mineral
particles in soil are rated by size. All soil
is made of various-sized particles referred
to as sand, silt, or clay, mixed with organic
matter. Varying amounts of these account for
differences in a garden soil's texture. While
large particles of sand (0.05 to 2.0 mm) make
a great beach, they're not the best soil to
garden in, as anyone from SE North Carolina
can attest too. Roots can grow through it easily,
and nutrients, water and air move through the
large spaces between particles quickly, but
too quickly. This phenomenon allows leaching,
which can quickly remove valuable nutrients
and water from your root zone. It can also have
a huge effect
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on your pocketbook,
from using too much water to the inability to keep anything
beneficial in your root zone. These properties make
sand an unsuitable medium for soil growth.
The next smallest
particle size is silt (.002 to .05 mm). Rain falling
on dry, silty soil has trouble penetrating to the
roots. It tends to run off before soaking in. But
because of those smaller particles, once silt is thoroughly
saturated, it holds more moisture and nutrients than
sand.
Then there's
clay (smaller than 0.002 mm) - too much of which is
the bane of every gardener's existence. When it's
dry, it shrinks and cracks. In fact, you could make
bricks out of the stuff. But, if you wet it, it'll
hold lots of water and nutrients. During rainy or
wet periods, it often becomes waterlogged. And it
doesn't warm up early in the spring, so getting into
the garden to plant can be difficult.
Most soils are
mixtures of sand, silt and clay. Between these inorganic
particles are decaying animal and plant materials
or organic matter, called humus. Living organisms
--like nematodes, earthworms, and bacteria-- move
through the soil, leaving miniature tunnels providing
oxygen and depositing feces providing valuable materials
for plant nutrition. The combination of these creatures'
waste products and their remains binds with the soil
particles. In clay, it forces the tightly packed particles
apart improving drainage and making it easier for
plant roots to penetrate the soil. In sand, it lodges
in the large pore spaces and acts as a sponge, slowing
drainage so the soil stays moist longer. All these
factors contribute to soil structure. Good soil structure
allows for the presence of oxygen in the root zone,
permits water to drain through it well, and harbors
nutrients for plant nutrition by preventing leaching.
A soil containing roughly equal amounts of sand, silt,
and clay is called loam and is considered to have
good tilth and ideal for cultivation. There are coarse
loams and fine loams. Fine loams have more silt and
clay than sand. Coarse loams are mainly sand, which
facilitates better drainage, but still contain enough
silt and clay to hold moisture and nutrients and thereby
support soil organisms. For this reason, coarse loams
are considered some of the best soils to cultivate,
with fine loams not far behind.
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Soil
Amendments
A soil amendment is any material that improves the
chemical or physical structure of the soil, such as
water retention, fertilizer retention, permeability,
water infiltration, drainage, aeration and structure;
with the goal of providing a better environment for
roots. There are organic and inorganic soil amendments:
organic being any material that was once or is alive,
ideally providing a form of nutrition; inorganic being
something mined or man-made, like perlite or vermiculite.
Most people are
not used to paying attention to soil nutrients past
a simple NPK. Growing plants are no different than
anything else, the more attention you pay to them
the better results you will have. The fact is, by
not paying attention to the nutrients and materials
in your soil and available to your plants you are
assuming your soil contains all the necessary components
for plant growth. This can be a fatal assumption,
especially on land that has been cleared for development,
over cropped, or is subject to erosion. These types
of land, including residential and commercial space,
are cleared and grated to enable the passage of building
inspections or have been stripped of their native
soil spectrum. In so doing, the top foot or so of
topsoil is cleared from the plot and all of the beneficial
soil microbes and most of the residual nutrient available
for plant growth is taken along with it. Keep this
in mind when planting your backyard garden.
Soil nutrients
exist both as complex, insoluble compounds and as
simple forms usually soluble in water and readily
available to plants. The complex forms must be broken
down through decomposition by soil microbes and processes
into simpler forms in order to benefit the plant.
Herein lies a fundamental difference between soilless
and soil-based cultivation and the reason why there
is not a 100% organic hydroponic nutrient. In order
for a plant to access a nutrient hydroponically the
fertilizer must be soluble in water. If not, the plant
cannot access it. By the nature of nutrient formulations,
everything a plant needs to grow available in an "organic"
form cannot yet be accomplished in one bottle.
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Beneficial
Fungi
Mycchorizae can make a tremendous difference
in your plant growth. Through a symbiotic relationship
with the plant, mycchorizae helps the plant
with nutrient uptake, amongst other things,
and in return allows the plant to feed off of
excess plant nutrients and carbohydrates.
Wetting
Agents
Wetting agents are extremely beneficial soil
conditioners. The chemical nature of water is
such that it likes to coalesce, forming water
beads similar to the beading nature of water
you witness when washing your car, or the reason
water bugs can skate around on a lake. This
concept is also the reason that in a hydroponic
system oxygen must be dissolved into your water
solution. Without DO the result is stagnant
water and unhappy plants. By breaking the natural
surface tension of water and overcoming its
tendency to form droplets a wetting agent allows
fertilizers, pesticides, etc. to penetrate a
variety of materials- including soil and plant
tissues.
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It is always
a good idea to implement a wetting agent when utilizing
a foliar spray in order to maximize coverage. Test
it yourself. Spray first using a water solution with
no wetting agent and then with a solution containing
a wetting agent. You will notice a more uniform coverage
with the wetting agent, actually laying down the spray
ensuring that 100% of your leaf or soil is covered.
Organic Materials
There are myriad materials in multiple forms that
can be utilized in soil to benefit plant growth. The
decision on what to use should be made regarding what
will improve the vitality of your soil, not simply
the plant. For example, a synthetic fertilizer like
Miracle Grow will provide needed nutrients to your
plants, but will lock out nutrients already found
in the ground or container and disrupt the soil processes
needed to make them available. Essentially a synthetic
nutrient schedule in soil is treating your soil as
an inert medium as opposed to the vibrant organism
that it is. This phenomenon is prevalent in the "chemlawn"
services provided by most local landscaping and lawn
care services. The following are several organic materials
that can enhance your soil zone and, in turn, your
plants. They can be utilized by working them into
the soil itself or as a top dress to an existing scenario:
Alfalfa meal
(~3-1-2) contains many beneficial plant materials,
including amino acids, trace minerals, proteins, and
sugars, and is commonly used as an animal feed. It
is an excellent fertilizer material in horticulture,
and is said to contain unknown growth factors, which
make its mineral content more effective as plant nutrients.
Blood meal
(~12-0-0) is very high in nitrogen and is very soluble
in water (unlike most other dry organic fertilizers).
It also contains plant growth regulators. All this
together means that its effect is strong and quick,
but its power will only last a short while, especially
in wet weather. When applying blood meal, take care,
as it will easily burn a plant's leaves.
Bone meal
(~1-13-0) is an organic fertilizer applied to increase
phosphorus levels in the soil (or compost). Although
phosphate rock can also be used for this, bone meal
will break down in the soil considerably faster and
can thus be used as a quick fix; but this also means
that it will not have a long-term effect on the soil.
Compost
is decomposed organic material. It's N-P-K depends
on the components of the compost itself. By piling
kitchen scraps and garden debris in a bin or heap,
gardeners create an ideal habitat for decay organisms.
These microorganisms break organic material down to
form humus. In addition, the heat inside the pile
from all the biologic activity will kill off many
disease organisms and unwanted seeds. There are multiple
ways to compost, for more info go here. (link to compost
page)
Cottonseed
meal (~6-1-1) is a rich source of nitrogen. Unfortunately,
a substantial percentage of the insecticides used
in the U.S. are applied to cotton, and some of these
tend to leave residues in the seeds. Most organic
certification programs restrict or prohibit the use
of cottonseed meal.
Cover crops
will often include leguminous plants like clover and
vetch, but they might also be grains like rye or oats.
Cover crops are often planted as a green manure, but
they also serve to prevent erosion, control weeds,
and conserve water in the soil from losses due to
evaporation. For more info on cover cropping go here.
(link to cover cropping)
Feather meal
(~12-0-0) is a common by-product of the poultry
slaughter industry. Although total nitrogen levels
are fairly high, the nature of feathers is such that
they break down and release their nitrogen much more
slowly than many products of similar price.
Fishmeal and
fish emulsion: Fishmeal is high in nitrogen, and
has relatively even NPK ratio of somewhere around
5-3-3. Unlike the emulsion, fishmeal is a dry organic
fertilizer. The fertilizer analysis of fish emulsion
varies with preparation method. Whole fish and fish
parts must be digested to form a slurry, a process
accomplished with the aid of either phosphoric acid
or special enzymes. Acid-digested fish emulsion usually
has an analysis around 4-4-1, while enzyme-digested
fish emulsion is usually measured as 4-1-1. Fish emulsion
may be fortified with chemical fertilizer, so organic
farmers should be suspicious of any product with a
nitrogen content in excess of 5%.
Green manures
improve the structure and nutrient load of the soil.
The most utilized green manure is mulch mowing. Removing
grass in bags from your lawn eliminates a crucial
nitrogen source from your lawn. Green manures may
be undersown between rows of plants or sown as a cover
crop. Between rows, green manures (like clover or
vetch) are often mowed --their clippings left as mulch.
At season's end, they are turned in to the soil like
other green manures (such as rye and soybeans).
Greensand
(~0-1-6) is mined from ancient sea beds; it is a dry
organic fertilizer. It is useful for its ability to
slowly supply to the soil as many as 22 trace minerals
and micronutrients, as well as potassium and phosphorous.
It has the consistency of sand, but can hold up to
15 times more moisture making it an exceptional soil
conditioner.
Gypsum,
which occurs naturally in sedimentary rocks, is a
dry organic material that supplies two important micronutrients:
calcium and sulfur. Some anecdotal data suggests that
applications of gypsum on lawns may mitigate problems
with turf pests such as grubs and chinch bugs.
Humus
is the end result of successful composting. It is
the rich, dark, and fine mixture of decomposed organic
materials. Humus contains the microorganisms necessary
for healthy soil, as well as a ready supply of the
macro- and micronutrients necessary for healthy plants.
Use humus in the garden to condition and amend soil.
Mix it with the soil for general improvement or use
it to side-dress hungry plants.
Kelp meal
(~1-0-2) is used as a dry organic fertilizer. Dehydrated
kelp contains a full compliment of minerals, trace
minerals, vitamins, and amino acids It is also rich
in micronutrients and plant growth hormones, as well
as being an excellent source of potassium. Kelp and
algae products are most utilized as a foliar spray.
Lime is
produced when calcium carbonate is finely ground.
Ground lime is readily
dissolved into the soil where it reduces soil acidity
by releasing calcium cations. It is also a potent
tool in combating grub infestations and unwanted odors
in compost piles.
Manure:
Nitrogen feeds the microorganisms in soil that make
humus from a compost pile. Manure is rich in nitrogen
(especially chicken, goat, and steer manures), and
is thus a valuable component of compost. It is also
rich in potassium and phosphorus. Manure should be
composted (or at least aged) before use in the garden
because of its high nitrogen --and ammonia-- content,
which can both easily burn plants. Composting will
also kill any weed seeds that may have survived the
animal's stomach(s).
Mulch:
Most mulches are made from organic materials, some
of the best being: hay, grass clippings, fallen leaves
(best when shredded), bark chips, and compost. Mulching
serves to prevent moisture loss from soil, protect
plants from temperature extremes, control weed growth
(weed before laying mulch!), prevent water from splashing
onto plant material, and as a slow-release soil amendment.
For more info on mulching go here.
Peat moss
is the partially decomposed remains of mosses harvested
commercially from the wild. Though difficult to wet
initially, peat moss can absorb up to 25 times its
own weight in water and is therefore valued as a an
organic soil amendment. Peat moss is acidic --with
a pH of about 3 or 4.0-- and should only be used around
acid-loving plants or to help lower the pH of alkaline
soils. Sphagnum moss is generally recommended over
standard peat moss.
Potash broadly
describes any material containing potassium. More
specifically, though, potash is potassium carbonate
derived from wood ashes. The term potash comes from
the process of extracting lye from wood ashes in iron
pots.
Rock phosphate
(~0-3-0) is a dry organic fertilizer used to boost
phosphorous levels in the soil. Rock phosphate is
slow to dissolve in water, so adding it will benefit
the soil over a period of years. The phosphate found
in many synthetic fertilizers is usually from rock
phosphate treated with sulfuric acid to make it more
soluble and thus more readily available to plants
(called superphosphate).
Wood ash
contains about 2% phosphate and 6% potash, but may
be contaminated with heavy metals or plastic and typically
has a high salt content. Wood ash is rather alkaline,
and excessive use can be quite damaging to many soils.
Some organic programs restrict its use.
Worm castings
are the excrement deposited by earthworms as they
tunnel through the soil. Castings are a rich soil
amendment containing nutrients in a form usable to
plants (they can be harvested and sold in bags). Over
the coarse of a single day, an earthworm will produce
castings equal to its own weight. For info on vermicomposting
go here.
As always, feel
free to contact us with any questions regarding organic
amendments, or anything gardening!
Cover
Cropping
Cover crops are grown to protect and improve the soil,
not to harvest. Cover crops have the potential to
improve soil tilth, control erosion and weeds, and
maintain soil organic matter. They can reduce compaction
and increase water infiltration, which decreases leaching
of nutrients. Cover crops retain and recycle plant
nutrients (especially nitrogen) between crops, provide
habitat for beneficial microorganisms, and increase
plant diversity. Cover crops may also be referred
to as "green manures". Traditionally the
term "green manures" has referred to plants
that are turned under or incorporated into the soil
while green, or soon after flowering, in order to
enrich the soil. In recent years however, the term
has been used more loosely, and green manure may sometimes
refer to plants or plant vegetation that may be applied
as mulch to the soil, both slashed and fresh or after
the plant has dried out.
The concept is
no different than mulch-mowing your lawn. All of the
clippings you laboriously carry away from your lawn
can actually be used by the growing grass as fertilizer
amounting to 1 or 2 fertilizer applications per year.
In fact, mulch itself is a valuable cover crop, albeit
maybe not a "crop". Mulches break down over
time into plant usable forms.
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