Feed the soil
Harvest Grow products contain the essential nutrients required to build, maintain, and restore soil fertility. .
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MicroorganismsSoil Food Web
pH factors
Cation Exchange Capacity
Organic Matter Content
Soil basics...
What is
soil…really? Soil is a
living thing requiring special care. The quality
of soil is the function of the chemical and
physical properties of the content of the soil
and the structure of the soil. Regarding
content, a healthy soil contains a balance
mixture of five constituents:
About two-thirds by
volume weathered rock ranging in size from small
stones all the down to the tiniest specs of clay
called aggregate.
About one-third by volume
dead and decomposing organic materials from
plant and animal sources.
A very substantial
population of living creatures, particularly
soil microorganisms
A large quantity of water
containing a variety of dissolved mineral
nutrients.
A remarkable amount of
air.
What is Soil Structure? Soil structure is the way in which the sand, silt, and clay particles are grouped together. The drainage capacity of the soils and the ability of the soils to make nutrients available to the plant are functions of soil structure. Harvest Grow products contain Humus which plays an important role in maintaining soil aggregates.
Why are
soil aggregates important? Soil
aggregates help to build and to sustain soil
porosity. A porous soil structure helps in
several ways:
It aids in the movement
and retention of water, air and nutrients in the
soil;
It helps to insulate the
soil from sharp changes in temperature and
pressure; and
It gives easier passage
to the roots and soil organisms.
Soil porosity is a function of the spacing
between the soil aggregates. The pores or
cavities between the soil particles or
aggregates are called microspores or macrospores
depending on their relative size. The
macrospores
are large enough to give free movement of water
and air into and through the soil. Macrospores
are essential to good drainage and giving soil
organisms and root hairs ready access to air.
They also give roots and root hairs easy
channels for growth.
Microspores are much smaller. Air and water pass
through these restricted cavities but slowly.
They seem to be of importance because they help
the soil to retain water. They do not seem to
help with the movement of air into or through
the soil.
What is
Topsoil? The roots of
most plants and all of the soil organisms need
oxygen to survive. Life in the soil is dependent
on both air and water. Topsoil differs from
subsoil primarily because topsoil has a more
open structure that contains sufficient oxygen
to support both root growth and soil organisms.
Topsoil is usually a darker color because of
it's higher organic content. The thickness can
be increased by mixing subsoil with the topsoil
and adding DirtFert. The mix becomes topsoil
once the blend establishes it's new ecosystem
and begins to support new communities of soil
micro and macro-organisms.
What is
the function of organic material in the soil?
Organic material has a number
of important functions in the soil:
It
is a primary source of nutrients for the plants
It is a primary nutrient
for the soil micro and macro-organisms
It is the parent source
for humus
It helps to hold moisture
and nutrients within the soil aggregates and
throughout the soil as a whole
It helps the soil
maintain a healthy environment for both plants
and soil organisms
It helps correct PH
excesses of both soil alkalinity and soil
acidity
It helps to prevent
erosion
What are Organic Soils? They are soils that were originally formed in shallow lake bottoms, swampy areas or bogs. They are relatively light but can hold up to four times their weight in water keeping the soil excessively moist. 15% by volume organic material is a good amount. Native soils frequently run as low as 3% by volume organic. They tend to be very rich in terms of the major nutrients but they are often shy in terms of the micro-nutrients and particularly zinc, copper, and manganese. Organic soils contain more than 20 percent organic material. Take it easy in terms of adding manures and composts to organic soils. Feeding with supplement materials containing trace micro-nutrients would be appropriate for organic soils like DirtFert. A foul smell indicates anaerobic decomposition. The soil doesn't have enough air. It can be corrected by adding DirtFert and turning it into the soil.
What is pH? Technically, pH is a measurement of the concentration of hydrogen ions. Common language, pH is a measurement of acidity or alkalinity. The pH of totally pure water is 7.0. The lower the numbers away from 7.0, the greater the acidity. The higher the numbers away from 7.0, the higher the alkalinity. It uses a logarithmic scale so a material with a pH of 4.0 is ten times as acidic as a material with a pH of 5.0 and a hundred times as acidic as a material with a pH of 6.0
What's the best pH for plants? Most plants will tolerate a range of soils extending from decidedly acid to moderately alkaline. Most, however, prefer a soil that is just slightly acidic. A pH range between 6.3 to 6.8 would be about right for most crops. A soil containing a significant amount of organic matter will often have a pH in that range as a result of the organic acids produced in the composting process.
Are soil tests really necessary? A single soil test will not give you a true picture of what is happening in your soil. Typically an initial soil test will determine nutrient deficiencies rather than soil microbial activity and its ability to convert nutrients into a form the plant can absorb. The first soil test is a baseline to compare supplemental soil tests against. Conduct several soil tests throughout the season to determine if your soil is headed in the right direction.
What are Soil Microorganisms? There are billions to hundreds of billions of soil microorganisms in a mere handful of a typical, garden soil. That single handful might well contain thousands of different species of bacteria (most of whom have yet to be classified), hundreds of different species of fungi and protozoa, dozens of different species of nematodes plus a goodly assortment of various mites and other micro arthropods. Almost all of these countless soil organisms are not only beneficial, but essential to the life giving properties of soil.
What do soil microorganisms do for the physical, chemical, and/or bio-chemical properties of soil? Soil microorganisms breakdown a variety of organic materials and use a portion of these breakdown products to generate or synthesize a series of compounds that make up humus. In addition to producing humus, the soil microorganisms breakdown and/or bind a variety of organic and inorganic materials and help to clean up corrupted or polluted soils referred to as bio-remediation.
What are humic substances? The relatively small and simple polymers, specifically those humic substances with a small molecular weight, are known as fulvic acids. The relatively large and complex polymers, specifically those humic materials with a high molecular weight, are known as humic acids. It is believed that fulvic acids become humic acids with more polymerization and that humic acids become humin with even more polymerization. Humic substances include fulvic acids, humic acids, the salts of both fulvic and humic acids, and humin.
What do
humic substances do for the soil? Harvest
Grow Humic substances perform at least five
critical functions:
They
increase adsorption of
minerals and bring into
solution mineral materials that would otherwise
be inert and convert them into forms that can be
taken up by the plants
as nutrients;
They
increase adsorption of
organic compounds which
aids in plant nutrition, plant physiology, and
in the cleanup of polluting or toxic materials
in the soil;
They increase the
water holding capacities of the soil
which makes water more available to the plants
for greater plant production;
They
increase the soil's
buffering capacity helping to
stabilize the soil's pH to help the plants to
take up mineral nutrients; and
They darken the soil
color which increases the soil's
adsorption of solar energy.
Fulvic acids are more chemically reactive than
humic acids and are mostly involved in the
chemical reactions that influence plant's growth
and nutrition while the humic acids are mostly
involved in altering the physical
characteristics of the soil.
What are
the Essential MACRO and MICRO Nutrient
Elements?
The essential
mineral macro nutrients are: nitrogen,
phosphorus (measured as an ingredient of
phosphoric acid or a phosphate), potassium,
sulfur, and calcium. Note that nitrogen is not a
mineral in the true sense of the word and is not
present in the soil particles, per se. Nitrogen
as a nutrient must come from organic matter,
air, or synthetic chemical sources rather than
from mineral or rock particles.
The essential mineral micro nutrients or
essential "trace elements" are: magnesium, iron,
copper, zinc, manganese, boron and molybdenum.
Certain plants also require: chlorine, aluminum,
sodium, silica, or cobalt. These are the
basic nutrients, there are many more the plant
uses that are essential to proper development.
Harvest Grow products provide these.
Sources of Micronutrients in Harvest Grow products. Kelp is valued not only for its macronutrient (N, P, and K) contributions but for micronutrients, trace minerals, amino acids and vitamins plus growth hormones that stimulate plant cell division. Our cold processed, liquid kelp has higher levels of growth hormones than most extracts. They may also be enzymatically digested, making the growth hormones even more available to the plants.
How roots
uptake nutrients.
Most
of the mineral nutrients in the soil are in the
form of mineral salts dissolved in the soil. The
roots feed on these nutrients and assimilate the
mineral nutrients into the plant by osmosis.
There are a couple of exceptions.
Nitrogen is the one essential macro nutrient
that is not a mineral. It must be in the nitrate
form before it can be taken up by the roots.
Nitrogen applied to the soil in the form of a
protein from organic sources, ammonia or
ammonium salts from organic or synthetic sources
must first be decomposed or oxidized to the
nitrite form and then decomposed or oxidized
further to the nitrate form. This oxidation
process is the work of special nitrobacteria
resident in the soil. Legumes have nodules on
their roots which contain "nitrogen fixing"
bacteria that can take nitrogen directly from
the air present in the soil to short-cut the
normal nitrogen cycle.
The second major exception is phosphorus which
is normally present in the soil in the form of
relatively insoluble phosphate salts. Very
little of the phosphate salt is released into
the soil soup. Instead, trace amounts of the
phosphate salt are released to the microscopic
film of moisture surrounding the nutrient
particles and the root hairs are left with the
responsibility of seeking out these phosphate
salts. This pushes the root hairs to seek the
phosphorus in new areas.
Nutrient uptake through the Mycorrhizae fungi Mycorrhizae are symbiotic soil fungi, present in most soils. They attach themselves directly onto the roots of most plants. They help the host plants absorb more water and nutrients while the host plants provide food for the fungi. Because the surface area of the hyphae, the feeding structures of the mycorrhizae, may be several hundred times the surface area of the roots, the mycorrhizae can feed on a larger soil mass and they can also feed more thoroughly. Mycorrhizae have the potential to be a central nutritional source for most plants.
How
Nitrogen Transformations in the Soil
Nitrogen exists in a number of
chemical forms and undergoes chemical and
biological reactions.
Organic nitrogen to
ammonium nitrogen (mineralization).
Organic nitrogen comprises over 95 percent of
the nitrogen found in soil. This form of
nitrogen cannot be used by plants but is
gradually transformed by soil microorganisms to
ammonium (NH4+). Ammonium
is not leached to a great extent. Since NH4+
is a positively charged ion (cation), it is
attracted to and held by the negatively charged
soil clay. Ammonium is available to plants.
Ammonium nitrogen to
nitrate nitrogen (nitrification).
In warm, well-drained soil, ammonium transforms
rapidly to nitrate (NO3-).
Nitrate is the principle form of nitrogen used
by plants. It leaches easily, since it is a
negatively charged ion (anion) and is not
attracted to soil clay. The nitrate form of
nitrogen is a major concern in pollution.
Nitrate or ammonium
nitrogen to organic nitrogen (immobilization).
Soil microorganisms use nitrate and ammonium
nitrogen when decomposing plant residues. These
forms are temporarily "tied-up" (incorporated
into microbial tissue) in this process. This can
be a major concern if crop residues are high in
carbon relative to nitrogen. Examples are wheat
straw, corn stalks and sawdust. The addition of
20 to 70 pounds of nitrogen per ton of these
residues is needed to prevent this
transformation. After the residues are
decomposed, the microbial population begins to
die back and processes 1 and 2 take place.
Nitrate nitrogen to
gaseous nitrogen (denitrification).
When soil does not have sufficient air,
microorganisms use the oxygen from NO3- in place
of that in the air and rapidly convert NO3-
to nitrogen oxide and nitrogen gases (N2).
These gases escape to the atmosphere and are not
available to plants. This transformation can
occur within two or three days in poorly aerated
soil and can result in large loses of
nitrate-type fertilizers.
Ammonium nitrogen to
ammonia gas (ammonia volatilization).
Soils that have a high pH (pH greater than 7.5)
can lose large amounts of NH4+ by conversion to
NH3 gas. To minimize these losses,
incorporate solid ammonium-type fertilizers,
urea and anhydrous ammonia below the surface of
a moist soil.
Harvest Grow products contain Nitrogen in significant amounts when you consider how the Nitrogen is maximized in the soil cycle.