Kelzyme is a unique agricultural soil conditioner
derived from a fossil deposit rich in calcium and containing an
abundance of trace minerals essential for enhanced plant
health and productivity. Our goals are to continue to provide
superior products for our global partners in agriculture,
ranching, forestry, and habitat
reclamation.
Kelzyme Natural Soil Conditioner for agriculture
is an unusually potent source of elemental calcium along with a
wide spectrum of trace minerals necessary for sustained growth of
agricultural crops in a variety of soil conditions. Kelzyme
can be used to stabilize depleted mineral content in soils that
have been continuously planted or where conventional fertilizers
have been used. In natural/organic farming operations Kelzyme will
improve the microbial health and overall physical structure of the
soil. Kelzyme assists in balancing pH and by increasing microbial
activity in soils Kelzyme will also help to metabolize soluble salts
in soils that can be harmful to crop production.
The origin of Kelzyme Organic Soil Conditioner
is a combination of marine and geothermal dynamics. The Paleozoic
algal mounds that formed the Kelzyme deposit are similar to many
other stromatolite formations within what was once a vast, inland
sea that covered the Great Basin of North America. These algal mounds
were often places of rich marine life including calcareous algae,
marine macroalgae, hermatypic coralline animals, mollusks, sessile
invertebrates, and a wide variety of pelagic species of plants and
animals. These mounds were formed and reformed as the accession
and recession of seawater ebbed and flowed over the environment.
This accounts for the many layers of materials in the Kelzyme deposit.
These carbonate facies were formed in the presence of a rich source
of marine calcium forming a limestone travertine deposit containing
the variety of minerals concentrated by the abundant marine life
forms that colonized this formation. During the continuous formation
of the stromatolitic mounds geothermal fresh water, super heated
by magma continued to purify and integrate the mineral constituents
of the Kelzyme deposit. This geothermal activity took place long
after the final recession of the marine environment further purifying
and integrating the deposit. This unusual combination of natural
forces formed the high calcium and trace mineral deposit now called
Kelzyme.
Kelzyme is available to farmers as a soil
conditioner for improving the overall quality of the crops
they produce due to abundance of trace minerals in an easily assimilated
high elemental calcium carrier. Kelzyme is non-burning and can be
applied pre-plant or a side dressing for orchards, vineyards, and
row crops. Kelzyme is useful to growers of grain crops because of
the high availability of the minerals it contains. Continuously
planted areas benefit from Kelzyme due to its long lasting nature.
The physical structure of soils is improved when Kelzyme is applied
due to a balancing of mineral content in the soil. Kelzyme improves
microbial health in soils thus making phosphate more available to
plants. By improving the health of beneficial soil microbes, Kelzyme
is also known to suppress the proliferation of pathogenic microbes
via the process of competitive exclusion. Drought resistance is
improved as cell wall strength is increased from the presence of
silica (Si) in Kelzyme. Frost resistance is also increased because
of this increase in cell wall turgidity.
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