| Humus material is material containing decayed and partially
decayed organic material such as plants, animals, microorganisms, and marine
life such as plankton. Humus material is formed in nature by the aerobic
and anaerobic decomposition of the organic material. Humus material contains
humic acid, fulvic acid and humin, which are known collectively as humic
substances. While the terms “ fulvic acid” and “humic acid” are used
extensively in scientific literature sources, these terms each include
the plural rather than the singular. In other words, “ fulvic acids” and
“humic acids” are the correct terms even though “ fulvic acid” and “humic
acid” are more commonly used. For consistency, the terms “ fulvic acid”
and “humic acid” are used herein to represent the plural of each of these
terms.
The terms fulvic acid, humic acid and humin do not refer
to discrete chemical compounds, but each term includes a wide variety of
compounds of varying molecular weight, solubilities and spectral characteristics.
However, in general terms, the distinction of humic substances as between
the categories of humic acid, fulvic acid and humin is based on their solubilities
in acidic and alkaline aqueous solutions.
Humin molecules are insoluble under both acidic and alkaline
conditions, and have larger molecular weights (generally greater than about
100,000 Daltons) than both humic acid and fulvic acid molecules.
Humic acid molecules are soluble under alkaline conditions,
but are insoluble in acidic conditions. The molecular weights of humic
acid molecules range from a lower limit from about 2500 to 12,500 Daltons,
to an upper limit somewhere from about 75,000 to 300,000 Daltons. Of these,
it is the molecules under about 50,000 Daltons which are biologically active.
It is known to use humic acid in agricultural applications since these
molecules complex nutrients, especially phosphorus and metal micronutrients,
keeping the nutrients soluble and available for plant uptake. Humic acid
molecules are absorbed and translocated by plants and also stimulate both
root and top growth in plants, increase chlorophyll density and may help
plants resist drought and heat stress. However, when applied to soils,
varying fractions of humic acid will become insoluble, depending on the
soil pH. Humic acid will also bind some pesticides, reducing its biological
activity.
Fulvic acid molecules are soluble under both acidic and
alkaline conditions. Fulvic acid is the lightest fraction of humic substances.
There is no consensus in the scientific literature as to the precise molecular
weight of fulvic acid molecules, but lower limits range from about 250
to 1,000 Daltons and upper limits range from about 2,500 to 12,500 Daltons,
depending upon the method of analysis. It is also known to use fulvic acid
in agricultural applications such as fertilizers and soil additives, since
fulvic acid has the highest degree of biological activity and nutrient
complexing ability among humic substances, and will not bind to most pesticides.
Sources of humus material include peats, peat moss, composts,
brown coals, soil, pond sediment, biosolids (sewage sludge) and oxidized
lignites. A particular deposit of naturally occurring oxidized lignite,
located in North Dakota, U.S.A., is called leonardite.
The most common method used to date for extracting fulvic
acid molecules from humus material has been a base-acid extraction wherein
the humus material is first contacted with an alkali to solubilize the
humic acid and fulvic acid molecules, thus allowing separation of the insoluble
humin molecules, followed by acidifying the solution to a pH of about 1-2
to precipitate out the humic acid molecules. One disadvantage to the base-acid
extraction method is the cost of using large amounts of acids and bases
to carry out the chemical extraction. Further, large scale chemical extraction
methods are inconsistent with today's increased environmental awareness.
Further still, the base-acid extraction method also leaves reaction salts,
iron, silica and other soluble organic compounds such as carbohydrates
in solution, thereby decreasing the yield of fulvic acid in the solution
and otherwise contaminating the solution. It is desirable to decrease the
amount of these impurities from the end solution.
A second method used to date to extract fulvic acid from
humus material involves using plain water in place of an alkali. The benefit
of this method relative to the base-acid extraction method is fewer salts
in the end solution, but the resultant fulvic acid solution does still
contain some iron and other soluble organic compounds. However, a disadvantage
to the water extraction method is that the yields are extremely low, and
for this reason the base-acid extraction method is used to produce almost
all currently commercially available fulvic acid products.
Also, it is advantageous for fulvic acid products to be
produced in such a manner that they can be used in agricultural applications
wherein the produce or crops produced thereby can be certified as “organic”.
The need has therefore arisen for a commercially-viable
yet environmentally sensitive method for extracting molecules of fulvic
acid from humus material. .
|