Comparisons of Organic Mineral Solutions

HealthTech International, presents a new technology in organic mineral extraction.  This technology has resulted in a highly purified organic complex solution far ahead of any organic minerals products available today.

 Some factors include:

 1.      Dissolved solids.  Many companies actually boast of solutions containing 32,000 to 38,000 mg of minerals per liter from which they recommend dosages of one or two ounces daily use.  These solutions may contain a small percentage of the organic complex in their total solution but are largely composed of useless water-soluble compounds or dissolved inorganic matter from reagents of extraction.  A typical humic deposit will contain less than one percent of the organically formed mineral complex molecules in the total minerals and elements of its structure.  Some of the water-soluble elements and compounds comprising the majority of most mineral solutions are useless toward nutrition and some could actually be toxic to the body.  With a technique involving isolation of extraction, Health Tech has recovered a concentrated solution containing just the molecular complex that is desired.  This solution is then prepared in dilutions matching nutritional needs.  The organic mineral complex produced by Health Tech in this pure form contains just the right amount of these specific molecules for optimum supplementation toward balanced health.

2.      Clarity of Solution.  The true organic mineral complex is composed of a carbon-based molecule that totally dissolves in water.  A laser light beam will pass through such a solution without diffusing any visible light by its passage.

3.      Taste.  An isolated and pure solution of the organic mineral complex will show by I.C.P. analysis to contain over 70 trace minerals and elements but will have only a slightly acidic taste and leave no unpleasant after taste.  This simple evaluation sorts out most of the true complexes from those composed of useless water-solubles.

4.      Balance.  The content of the major and trace elements in the organic mineral complex are in balance with the same balance that exist in living plants and organisms.  This balance is reflected in the general profile shown in I.C.P. analysis. 

5.      Results.  In nature, the organic mineral complex provides some of the major and trace elements of nutrition, but fills a role far beyond providing just those nutrients.  The complex aids in the absorption and assimilation of all other nutrients it comes in contact with from foods, supplements and other sources.  It increases assimilation by complexing through a natural chelation process with foods and other nutrients.  The chelation structure improves the delivery of key nutrients to the cells both in the time of arrival, and increased potency after delivery.  It supports enzyme reactions and catalyst factors to provide increased potency of the nutrients it has helped to deliver. It provides natural electrolyte needs and helps bring chemical balance within the cells.   It also assists to neutralize toxins within the cells and other parts of the body.  When the purity of the complex is at a proper level, the benefits are maximized and enhanced. 

 The remarkable ability of the organic mineral complex in providing these benefits is that these benefits are supplied when the complex is present in very small trace amounts.  In research studies with plants in which the complex was present in amounts between 2.5 ppm (.00025%) and 5 ppm (.0005%), the increased plant growth over control plants was 30 to 50%.  Additional studies utilizing concentrations of the complex between 15 ppm (.0015%) and 60 ppm (.006%) resulted in increased shoot growth between 13% to 170% and increased root growth between 122% to 477%.  Those results at those concentrations seem almost unbelievable, but the mechanics of the effect which resulted in those benefits were scientifically observed.  They included:

 1.      Increased oxygen uptake

2.      Active chelation with adjacent nutrients providing:

a.       Improved solubility and availability of chelated nutrients

b.      Chelation with nutrients that would otherwise have been unavailable

c.       Prolonged availability and residence time of nutrients to the cells

d.      Triggering new nutrients through chelation of multiple structures

e.       Delaying the precipitation of trace minerals

3.      Improved respiration

4.      Enabled plants to endure conditions of stress positively, ie drought

5.      Increased the chlorophyll content

6.      Increased the cell permeability        

7.      Increased the formation of carbohydrates and sugars

8.      Resulted in increased growth and production 

The benefits that have been scientifically established during the last century in the biological and plant world are just now beginning to be established in human nutrition and supplementation.  The same principle is observable, small concentrations yield very dramatic benefits and the more pure and refined the complex the greater are the benefits.

 In the 20^th anniversary conference (2002) of the International Humic Substances Society, the 10^th presentation pointed to one of the most interesting admissions of the nature of the organic mineral complex stated by academia.  It cited the earlier research in 1981 in which the society established three standard samples of the complex to use as a basis of research in the scientific community.  In 2001, after evaluation of accumulated research and in an effort to identify a more exacting standard for research, researchers came forward with the admission that humic substances comprise an extraordinary complex amorphous mixture of highly reactive molecules devoid of a regularly recurring skeletal entity.  They have come to this conclusion through applied technology of every known approach, asserting that these substances are unresolvable into significant amounts of pure components in the traditional sense. 

 Scientists have observed that humic substances are composed of a broad spectrum of related molecules, each one differing almost imperceptibly from the next in its specific properties.  Some researches have stated that perhaps no two molecules of humic substances are exactly alike.  The evaluation of this research taken together causes researchers to describe these substances as supermixtures in their complexity.  These supermixtures demonstrate a high multiplicity, diversity and highly reactive polydiverse nature.  It is in fact their random complexity and high chemical reactivity that constitute the very essence of the organic mineral complex. 

 These scientific evaluations of the complex help to explain the multiple beneficial potential that these complexes provide to nutrition.  They comprise one of the unique gifts of nature.  They are formulated inside the cells of living organisms that synthesize these nutrient combinations from an array of billions of molecules of captured solar energy substances formed by plants.  It should really be no surprise that like snowflakes, they are formed by nature so that perhaps not one of these molecules are exactly alike, but unlike snowflakes they carry an astronomical variety of helpful elements and nutrient complexes. 

Bibliography

 Balch, James F., M.D., & Balch, Phyllis A., CNC,  Prescription for Nutritional Healing, third edition, Avery Publishing, New York, New York p. 776  

Fernandez, H. Raul. Research Findings of Characteristics of The Organic Mineral Complex, 2002, HealthTech International, Inc. St. George, UT p. 17.

 Frimmel, F.H.., and Christman, R.F. (1988) Humic Substances and Their Role in the Environment.  Chichester, Great Britain:  John Wiley and Bath.

 Halstead, B.W., and T.C. Rozema, The scientific basis of EDTA chelation therapy, T.R.C. Publishing, Landrum, S.C., p. 267

 Halstead, B.W., M.D. Fossil Stony Coral Minerals and Their Nutritional Application, Health Digest Publishing Co., Cannon Beach, Ore. p. 141

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 McCarthy, Patrick, (2001) The Principles of Humic Substances:  An Intro to the First Principle.  In E.A. Ghabbour & G. Davis (Eds.), Humic Substances, Models and Functions, (pp. 19-30) Boston, MA:  Northeastern University.

 Schnitzer, M., and Khan, S.U. (1978) Soil Organic Matter. New York:  Elsevier.

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