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Inside every bottle of Fulvic Ionic Minerals x350 you'll find:
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Fulvic Acid
✓ Enhanced Nutrient Absorption
✓ Powerful Antioxidant Properties
✓ Detoxification and Immune Support
Trace Minerals
✓ Enzyme Function and Regulation
✓ Antioxidant Defense
✓ Immune Function and Health
Electrolytes
✓ Helps Regulate Fluid Balance
✓ Muscle contraction and relaxation
✓ Nerve Function
Amino Acids
✓ Protein Synthesis
✓ Energy Production
✓ Regulation of Metabolism and Immune Function
Water
✓ Hydration
✓ Supporting Metabolism and Digestion
✓ Promoting Overall Health
Powered By Nature
Plant Ingredients
Non-GMO
Soy & Dairy Free
Tasteless/Dissolves Instantly
Non-Habit Forming
SPECIAL INTRODUCTORY OFFER!
1 BOTTLE
60 Day Supply
3 BOTTLES
180 Day Supply
2 BOTTLES
120 Day Supply
YOU SAVE $262!!
100% MONEY BACK GUARANTEE
EVERY 3 BOTTLE PACKAGE GETS HUGE DISCOUNT TOO!
FULVIC IONIC MINERALS X350 FAQs
Research shows it's best to take Fulvic Ionic Minerals X350™ consistently for 180 days for optimal results. The longer you take it, the more you benefit. We recommend our 180-day supply for the best deal or our popular 120-day package. This special pricing is guaranteed only for today or until our limited stock runs out, so act fast to secure the lowest price.
Fulvic Ionic Minerals X350™ is 100% natural, safe, and effective. Thousands use it daily with zero side effects reported. Manufactured in the USA in an FDA-approved, GMP-certified facility, it is vegetarian, gluten-free, and non-GMO. Consult your doctor if you have a medical condition.
Will Fulvic Ionic Minerals X350™ work for me?
YES! Fulvic Ionic Minerals X350™ is a unique, 100% safe and natural formula with essential minerals and trace elements, proven to enhance overall health and wellness.
Will Fulvic Ionic Minerals X350™ affect the taste of my drink?
Absolutely not. Fulvic Ionic Minerals X350™ is totally tasteless and dissolves instantly into your drink. It works just as well regardless of what kind of beverage you drink or what you like to put in it.
What is the best way to take Fulvic Ionic Minerals X350™?
For best results, simply mix a few drops of Fulvic Ionic Minerals X350™ into your water, juice, or any other beverage each day. Then enjoy your drink as normal with or without food.
Do I have to take Fulvic Ionic Minerals X350™ in the morning?
No, you do not. You can enjoy and benefit from Fulvic Ionic Minerals X350™ at any time of the day. However, for best results, it is recommended to take it consistently every day.
Does Fulvic Ionic Minerals X350™ work with any beverages?
Yes, Fulvic Ionic Minerals X350™ is designed to work synergistically with any beverage to deliver its health benefits, including improved absorption of minerals and overall health support.
How will Fulvic Ionic Minerals X350™ be shipped to me and how quickly?
We will ship your order directly to your home or office using a premium carrier such as FedEx or UPS, and if you’re in the US or Canada you can expect your order within 5 to 7 business days. International orders typically take 8 – 15 business days (plus customs clearance time). Rush shipping is available!
Will I be billed anything else after I order?
Absolutely not! Rest assured this is a one-time payment only. This is not an auto-ship program of any kind. There are no hidden charges or subscription fees whatsoever. We’ve always hated that stuff as much as you do!
Is Fulvic Ionic Minerals X350™ Guaranteed?
Fulvic Ionic Minerals X350™ comes with a 60-day, 100% money-back guarantee. If you're not satisfied, just email us within 60 days for a full refund. No risk, no hassle. It's time to get started!
I take supplements and I can’t think of any reason not to use Fulvic Ionic Minerals X350™. Am I missing something!?
Nope, absolutely not. Allowing Fulvic Ionic Minerals X350™ to enhance your health, energy, and overall wellness is a total no-brainer :)
SPECIAL INTRODUCTORY OFFER!
1 BOTTLE
60 Day Supply
3 BOTTLES
180 Day Supply
2 BOTTLES
120 Day Supply
YOU SAVE $262!!
Scientific References
1. Senesi, N. (1990). Analytica Chimica Acta, 232, 51-75. Amsterdam, The Netherlands: Elsevier.
2. Vital electrolytes – Baker, W.E. (1973). Geochimica et Cosmochimica Acta, 37, 269-281.
3. Gamble, D.S., & Schnitzer, M. (1974). Trace Metals and Metal-Organic Interactions in Natural Waters. Ann Arbor, Mi: Ann Arbor Science.
4. Power of an electorlyte – Crile, G. (1926). A bipolar theory of living processes. New York: McMillan.
5. Decrease in electrical potential - Crile, G. (1926). A bipolar theory of living processes. New York: McM
6. Powerful electrolyte - Jackson, William R. (1993). Humic, Fulvic and Microbial Balance: Organic Soil Conditioning, 329. Evergreen, Colorado: Jackson Research Center.
7. New Electronic Encyclopedia. (1991). Photosynthesis. Grolier Electronic Publishing.
8. Donor and acceptor – Jackson, William R. (1993). Humic, Fulvic and Microbial Balance: Organic Soil Conditioning. Evergreen, Colorado: Jackson Research Center.
9. Donor and receptor - Rashid, M.A. (1985). Geochemistry of marine humic substances. New York: Springer-Verlag.
10. Donor, receptor - Sposito, G., Holtzclaw, K.M., LeVesque, C.S., & Johnston, C.T.(1982). Trace metal chemistry in arid-zone field soils amended with sewage sludge. II. Comparative study of the fulvic acid fraction. Soil Science Society America Journal, 46. 265-270.
11. Mineral complexes in fulvic may serve as electrodes – Rashid, M.A. (1985). Geochemistry of marine humic substances. New York: Springer-Verlag.
12. Free radical – Senesi, N. (1990) Analytica Chmica Acta, 232, 51-75. Amsterdam, The Netherlands: Elsevier.
13. Free radical – Senesi, N., Chen, Y., & Schnitzer, M. (1977b). The role of humic acids in extracellular electron transport and chemical determination of pH in natural waters. Soil Biology and Biochemistry, 9,397-403.
14. Oxidation reduction – Senesi, N., Chen, Y., & Schnitzer, M. (1977b). The role of humic humic acids in extracellular electron transport and chemical determination of pH in natural wates. Soil Biology and Biochemistry, 9, 397-403.
15. Dissolves metals and minerals – Ong, H.L., Swanson, V.D., & Bisque, R.E. (1970) Natural organic acids as agents of chemical weathering (130-170). U.S. Geological Survey Professional Paper 700 c. Washngton, DC: U.S. Geological Survey.
16. Enhance and transport nutrients – Christman, R.F., & Gjessing, E.T. (1983). Aquatic and terrestrial humic materials. The Butterworth Grove, Kent, England: Ann Arbor Science. Also: Prakash, A. (1971). Terrigenous organic matter and coastal phytoplankton fertility. In J.D. Costlow (Ed), Fertility of the sea, 2, 351-368. (Proceedings of an International Symposium on Fertilty of the Sea, Sao Paulo, Brazil, London, and New York: Gordon and Breach Science)
17. Enhance and transport nutrients – Prakish, A. (1971). Fertility of the Sea, 2, 351-368.
18. Williams, S. T. (1963). Are antibiotics produced in soil? Pedobiologia, 23, 427-435.
19. Stimulate growth - Konovona, M.M. (1966). Soil organic matter. Elmsford, NY: Pergamon.
20. All known vitamins in soil – Konovova, M. M. (1966). Soil organic matter. Elmsford, NY: Pergamon.
21. Many times its weight- Deb, B. C. (1949). The movement and precipitation of iron oxides in podzol soils. Journal of Soil Science, 1, 112-122.
22. Catalyzes enzyme reactions – Khristeva, L. A., Luk'Yanonko, M.V. (1962). Role of physiologically active substances in soil-humic acids, bitumens and vitamins B, C, P-P A and D in the life of plants and their replenishment. oviet Soil Science, 10, 1137-1141.
23. Fulvic and enzymes – Pardue, H.L, Townshend, A., Clere, J.T., VanderLinden (Eds.), (1990, May 1). Analytica chimica Acta, Special Issue, Humic and Fulvic compounds, 232 (1), 1-235. (Amsterdam, Netherlands: Elsevier Science Publishers)
24. Increase assimilation - Buffle
25. Low molecular weight, Aiken, G.R., McKnight, D.M., & VacCarthy, P.1985). Humic substances of soil, sediment and water, New York: Wiley-Interscience.
26. Sensitize cell membranes- Rashid, M.A. (1985). Geochemistry of Marine Humic Substances. New York: Spriner-Verlag.
27. Stimulte metabolism-Rashid, M.A. (1985). Geochemistry of Marine Humic Substances. New York: Springer-Verlag.
28. Genetic and growth - Jackson, William R. (1993). Humic, Fulvic and Microbial Balance: Organic Soil Conditioning, 538. Evergreen, Colorado: Jackson Research Center.
29. Oxygen is absorbed – Kononova, M.M. (1966). Soil organic matter. Elmsford, NY: Pergamon.
30. Rapid transport to shoots - Kononova, M.M. (1966). Soil organic matter. Elmsford, NY: Pergamon
31. Immune system – Syltic, P.W. (1985). Effects of very small amounts of highly active biological substances on plant growth. Biological Agriculture and Horticulture, 2, 245-269; and, Research reports and studies, Appropriate Technology Ltd. Dallas, TX: Murray Sinks II of ATL (Publisher).
32. Modify damage by toxic compounds – Christman, R.F., & Gjessing, E.T. (1983). Aquatic and terrestrial humic materials. The Butterworth Grove, Kent, England: Ann Arbor Science. Also: Prakash, A. (1971). Terrigenous organic matter and coastal phytoplankton fertility. In J.D. Costlow (Ed.), Fertility of the sea, 2, 351-368. (Proceedings of an International Symposium on Fertility of the Sea, Sao Paulo, Brazil, London, and New York: Gordon and Breach Science.)
33. Paraquat - Fisher, A.M., Winterle, J.S., & Mill, T. (1967). Primary photochemical processes in photolysis mediated by humic substances. In R.G. Zika & W. J. Cooper (Eds). Photochemistry of environmental aquatic system (141-156). (ACS Sympoium Series 327). Washington DC: American Chemical Society.
34. Pesticides - Aiken, G.R., McKnight, D.M., & MacCarthy, P. (1985). Humic substances os oil,sediment and water. New York: Wiley-Interscience.
35. Radioactive properties - Szalay, A. (1958). The signifiicance of humus in the geochemical enrichment of uranium. Proceedings of the 2nd International Conference on the Peaceful Uses of Atomic Energy, 2, 12-186 (London: Pergamon)
36. Dissolves and weathers silica- Huang, W.H., & Deller, W.D. (1970). Dissolution of rock-forming silicate minerals in organic acids; simulated first-stage weathering of fresh mineral surfaces. American Mineralogical Journal, 55, 2076-2094.
37. Dissolves silica- Kodama, H., Schnitzer, M., & Jaakkimainen, M. (1983). Chlorite and biotite weathering by fulvic acid solutions in closed and open systems. Canadian Journal of Soil Science, 63, 619-629.
38. Transmutate or synthesis of new minerals - Shnitzer, M., Dodama. H. (1977). Reactions of minerals with soil humic substances. In J.B. Dixon & S.B. Weed (Eds.), Minerals in soil environments (Chap.21)). Madison, WI: Soil Science Society of America.
39. See “The Fulvic Acid, Vegetal Silica Miracle” later in this report, and further documentation of Kervran, Louis C, Biological Transmutations.
40. Cell elongation - Poapst, P.A., & Schnitzer, M. (1971). Fulvic acid and adventitious root formation. Soil Biology and Biochemistry, 3, 215-219.
41. Enhance permeability of cell membranes – Christman, R.F., & Gjessing, E.T. (1983). Aquatic and terrestrial humic materials. The Butterworth Grove, Kent, England: Ann Arbor Science. Also: Prakash, A. (1971). Terrigenous organic matter and coastal phytoplankton fertility. In J.D. Costlow (Ed.), Fertility of the sea, 2, 351-368. (Proceedings of an International Symposium on Fertility of the Sea, Sao Paulo, Brazil, London, and New York: Gordon and Breach Science) low molecular weight, Aiken, G.R., McKnight, D.M., & VacCarthy, P. 1985). Humic substances of soil, sediment and water, New York: Wiley – Interscience.
42. Sensitizing agent – Prakash, A. (1971). Terrigenous organic matter and coastal phytoplankton fertility. In J.D. Costlow (Ed.), Fertility of the sea, 2, 351-368. (Proceedings of an International Symposium on Fertility of the Sea, Sao Paulo, Brazil, London, andNew York: Gordon and Breach Science)
43. Increase metabolism of proteins – Christman, R.F., & Gjessing, E.T. (1983). Aquatic and terrestrial humic materials. The Butterworth Grove, Kent, England: Ann Arbor Science. Also: Prakash, A. (1971). Terrigenous organic matter and coastal phytoplankton fertility. In J.D. Costlow (Ed.), Fertility of the sea, 2, 351-368. (Proceedings of an International Symposium on Fertility of the Sea, Sao Paulo, Brazil, London, and New York: Gordon and Breach Science)
44. Proteins, DNA, RNA – Khristeva, L.A., Soloche, K.I., Dynkina, R.L., Kovalenko, V.E., & Gorobaya, A.I. (1967). Influence of physiologically active substances of soil humus and fertilizers on nucleic acid metabolism, plant growth and subsequent quality of the seeds. Humus et Planta, 4, 272-276.
45. Proteins, DNA, RNA – Jackson, William R. (1993). Humic, Fulvic and Microbial Balance: Organic Soil Conditioning, 569-570. Evergreen, Colorado: Jackson Research Center.
46. Synthesis of RNA and DNA – Khristeva, L.A. (1968). About the nature of physiologically active substances of the soil humus and of organic fertilizers and their agricultural importance. In F.V. Hernando (Ed,), Pontifica academec scientarium citta del vaticano (701-721). New York: John Wiley.
47. Catalyst to vitamins within the cell – Williams, Dr. Roger J. (1977). The Wonderful World Within You. Bio-Communications Press. Wichita, Kansas.
48. Transport metal ions – Schnitzer, M., & Khan, S.U. (1972). Humic substances in the environment New York: Decker.
49. Acidity of fulvic acid – Schnitzer, M. (1977). Recent findings of the characterization of humic substances extracted fromsoils from widely differing climatic zones. Proceedings of the Symposium on Soil Organic Matter Studies, Braunsweig (117-131).
50. Environment with adeequate oxygen – Schnitzer, M. (1977). Recent findings of the characterization of humic substances extracted from soils from widely differing climatic zones. Proceedings of the Symposium on Soil Organic Matter Studies, Braunsweig (117-131).
51. Low molecular weight – Aiken, G. R., McKnight, D.M., & MacCarthy, P. 1985). Humic substances of soil, sediment and water, New York: Wiley-Interscience.
52. Absorption by cells – Azo, S. & Sakai, I (1963). Studies on the physiological effects of humic acid. Part 1. Uptake of humic acid by crop plants and its physiological effects. Soil Science and Plant Nutrition, 9(3), 1-91. (Tokyo)
53. https://pubmed.ncbi.nlm.nih.gov/30818142/