Adept Alchemy. Part II. Chapter 8. Biological Transmutations
The study of biological transmutation can be said to have begun in the 17th century with the famous experiment by von Helmont, who grew a willow tree in a clay vase with 200 pounds of soil. After 5 years, he dried the soil and found that its weight had decreased by only 2 ounces: "Water alone had, therefore, been sufficient to produce 160 pounds of wood, bark and roots" (plus fallen leaves which he did not weigh). Presumably, there were some minerals in the water he fed to the tree. Nowadays we know that plants form carbohydrates from atmospheric carbon dioxide, but their mineral content is derived from soil, not air. It may be possible, however, that the ORMEs (Orbitally Rearranged Monoatomic Elements), discovered by David Hudson in the 1980s, exist in the atmosphere and are utilized by plants. In 1799, the French chemist Vauquelin became intrigued by the quantity of lime which hens excrete every day. He isolated a hen and fed it a pound of oats which were analyzed for lime (CaO). Vauquelin analyzed the eggs and feces and found five times more Ca was excreted than was consumed. He concluded that lime had been created, but could not figure out how it happened. In 1822, the English physiologist Prout studied the increase of calcium carbonate inside incubating chicken eggs, and was able to show that it was not contributed by the shell. In 1831, Choubard germinated watercress seeds in clean glass vessels and showed that the sprouts contained minerals which did not previously exist in the seeds.
The study of biological transmutation can be said to have begun in the 17th century with the famous experiment by von Helmont, who grew a willow tree in a clay vase with 200 pounds of soil. After 5 years, he dried the soil and found that its weight had decreased by only 2 ounces: "Water alone had, therefore, been sufficient to produce 160 pounds of wood, bark and roots" (plus fallen leaves which he did not weigh). Presumably, there were some minerals in the water he fed to the tree. Nowadays we know that plants form carbohydrates from atmospheric carbon dioxide, but their mineral content is derived from soil, not air. It may be possible, however, that the ORMEs (Orbitally Rearranged Monoatomic Elements), discovered by David Hudson in the 1980s, exist in the atmosphere and are utilized by plants.
In 1799, the French chemist Vauquelin became intrigued by the quantity of lime which hens excrete every day. He isolated a hen and fed it a pound of oats which were analyzed for lime (CaO). Vauquelin analyzed the eggs and feces and found five times more Ca was excreted than was consumed. He concluded that lime had been created, but could not figure out how it happened.
In 1822, the English physiologist Prout studied the increase of calcium carbonate inside incubating chicken eggs, and was able to show that it was not contributed by the shell.
In 1831, Choubard germinated watercress seeds in clean glass vessels and showed that the sprouts contained minerals which did not previously exist in the seeds.
