Fresh-water Diatomite in the Pacific Coast Region

The American Institute of Mining, Metallurgical, and Petroleum Engineers
Henry Mulryan
Organization:
The American Institute of Mining, Metallurgical, and Petroleum Engineers
Pages:
8
File Size:
1588 KB
Publication Date:
Jan 1, 1939

Abstract

DIATOMS are microscopic aquatic plants of the order Bacillariaceae. They are unicellular plants with skeletons made up of amorphous opaline silica. The skeletons show highly ornate, complicated geometrical designs. Diatoms live in water virtually everywhere. They are found in clean sea water, brackish water, and fresh-water lakes and ponds. When conditions are right, diatoms propagate by subdivision in huge numbers. Alkalinity, temperature, and the presence of high concentrations of silica in the water largely control diatom life. When the diatoms die the skeletons drop to the bottom of their habitat to form oozes of vary-ing thicknesses. DIATOMITES Diatomite, or diatomaceous earth, is composed essentially of the siliceous remains of the diatoms, although other organic skeletons are also present, especially in sea-water deposits where radiolaria, sponges and silico-flagellates are common. Impurities are generally carbonaceous material, fine-grained silt, volcanic ash and dust, and occasional coarse grains of sand. Diatomites are marine, brackish, or fresh-water, depending upon types of diatoms and their method of deposition.
Citation

APA: Henry Mulryan  (1939)  Fresh-water Diatomite in the Pacific Coast Region

MLA: Henry Mulryan Fresh-water Diatomite in the Pacific Coast Region. The American Institute of Mining, Metallurgical, and Petroleum Engineers, 1939.

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