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Sapropel

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sapropel [′sap·rə‚pel]
(geology)
A mud, slime, or ooze deposited in more or less open water.

Sapropel 

freshwater silt deposits containing large amounts of organic matter—for example, lignin and humus complexes, carbohydrates, and bitumens—in a colloidal state. Sapropels are used in medicine (physical therapy) for applications and diluted baths.

In agriculture sapropel is used after aeration as a fertilizer, especially on acid and light sandy soil and sandy loam; 30–40 tons/hectare are used for grain crops, and 60–70 tons/hectare are used for vegetable, potato, and root crops. Sapropel is also used in the preparation of composts. Sapropels, which are rich in salts of calcium, iron, and phosphorus, contain no sand and are poor in clay. They are added to the rations given agricultural animals as a mineral supplement; daily sapropel supplements reach 2 kg for hogs, 3 kg for cows, and 10–15 g for hens.



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Nine of these (limestone, dolomite, sand, gravel, clay, chalky marl, peat, sapropel, and oil) are under exploitation, and the exploitation of gaize (opoka) was suspended in the 1990s.
Data obtained from experiments with these oil shales were correlated with the corresponding data on black shales and sapropels rich in organic matter.
Magnetic properties and geochemistry of the active oxidation front and the youngest sapropel in the eastern Mediterranean Sea.
 
 
 
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