orthosilicic Antonyms

No Synonyms and anytonyms found

Meaning of orthosilicic

Webster

orthosilicic (a.)

Designating the form of silicic acid having the normal or highest number of hydroxyl groups.

orthosilicic Sentence Examples

  1. Orthosilicic acid, an inorganic compound, serves as the primary constituent of many silicates.
  2. Orthosilicic acid's chemical structure consists of a silicon atom surrounded by four hydroxyl groups.
  3. The reactivity of orthosilicic acid enables it to undergo various chemical reactions, such as condensation and hydrolysis.
  4. Orthosilicic acid's solubility plays a crucial role in the formation of silicate minerals and the weathering of rocks.
  5. Orthosilicic acid's acidity contributes to the protonation of other molecules and the release of protons in solutions.
  6. Orthosilicic acid's polymerization can lead to the formation of silicic acid, a polymeric species with a complex structure.
  7. Orthosilicic acid's presence in marine environments affects the growth and physiology of diatoms and other marine organisms.
  8. Orthosilicic acid's industrial applications include its use as a coagulant in water treatment and a precursor in the synthesis of silicones.
  9. Orthosilicic acid's potential health benefits, including its role in bone health and collagen synthesis, are still being studied.
  10. Orthosilicic acid's environmental impact is a subject of ongoing research due to its potential interactions with soil, water, and biota.

FAQs About the word orthosilicic

Designating the form of silicic acid having the normal or highest number of hydroxyl groups.

No synonyms found.

No antonyms found.

Orthosilicic acid, an inorganic compound, serves as the primary constituent of many silicates.

Orthosilicic acid's chemical structure consists of a silicon atom surrounded by four hydroxyl groups.

The reactivity of orthosilicic acid enables it to undergo various chemical reactions, such as condensation and hydrolysis.

Orthosilicic acid's solubility plays a crucial role in the formation of silicate minerals and the weathering of rocks.