'Choke damp' definitions:

Definition of 'Choke damp'

From: GCIDE

Definition of 'Choke damp'

From: GCIDE
  • Damp \Damp\ (d[a^]mp), n. [Akin to LG., D., & Dan. damp vapor, steam, fog, G. dampf, Icel. dampi, Sw. damb dust, and to MNG. dimpfen to smoke, imp. dampf.]
  • 1. Moisture; humidity; fog; fogginess; vapor. [1913 Webster]
  • Night . . . with black air Accompanied, with damps and dreadful gloom. --Milton. [1913 Webster]
  • 2. Dejection; depression; cloud of the mind. [1913 Webster]
  • Even now, while thus I stand blest in thy presence, A secret damp of grief comes o'er my soul. --Addison. [1913 Webster]
  • It must have thrown a damp over your autumn excursion. --J. D. Forbes. [1913 Webster]
  • 3. (Mining) A gaseous product, formed in coal mines, old wells, pints, etc. [1913 Webster]
  • Choke damp, a damp consisting principally of carbonic acid gas; -- so called from its extinguishing flame and animal life. See Carbonic acid, under Carbonic.
  • Damp sheet, a curtain in a mine gallery to direct air currents and prevent accumulation of gas.
  • Fire damp, a damp consisting chiefly of light carbureted hydrogen; -- so called from its tendence to explode when mixed with atmospheric air and brought into contact with flame. [1913 Webster]

Definition of 'choke damp'

From: GCIDE
  • Carbonic \Car*bon"ic\, a. [Cf. F. carbonique. See Carbon.] (Chem.) Of, pertaining to, or obtained from, carbon; as, carbonic oxide. [1913 Webster]
  • Carbonic acid (Chem.), an acid HO.CO.OH, not existing separately, which, combined with positive or basic atoms or radicals, forms carbonates. In common language the term is very generally applied to a compound of carbon and oxygen, CO2, more correctly called carbon dioxide. It is a colorless, heavy, irrespirable gas, extinguishing flame, and when breathed destroys life. It can be reduced to a liquid and solid form by intense pressure. It is produced in the fermentation of liquors, and by the combustion and decomposition of organic substances, or other substances containing carbon. It is formed in the explosion of fire damp in mines, and is hence called after damp; it is also know as choke damp, and mephitic air. Water will absorb its own volume of it, and more than this under pressure, and in this state becomes the common soda water of the shops, and the carbonated water of natural springs. Combined with lime it constitutes limestone, or common marble and chalk. Plants imbibe it for their nutrition and growth, the carbon being retained and the oxygen given out.
  • Carbonic oxide (Chem.), a colorless gas, CO, of a light odor, called more correctly carbon monoxide. It is almost the only definitely known compound in which carbon seems to be divalent. It is a product of the incomplete combustion of carbon, and is an abundant constituent of water gas. It is fatal to animal life, extinguishes combustion, and burns with a pale blue flame, forming carbon dioxide. [1913 Webster]