Gaois

Similar terms:

This is a static copy of data that is exported from IATE on an occasional basis. It should not be assumed that information provided about an entry here will always correspond to the current version of the entry in IATE. That current version can be checked by clicking on the link on the upper right hand side of each entry. More information »

2 results

  1. AGRI-FOODSTUFFS|food technology|food additive · INDUSTRY|chemistry|chemical compound
    carbónáit chailciam Reference Faomhadh an téarma seo mar chuid de Thionscadal Lex
    ga
    cailc Reference Faomhadh an téarma seo mar chuid de Thionscadal Lex
    ga
    lí bhán CI 18 Reference Faomhadh an téarma seo mar chuid de Thionscadal Lex
    ga
    Calciumcarbonat | Kalziumkarbonat | Calciumhydrogencarbonat | Kreide
    de
    Definition neutrales, zur Entsäuerung verwendetes kohlensaures Calcium Reference office international de la vigne et du vin
    calcium carbonate | CI pigment white 18 | chalk
    en
    Definition product obtained from ground limestone or by the precipitation of calcium ions with carbonate ions Reference "Directive 95/45/EC laying down specific purity criteria concerning colours for use in foodstuffs http://eur-lex.europa.eu/LexUriServ/site/en/consleg/1995/L/01995L0045-20060410-en.pdf (17.6.2009)"
    carbonate de calcium | pigment blanc CI 18 | craie
    fr
    Definition sel neutre de chaux de l'acide carbonique employé pour désacidifier les mouts ou les vins Reference office international de la vigne et du vin
    CaCO3 | CaCO3 | CCaO3 | E 170 (i) | E170 (i) | E170(i) | E 170i | E170i | E 170 | E170
    mul
  2. ENVIRONMENT
    cailc Reference an Ghníomhaireacht Eorpach Comhshaoil (GEC)
    ga
    Kreide
    de
    chalk
    en
    Definition 1.A soft, pure, earthy, fine-textured, usually white to light gray or buff limestone of marine origin, consisting almost wholly (90-99%) of calcite, formed mainly by shallow-water accumulation of calcareous tests of floating microorganisms (chiefly foraminifers) and of comminuted remains of calcareous algae (such as cocoliths and rhabdoliths), set in a structureless matrix of very finely crystalline calcite. The rock is porous, somewhat friable, and only slightly coherent. It may include the remains of bottom-dwelling forms (e.g. ammonites, echinoderms, and pelecypods), and nodules of chert and pyrite. The best known and most widespread chalks are of Cretaceous age, such as those exposed in cliffs on both sides of the English Channel. Reference 1.BJGEO;
    craie
    fr