Gaois

Téarmaí cosúla:

Cóip statach de shonraí a easpórtáiltear ó IATE ó am go chéile atá sa chnuasach seo. Níor cheart glacadh leis gurb ionann i gcónaí an t-eolas a thugtar faoi iontráil anseo agus a bhfuil sa leagan reatha den iontráil ar IATE. Is féidir an leagan reatha sin a cheadú ach cliceáil ar an nasc atá ar thaobh na láimhe deise ag barr gach iontrála. Breis eolais »

2 thoradh

  1. AGRI-FOODSTUFFS|food technology|food additive · INDUSTRY|chemistry|chemical compound

    #632862

    IATE #1617472
    carbónáit chailciam Tagairt Faomhadh an téarma seo mar chuid de Thionscadal Lex
    ga
    cailc Tagairt Faomhadh an téarma seo mar chuid de Thionscadal Lex
    ga
    lí bhán CI 18 Tagairt Faomhadh an téarma seo mar chuid de Thionscadal Lex
    ga
    Calciumcarbonat | Kalziumkarbonat | Calciumhydrogencarbonat | Kreide
    de
    Sainmhíniú neutrales, zur Entsäuerung verwendetes kohlensaures Calcium Tagairt office international de la vigne et du vin
    calcium carbonate | CI pigment white 18 | chalk
    en
    Sainmhíniú product obtained from ground limestone or by the precipitation of calcium ions with carbonate ions Tagairt "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
    Sainmhíniú sel neutre de chaux de l'acide carbonique employé pour désacidifier les mouts ou les vins Tagairt 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

    #670409

    IATE #45554
    cailc Tagairt an Ghníomhaireacht Eorpach Comhshaoil (GEC)
    ga
    Kreide
    de
    chalk
    en
    Sainmhíniú 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. Tagairt 1.BJGEO;
    craie
    fr