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单词 allophane
释义

allophanen.

Brit. /ˈaləfeɪn/, U.S. /ˈæləˌfeɪn/
Forms: 1800s allophan, 1800s– allophane.
Origin: Formed within English, by compounding; modelled on a German lexical item. Etymons: allo- comb. form, -phane comb. form.
Etymology: < allo- comb. form + -phane comb. form, after German Allophan (F. Stromeyer & J. F. L. Hausmann 1816, in Annalen der Physik 54 120), itself apparently after Byzantine Greek ἀλλοϕανής (see allophanic adj.1), the mineral being so named on account of its unusual appearance (compare quot. 1817). Compare French allophane (1816 in an abstract of the German coinage paper).In form allophan after the German form.
Mineralogy.
An amorphous clay mineral, typically pale blue, consisting essentially of hydrated aluminium silicate.
ΘΚΠ
the world > the earth > minerals > types of mineral > silicates > tectosilicate > [noun] > other tektosilicates
sarcolite1814
allophane1817
gmelinite1825
levyne1825
schrötterite1844
levynite1868
maskelynite1875
steatoid1877
griqualandite1887
tiger-eye1891
pennantite1946
tacharanite1961
the world > the earth > minerals > types of mineral > silicates > miscellaneous silicates > [noun] > silicate of aluminium
allophane1817
newtonite1891
1817 Ann. Philos. 9 244 Allophan. This name has been given by Stromeyer to a new mineral lately analysed by him, because it has very much the appearance of a copper salt.
1875 R. Hunt & F. W. Rudler Ure's Dict. Arts (ed. 7) I. 90 Allophanes have been found containing from 14 to 19 per cent. of oxide of copper, which gives them a green colour.
1930 Amer. Jrnl. Police Sci. 1 410 From the mineralogical aspect clay is found in many forms, such as allophane, kaolin, holloysite, etc.
1994 M. B. McBride Environmental Chem. Soils ii. 53 Soils formed from volcanic ash commonly contain allophane, a noncrystalline hydrous aluminosilicate.
2008 B. Velde & A. Meunier Origin Clay Minerals in Soils viii. 327 The key to the presence of both imogolite and allophane is a continuous humid condition.
This entry has been updated (OED Third Edition, September 2012; most recently modified version published online December 2021).
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n.1817
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