Chalcedony: Béda antara owahan
Kaca anyar: {{Infobox mineral | name = Chalcedony | category = Mineral oksida | image = Chalcedony geode.JPG | imagesize = 250 | caption = Batu chalcedony | formul... |
(Ora ana béda)
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Révisi kala 20 Fèbruari 2018 02.42
Chalcedony /kælˈsɛdəni/ inggih menika satunggaling wujud ingkang sami tumpuk-
Chalcedony | |
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250px|alt= | |
Umum | |
Kategori | Mineral oksida |
Rumus kimia | Silika (silikon dioksida, SiO2) |
Identifikasi | |
Massa molekul | 60 g / mol |
Warna | maneka werna |
Skala kekerasan Mohs | 6 - 7 |
Berat jenis | 2.59 - 2.61 |
Referensi | [1] |
tumpukan.[2] Kuarsa lan moganit
menika kalebet mineral silika, ananging kuarsa menika kagungan perangan trigonal wondene ingkang
moganit menika gadhah sifat ingkang monoklinik. Struktur kimia saking chalcedony inggih menika
SiO2.
Nama chalcedony menika asalipun saking basa Latin chalcedonius (utawi calchedonius).
Istilah menika ingkang kaping sepisan wonten ing satunggaling karyanipun Pliny the Elder,
Naturalis Historia ingkang dipunginakaken kangge nyebat batuan Jaspis ingkang asifat
transparan.Masalah sitiran: </ref>
panutup ora ana tumrap tenger <ref>
Ananging
istilah khalkedon (χαλκηδών) menika ugi medal wonten ing Book of Revelation.[3]
Geokimia
Struktur
Chalcedony menika nate dipunwastani minangka kriptokristalin kuarsa ingkang gadhah kandhutan
serat[4] ananging
samenika dipunmangertosi bilih chalcedony menika ugi gadhah sifat ingkang polimorf amargi wonten
moganit wonten ing salebeting chalsedony kasebat.[2][5][6] Kadar moganit ing satunggal sampel chalcedony maneka werna, Padatanipun
ing antawisipun 5 dumugi 20 persen.[7]
Kelarutan
Sinaosa gadhah senyawa kimia ingkang memper kaliyan kuarsa, ananging chalcedony menika gadhah sifat
langkung larut tinimbang kaliyan kuarsa wonten ing temperatur ingkang andhap. Bab menika saged amargi
kristal chalcedony menika langkung alus satemah gadhah rasio wiyaring permukaan lan volume ingkang
langkung inggil ingkang dipunprakirakaken amargi wontenipun moganit.[7]
Referensi
- ↑ Rudolf Duda and Lubos Rejl: Minerals of the World (Arch Cape Press, 1990)
- ↑ a b Heaney, Peter J., 1994. Structure and Chemistry of the low-pressure silica polymorphs. In: Reviews in Mineralogy v. 29; Silica: Physical Behavior, geochemistry and materials applications. Ed. Heaney, P.J., Prewitt, C.T., Gibbs, G.V., 1-40
- ↑ James Orr, èd. (1915). "Chalkēdōn". [http://books.google.com/?
id=CqPNAAAAMAAJ&pg=PA2859&dq=chalcedony+Chalkedon#v=onepage&q=chalcedony%20Chalkedon&f=false The International Standard Bible Encyclopaedia]. The Howard-Severance
company. kc. 2859.
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at position 22 (pitulung); line feed character in|url=
at position 26 (pitulung) - ↑ Chalcedony mineral information and data. http://www.mindat.org/min-960.html
- ↑ Origlieri, Marcus. "Moganite: a New Mineral -- Not!" Lithosphere (1994). Aug. 2007 <http://fgms.home.att.net/moganite.htm>.
- ↑ Nickel, Ernest H., and Monte C. Nichols. "IMA/CNMNC List of Mineral Names." Materials Data. June 2007. Aug. 2007 <http://www.geo.vu.nl/users/ima- cnmmn/MINERALlist.pdf>
- ↑ a b Heaney, Peter J., and Jeffrey E. Post. "The Widespread Distribution of a Novel Silica Polymorph in Microcrystalline Quartz Varieties." Science ns 255 (1992): 441-443. JSTOR. Aug. 2007. Keyword: moganite
Pranala njawi
Wikisource ndhuweni teks artikel Ensiklopedia Britannica 1911 babagan Chalcedony. |
Wikimedia Commons duwé médhia ngenani chalcedony. |
- Mindat: mineralogical data Chalcedony
- [http://minerals.usgs.gov/minerals/pubs/commodity/gemstones/sp14-95/chalcedony.html USGS: US
Chalcedony locations]