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Please use this identifier to cite or link to this item: http://scholars.ntou.edu.tw/handle/123456789/19999
DC FieldValueLanguage
dc.contributor.author江支豪en_US
dc.contributor.author陳惠芬en_US
dc.contributor.author方建能en_US
dc.contributor.author林怡君en_US
dc.date.accessioned2022-01-19T03:50:17Z-
dc.date.available2022-01-19T03:50:17Z-
dc.date.issued2008-03-
dc.identifier.urihttp://scholars.ntou.edu.tw/handle/123456789/19999-
dc.description.abstract本研究收集十九個分屬相同或相異二級構造單元之天然與合成沸石標本,其目的在於探究,相同二級構造單元之沸石礦物是否具有相似之拉曼光譜,而不同二級構造單元之沸石礦物則有不同之拉曼光譜。因此,本研究選用 390~530 cm-1範圍之拉曼光譜特徵峰,來探究上述問題。 實驗結果顯示,相同二級構造單元之沸石礦物,確實具有相似之拉曼光譜,以致於難以用來區分彼此。相反的,不同二級構造單元之沸石礦物,卻能用其獨特拉曼光譜區分如下:纖維狀沸石用 436~445 cm-1 和533~536 cm-1,單連結四環鏈沸石用 382~387cm-1,雙連結四環鏈沸石用 421~426 cm-1,六環沸石用 479~484 cm-1 ,絲光沸石群用 397~406 cm-1 和513~529 cm-1,以及片沸石群用 404~410 cm-1。en_US
dc.language.isozhen_US
dc.relationMineral and gemstone researchen_US
dc.subject沸石en_US
dc.subject拉曼光譜en_US
dc.subject二級構造單元en_US
dc.title由拉曼光譜區分沸石礦物之二級構造單元en_US
item.fulltextno fulltext-
item.grantfulltextnone-
item.languageiso639-1zh-
crisitem.author.deptCollege of Ocean Science and Resource-
crisitem.author.deptInstitute of Earth Sciences-
crisitem.author.deptNational Taiwan Ocean University,NTOU-
crisitem.author.orcid0000-0003-0188-9342-
crisitem.author.parentorgNational Taiwan Ocean University,NTOU-
crisitem.author.parentorgCollege of Ocean Science and Resource-
Appears in Collections:地球科學研究所
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