稀土礦物:修订间差异
补救3个来源,并将0个来源标记为失效。) #IABot (v2.0.7 |
ThomasYehYeh(留言 | 贡献) 把[rare earth mineral]翻譯為中文,雖說這篇在2006年就已經由前輩起頭,但篇幅增加有限。我將[稀土元素]和[白雲鄂博礦區]英文版中部分資料引用,融入這一篇中,並將之前的作品覆蓋。這兩天看到有"2022年古羅斯相關條目偽造事件"宣導,我逐一檢查英文版中所列的礦物,確定沒造假,但是否就包含重要的礦物,請先進們指教。 |
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{{main|稀土元素}} |
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{{Missing information|1=稀土矿物的特征、分类、(晶体)结构等|time=2019-12-31T08:20:49+00:00}} |
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[[File:RareEarthOreUSGOV.jpg|thumb|稀土礦物 (以一枚直徑19[[毫米]]的[[1美分硬幣]]來與礦石做對比)]] |
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[[File:USGS_rare_earth_oxides_production_graph.PNG|thumb|right|upright=1.5|全球稀土來源 ([[美國]]用淺[[藍色]]表示, 中國用[[紅色]]表示)]] |
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[[File:Baiyunebo ast 2006181.jpg|thumb|位於中國[[包頭]][[白雲鄂博礦區]]的[[假色]]衛星相片,2006年]] |
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{{main|稀土金属}} |
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'''稀土礦物''' ({{Lang-en|Rare-earth mineral}})指主要[[金屬]]成份為一種或多種[[稀土金属]]的[[礦物]],是中國[[改革開放]]後十份重視的[[自然資源|資源]]。由於稀土用途廣泛,<ref>{{cite web |author1=Simon Webb |author2=Lisa Shumaker |author3=Jonathan Oatis |title=U.S. dependence on China's rare earth: Trade war vulnerability |url=https://www.reuters.com/article/us-usa-trade-china-rareearth-explainer/u-s-dependence-on-chinas-rare-earth-trade-war-vulnerability-idUSKCN1TS3AQ |website=Reuters |accessdate=2019-12-31 |archive-date=2019-12-23 |archive-url=https://web.archive.org/web/20191223200213/https://www.reuters.com/article/us-usa-trade-china-rareearth-explainer/u-s-dependence-on-chinas-rare-earth-trade-war-vulnerability-idUSKCN1TS3AQ |dead-url=no }}</ref>故有此一說:「[[中東]]有[[石油]],中國有稀土」。<ref>{{cite web |author1=陳子凌 |title=稀土是中國「秘密武器」? 事實卻不盡然... |url=https://www.mpfinance.com/fin/instantf2.php?node=1558425600156&issue=20190521 |website=[[明報]] |accessdate=2019-12-31 |archive-date=2019-12-31 |archive-url=https://web.archive.org/web/20191231074304/https://www.mpfinance.com/fin/instantf2.php?node=1558425600156&issue=20190521 |dead-url=no }}</ref>[[日本]]一直都想減低對[[進口]]中國稀土礦物的依賴。<ref>歌籃. [https://www.voacantonese.com/a/how-japan-handled-rare-earth-threats-02062019/4943268.html 日本如何成功對抗中國限制稀土貿易“殺手鐧”] {{Wayback|url=https://www.voacantonese.com/a/how-japan-handled-rare-earth-threats-02062019/4943268.html |date=20190607081902 }}. [[美國之音]]. 2019/6/3</ref> |
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所稱的'''稀土礦物'''({{lang-en|Rare earth mineral}})中,通常會含有一種或是多種[[稀土元素]]的成分。稀土礦物通常與[[鹼]]性至{{le|高鹼性岩石|Peralkaline rock|高鹼性}}[[火成岩]]複合物有關聯,與鹼性[[岩漿]]相關的[[偉晶岩]]、或是存在{{le|碳酸鹽岩|carbonatite|碳酸}}[[深成岩]]中,或是與之有關聯。<ref name=“rare metal”>{{cite journal |last1=Dostal|first1= Jaroslav |last2=|first2= |date=April 2016|title= Rare Metal Deposits Associated with Alkaline/Peralkaline Igneous Rocks |
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==參考資料== |
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|url= |journal=ResearchGate |volume= |issue= |pages= |doi= 10.5382/Rev.18.02|access-date=2022-1-7}}</ref>具有[[鈣鈦礦 (結構)|鈣鈦]]礦物相(mineral phase)的岩石是鹼性複合物中稀土元素的共同宿主。<ref>{{cite journal |last1= Campbell|first1= Linda S |last2=Henderson|first2=Paul |date=April 1997|title= Rare Earth Chemistry of Perovskite Group Minerals from the Gardiner Complex, East Greenland |
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{{reflist}} |
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|url= |journal=Mineralogical Magazine |
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|volume= 61|issue= 405|pages=1970212 |doi= 10.1180/minmag.1997.061.405.04|access-date=2022-1-7}}</ref>來自[[地幔]]的碳酸鹽熔體也是稀土的載體。<ref>{{cite book |last1= Yaxley|first1= Gregory M. |last2= Sujoy Ghosh|first2=Sujoy |date= |title= Deep Carbon|url= https://www.cambridge.org/core/books/deep-carbon/co2rich-melts-in-earth/D59E43A67373FD4BA68E2D7969F1614F|location= 6 - CO2-Rich Melts in Earth |
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|quote=They are also of particular economic importance as hosts or sources of many critical metals, including the rare earth elements (REEs) Nb, Ta, P, and others.|publisher= Cambridge University Press|page=129 - 162 |isbn= |author-link= }}</ref>與鹼性[[岩漿作用]]相關的[[熱液系統|熱液]]礦床含有多種稀土礦物。<ref name=“rare metal”/> |
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而稀土元素是一組共17種,具有光澤,但之間難以區別的銀白色軟性重金屬。<ref name="ASella2016">Professor of Chemistry at [[University College London]], [[Andrea Sella]], {{YouTube|UvQMiqqzcZE |Andrea Sella: "Insight: Rare-earth metals"}}, Interview on [[TRT World]] / Oct 2016, minutes 4:40 - ff.</ref><ref>{{cite book|title=The Elements|author=T Gray|publisher=Black Dog & Leventhal|year=2007|pages=118–122|chapter=Lanthanum and Cerium}}</ref> |
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雖然名為稀土元素,但實際上這些元素在地殼中的數量相對豐富,鈰是地球中排名第25最豐富的元素(參見[[地球的地殼元素豐度列表|地殼元素豐富度列表]])佔68百萬分率,數量超過[[銅]]。由於稀土元素具有的[[地球化學]]特性,它們通常是呈分散狀態,而不常有高濃度的稀土礦物存在。因此世界上少有經濟上值得開採的礦場(因此而得「稀土」之名)。<ref name="Haxel02">{{cite web|url=http://pubs.usgs.gov/fs/2002/fs087-02/fs087-02.pdf|title=Rare Earth Elements—Critical Resources for High Technology|author=Haxel G.|author2=Hedrick J.|date=2002|publisher=United States Geological Survey|others=Edited by Peter H. Stauffer and James W. Hendley II; Graphic design by Gordon B. Haxel, Sara Boore, and Susan Mayfield|id=USGS Fact Sheet: 087‐02|access-date=2012-03-13|quote=However, in contrast to ordinary base and [[precious metals]], REE have very little tendency to become concentrated in exploitable ore deposits. Consequently, most of the world's supply of REE comes from only a handful of sources.|author3=Orris J.}}</ref> |
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[[中國]]的儲藏量佔全世界的36.7%,<ref name="gu">{{cite news|url=https://www.theguardian.com/environment/2010/dec/26/rare-earth-metals-us|title=Rare earth metals mine is key to US control over hi-tech future: Approval secured to restart operations, which could be crucial in challenging China's stranglehold on the market|date=26 December 2010|work=The Guardian|author=Suzanne Goldenberg|location=London}}</ref>但中國的產量曾佔全世界的95%以上,<ref name=":2">{{Cite web|url=https://pubs.usgs.gov/of/2011/1042|title=USGS Report Series 2011–1042: China's Rare-Earth Industry|last=Tse|first=Pui-Kwan|website=pubs.usgs.gov|access-date=2018-04-04}}</ref>在2017年佔全世界的81%。到2021年中國的產量佔全世界的60.63%,而同年[[美國]]的產量排名第2,佔比為15.52%。<ref>{{cite web| url =https://www.statista.com/statistics/270277/mining-of-rare-earths-by-country/| title = Distribution of rare earths production worldwide as of 2021, by country| publisher = statista| date =2022-03-04| accessdate =2022-06-12}}</ref> |
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中國的[[白雲鄂博礦區]]是世界已知最大的稀土礦物蘊藏區。<ref name="Distillations">{{cite web |title=Rare Earths: The Hidden Cost to Their Magic" (Part 2), Distillations Podcast and transcript, Episode 242 |url=https://www.sciencehistory.org/distillations/podcast/rare-earths-the-hidden-cost-to-their-magic |website=Science History Institute|date=June 25, 2019 |access-date=2019-8-28}}</ref>在2005年,這個礦區的稀土元素產量曾高達全世界的45%。<ref>{{cite journal |
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| title = The Bayan Obo iron-rare-earth-niobium deposits, Inner Mongolia, China |
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| author = Lawrence J. Drewa, Meng Qingrunb and Sun Weijun |
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| journal = [[Lithos (journal)|Lithos]] |
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| volume = 26 |
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| issue = 1–2 |
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| pages = 43–65 |
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| year = 1990 |
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| doi = 10.1016/0024-4937(90)90040-8 }}</ref><ref>{{cite journal |
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| title = Chemical compositions of carbonate minerals from Bayan Obo, Inner Mongolia, China: implications for petrogenesis |
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| author = Xue-Ming Yang, Michael J. Le Bas |
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| journal = Lithos |
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| volume = 72 |
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| issue = 1–2 |
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| pages = 97–116 |
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| year = 2004 |
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| doi = 10.1016/j.lithos.2003.09.002 }}</ref><ref>{{cite journal |
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| title = Bayan Obo Controversy: Carbonatites versus Iron Oxide-Cu-Au-(REE-U) |
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| author = Chengyu Wu |
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| journal = Resource Geology |
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| volume = 58 |
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| issue = 4 |
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| pages = 348–354 |
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| year = 2007 |
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| url = http://www3.interscience.wiley.com/journal/121496988/abstract |
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| archive-url = https://archive.today/20121217213134/http://www3.interscience.wiley.com/journal/121496988/abstract |
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| url-status = dead |
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| archive-date = 2012-12-17 |
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| doi = 10.1111/j.1751-3928.2008.00069.x }}</ref> |
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==常見稀土礦物== |
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以下所列的是比較常見的熱液稀土礦物,以及經常含有顯著稀土元素替代物的礦物:<ref>{{cite web |
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| url =https://www.chemistryworld.com/news/rare-element-substitution-a-tricky-proposition/6936.article |
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| title = Rare element substitution a tricky proposition |
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| publisher = CHEMISTRYWORLD |
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| date = 2014-1-6 |
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| accessdate = 2022-1-7 |
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}}</ref> |
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{{div col|colwidth=20em}} |
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*[[釔易解石]]或[[鈰易解石]] |
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*{{le|褐簾石|allanite}} |
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*[[磷灰石]] |
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*{{le|氟碳鈰礦|bastnäsite}} |
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*{{le|磷灰石|Britholite-(Ce) }}或釔矽磷灰石 |
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*{{le|板鈦礦|brockite}} |
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*{{le|矽鈰石礦|cerite}} |
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*{{le|硫矽酸鹽綠簾石Dollaseite-(Ce)}} |
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*{{le|氟鈰石|fluocerite}} |
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*[[螢石]] |
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*[[硅鈹釔礦]] |
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*[[獨居石]] |
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*{{le|氟碳鈰鈣石|Parisite-(Ce)}}或氟碳鑭鈣石(Parisite-(La)) |
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*{{le|菱硼硅鈰礦|Stillwellite-(Ce)}} |
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*{{le|直碳鈣鈰礦|Synchysite-(Ce)}} |
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*[[榍石]] |
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*{{le|氧釩釔礦|wakefieldite}} |
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*[[磷釔礦]] |
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*[[鋯石]] |
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{{div col end}} |
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==開採作業對環境的可能影響== |
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在自然環境中的稀土元素濃度非常低。蘊藏這類資源的礦山通常位於環境和社會標準非常低的國家,因為礦山的開發,而導致有侵犯人權、森林砍伐的情事,並且污染到當地的土地和水源。<ref name=rizk>{{Cite web|title=What colour is the cloud?|first1=Shirley |last1=Rizk |date=2019-06-21|url=https://www.eib.org/en/stories/digital-footprint|access-date=2020-09-17|website=European Investment Bank|language=en}}</ref><ref name=standaert>{{Cite web|title=China Wrestles with the Toxic Aftermath of Rare Earth Mining|url=https://e360.yale.edu/features/china-wrestles-with-the-toxic-aftermath-of-rare-earth-mining|first1=Michael|last1=Standaert|date=2019-07-02|access-date=2021-06-16|publisher=Yale School of the Environment|work=Yale Environment 360}}</ref> |
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在採礦和工業生產場所附近,稀土元素的濃度會上升到正常背景水準的許多倍。稀土元素一旦進入環境,就會滲入土壤中,然後它們的遷移取決於多種因素,例如侵蝕作用、風化作用、pH值、降水和地下水等。如同金屬一樣,它們可根據土壤條件形成,無論是移動,或是被吸附到土壤顆粒中。根據它們的生物利用度,稀土元素可被植物吸收,然後被人類和牲畜攝入。對於稀土元素的開採,使用( 肥料添加劑)和磷肥的生產,都會導致稀土元素污染 。<ref name="Volokh">{{Cite journal |date=1990-06-01 |title=Phosphorus fertilizer production as a source of rare-earth elements pollution of the environment |journal=Science of the Total Environment |language=en |volume=95 |pages=141–148 |doi=10.1016/0048-9697(90)90059-4 |pmid=2169646 |issn=0048-9697|bibcode=1990ScTEn..95..141V |last1=Volokh |first1=A. A. |last2=Gorbunov |first2=A. V. |last3=Gundorina |first3=S. F. |last4=Revich |first4=B. A. |last5=Frontasyeva |first5=M. V. |author6=Chen Sen Pal }}</ref>此外,在萃取稀土元素的過程中會用到強酸,而這些酸會滲入環境,並通過水體而導致水生環境酸化。 |
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對於稀土元素的開採、提煉和回收,如果管理不當,會對環境造成嚴重後果。稀土元素尾礦中的釷和鈾因有低放射性,而存有潛在危害,<ref>Bourzac, Katherine. [http://www.technologyreview.com/energy/26655/?p1=MstCom "Can the US Rare-Earth Industry Rebound?"] ''Technology Review''. 2010-10-29.</ref>這些物質如果處理不當,會對環境造成廣泛的傷害。 |
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==參見== |
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*[[稀土元素]] |
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*[[中國稀土業]] |
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*[[稀土貿易糾紛]] |
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* [[矿物]] |
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* [[岩石]]/[[岩石列表]] |
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* [[地质学]] |
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==參考文獻== |
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* Jones, Adrian P., Francis Wall and C. Terry Williams, eds. (1996) ''Rare Earth Minerals: Chemistry, Origin and Ore Deposits'', The Mineralogy Society Series #7, 372 pp. {{ISBN|978-0-412-61030-1}} |
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{{reflist|2}} |
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*[https://web.archive.org/web/20150402100826/http://prysmag.com/News/New-Policy-Affect-RE-Price.html China New Policy Affect Rare Earth Price] |
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== 外部連結 == |
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* {{Commons category-inline|Rare earth elements}} |
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{{external media |
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| audio1 = [https://www.sciencehistory.org/distillations/podcast/rare-earths-the-hidden-cost-to-their-magic "Rare Earths: The Hidden Cost to Their Magic"], Distillations Podcast and transcript, Episode 242, June 25, 2019, Science History Institute | video1 = [https://www.sciencehistory.org/rare-earth-elements-project “10 ways rare earth elements make life better”], animation, Science History Institute | video2 = [https://www.youtube.com/watch?v=aglMNj4hld0 Rare Earth Elements: The Intersection of Science and Society], presentation and discussion led by Ira Flatow, Science History Institute, 2019-9-24 }} |
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[[Category:稀土矿物]] |
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[[Category:金屬元素]] |
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[[Category:稀土金属]] |
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[[分類:稀土礦物]] |
2022年6月20日 (一) 09:17的版本
所稱的稀土礦物(英語:Rare earth mineral)中,通常會含有一種或是多種稀土元素的成分。稀土礦物通常與鹼性至高鹼性火成岩複合物有關聯,與鹼性岩漿相關的偉晶岩、或是存在碳酸深成岩中,或是與之有關聯。[1]具有鈣鈦礦物相(mineral phase)的岩石是鹼性複合物中稀土元素的共同宿主。[2]來自地幔的碳酸鹽熔體也是稀土的載體。[3]與鹼性岩漿作用相關的熱液礦床含有多種稀土礦物。[1]
而稀土元素是一組共17種,具有光澤,但之間難以區別的銀白色軟性重金屬。[4][5] 雖然名為稀土元素,但實際上這些元素在地殼中的數量相對豐富,鈰是地球中排名第25最豐富的元素(參見地殼元素豐富度列表)佔68百萬分率,數量超過銅。由於稀土元素具有的地球化學特性,它們通常是呈分散狀態,而不常有高濃度的稀土礦物存在。因此世界上少有經濟上值得開採的礦場(因此而得「稀土」之名)。[6]
中國的儲藏量佔全世界的36.7%,[7]但中國的產量曾佔全世界的95%以上,[8]在2017年佔全世界的81%。到2021年中國的產量佔全世界的60.63%,而同年美國的產量排名第2,佔比為15.52%。[9]
中國的白雲鄂博礦區是世界已知最大的稀土礦物蘊藏區。[10]在2005年,這個礦區的稀土元素產量曾高達全世界的45%。[11][12][13]
常見稀土礦物
以下所列的是比較常見的熱液稀土礦物,以及經常含有顯著稀土元素替代物的礦物:[14]
開採作業對環境的可能影響
在自然環境中的稀土元素濃度非常低。蘊藏這類資源的礦山通常位於環境和社會標準非常低的國家,因為礦山的開發,而導致有侵犯人權、森林砍伐的情事,並且污染到當地的土地和水源。[15][16]
在採礦和工業生產場所附近,稀土元素的濃度會上升到正常背景水準的許多倍。稀土元素一旦進入環境,就會滲入土壤中,然後它們的遷移取決於多種因素,例如侵蝕作用、風化作用、pH值、降水和地下水等。如同金屬一樣,它們可根據土壤條件形成,無論是移動,或是被吸附到土壤顆粒中。根據它們的生物利用度,稀土元素可被植物吸收,然後被人類和牲畜攝入。對於稀土元素的開採,使用( 肥料添加劑)和磷肥的生產,都會導致稀土元素污染 。[17]此外,在萃取稀土元素的過程中會用到強酸,而這些酸會滲入環境,並通過水體而導致水生環境酸化。
對於稀土元素的開採、提煉和回收,如果管理不當,會對環境造成嚴重後果。稀土元素尾礦中的釷和鈾因有低放射性,而存有潛在危害,[18]這些物質如果處理不當,會對環境造成廣泛的傷害。
參見
參考文獻
- Jones, Adrian P., Francis Wall and C. Terry Williams, eds. (1996) Rare Earth Minerals: Chemistry, Origin and Ore Deposits, The Mineralogy Society Series #7, 372 pp. ISBN 978-0-412-61030-1
- ^ 1.0 1.1 Dostal, Jaroslav. Rare Metal Deposits Associated with Alkaline/Peralkaline Igneous Rocks. ResearchGate. April 2016. doi:10.5382/Rev.18.02.
- ^ Campbell, Linda S; Henderson, Paul. Rare Earth Chemistry of Perovskite Group Minerals from the Gardiner Complex, East Greenland. Mineralogical Magazine. April 1997, 61 (405): 1970212. doi:10.1180/minmag.1997.061.405.04.
- ^ Yaxley, Gregory M.; Sujoy Ghosh, Sujoy. Deep Carbon. 6 - CO2-Rich Melts in Earth: Cambridge University Press. : 129 - 162.
They are also of particular economic importance as hosts or sources of many critical metals, including the rare earth elements (REEs) Nb, Ta, P, and others.
- ^ Professor of Chemistry at University College London, Andrea Sella, YouTube上的Andrea Sella: "Insight: Rare-earth metals", Interview on TRT World / Oct 2016, minutes 4:40 - ff.
- ^ T Gray. Lanthanum and Cerium. The Elements. Black Dog & Leventhal. 2007: 118–122.
- ^ Haxel G.; Hedrick J.; Orris J. Rare Earth Elements—Critical Resources for High Technology (PDF). Edited by Peter H. Stauffer and James W. Hendley II; Graphic design by Gordon B. Haxel, Sara Boore, and Susan Mayfield. United States Geological Survey. 2002 [2012-03-13]. USGS Fact Sheet: 087‐02.
However, in contrast to ordinary base and precious metals, REE have very little tendency to become concentrated in exploitable ore deposits. Consequently, most of the world's supply of REE comes from only a handful of sources.
- ^ Suzanne Goldenberg. Rare earth metals mine is key to US control over hi-tech future: Approval secured to restart operations, which could be crucial in challenging China's stranglehold on the market. The Guardian (London). 26 December 2010.
- ^ Tse, Pui-Kwan. USGS Report Series 2011–1042: China's Rare-Earth Industry. pubs.usgs.gov. [2018-04-04].
- ^ Distribution of rare earths production worldwide as of 2021, by country. statista. 2022-03-04 [2022-06-12].
- ^ Rare Earths: The Hidden Cost to Their Magic" (Part 2), Distillations Podcast and transcript, Episode 242. Science History Institute. June 25, 2019 [2019-8-28].
- ^ Lawrence J. Drewa, Meng Qingrunb and Sun Weijun. The Bayan Obo iron-rare-earth-niobium deposits, Inner Mongolia, China. Lithos. 1990, 26 (1–2): 43–65. doi:10.1016/0024-4937(90)90040-8.
- ^ Xue-Ming Yang, Michael J. Le Bas. Chemical compositions of carbonate minerals from Bayan Obo, Inner Mongolia, China: implications for petrogenesis. Lithos. 2004, 72 (1–2): 97–116. doi:10.1016/j.lithos.2003.09.002.
- ^ Chengyu Wu. Bayan Obo Controversy: Carbonatites versus Iron Oxide-Cu-Au-(REE-U). Resource Geology. 2007, 58 (4): 348–354. doi:10.1111/j.1751-3928.2008.00069.x. (原始内容存档于2012-12-17).
- ^ Rare element substitution a tricky proposition. CHEMISTRYWORLD. 2014-1-6 [2022-1-7].
- ^ Rizk, Shirley. What colour is the cloud?. European Investment Bank. 2019-06-21 [2020-09-17] (英语).
- ^ Standaert, Michael. China Wrestles with the Toxic Aftermath of Rare Earth Mining. Yale Environment 360. Yale School of the Environment. 2019-07-02 [2021-06-16].
- ^ Volokh, A. A.; Gorbunov, A. V.; Gundorina, S. F.; Revich, B. A.; Frontasyeva, M. V.; Chen Sen Pal. Phosphorus fertilizer production as a source of rare-earth elements pollution of the environment. Science of the Total Environment. 1990-06-01, 95: 141–148. Bibcode:1990ScTEn..95..141V. ISSN 0048-9697. PMID 2169646. doi:10.1016/0048-9697(90)90059-4 (英语).
- ^ Bourzac, Katherine. "Can the US Rare-Earth Industry Rebound?" Technology Review. 2010-10-29.
外部連結
外部媒体链接 | |
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音频 | |
"Rare Earths: The Hidden Cost to Their Magic", Distillations Podcast and transcript, Episode 242, June 25, 2019, Science History Institute | |
视频 | |
“10 ways rare earth elements make life better”, animation, Science History Institute | |
Rare Earth Elements: The Intersection of Science and Society, presentation and discussion led by Ira Flatow, Science History Institute, 2019-9-24 |
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