Identifying the roles of major phosphorus fractions in REY enrichment of Pacific deep-sea sediments using sequential extraction and mineralogical analysis
文献类型:期刊论文
作者 | Fan, Wenxiao1,6; Zhou, Junming5; Yuan, Peng1,4; Zhang, Huan1,6; Wang, Fenlian2; Liu, Dong1![]() |
刊名 | ORE GEOLOGY REVIEWS
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出版日期 | 2023-06-01 |
卷号 | 157页码:9 |
关键词 | Deep-sea sediments P fraction REY Apatite Micro-scale analysis |
ISSN号 | 0169-1368 |
DOI | 10.1016/j.oregeorev.2023.105430 |
英文摘要 | Bioapatite (i.e., fish teeth and debris) is considered the predominating carrier of rare earth elements (REY, including lanthanide (Ln) and yttrium (Y)) due to the positive correlation between phosphorus (P) and REY in REY-rich deep-sea sediments. Besides bioapatite, the presence of various P species such as vivianite and authi- genic carbonate-fluorapatite suggests other P species may have also contributed to the enrichment of REY in the REY-rich deep-sea sediments, yet their roles in REY enrichment are still unclear. This study investigated the REY characteristics of five P species (fractions), including exchangeable and loosely adsorbed P (Ex-P), Fe oxides bound P (Fe-P), authigenic apatite, and biogenic apatite (Ca-P), detrital apatite (Detrital-P), and organic-P (Org- P), in deep-sea sediments from the Pacific Ocean by using the sedimentary extraction (SEDEX) method and micro-scale analysis. The results show that Ca-P contributes 49.42% of the total P, while Fe-P and Detrital-P comprise 45.04% of the total P. The heavy rare earth enrichment is more visible in Fe-P and Ca-P compared to insignificant trends in the other fractions. Meanwhile, multiple forms of apatite demonstrate varied sources of REY in the Ca-P fraction. For instance, the formation of new apatite on the surface of a phillipsite explains the exceptionally high REY content in the Ca-P fraction. These results suggest that all investigated P fractions in deep-sea sediments positively contribute to REY enrichment and that in addition to fish teeth, other types of biogenic and authigenic apatites may also be important REY carriers. |
WOS研究方向 | Geology ; Mineralogy ; Mining & Mineral Processing |
语种 | 英语 |
WOS记录号 | WOS:000985254400001 |
源URL | [http://ir.gig.ac.cn/handle/344008/74182] ![]() |
专题 | 中国科学院矿物学与成矿学重点实验室 |
通讯作者 | Yuan, Peng |
作者单位 | 1.Chinese Acad Sci, Guangzhou Inst Geochem, CAS Ctr Excellence Deep Earth Sci, CAS Key Lab Mineral & Metallogeny,Guangdong Prov K, Guangzhou 510640, Peoples R China 2.Minist Nat Resources, Key Lab Marine Mineral Resources, Guangzhou Marine Geol Survey, Guangzhou 510075, Peoples R China 3.Minist Nat Resources, Inst Oceanog 2, Hangzhou 310012, Peoples R China 4.Guangdong Univ Technol, Sch Environm Sci & Engn, Guangzhou 510006, Peoples R China 5.Southern Marine Sci & Engn Guangdong Lab Guangzhou, Guangzhou 511458, Peoples R China 6.Univ Chinese Acad Sci, Beijing 100049, Peoples R China |
推荐引用方式 GB/T 7714 | Fan, Wenxiao,Zhou, Junming,Yuan, Peng,et al. Identifying the roles of major phosphorus fractions in REY enrichment of Pacific deep-sea sediments using sequential extraction and mineralogical analysis[J]. ORE GEOLOGY REVIEWS,2023,157:9. |
APA | Fan, Wenxiao.,Zhou, Junming.,Yuan, Peng.,Zhang, Huan.,Wang, Fenlian.,...&Dong, Yanhui.(2023).Identifying the roles of major phosphorus fractions in REY enrichment of Pacific deep-sea sediments using sequential extraction and mineralogical analysis.ORE GEOLOGY REVIEWS,157,9. |
MLA | Fan, Wenxiao,et al."Identifying the roles of major phosphorus fractions in REY enrichment of Pacific deep-sea sediments using sequential extraction and mineralogical analysis".ORE GEOLOGY REVIEWS 157(2023):9. |
入库方式: OAI收割
来源:广州地球化学研究所
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