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Rare earth element characteristics of Pahang River and Kelantan River sediments and their tracing implication
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Kaikai Wu1, 2, Shengfa Liu2, 3, Aimin Jin1, Zhanghua Lou1, Bin Wu2, 3, Jingrui Li2, 3, Hui Zhang2, Xisheng Fang2, 3, Abd.Rahim Bin Mohamed Che4, Xuefa Shi2, 3, *
Haiyang Xuebao | 2019, 41(7) : 77 - 91
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Haiyang Xuebao | 2019, 41(7): 77-91
Marine Geology
Rare earth element characteristics of Pahang River and Kelantan River sediments and their tracing implication
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Kaikai Wu1, 2, Shengfa Liu2, 3, Aimin Jin1, Zhanghua Lou1, Bin Wu2, 3, Jingrui Li2, 3, Hui Zhang2, Xisheng Fang2, 3, Abd.Rahim Bin Mohamed Che4, Xuefa Shi2, 3, *
Affiliations
  • 1 Institute of Marine Geology and Resources, Ocean College, Zhejiang University, Zhoushan 316021, China
  • 2 First Institution of Oceanography, Ministry of Natural Resources, Qingdao 266061, China
  • 3 Laboratory for Marine Geology and Environment, Pilot National Laboratory for Marine Science and Technology (Qingdao), Qingdao 266061, China
  • 4 College of Environmental Science and Natural Resources, National University of Malaysia, Bandar Baru Bangi 43600, Malaysia
Published: 2019-07-25 doi: 10.3969/j.issn.0253-4193.2019.07.007
Outline
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Rare earth element (REE) in the surface sediments from Pahang River (28 samples) and Kelantan River (22 samples) in the eastern portion of Malay Peninsula are analyzed to decipher the characteristics of REE composition and distribution, to discern the controlling factors of REE composition, and to illustrate the significances of provenance tracing of REE. The results show that the total REE ranges from 24.88 μg/g to 304.29 μg/g, with an average of 165.22 μg/g, for the Pahang River; and 126.02 μg/g to 281.40 μg/g, with an average of 181.15 μg/g, for the Kelantan River, respectively. The UCC standardization of REE indicates that Pahang River sediments enrich with heavy rare earth elements, in relative to light rare earth elements. However, there is no significant difference between light and heavy rare earth elements in the Kelantan River. The composition of source rocks and minerals plays a controlling role in the REE composition of the two rivers. The influence of chemical weathering in the Pahang River is greater than Kelantan River, and the difference of grain size among the Pahang River sediments leads to larger REE variations. δEuUCC-(Gd/Yb)UCC discrimination diagram demonstrates that it can be used as an effective index to qualitatively seperate the sediment source of two rivers. It can further be used to trace and identify the source of sediments quantitatively on the continental shelf of Malay Peninsula.

sediment  /  rare earth element  /  controlling factors  /  provenance tracing  /  Pahang River  /  Kelantan River  /  Malay Peninsula
Kaikai Wu, Shengfa Liu, Aimin Jin, Zhanghua Lou, Bin Wu, Jingrui Li, Hui Zhang, Xisheng Fang, Abd.Rahim Bin Mohamed Che, Xuefa Shi. Rare earth element characteristics of Pahang River and Kelantan River sediments and their tracing implication[J]. Haiyang Xuebao, 2019 , 41 (7) : 77 -91 . DOI: 10.3969/j.issn.0253-4193.2019.07.007
Year 2019 volume 41 Issue 7
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Article Info
doi: 10.3969/j.issn.0253-4193.2019.07.007
  • Receive Date:2018-05-22
  • Online Date:2026-04-02
  • Published:2019-07-25
Article Data
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History
  • Received:2018-05-22
  • Revised:2018-07-19
Funding
Affiliations
    1 Institute of Marine Geology and Resources, Ocean College, Zhejiang University, Zhoushan 316021, China
    2 First Institution of Oceanography, Ministry of Natural Resources, Qingdao 266061, China
    3 Laboratory for Marine Geology and Environment, Pilot National Laboratory for Marine Science and Technology (Qingdao), Qingdao 266061, China
    4 College of Environmental Science and Natural Resources, National University of Malaysia, Bandar Baru Bangi 43600, Malaysia
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表12种不同金属材料的力学参数

Family
属数
Number of
genus
种数
Number of
species
占总种数比例
Percentage of
total species (%)

Genus
种数
Number of
species
占总种数比例
Percentage of total
species (%)
鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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