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The Enrichment Regularity of Rare Earth Elements and Resource Characteristics in Polymetallic Nodules/Crusts

机译:多金属结节/外壳中稀土元素的富集规律和资源特征

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Polymetallic nodules/crusts are one of the most important mineral deposits in the ocean, in which iron, manganese, copper, cobalt, nickel and other metals are rich, and rare earth elements are rich, too. In this study, the contents of 11 rare earth samples in polymetallic nodules/crusts from the Pacific, Atlantic, Indian Ocean and north of the South China Sea are analyzed. The average content of rare earth in polymetallic nodules/crusts is 1265.57x10~(-6), the average content of nodules is 1096.96x10~(-6), and the average content of crust is 1623.88x10~(-6). The enrichment of rare earth elements is controlled by iron and manganese oxides and clay minerals in nodules/crusts, which could absorb rare earth elements from seawater and sediment. Ce elements are highly enriched, making polymetallic nodules/crusts become the first used rare earth elements in mineral development.
机译:多金属结节/外壳是海洋中最重要的矿物沉积物之一,其中铁,锰,铜,钴,镍等金属丰富,稀土元素也丰富。在这项研究中,分析了11种稀土样品中的11个稀土样品的含量,来自太平洋,大西洋,印度洋和南海北部的多孔结节/地壳。多金属结节/地壳中稀土的平均含量为1265.57×10〜(-6),结节的平均含量为1096.96×10〜( - 6),外壳的平均含量为1623.88x10〜(-6)。稀土元素的富集由铁结核/外壳中的铁和锰氧化物和粘土矿物控制,这可以吸收来自海水和沉积物的稀土元素。 CE元素是高度富集的,使多种结节/地壳成为矿物发育中的第一个使用的稀土元素。

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