深海多金属结核和沉积物连续浸出相中的 REE 分布

A. Hikov, Z. Milakovska, Valentina Lyubomirova, Nadezhda Lihareva
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引用次数: 0

摘要

研究了来自东北太平洋克拉里昂-克利珀顿断裂带东部的深海多金属结核和沉积物的连续浸出相中主要元素和稀土元素的分布情况。结果表明,在结核和沉积物的浸出 2 中都提取了锰。结核和沉积物的浸出 2、浸出 3 和残余部分对铁、磷和稀土元素的提取不同。磷和稀土元素具有很强的正相关性,这表明磷酸盐成分是结核和沉积物中稀土元素的主要重要载体,但也不能排除铁-锰氧氢氧化物和粘土矿物是稀土元素的载体。
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REE distribution in sequential leached phases from deep-sea polymetallic nodules and sediments
The distribution of main elements and REE in sequential leached phases from deep-sea polymetallic nodules and sediments from the eastern part of the Clarion-Clipperton fractures zone, NE Pacific are studied. Results show extraction of Mn in the leach 2 in both nodules and sediments. The extraction of Fe, P and REE is different for leach 2, 3 and residual fraction for nodules and sediments. Phosphorous and REE have strong positive correlation which suggests that the phosphate component is the main important carrier of REE in both nodules and sediments but Fe-Mn oxyhydroxides and clay minerals cannot be excluded as carriers of REE.
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