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Inorganic Speciation of Rare Earth Elements in Chaohu and Longganhu Lakes, East China

机译:中国东部巢湖和龙潭湖的稀土元素的无机形态

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Inorganic speciation of dissolved rare earth elements (REEs) were calculated for Chaohu Lake and Longganhu Lake by using the program MINTEQ 2.30. The result shows that REE-Carbonate complexes, which account for more than 93 percent of total REE are the dominate and typically species in solution. Moreover, carbonator complexes (LnCO~(3+) ) were predicted to be the dominant species when pH between 7,2 and 8.0 and bicarbonate complexes (Ln (CO_3)~(2-) ) were predicted to be the dominant species when pH > 8.0. The free ion specie (i.e. , Ln~(3+) ) increases in these waters with pH decreasing and accounts for about 5.03 percent . The percentage of REE-phosphate complexes account for 1.61 percent of the dissolved REEs. REE-phosphate for light REEs complexes are supersaturated in Chaohu Lake and Longganhu Lake. Furthermore, LnP04 for heavy REEs are supersaturated in west of Chaohu Lake in high water period. PO_4~(3-) is responsible for limiting the dissolved REEs concentrations. REE-sulfate, REE-chloride, REE-fluoride and REE-hydroxide complexes, are negligible and generally account for less than percent of the total dissolved REEs.
机译:使用MINTEQ 2.30程序计算了巢湖和龙潭湖的溶解稀土元素的无机形态。结果表明,占REE总量93%以上的REE-碳酸盐复合物是主要的,通常是溶液中的物质。此外,当pH在7,2和8.0之间时,碳酸酯络合物(LnCO〜(3+))被认为是主要物质,而当pH值时,碳酸氢盐络合物(Ln(CO_3)〜(2-))被认为是主要物质。 > 8.0。这些水中的自由离子物种(即Ln〜(3+))随着pH的降低而增加,约占5.03%。 REE-磷酸盐复合物的百分比占溶解的REE的1.61%。巢湖和龙潭湖的轻稀土元素复合物中的稀土磷酸盐过饱和。此外,在高水期,巢湖以西的重稀土元素LnP04饱和。 PO_4〜(3-)负责限制溶解的稀土元素浓度。稀土硫酸盐,稀土氯化物,稀土氟化物和稀土氢氧化物络合物可以忽略不计,通常只占溶解的稀土总量的不到百分之一。

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