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The extraction of potassium from K-feldspar ore by low temperature molten salt method 被引量:3
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作者 Zhao Wang Quanyou Zhang +2 位作者 Ying Yao Yongzhong Jia Bingjun Xie 《Chinese Journal of Chemical Engineering》 SCIE EI CAS CSCD 2018年第4期845-851,共7页
The low temperature molten salt method was used to extract potassium from K-feldspar ore, and some related factors including mass ratio between NaNO_3, NaOH, H_2O and K-feldspar ore, particle size of K-feldspar ore,re... The low temperature molten salt method was used to extract potassium from K-feldspar ore, and some related factors including mass ratio between NaNO_3, NaOH, H_2O and K-feldspar ore, particle size of K-feldspar ore,reaction temperature and time were investigated, respectively. In addition, the optimum condition for this method was determined by a series of condition experiments. What was more, the K-feldspar ore and the leach residue after reaction based on the above optimum condition were analyzed by XRD, SEM and EDS,separately. The results of which indicated that the mechanism of extraction of potassium for this method was according to the ion exchange reaction between sodium ion and potassium ion, and the extraction ratio of potassium had an obvious improvement than that of traditional methods, which could reach up to 96.25%.Therefore, this method can be a feasible solution to extract potassium from K-feldspar ore for its low energy consumption and high efficiency. 展开更多
关键词 Low temperature molten salt k-feldspar Mechanism Extraction ratio
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中国沙漠的碎屑长石矿物与冰期风尘示踪
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作者 李娟 何同 《高校地质学报》 CAS CSCD 北大核心 2021年第3期366-374,共9页
文章采用了新型自动矿物相识别技术(INCA Mineral)对中国北方10个沙漠盆地以及蒙古戈壁沉积物的碎屑长石开展了矿物定量研究。钾长石/钠长石和钙质斜长石/石英的比值指示了沙漠沉积物的长石矿物含量特征,表现出显著的地球化学区域分布... 文章采用了新型自动矿物相识别技术(INCA Mineral)对中国北方10个沙漠盆地以及蒙古戈壁沉积物的碎屑长石开展了矿物定量研究。钾长石/钠长石和钙质斜长石/石英的比值指示了沙漠沉积物的长石矿物含量特征,表现出显著的地球化学区域分布特证。沿着青藏高原北部边缘分布的塔克拉玛干、柴达木、腾格里、巴丹吉林与毛乌素沙漠的沉积物中两种长石矿物比值均较低;中亚造山带以北的古尔班通古特、蒙古戈壁、浑善达克、呼伦贝尔和科尔沁沙漠的沉积物中两种长石矿物指标均具有较高值。长石矿物含量特征揭示的“两单元”区域分布结果,可以由过去采用Nd-Sr-Hf同位素示踪结果来验证。东亚沙漠长石含量的二元空间分布特征,支持了构造成山控制盆地沉积物矿物成分的假说。黄土高原末次冰期黄土的长石含量特征,与青藏高原北缘的长石分布特征一致,该区域可能是末次冰期黄土高原物质的主要来源,但也并不排除中亚造山带物质通过远距离搬运传输对末次冰期风尘的贡献。 展开更多
关键词 中国沙漠 碎屑长石矿物 钾长石/钠长石比值 末次冰期黄土 青藏高原北缘
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