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Characterization of the adsorption behavior of aqueous cadmium on nanozero-valent iron based on orthogonal experiment and surface complexation modeling 被引量:2
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作者 Dongmei Liu Huan Tang +2 位作者 Ying Zhao Fuyi Cui Jing Lu 《Chinese Journal of Chemical Engineering》 SCIE EI CAS CSCD 2016年第9期1270-1274,共5页
Polyvinylpyrrolidone K-30(PVP) was introduced into the preparation of nanozero-valent iron(n ZVI) and the traditional liquid-phase reduction was improved. The introduction of PVP simplified the traditional method.The ... Polyvinylpyrrolidone K-30(PVP) was introduced into the preparation of nanozero-valent iron(n ZVI) and the traditional liquid-phase reduction was improved. The introduction of PVP simplified the traditional method.The n ZVI prepared with this new approach showed excellent surface characters and high performance on the removal of cadmium. TEM results showed that the aggregates of n ZVI can reach to several micrometers in length but less than 100 nm in diameter. The iron particles that were enclosed by a layer of oxide film that is less than10 nm, demonstrated that the n ZVI possesses a core–shell structure. BET results indicate that the specific surface area of the n ZVI was 20.3159 m^2g^(-1). A three factor and three level orthogonal experiment was employed to find out the dominant factor that affects the removal rate of cadmium by n ZVI. Based on the range values, the prominence order of each factor was: initial p H of the solution N initial concentration of cadmium N dosage of n ZVI, the range was 96.453, 3.294 and 1.747, respectively. A simulation was performed under the same condition and a same conclusion was derived, this consistence confirmed the validity of the conclusion that p H is the most significant factor that affects the adsorption efficiency. 展开更多
关键词 Cadmium Nanozero-valent iron synthesis Polyvinylpyrrolidone Orthogonal experiment Diffuse layer model
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地球深处形成含硼金刚石的可行机制
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作者 刘思瑜 陆文成 +6 位作者 张晓冉 宋京岩 吕健 刘晓兵 王彦超 陈长风 马琰铭 《Science Bulletin》 SCIE EI CAS CSCD 2023年第13期1456-1461,M0004,共7页
近年来,以“希望之钻”为代表天然蓝色钻石(蓝钻)的形成机制引起科学界和大众的广泛兴趣.天然蓝钻是形成于地球最深处的珍贵矿物,含约0.011~10μg/g棚杂质.现行地球化学模型表明地球内部硼元素主要富集于大陆和大洋地壳,极难进入地球内... 近年来,以“希望之钻”为代表天然蓝色钻石(蓝钻)的形成机制引起科学界和大众的广泛兴趣.天然蓝钻是形成于地球最深处的珍贵矿物,含约0.011~10μg/g棚杂质.现行地球化学模型表明地球内部硼元素主要富集于大陆和大洋地壳,极难进入地球内部的下地幔深度.蓝钻的存在为地球下地幔环境中存在硼元素提供了有力证据,然而其地质起源与循环机制是当前领域内亟待解决的科学难题之一.在本研究中,我们提出金属硼化物随地球板块运动进入下地幔深处,在高温高压环境下与碳酸盐发生氧化还原反应,从而形成蓝钻的物理机制.通过第一性原理计算提出了多种可能形成蓝钻的化学反应途径,并在下地幔压力与温度条件下(22.5 GPa,2100 K),利用CaCO_(3)和FeB的直接氧化还原反应,成功制备“类天然”蓝钻.这一发现揭示了地球深处蓝钻形成之谜,并为进一步深入探索地球内部的物质循环和矿物形成机制提供了新思路. 展开更多
关键词 Boron-bearing diamonds indeep Earth First-principlescalculations High-pressureandhigh-temperature experimental synthesis Redoxreactions
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