期刊文献+
共找到2篇文章
< 1 >
每页显示 20 50 100
温度影响溴和铷分配的热力学分析及在钾盐矿床中的应用 被引量:1
1
作者 程怀德 马海州 +4 位作者 山发寿 高东林 李善平 王明相 唐启亮 《矿床地质》 CAS CSCD 北大核心 2010年第4期704-712,共9页
在海相蒸发岩矿床的地质-地球化学研究中,常应用盐类矿物中的微量元素来研究钾盐矿床的成因和成矿指示标志,Br、Rb就是其中很重要的2种微量元素。缺硫酸镁型钾盐矿床在成盐过程中会蒸发沉积形成氯化物型的盐类物质,Br、Rb按一定的规律... 在海相蒸发岩矿床的地质-地球化学研究中,常应用盐类矿物中的微量元素来研究钾盐矿床的成因和成矿指示标志,Br、Rb就是其中很重要的2种微量元素。缺硫酸镁型钾盐矿床在成盐过程中会蒸发沉积形成氯化物型的盐类物质,Br、Rb按一定的规律分配到这些盐类物质中而不形成独立矿物。在盐类物质蒸发结晶过程中,Br、Rb在固-液相之间的分配主要受温度控制。文章通过Br和Rb的地球化学特征及微量元素分配的热力学分析,建立了Br、Rb在盐类矿物相中的分配系数与温度间的热力学函数模型:InDBr=(μФBr(L)-μФBr(ss))/RT+InKBr(L)/KBr(ss),以及DRb=KKMGCL3·6H2O/KRbMgCl3·6H2O(rRb+/rK+)exp(-RΔTμ),并探讨了利用这些公式来计算出钾盐矿床结晶作用形成盐类物质时的古温度,这对研究钾盐矿床形成时的古环境、物质基础条件、物理化学条件等具有重要意义。 展开更多
关键词 地球化学 Br、Rb分配系数 热力学函数模型 古温度 钾盐矿床
下载PDF
Thermal dehydration kinetic mechanism of Mn_(1.8)Co_(0.1)Mg_(0.1)P_2O_7·2H_2O using Málek's equations and thermodynamic functions determination
2
作者 Chuchai SRONSRI 《Transactions of Nonferrous Metals Society of China》 SCIE EI CAS CSCD 2018年第5期1016-1026,共11页
Mn1.8Co0.1Mg0.1P2O7·2H2O was synthesized via hydrothermal method and the thermal dehydration product was confirmed to be Mn1.8Co0.1Mg0.1P2O7.The thermogravimetry/differential thermogravimetry/differential thermal... Mn1.8Co0.1Mg0.1P2O7·2H2O was synthesized via hydrothermal method and the thermal dehydration product was confirmed to be Mn1.8Co0.1Mg0.1P2O7.The thermogravimetry/differential thermogravimetry/differential thermal analysis,Fourier transform infrared,atomic absorption spectrophotometry,X-ray diffraction and scanning electron microscopy techniques were employed for sample characterization.Non-isothermal kinetics was studied under air atmosphere at four heating rates and the single thermal dehydration process was observed.Iterative Kissinger-Akahira-Sunose equation was used to calculate the apparent activation energy Eαvalues.Dehydration process was confirmed to be a single-step kinetic process with the unique kinetic triplets.Málek’s equations were used to determine the kinetic model f(α)and pre-exponential factor A.?esták-Berggren model was suggested to be the mechanism function for the dehydration process.The best fit led to the kinetic triplets of Eα=(79.97±6.51)k J/mol,ln A=16.83 and f(α)=α^0.520(1-α)^1.255(αis the extent of conversion).The thermodynamic functions of activation were calculated using activated complex theory together with A value. 展开更多
关键词 non-isothermal kinetics DEHYDRATION kinetic mechanism Sestak-Berggren model thermodynamic function
下载PDF
上一页 1 下一页 到第
使用帮助 返回顶部