摩尔浓度
均质化(气候)
超临界流体
流体包裹体
热力学
石英
水溶液
材料科学
化学
分析化学(期刊)
矿物学
色谱法
物理
复合材料
生物多样性
生态学
生物
物理化学
作者
Yigang Zhang,John D. Frantz
标识
DOI:10.1016/0009-2541(87)90012-x
摘要
Synthetic fluid inclusions were experimentally produced by equilibrating small fractured prisms of quartz with aqueous solutions at temperatures from 300° to 700°C and pressures of 1000, 2000 and 3000 bar. Solution compositions included: 0.500, 2.000 and 4.500 molal NaCl; 0.500, 2.000 and 4.500 molal KCl; 0.50 and 2.00 molal CaCl2; and H2O. The homogenization temperatures of the synthetic fluid inclusions were analyzed by microthermometry. Plots of homogenization temperatures as a function of experimental temperature and pressure indicate that lines of constant homogenization temperature are linear and intersect the liquid-vapor curve at the homogenization temperature. For each of the four chemical systems, a relatively simple function was developed by which the homogenization temperature can be related to the temperature (°C) and pressure (bar) of inclusion formation and the composition (m) of the trapped fluid:P=A1+A2TA1=6.100·10−3 + (2.385·10−1−a1)Th−(2.855·10−3+a2)T22−(A3Th+a4T2h)m A2=a1+a2Th+9.888·10−6T2h+(A3+A4Th)m where m is the molality; Th is the homogenization temperature; and a1, a2, a3 and a4 are constants fit to the data sets of each of the four chemical systems. Ten-parameter polynomial regressions are given for the densities of the solutions on their liquid-vapor surfaces as functions of temperature and composition. These functions combined with the above equations permit calculation of the density as a function of temperature, pressure, solute and solute concentration in the supercritical region. A function is also given which permits calculation of isochores for fluids containing more than one solute. The results of these experiments compare favorably to previously published ones.
科研通智能强力驱动
Strongly Powered by AbleSci AI