搜索结果: 1-8 共查到“矿床学与矿相学 NaCl”相关记录8条 . 查询时间(0.125 秒)
NaCl-H2O体系中WO3溶解度超临界现象实验探讨
超临界现象 临界区域 溶解度 钨矿床
2009/5/18
以适量Na2WO4·2H2O, HCl, NaCl和H2O为原料, 从过饱和的角度对4.0% NaCl水溶液中WO3溶解度的超临界现象进行实验探讨. 压力恒定在34 MPa, 接近临界压力31.4 MPa, 温度变化于250~550℃之间, 在快速淬火高压釜中进行实验. 结果表明在临界区域内, WO3溶解度具有超临界现象, 溶解度对温度、密度的变化反应敏感. 本实验温、压条件与许多钨矿床成矿流体的...
红透山块状硫化物矿石主要成分为黄铁矿、磁黄铁矿、黄铜矿、闪锌矿和石英、角闪石、黑云母等脉石矿物。切成长40mm 直径17mm 的矿石圆柱用20wt%NaCl 溶液浸泡260小时后装入长江500型活塞-圆筒式三轴应力试验机,在362℃414MPa 围压下加1342MPa 轴压,13小时后于空气中自然冷却。实验后试样长度压缩为32.3mm,算得应变速率为4.1×10~(-6)/s。实验产物中出现大量垂...
High-pressure X-ray diffraction study on the structure of NaCl melt using synchrotron radiation
NaCl high-pressure X-ray synchrotron radiation
2012/3/30
MoltenNaClwasanalyzedbyhigh-pressureX-raydiffractionexperimentsusingsyn-
chrotronradiationupto5GPaand1600Calongthemeltingcurve.Theinterference
function Qi(Q)andthecorrelationfunction g(r)werederived...
Phase relations in the system MgO-NaCl-H2O: The dehydroxylation of brucite in the presence of NaCl-H2O fluids
Phase relations MgO-NaCl-H2O dehydroxylation NaCl-H2O fluids
2012/3/31
The dehydroxylation of brucite was determined in the presence of NaCl-H2O fluids containing 0, 2, 6, 11, 14, 18, 30, and 38 mol% NaCl (0.0, 5.5, 17.0, 28.8, 34.5, 41.7,58.2, and 66.6 wt% NaCl) to ;250...
Molecular dynamics of NaCl (B1 and B2) and MgO (B1) melting: Two-phase simulation
Molecular dynamics NaCl (B1 and B2) MgO (B1) Two-phase simulation
2012/4/5
Melting of NaCl and MgOhas been simulated witha two-phase molecular dynamics method at constant pressure using newly developed interaction potentials. Equations of state for NaCl and MgOsimulated by m...
Structural Characterisation of Kaolinite:NaCl Intercalate and its Derivatives
FTIR Intercalate Kaolinite NaCl NMR Structure Synthesis XRD
2011/12/31
Kaolinite:NaCl intercalates with basal layer dimensions of 0.95 and 1.25 nm have been prepared by direct reaction of saturated aqueous NaCl solution with well-crystallized source clay KGa-1. The inter...
Crystalline Swelling of Smectite Samples in Concentrated NaCl Solutions in Relation to Layer Charge
Electrolyte Layer charge Smectite Swelling Vapor pressure X-ray powder diffraction
2011/12/31
The basal spacing of a set of smectites, with layer charges between 0.74 and 1.14 electrons per unit cell, have been measured while the smectites were in equilibrium with NaCl solutions having concent...
Hydration States of Smectite in NaCl Brines at Elevated Pressures and Temperatures
Brine Diagenesis Hydration Pressure Smectite Temperature
2012/1/12
A high-pressure, high-temperature cell was used to monitor the basal X-ray powder diffraction spacing of Na-saturated Cheto montmorillonite in contact with NaCl solutions at temperatures as high as 20...