Natural convection flow of unsteady Maxwell fluid with the effects of constant magnetic force in the course of a porous media is investigated in this research work. Fluid motion between a channel of parallel plates is...Natural convection flow of unsteady Maxwell fluid with the effects of constant magnetic force in the course of a porous media is investigated in this research work. Fluid motion between a channel of parallel plates is tempted by time dependent shear stress applied on one plate. The governing partial differential equations of a model under consideration are transformed into ordinary differential equations by Laplace transform method and then solved for temperature and velocity fields. The obtained results for temperature fields are expressed in terms of complementary error function. The influences of involved parameters likes Hartmann number, Grashf number, Prandlt number and porosity parameter, on temperature and velocity profiles are shown graphically. There is no such result regarding Maxwell fluid in the existing literature.展开更多
Systematic microthermometric measurements of fluid inclusions in the PGE-polymetallic deposits hosted in the Lower Cambrian black rock series in southern China were performed, and the results suggest: (1) there exist ...Systematic microthermometric measurements of fluid inclusions in the PGE-polymetallic deposits hosted in the Lower Cambrian black rock series in southern China were performed, and the results suggest: (1) there exist two types of fluid inclusions. TypeⅠis of NaCl-H-2O system with low-medium salinity, and its homogenization temperatures (T-h) and salinities are {106.9}-{286.4℃} and ({0.8}-{21.8}) wt%NaCl eq. respectively; TypeⅡ is of CaCl-2-NaCl-H-2O system with medium-high salinities, and its homogenization temperatures and salinities range from {120.1℃} to {269.6℃} and ({11.4}-{31.4}) wt%NaCl eq., respectively. The typeⅡ fluid inclusions have been discovered for the first time in this kind of deposits; (2) two generations of ore-forming fluids were recognized. Characteristics of fluid inclusions in the PGE-polymetallic ores and carbonate-quartz stockworks in the underlying phosphorites are almost of no difference, they may represent ore-forming fluids at the main metallogenic stage. The peak value of homogenization temperature of those fluid inclusions is about 170℃, while their salinities possess a remarkable bimodal distribution pattern with two peak values of (27-31) wt%NaCl eq. and (4-6) wt%NaCl eq. On the contrary, fluid inclusions in the carbonate-quartz veins in the hanging wall may represent ore-forming fluids at the post-metallogenetic stage. The homogenization temperatures and the peak values of salinities are mostly 130-170℃ and (12-14) wt%NaCl eq., respectively; (3) nobel gas isotopic composition analyses in combination with the microthermometric measurements of fluid inclusions suggest that the ore-forming fluids at the main metallogenetic stage were probably derived from mixing of basinal hot brines with the CaCl-2-NaCl-H-2O system and seawater with the NaCl-H-2O system; (4) in the Early Cambrian, the basinal hot brines were trapped in the Caledonian basins, which were distributed along the southern margin of the Yangtze Craton, and where giant thick sediments were accumulated, and expelled and migrated laterally along the strata because of the pressure caused by overlying sediments. The basinal hot brines absorbed Ni, Mo, V, PGE from the surrounding rocks and were transformed into ore-bearing hydrothermal fluids with the CaCl-2-NaCl-H-2O system and medium-high salinities, then ascended along faults and mixed with seawater of the NaCl-H-2O system, and finally PGE-polymetallic deposits or occurrences were formed in the black rock series.展开更多
He-Ar isotopic compositions of fluid inclusions trapped in pyrites from some representative PGE-polymetallic deposits in Lower Cambrian black rock series in South China were analyzed by using an inert gas isotopic mas...He-Ar isotopic compositions of fluid inclusions trapped in pyrites from some representative PGE-polymetallic deposits in Lower Cambrian black rock series in South China were analyzed by using an inert gas isotopic mass spectrometer. The results show that the ore-forming fluids possess a low 3He/4He ratio, varying from 0.43×10-8 to 26.39×10-8, with corresponding R/Ra value of 0.003-0.189. The 40Ar/36Ar ratios are 258-287, close to those of air saturated water (ASW). He-Ar isotopic indicator studies show that the ore-forming fluids were mainly derived from the formation water or basinal hot brine and sea water, while the content of mantle-derived fluid or deep-derived magmatic water might be negligible. The PGE-polymetallic mineralization might be related to the evolution of the Caledonian miogeosynclines distributed along the southern margin of the Yangtze Craton. During the Early Cambrian, the formation water or basinal hot brine trapped in Caledonian basins which accumulated giant thick sediments was expelled and migrated laterally along strata because of the pressure generated by overlying sediments. The basinal hot brine ascended along faults, mixed with sea water and finally deposited ore minerals.展开更多
严寒、寒冷地区液体型集热器应用时需考虑防冻性能,工程常使用乙二醇型防冻液作为循环工质。但其导热系数仅为水的60%,集热循环过程中防冻液与太阳能集热器基板传热不充分导致基板过热和集热热损过大。为解决上述问题,通过乙二醇型防冻...严寒、寒冷地区液体型集热器应用时需考虑防冻性能,工程常使用乙二醇型防冻液作为循环工质。但其导热系数仅为水的60%,集热循环过程中防冻液与太阳能集热器基板传热不充分导致基板过热和集热热损过大。为解决上述问题,通过乙二醇型防冻液及相变材料配制不同浓度的传热蓄热流体(heat transfer and heat storage fluid, HTHSF),在考虑防冻的基础上,以增加HTHSF综合导热系数为目的,通过瞬态热线法实验研究HTHSF相变过程中导热系数的变化规律。结果表明:当温度升高或浓度减小时载流体导热系数增大。配制的HTHSF呈水基溶液的特性,在单一相时导热系数与温度呈正比关系,相变使得导热系数有所减小。寒地太阳能供暖用新型HTHSF 10%、冰点-20℃时性能较好,此外拟合公式与实测数据误差在0.5%以内。展开更多
文摘Natural convection flow of unsteady Maxwell fluid with the effects of constant magnetic force in the course of a porous media is investigated in this research work. Fluid motion between a channel of parallel plates is tempted by time dependent shear stress applied on one plate. The governing partial differential equations of a model under consideration are transformed into ordinary differential equations by Laplace transform method and then solved for temperature and velocity fields. The obtained results for temperature fields are expressed in terms of complementary error function. The influences of involved parameters likes Hartmann number, Grashf number, Prandlt number and porosity parameter, on temperature and velocity profiles are shown graphically. There is no such result regarding Maxwell fluid in the existing literature.
文摘Systematic microthermometric measurements of fluid inclusions in the PGE-polymetallic deposits hosted in the Lower Cambrian black rock series in southern China were performed, and the results suggest: (1) there exist two types of fluid inclusions. TypeⅠis of NaCl-H-2O system with low-medium salinity, and its homogenization temperatures (T-h) and salinities are {106.9}-{286.4℃} and ({0.8}-{21.8}) wt%NaCl eq. respectively; TypeⅡ is of CaCl-2-NaCl-H-2O system with medium-high salinities, and its homogenization temperatures and salinities range from {120.1℃} to {269.6℃} and ({11.4}-{31.4}) wt%NaCl eq., respectively. The typeⅡ fluid inclusions have been discovered for the first time in this kind of deposits; (2) two generations of ore-forming fluids were recognized. Characteristics of fluid inclusions in the PGE-polymetallic ores and carbonate-quartz stockworks in the underlying phosphorites are almost of no difference, they may represent ore-forming fluids at the main metallogenic stage. The peak value of homogenization temperature of those fluid inclusions is about 170℃, while their salinities possess a remarkable bimodal distribution pattern with two peak values of (27-31) wt%NaCl eq. and (4-6) wt%NaCl eq. On the contrary, fluid inclusions in the carbonate-quartz veins in the hanging wall may represent ore-forming fluids at the post-metallogenetic stage. The homogenization temperatures and the peak values of salinities are mostly 130-170℃ and (12-14) wt%NaCl eq., respectively; (3) nobel gas isotopic composition analyses in combination with the microthermometric measurements of fluid inclusions suggest that the ore-forming fluids at the main metallogenetic stage were probably derived from mixing of basinal hot brines with the CaCl-2-NaCl-H-2O system and seawater with the NaCl-H-2O system; (4) in the Early Cambrian, the basinal hot brines were trapped in the Caledonian basins, which were distributed along the southern margin of the Yangtze Craton, and where giant thick sediments were accumulated, and expelled and migrated laterally along the strata because of the pressure caused by overlying sediments. The basinal hot brines absorbed Ni, Mo, V, PGE from the surrounding rocks and were transformed into ore-bearing hydrothermal fluids with the CaCl-2-NaCl-H-2O system and medium-high salinities, then ascended along faults and mixed with seawater of the NaCl-H-2O system, and finally PGE-polymetallic deposits or occurrences were formed in the black rock series.
基金the National Natural Sciences Foundation of China(grants40173025,49928201)Trans-century Training Program Foundation for the Talents by the Ministry of Education the Visiting Scholar Foundation of Labs in Universities.
文摘He-Ar isotopic compositions of fluid inclusions trapped in pyrites from some representative PGE-polymetallic deposits in Lower Cambrian black rock series in South China were analyzed by using an inert gas isotopic mass spectrometer. The results show that the ore-forming fluids possess a low 3He/4He ratio, varying from 0.43×10-8 to 26.39×10-8, with corresponding R/Ra value of 0.003-0.189. The 40Ar/36Ar ratios are 258-287, close to those of air saturated water (ASW). He-Ar isotopic indicator studies show that the ore-forming fluids were mainly derived from the formation water or basinal hot brine and sea water, while the content of mantle-derived fluid or deep-derived magmatic water might be negligible. The PGE-polymetallic mineralization might be related to the evolution of the Caledonian miogeosynclines distributed along the southern margin of the Yangtze Craton. During the Early Cambrian, the formation water or basinal hot brine trapped in Caledonian basins which accumulated giant thick sediments was expelled and migrated laterally along strata because of the pressure generated by overlying sediments. The basinal hot brine ascended along faults, mixed with sea water and finally deposited ore minerals.
文摘严寒、寒冷地区液体型集热器应用时需考虑防冻性能,工程常使用乙二醇型防冻液作为循环工质。但其导热系数仅为水的60%,集热循环过程中防冻液与太阳能集热器基板传热不充分导致基板过热和集热热损过大。为解决上述问题,通过乙二醇型防冻液及相变材料配制不同浓度的传热蓄热流体(heat transfer and heat storage fluid, HTHSF),在考虑防冻的基础上,以增加HTHSF综合导热系数为目的,通过瞬态热线法实验研究HTHSF相变过程中导热系数的变化规律。结果表明:当温度升高或浓度减小时载流体导热系数增大。配制的HTHSF呈水基溶液的特性,在单一相时导热系数与温度呈正比关系,相变使得导热系数有所减小。寒地太阳能供暖用新型HTHSF 10%、冰点-20℃时性能较好,此外拟合公式与实测数据误差在0.5%以内。
