笔者在琼州海峡西口第四系松散沉积物中新发现碳酸盐胶结岩,通过生物碎屑AMS14C同位素定年、全岩X衍射定量分析、扫描电镜、阴极发光、全岩主微量元素地球化学测试等方法对其进行了年代学和成因研究。结果显示,碳酸盐胶结岩的成岩时代...笔者在琼州海峡西口第四系松散沉积物中新发现碳酸盐胶结岩,通过生物碎屑AMS14C同位素定年、全岩X衍射定量分析、扫描电镜、阴极发光、全岩主微量元素地球化学测试等方法对其进行了年代学和成因研究。结果显示,碳酸盐胶结岩的成岩时代为早—中全新世,具有等厚纤柱状环边胶结、重力悬挂胶结、马牙状胶结、(似)共轴增生胶结、非等轴胶结等5种胶结物特征;阴极发光环带具有广泛发育、环带密集,可见淡水和海水相互作用的咸淡水混合带,说明其成岩环境包括淡水渗流带、咸淡水混合带、海水渗流带、海水潜流带;结合其沉积主微量元素特征,其赋存层位的沉积环境为海岸沉积环境,滨岸沉积相障壁岛亚相,属于海滩岩。综合雷州半岛西南部灯楼角珊瑚礁的海平面记录,重建了全新世琼州海峡西口地区海平面演化历史:9.9~6.7 ka BP海侵期、6.7~6.2 ka BP海退期、6.2~4.2 ka BP海侵期和4.2 ka BP至今的稳定期等四个阶段。展开更多
A hydrodynamic model of liquid-solid circulating fluidized bed is proposed to predict the slip velocity between fluid and solid particles and bed voidage by applying the theory of two-phase flow.The slip velocity can ...A hydrodynamic model of liquid-solid circulating fluidized bed is proposed to predict the slip velocity between fluid and solid particles and bed voidage by applying the theory of two-phase flow.The slip velocity can be represented by the following equation.u s =u-v=(1-ε)(ρ p -ρ f )g+F p -(1-ε)F f /εβ/εExperiments were carried out by using water and ceramic spheres,1.43 and 3.06 mm in mean diameter in a circulating fluidized bed of 31 mm diameter and 1700 mm height.The voidage was from 0.96 to 1,and the ratio between superficial liquid velocity and particle terminal velocity varied from 1.22 to 10.1 in the experiments.The fluid-particle interphase drag coefficient in the model was correlated from experimental data as followsd p βρ f =0.1881(1-ε) 1.0089 UU t -0.8043 d p D t -0.3228 The predicted values by the model proposed agreed with the experimental data well.In the meantime,the variation of slip velocity with superficial liquid velocity,bed voidage and particle diameter was discussed.The results showed that the model in the paper can well predict the hydrodynamics of liquid-solid two-phase flow in circuiating fluidized bed.The model is suitable for liquid-solid circulating fluidized bed under high flow rate and low concentration and can be also used on each tube in liquid-solid circulating fluidized bed heat exchanger.展开更多
文摘笔者在琼州海峡西口第四系松散沉积物中新发现碳酸盐胶结岩,通过生物碎屑AMS14C同位素定年、全岩X衍射定量分析、扫描电镜、阴极发光、全岩主微量元素地球化学测试等方法对其进行了年代学和成因研究。结果显示,碳酸盐胶结岩的成岩时代为早—中全新世,具有等厚纤柱状环边胶结、重力悬挂胶结、马牙状胶结、(似)共轴增生胶结、非等轴胶结等5种胶结物特征;阴极发光环带具有广泛发育、环带密集,可见淡水和海水相互作用的咸淡水混合带,说明其成岩环境包括淡水渗流带、咸淡水混合带、海水渗流带、海水潜流带;结合其沉积主微量元素特征,其赋存层位的沉积环境为海岸沉积环境,滨岸沉积相障壁岛亚相,属于海滩岩。综合雷州半岛西南部灯楼角珊瑚礁的海平面记录,重建了全新世琼州海峡西口地区海平面演化历史:9.9~6.7 ka BP海侵期、6.7~6.2 ka BP海退期、6.2~4.2 ka BP海侵期和4.2 ka BP至今的稳定期等四个阶段。
文摘A hydrodynamic model of liquid-solid circulating fluidized bed is proposed to predict the slip velocity between fluid and solid particles and bed voidage by applying the theory of two-phase flow.The slip velocity can be represented by the following equation.u s =u-v=(1-ε)(ρ p -ρ f )g+F p -(1-ε)F f /εβ/εExperiments were carried out by using water and ceramic spheres,1.43 and 3.06 mm in mean diameter in a circulating fluidized bed of 31 mm diameter and 1700 mm height.The voidage was from 0.96 to 1,and the ratio between superficial liquid velocity and particle terminal velocity varied from 1.22 to 10.1 in the experiments.The fluid-particle interphase drag coefficient in the model was correlated from experimental data as followsd p βρ f =0.1881(1-ε) 1.0089 UU t -0.8043 d p D t -0.3228 The predicted values by the model proposed agreed with the experimental data well.In the meantime,the variation of slip velocity with superficial liquid velocity,bed voidage and particle diameter was discussed.The results showed that the model in the paper can well predict the hydrodynamics of liquid-solid two-phase flow in circuiating fluidized bed.The model is suitable for liquid-solid circulating fluidized bed under high flow rate and low concentration and can be also used on each tube in liquid-solid circulating fluidized bed heat exchanger.
