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Based on the analysis of the mutual action between CO2 fluids and sandstone, it is found that the higher content of dawsonite is the main cause for poorer reservoir properties, and the dawsonite is formed later than other authigenic minerals and no erosion occurres after the pores filling, which are the basic factors resulting in poor reservoir properties.

分析CO2流体与砂岩的相互作用发现,片铝石含量较高是储层物性变差的直接原因,而片铝石生长时间晚于其它自生矿物且在充填孔隙后没有发生溶蚀是储层物性变差的根本原因。

At the same time, the SEM study shows that gibbsite occurs on the sample surface. At 200 ℃, as dawsonite sandstone is being dissolved authigenic siderite forms. At 300℃, chlorite deposit on parts of the sample surface. The weak solution of dawsonite sandstone at 100℃ and the formation of siderite at 200℃ illuminate that CO2 being in carbonates in the strata can not be released when CO2 phase is adding to the system.

同时,各温度下样品表面均有一水软铝石放射状集合体沉淀。200℃时,随着片铝石的溶解有自生菱铁矿生成,300℃时样品局部有绿泥石沉淀。100℃下片铝石的微弱溶解及200℃下菱铁矿的形成表明,在地层条件下以碳酸盐矿物形式捕获的CO2,不会由于CO2的二次注入而重新释放。

Research shows that the dawsonite in Hailaer Basin exists in both the eroded volcano tuff and sedimentary volcano tuff,and is paragenous with corrensite and allevardite frequently.

研究表明,海拉尔盆地的碳铝石存在于火山凝灰岩或沉积凝灰岩中,常与柯绿泥石和板石共生,形成凝灰质蚀变的特征标型矿物组合。

The calculated δ13C values of CO2 gas being in equilibrium with dawsonite ranged from -8.7‰ to-6.9‰ and was in coincidence with the δ13C values ranging from -9.76‰to -5.74‰ of CO2 gas in Gudian carbonate dioxide gas field.

由于含片铝石砂岩与CO2气的分布都受控于深大断裂和玄武岩,CO2气和形成片铝石的CO2绝大部分属于幔源岩浆型。

However, dawsonite can be acted as trace mineral suggesting migration or accumulation of fluids with abundant carbon dioxide to whatever origin it belongs. In geological background, occurrence or enrichment of dawsonite indicates that migration or accumulation of carbon dioxide with large scale has happened.

然而,不论源于有机成因CO2气还是无机成因CO2气,片铝石均可作为富CO2流体运移或聚集的"示踪矿物",地质过程中片铝石的出现或富集表明该区曾存在大量CO2运移或聚集。

In this paper a full density matrix treatment is adopted to deal with the interaction between long-pulse,circularly-polarized light and the sodium atoms.

采用密度矩阵方法来处理长脉冲光与原子的相互作用,求解24能级精细结构的布洛赫方程,给出参与跃迁的每个态密度随时间的演化曲线。

Methods Enamel surface specimens were randomly allocated into 3 groups: 1 450 mg/L sodium fluoride dentifrice group, 1 450 mg/L sodium monofluorophosphate dentifrice group and non-fluoride dentifrice control group. Sound enamel surfaces were dematerialized in bacteria model in vitro. QLF was used to analyze the area of lesionsArea, the loss of fluorescenceΔF and ΔQArea×ΔF on enamel surfaces after demineralization.

将30个牙釉质块开窗后分为3组,分别使用氟含量1 450 mg/L的氟化牙膏、单氟磷酸牙膏和无氟牙膏的处理液处理,并在体外恒化器龋病模型中进行脱矿循环,定量光导荧光技术QLF分析病损脱矿后的面积、荧光损失和总荧光损失量,激光扫描共聚焦显微镜CLSM分析脱矿后矿物质含量变化。

Methods Enamel surface specimens were randomly allocated into 3 groups: 1 450 mg/L sodium fluoride dentifrice group, 1 450 mg/L sodium monofluorophosphate dentifrice group and non-fluoride dentifrice control group. Sound enamel surfaces were dematerialized in bacteria model in vitro. QLF was used to analyze the area of lesions, the loss of fluorescence and ΔQ on enamel surfaces after demineralization.

将30个牙釉质块开窗后分为3组,分别使用氟含量1 450 mg/L的氟化牙膏、单氟磷酸牙膏和无氟牙膏的处理液处理,并在体外恒化器龋病模型中进行脱矿循环,定量光导荧光技术分析病损脱矿后的面积、荧光损失和总荧光损失量,激光扫描共聚焦显微镜分析脱矿后矿物质含量变化。

Enamel surface ecime were randomly allocated into 3 grou : 1 450 mg/L sodium fluoride dentifrice group, 1 450 mg/L sodium monofluoropho hate dentifrice group and non-fluoride dentifrice control group. Sound enamel surfaces were dematerialized in bacteria model in vitro. QLF was used to analyze the area of lesio, the lo of fluorescence and ΔQ on enamel surfaces after demineralization.

将30个牙釉质块开窗后分为3组,分别使用氟含量1 450 mg/L的氟化牙膏、单氟磷酸牙膏和无氟牙膏的处理液处理,并在体外恒化器龋病模型中进行脱矿循环,定量光导荧光技术分析病损脱矿后的面积、荧光损失和总荧光损失量,激光扫描共聚焦显微镜分析脱矿后矿物质含量变化。

The factors that affected the content of dialdehyde in dialdehyde starch included reaction time, reaction temperature, concentrations of sodium periodate, reaction pH, and the ratio of sodium periodate to starch.

影响双醛淀粉的双醛含量的因素有反应时间、反应温度、高碘酸浓度、反应pH值及高碘酸与淀粉的摩尔比。

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