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A statistics in world range indicates that the Sr/Eu ratios in the peraluminous granites show similar variation trend to those in pegmatitic apatites. This paper suggests that the high Sr/Eu ratio (>300) in apatites or peraluminous granites is due to the strong partition of Eu〓 into the aqueous fluid, and this ratio can be used as an excellent geochemical indicator of fluid exsolution from magmatic melts.

对世界范围内的过铝质花岗岩统计表明,过铝质岩浆岩的全岩样品中的Sr/Eu也呈现二歧变化,由此本文提出Sr/Eu比值是指示过铝质岩浆体系中岩浆流体相出溶的有效地球化学参数,大于300的Sr/Eu比值是Eu〓强烈分配进入流体相的地球化学标志。

The experimental products include crystal phase quartz, feldspar (alkila-feldspar, albite, K-feldspar), zinnwaldite and topaz, a melt phase and a trace vapour. The solid products were been studied by optics method, electron microprobe and X-ray analysis. The results show that liquidus temperature raises slightly and solidus temperature falls down obviously and that the upper temperature limit raises for the stability field of quartz and topaz, and falls down for the stability field of alkila-feldspar as F contents in crease.

实验淬火产物包括结晶相石英,长石(碱性长石,钠长石、钾长石),铁锂云母和黄玉及玻璃相和微量流体,对固相淬火产物进行了系统和详细的显微观察及电子探针和x射线分析,研究了F对钠长花岗岩液、固相线温度、相关系和相组合的影响和含F钠长花岗岩的结晶序列和熔体演化、F在流体和熔体之间的分配及F对花岗质熔体结构的影响,对含黄玉矿物组合进行了一系列热力学矿物平衡计算,获得如下重要结论

The zonality of abnormal pressure is closely correspondent to the breakthrough pressure (or pressure preservative ability) of mudstones in the Dongying Sag. The breakthrough pressures and formation fluid pressure coefficients rise with increasing depth. The preservation of isolated mudstone intervals is also important to the abnormal pressure formation.

东营凹陷异常压力的分带性与泥岩的突破压力具有明显的对应关系,随着深度增加,泥岩突破压力及地层流体压力系数均增大,泥岩封隔层对流体压力的保存也是形成异常压力的重要条件。

Accompany with the subduction of Pacific and Indian plates, upper mantle convected more violently, and new upwelling astheosphere replaced and eroded the lithosphere, and resulted in irregular thinning of cloud-like mantle along reticulated or dondroid weak zones. The thinning was dominated by replacement of lithosphere with new upwelling astheosphere, and accompanied possibly by delamination.

在这过程中,特别是伴随太平洋、印度洋板块的俯冲作用,地幔对流加剧,上涌的新生软流体顶蚀置换岩石圈,从而造成了沿早期业已存在的幔内薄弱带网络,出现类以&蘑菇云状&的地幔不规则减薄,这种减薄以新生软流体取代岩石圈为主,并可能伴随一定程度的岩石圈拆沉作用发生。

The earth is a complicated system, and it has been continuously moving differentiating and evolving since it had been formed. Not only has the earth layering structure, but it has vertical movement of materials. The movement is prompted by the mechanism of force and heat of the centrifugal force to be formed by the rotation and revolution of the earth, and difference of temperature, pressure, density, viscosity and velocity in the between core and mantle, and radioactive heat, et al. The expressive means of the mechanism of force and heat are the precesses of mantle plume and mantle fluid. Not only are ore-materials of core and mantle carried directly into crust, but ore-materials of crust are activated and accumulated into proper location by the mantle fluid having the supercritical nature.

地球是一个复杂的系统,自形成以来,一直处于不停地运动、分异和演化过程;它不仅存在着圈层结构,而且伴随其自转和公转的离心力,以及核幔间的温度差、压力差、密度差、粘度差、速度差和放射性蜕变热等动热机制,同时存在着以地幔柱和地幔流体作用方式的物质垂向运动;这一过程,不仅直接向地壳带入核幔成矿物质,而且通过流体自身的超临界性质,将沿途活化已有初步富集的成矿物质转移至地壳适宜部位集中成矿。

The iron isotopic composition lightly from hydrothermal fluid upwelled into ocean, BIFs are enriched in heavy isotopes of Fe by partial oxidation and precipitation, and iron isotopic composition was homogenous and reequilibrium during different minerals by metamorphism.

提出了地球早期海洋中Fe的循环模式:洋中脊喷发富集Fe轻同位素的二价铁热液流体,流体进入海洋后经过部分氧化和沉淀的过程使得BIF富集Fe的重同位素,后期的变质作用使得不同矿物间发生了Fe的均一化及再平衡

The plasma arc generator comprises cathode, two anodes and insulating strip between two anodes, first anode is cylindrical hollow sleeve, the cylinder cathode is placed in the centre of said sleeve, and an annular fluid channel is formed between both the lower portion of first anode is equipped with a hole as fluid outlet, and second anode is a circular plate with central hole, between two anodes there is an insulating strip, the diameter of central hole of second anode is less than the diameter of lower hole of first anode.

本发明是一种串式多级压缩等离子弧发生器,由阴极、两阳极及阳极之间的绝缘片组成,第一阳极为圆柱形空心套管,圆柱体阴极处于该套管中心,并在两者之间形成环状流体通道,第一阳极下部是一个供流体出口的横截面为圆的孔,第二阳极是中心开孔的圆形板,两阳极之间有绝缘片,第二阳极中心孔的直径小于第一阳极下部孔的直径。

This paper gives a review of the heat transfer of supercritical carbon dioxide in-tube flow and points out that the main factors to influence heat transfer are heat flux, buoyancy, pressure,lubricant and so on.

概述了超临界CO2流体管内对流换热的研究,指出了影响换热的主要因素有热流密度、浮升力、压力、润滑油等,提供了多种公开发表的超临界流体在冷却工况下的换热关联式,同时指出了现有研究内容的不足。

According to the CFD models of the paper, the fields of the cone valve, multi orifice valve and wedge valve as well as the coupling of the fluid and solid were studied, which included the pressure field, velocity field and streamline charts.

根据本文建立的CFD流体动力学计算模型,研究了锥形阀、多孔阀板型节流阀、楔形阀内的流场分布,包括压力场、速度场、流线图谱以及阀体的结构应力场等,同时对流体介质与阀杆相互作用进行了复杂的流固耦合的数值模拟分析。

Three dimension and turbulent are common characteristic of fluid flow problem in nature and added free surface for the best familiar fluid-water, such as flood discharge flow around frusta of brake in waterpower project, flow around hull in ship engineering, and so on, all have the three characteristics which are the very important study content and aspects in CFD.

摘要自然界中的流体流动问题一般都具有三维性和湍动性,对于最常见的流体—水则同时还拥有自由表面,水利工程中绕闸墩的泄洪水流、船舶工程中的船体绕流等均具有上述流动的三种特性,这三种特性是计算流体力学领域非常重要的研究内容和方向。

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