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In sinter s,MgO mainly distributes in ferric phase and reacts with hematite and wustite generating magnesioferrite and MgO-bearing wustite.

烧结矿中MgO主要分布于铁相中与赤铁矿和富士体固溶形成镁质赤铁矿和镁质富士体,Mg2+在硅酸盐粘结相中的固溶量很低。

The present invention relates generally to UV photosensitive bulk glass, and particularly to batch meltable alkali boro-alumino-silicate and germanosilicate glasses.

本发明一般涉及UV光敏玻璃块,具体地说,涉及可熔融碱金属硼-铝-硅酸盐玻璃和硅酸锗玻璃料。

An investigation to the microstructure of worn sample of dry vibratable materials for tundish working lining after using 40 hours shows that the materials changes the properties of slag by the chemical filter, increases the viscosity of slag, forms a dense layer at slag/refactories interface, then blocks the more slag penetrate in it. The complex phase formed at the interface, such as magnesiowusite and complex spinel et al, would absorb in more low-melting point minerals, then degrade its melting point and dissolve into slag, which forms low-melting point silicate phase, penetrates into dry vibratable materials along with Monticellite and Merwinite bonding phase by diffusion.

根据使用40小时后的中间包工作层残衬结构分析,其侵蚀机理为:干式料对渗入熔渣产生化学过滤作用,增大熔渣粘度,在干式料/熔渣界面形成致密结构,阻碍熔渣的进一步渗透;随着反应的进行复合矿物中熔剂含量的增多,熔点降低,溶于熔渣形成低熔点的硅酸盐相,并沿着干式料中的钙镁橄榄石和镁蔷薇辉石等结合相向干式料基质中扩散渗透。

Major element abundances of the silicate phase of the two mesosiderites are similar to those of howardites. The cosmic ray exposure ages are (242± 50) Ma for Dong Ujimqin Qi mesosiderite and (25.4± 5.0) Ma for Weiyuan mesosiderite.

东乌珠穆沁旗及渭源中铁陨石的硅酸盐相在主元素丰度上类似于紫苏钙长无球粒陨石,其宇宙射线暴露年龄分别为(252±50)Ma和(25.9±5.0)Ma。

Phosphate, Metasilicate, Nonionic Surfactant, Anionic Surfactant, Dye

磷酸盐,硅酸盐,非离子表面活性剂,阴离子表面活性剂,颜料

The possible metasomatic agent was silicate melt in terms of Pb abnormality, which is characterized by enrichment in Pb and depletion in Y and LREE.

依据Pb的异常,可以推断交代物质可能为硅酸盐熔体,且熔体具有较高的Pb和较低的Y含量以及轻稀土富集的特征。

The mantle metasomatism in western Liaoning is representive of the disseminated amphibole, which implies that the metasomatic medium could be a relatively Na-rich silicate melt.

辽西区地幔交代作用以弥漫型角闪石的形成为代表,表明交代介质为相对富含钠质的硅酸盐熔体。

Any of a group of micaceous hydrated silicate minerals related to the chlorites and used in heat-expanded form as insulation and as a planting medium.

蛭石与绿混石有关的一组含云母的水合硅酸盐矿物质的统称,并以热膨胀形式用作绝缘材料和种植媒介

Bacillus mucilaginous; silicate mineral; weathering; molecule mechanism; polysaccharide; protein

胶质芽孢杆菌;硅酸盐矿物;风化;分子机制;多糖;蛋白质

Based on above studies, some main conclusions were obtained as follows : 1 the diatoms forming mats in low latitude west pacific is"shade flora"diatom Ethmodiscus rex Hendey; 2 the sites found diatom mats are zone distributed, the direction is NW-SE and most distribute in the deep water area with flat seafloor, between 17°N~20°N and the water depth 4837-6150 m below Carbonate Compensation Depth (CCD 3) AMS 14C dates show that the sediments rich in diatom mats occurred during 16.0 ~ 28.6 ka B.P., which means the bloom mainly occurred in last glacial maximum, while there are not diatom mats deposits in other layers; 4 A total of 101 diatom taxa belonging to 40 genera had been identified from the 155 samples in the two cores WPD 03 and WPD 12, and the relative percentage of Thalassionema frauenfeldii are the highest, Thalassionema nitzschioides、Azpeitia nodulifera、Hemidiscus cuneiformis、Nitzschia marina take the second place.

14C年期间,即&勃发&发生于末次冰期最盛期;4在WPD 03和WPD 12两个岩芯共155个样品中共鉴定硅藻40属101种,且Thalassionema frauenfeldii的相对百分含量最高,Thalassionema nitzschioides、Azpeitia nodulifera、Nitzschia marina、Hemidiscus cuneiformis等次之,这五种硅藻占整个硅藻物种相对百分含量的85%左右,说明在该海域表层水体硅藻席沉积过程中,这五种硅藻最容易与成席硅藻在同时期的环境中生存,形成勃发;5MIS3期的晚期,该区域表层海水盐度降低,这有助于该区水体的成层化,从而使&树荫种&硅藻开始勃发,导致&秋季倾泻&;6末次冰期由于南极中层水北扩,南大洋中层水将富含硅酸盐的海水带入了研究区,即南大洋的&硅溢漏&作用,使该区域硅藻得以勃发,同时,铁输入的增多,可能也是造成硅藻勃发的主要原因之一。

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