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The intensity of humic acid sorption on kaolinite, gibbsite and quartz is related to the nature and number of adsorption site of the minerals, the electricity and the specific surface.

矿物结合的腐殖质可改变矿物的表面性质,矿物对腐殖酸的吸附强度与矿物的吸附位性质、密度、荷电性及比表面积有关。

With some examples, the correlat ions between the thermal expansion coefficients of minerals and the types of cr ystal structures, the nature of chemical bonds, the valencies of ions , the interionic distances, the percentage ionic characters, the electronic conf igurations of ions and the chemical compositions are discussed and summarised . The crystal chemistry approach has been used in the calculation of the th ermal expansion coefficients for minerals with simple structures and composition s.

晶体化学方法是研究矿物热膨胀系数的有效方法,但由于矿物的热膨胀系数和晶体化学参数之间的定量关系尚未完全弄清,目前仅仅能对简单结构矿物的热膨胀系数进行计算,结构、成分较复杂的矿物的热膨胀系数计算尚缺乏好的晶体化学模型。

Clay minerals in the laterite come directly from carbonate rocks and secondary evolution of silicates in carbonate rocks.

红土中粘土矿物来源应该有二,一是原岩所夹粘土矿物,二是原岩中硅酸盐矿物溶解形成的次生粘土矿物;铁氧化物应该来自原岩中黄铁矿的次生演化。

With a quantitative research on the chemical and clay compositions of marly stones, their weathering rocks and residuals, as well as SEM observations, the process of dissolution of CaCO 3 and concentration of clay minerals with complex...

通过泥灰质岩石及其不同风化岩和残坡积土的化学成分、粘土矿物成分定量研究和扫描电镜观察,揭示了 Ca CO3溶蚀和粘土矿物富集过程及粘土矿物的复杂成分,发现了风化过程中伊利石向伊利石/蒙脱石混层粘土矿物的转化,解释了岩土工程性质恶化的原因,从而提高了地质研究和地质灾害研究的水平。

With a quantitative research on the chemical and clay compositions of marly stones, their weathering rocks and residuals, as well as SEM observations, the process of dissolution of CaCO 3 and concentration of clay minerals with complex components has been disclosed, and the conversion of illite to mixed-layer illite/montmorillonite discovered, which explain the reason for deterioration of geotechnical properties of the rocks and soils, thereby enhancing the level of geological and geohazards researches.

通过泥灰质岩石及其不同风化岩和残坡积土的化学成分、粘土矿物成分定量研究和扫描电镜观察,揭示了CaCO3溶蚀和粘土矿物富集过程及粘土矿物的复杂成分,发现了风化过程中伊利石向伊利石/蒙脱石混层粘土矿物的转化,解释了岩土工程性质恶化的原因,从而提高了地质研究和地质灾害研究的水平。

In terms of environmental mineralogy, the application of nonmetallic and metallic minerals to contamination control and environmental protection is summarized in this paper.

简述了环境保护的紧迫性,从环境矿物学角度综述了矿物或经改性的矿物,在环境污染控制和环境修复中的作用及其应用现状,并简要分析了矿物材料在环保方面的应用前景。

It is of significance to study mineral materials, definition, classification research contents, relationship with mineralogy, development of mineral materials in the new century.

矿物材料研究具有重要意义,本文探讨了矿物材料的涵义、分类、研究内容、与矿物学的关系等问题,并思考了新世纪矿物材料的研究和开发。

The results show that REEs oxide have little effect on the decomposition of carbonate and they improve the sinterability of the raw meal;they also promote the formation of alite and growth of clinker minerals,and have beneficial effect on the uniformity of crystal size and well-distributed minerals. But some REEs result in the corrosion of alite when they are excessive,which may influence the hydration reactivity of alite.When clinker is well sintered, REEs oxide and its tailing improve the strength of cement clinker, and have little effect on setting time of cement.

研究结果表明,稀土氧化物对碳酸盐的分解影响不大,对生料的易烧性有改善作用;稀土氧化物能促进熟料中A矿的形成和矿物的发育,有利于熟料中矿物结晶尺寸和分布均匀,但部分稀土在掺量过量时可能造成矿物的熔蚀,影响矿物的水化活性;在煅烧良好的条件下,稀土氧化物和尾矿对熟料强度有增进作用,对水泥凝结时间影响较小。

Recently a mantle mineral group including about 70~80 subtipys of mineral have been discovered from podiform chromitite in Tibet,China.

最近在西藏罗布莎村豆荚状铬铁矿石中发现一个由70~80种矿物组成的地幔矿物群,其中包括新矿物罗布莎矿,还有金刚石、柯石英、碳硅石、方铁矿、以及Fe-Si相矿物

The chemistry behavior research of wollastonite indicated that the silicon-potassium fertilizer has a chemical active in organic acid.The factors affecting manurial effect of silicon-potassium fertilizer are not only soil pH and desilicification,but also content and type of organ in the soil.Wollastonite chemistry behavior indicates that silicic acid can be dissolved out from silicon-potassium fertilizer in chlorhydric acid solution if pH of solution is not smaller than 2. The drop of apparent density,increase of DBP sorptive rate and specific surface for leavings indicate that hydrated silicon oxide is polyporous,and those mineralogic feature presignify that silicon-potassium fertilizer has a role of conservation of both Moisture and Fertility and improving soil structure.After active ingredient releasing,silicon-potassium fertilizer leaves half the substance (non-active ingredient)in soil.

熟料单矿物在酸溶液中的化学行为研究表明,硅钾肥矿物在有机弱酸中的化学活性较好,影响硅钾肥肥效发挥的因素是土壤pH值和土壤的去硅化程度,还有土壤有机质的含量与种类;硅灰石在盐酸溶液中化学行为表明,在反应体系pH不小于2的情况下,硅钾肥矿物大量溶出硅酸根组分;溶解残余物表观密度降低、DBP吸着率和比表面积增加表明水合二氧化硅是以多孔形式存在,为硅钾肥具有保水保肥、改良土壤结构的提供了矿物学依据。

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