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As a result, the author discusses the thermodynamics habitus for the minerals either. With the calculation of the thermodynamics modeling, we run the dissolutionmodeling experiments for primary minerals (potash feldspar, albite, anorthite, andpyroxene, hornblende), which is under the conditions of organic acidic and 20 varietytemperature and pressure. The dissolution modeling experiments include 4 anorthitedissolution experiments, 8 pyroxene dissolution experiments, 8 hornblendedissolution experiments. We catch the records on the X ray diffraction, chemistryanalysis, SEMphotos, and the PH parameters. By theway, we discuss the dissolution habitus for the minerals either.

在热力学模拟计算的基础之上,进行20个不同温度和压力条件下,以有机酸作为溶解介质的储层砂岩骨架颗粒(钾长石、钠长石、钙长石以及铁镁暗色矿物中的辉石、角闪石等)的水—岩相互作用的溶解模拟实验,包括:4个钙长石的溶解实验、8个辉石的溶解实验和8个角闪石的溶解实验,获得了溶解模拟实验前后全部参与实验矿物的X射线衍射分析、化学全分析数据、扫描电镜照片,以及介质流体在实验过程中化学参数pH值的检测,在此基础上讨论了铁镁暗色矿物、长石等铝硅酸盐矿物在埋藏成岩过程中酸性介质条件下的溶解习性。

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。

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。

That is why field geologists usually take a pocketknife which can be used to test minerals for hardness .

这就是为什么野外地质工作者通常携带一把小刀,利用小刀刻划矿物可以确定矿物的硬度以达到鉴定矿物的目的。

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。

Applying the theory of deformation partitioning to this area, the author discuss the relationship between deformation and porphyroblast growth, and get the conclusion of the sequence of deformation and metamorphism. At the first time we measure the distribution of chemical composition within the porphyroblast by XRF and confirm the theory of deformation partitioning quantitative.

利用宝音图群泥质变质岩中的存在大量变斑晶矿物,应用变形分解理论,讨论了变斑晶生长和变形关系,确定了变质变形演化序列,提出了变斑晶的生长相,并首次利用同步辐射XRF技术测定了变斑晶矿物的化学成分分布,主要是微区的微量元素成分分布,定量地证实了变斑晶矿物生长相的存在,进而讨论了与变形关系,并进行了变斑晶矿物不同生长相的温压计算。

In order to study degradation of potassic mineral by fungi, we isolated a thermophilic fungi strain TH003 from compost. The strain can use extract potassium from rocks as a nutrient. The strain was identified as Aspergillus fumigatus based on its morphological characteristics and molecular result.

为研究真菌对含钾矿物的吸附降解作用,作者从高温堆肥中分离选育出了一株丝状真菌TH003菌株,通过在含有矿物颗粒的改进PDA培养基中培养,使其在培养液中与矿物颗粒发生作用,再取样进行电镜观察和X-射线衍射分析以及电子探针观察。

For further understanding the effect of the strain on K-bearing silicate mineral, an experiment with KO2 strain cultured in nitrogen-containing and nitrogen-free medium was conducted. By putting mineral powders into the medium and measuring the concentration of capsular polysaccharides, we concluded that the strain can accelerate the weathering rate of silicate minerals. The results showed that the polysaccharides secreted by the strain in the growth process could help the bacterial to adhere to the mineral surface effectively, and created the bacterium-mineral complex, which formed a mircro-enviorment avail the release of potassium. Another result was that there was higher level of Carbonic Anhydrase activity, which revealed that some exo-protein or enzyme produced by the bacterial had postive impact on the process of releasing potassium ion. We carried out the bacterial fermentation for larger scale production of the bacterial secretion, which was used to sperate, and identify the small molecules related to the mineral-bacterial interaction. After the analysis, it was found that the strain can produce many kinds of small molecules, such as 2-Hydroxybenzoic acid, 4-Hydroxyphenylacetic acid, methyl-4-hydroxybenzoate, etc.

分别将菌株接入含有不同矿粉的培养基中培养,检测其在有氮、无氮培养基中荚膜多糖含量的变化,并在以钾长石和黑云母为矿源的情况下,比较研究了菌株在有氮、无氮培养基中对矿物的风化能力,通过一系列的实验,证实胶质芽孢杆菌在生长过程中所分泌的粘稠胞外聚糖可帮助细菌有效黏附在矿物表面,形成细菌-矿物复合体,并改变及维持该复合体内部的微环境,有助于该菌的解钾作用,而且细菌分泌的胞外蛋白质在该菌对含钾硅酸盐矿物的解钾作用过程中发挥重要作用;将胶质芽孢杆菌接入以钾长石和黑云母为矿源的有氮、无氮培养基中培养,检测到该菌碳酸酐酶活性的变化,并进行批量发酵后小分子酸性分泌产物的提取、分离、纯化与鉴定等方面的研究,结果表明,该菌可产生2-羟基苯甲酸,4-羟基苯乙酸,4-羟基苯甲酸甲酯等小分子物质。

The minerals of igneous formations were described and a bulk volume model based on mineral and including porosity was established. The logging response equations of density, apparent neutron porosity, acoustic travel time,gamma ray and volume photoelectric cross index were deduced. The volume content of four minerals in matrix was calculated. The igneous rocks were classified according to the international igneous classification scheme proposed by IUGS (International Union of Geological Society).

分析了火成岩中的矿物成分,并基于此建立了以矿物为基础并包含孔隙度的体积模型;建立了密度、视中子孔隙度、声波时差、伽马射线和体积光电吸收截面指数的测井响应方程,计算了岩石骨架中4种矿物的体积含量,依据国际地质科学联合会提出的火成岩矿物分类方案对火成岩进行了分类。

The strength development of the system is also studied.The result shows that the strength of the minerals is obviously higher than calcium sulphoaluminate and the optimum composition is found.In addition,we have analysed the formation and hydration mechanism of the clinkers by means of XRD,IR,SEM,DTA and so on.

发现该系列部分矿物的强度明显高于硫铝酸钙,并找到了最佳矿物组成点﹔应用X射线衍射仪、红外光谱仪、扫描电子显微镜和差热分析等测试手段,对熟料矿物的形成和水化机理进行了初步分析研究。

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