High-temperature, low-H₂O silicic magmas of the Yellowstone Hotspot: an experimental study of Rhyolite from the Bruneau-Jarbidge eruptive center, Central Snake River Plain, USA

The phase relations have been investigated experimentally at 200 and 500 MPa as a function of water activity for one of the least evolved (Indian Batt Rhyolite) and of a more evolved rhyolite composition (Cougar Point Tuff XV) from the 12·8-8·1 Ma Bruneau-Jarbidge eruptive center of the Yellowstone hotspot. Particular priority was given to accurate determination of the water content of the quenched glasses using infrared spectroscopic techniques. Comparison of the composition of natural and experimentally synthesized phases confirms that high temperatures (>900°C) and extremely low melt water contents (<1·5 wt % H₂O) are required to reproduce the natural mineral assemblages. In melts containing 0·5-1·5 wt % H₂O, the liquidus phase is clinopyroxene (excluding Fe-Ti oxides, which are strongly dependent on fO₂), and the liquidus temperature of the more evolved Cougar Point Tuff sample (BJR; 940-1000°C) is at least 30°C lower than that of the Indian Batt Rhyolite lava sample (IBR2; 970-1030°C). For the composition BJR, the comparison of the compositions of the natural and experimental glasses indicates a pre-eruptive temperature of at least 900°C. The composition of clinopyroxene and pigeonite pairs can be reproduced only for water contents below 1·5 wt % H₂O at 900°C, or lower water contents if the temperature is higher. For the composition IBR2, a minimum temperature of 920°C is necessary to reproduce the main phases at 200 and 500 MPa. At 200 MPa, the pre-eruptive water content of the melt is constrained in the range 0·7-1·3 wt % at 950°C and 0·3-1·0 wt % at 1000°C. At 500 MPa, the pre-eruptive temperatures are slightly higher (by 30-50°C) for the same ranges of water concentration. The experimental results are used to explore possible proxies to constrain the depth of magma storage. The crystallization sequence of tectosilicates is strongly dependent on pressure between 200 and 500 MPa. In addition, the normative Qtz-Ab-Or contents of glasses quenched from melts coexisting with quartz, sanidine and plagioclase depend on pressure and melt water content, assuming that the normative Qtz and Ab/Or content of such melts is mainly dependent on pressure and water activity, respectively. The combination of results from the phase equilibria and from the composition of glasses indicates that the depth of magma storage for the IBR2 and BJR compositions may be in the range 300-400 MPa (13 km) and 200-300 MPa (10 km), respectively.

Environmentally benign Fe chelates in plant nutrition

The low solubility of iron (Fe) depresses plant growth in calcareous soils. In order to improve Fe availability, calcareous soils are treated with synthetic ligands, such as ethylenediaminetetraacetic acid (EDTA) and ethylenediimi-nobis(2-hydroxyphenyl)acetic acid (EDDHA). However, high expenses may hinder their use (EDDHA), and the recalcitrance of EDTA against biodegra-dation may increase the potential of cadmium (Cd) and lead (Pb) leaching. This study evaluated the ability of biodegradable ligands, i.e. different stereo-isomers of ethylenediaminedisuccinic acid (EDDS), to provide Fe for lettuce (Lactuca sativa L.) and ryegrass (Lolium perenne cv. Prego), their effects on uptake of other elements and solubility in soils and their subsequent effects on the activity of oxygen-scavenging enzymes in lettuce. Both EDTA and EDDHA were used as reference ligands. In unlimed and limed quartz sand both FeEDDS(S,S) and a mixture of stereo-isomers of FeEDDS (25% [S,S]-EDDS, 25% [R,R]-EDDS and 50% [S,R]/[R,S]-EDDS), FeEDDS(mix), were as efficient as FeEDTA and FeEDDHA in providing lettuce with Fe. However, in calcareous soils only FeEDDS(mix) was comparable to FeEDDHA when Fe was applied twice a week to mimic drip irrigation. The Fe deficiency increased the manganese (Mn) concentration in lettuce in both acidic and alkaline growth media, whereas Fe chelates depressed it. The same was observed with zinc (Zn) and copper (Cu) in acidic growth media. EDDHA probably affected the hormonal status of lettuce as well and thus depressed the uptake of Zn and Mn even more. The nutrient concentrations of ryegrass were only slightly affected by the Fe availability. After Fe chelate splitting in calcareous soils, EDDS and EDTA increased the solubility of Zn and Cu most, but only the Zn concentration was increased in lettuce. The availability of Fe increased the activity of oxygen-scavenging enzymes (ascorbate peroxidase, guaiacol peroxidase, catalase). The activity of Cu/ZnSOD (Cu/Zn superoxide dismutase) and MnSOD in lettuce leaves followed the concentrations of Zn and Mn. In acidic quartz sand low avail-ability of Fe increased the cobalt (Co) and nickel (Ni) concentrations in let-tuce, but Fe chelates decreased them. EDTA increased the solubility of Cd and Pb in calcareous soils, but not their uptake. The biodegradation of EDDS was not affected by the complexed element, and [S,S]-EDDS was biodegraded within 28 days in calcareous soils. EDDS(mix) was more recalcitrant, and after 56 days of incubation water-soluble elements (Fe, Mn, Zn, Cu, Co, Ni, Cd and Pb) corresponded to 10% of the added EDDS(mix) concentration.

Magmatic evolution of topaz-bearing granite stocks within the Wiborg rapakivi granite batholith

This study brings new insights into the magmatic evolution of natural F-enriched peraluminous granitic systems. The Artjärvi, Sääskjärvi and Kymi granite stocks within the 1.64 Ga Wiborg rapakivi granite batholith have been investigated by petrographic, geochemical, experimental and melt inclusion methods. These stocks represent late-stage leucocratic and weakly peraluminous intrusive phases typical of rapakivi granites worldwide. The Artjärvi and Sääskjärvi stocks are multiphase intrusions in which the most evolved phase is topaz granite. The Kymi stock contains topaz throughout and has a well-developed zoned structure, from the rim to the center: stockscheider pegmatite equigranular topaz granite porphyritic topaz granite. Geochemically the topaz granites are enriched in F, Li, Be, Ga, Rb, Sn and Nb and depleted in Mg, Fe, Ti, Ba, Sr, Zr and Eu. The anomalous geochemistry and mineralogy of the topaz granites are essentially magmatic in origin; postmagmatic reactions have only slightly modified the compositions. The Kymi equigranular topaz granite shows the most evolved character, and the topaz granites at Artjärvi and Sääskjärvi resemble the less evolved porphyritic topaz granite of the Kymi stock. Stockscheiders are found at the roof contacts of the Artjärvi and Kymi stocks. The stockscheider at Artjärvi is composed of biotite-rich schlieren and pegmatite layers parallel to the contact. The schlieren layering is considered to have formed by velocity-gradient sorting mechanism parallel to the flow, which led to the accumulation of mafic minerals along the upper contact of the topaz granite. Cooling and contraction of the topaz granite formed fractures parallel to the roof contact and residual pegmatite magmas were injected along the fractures and formed the pegmatite layers. The zoned structure of the Kymi stock is the result of intrusion of highly evolved residual melt from deeper parts of the magma chamber along the fractured contact between the porphyritic granite crystal mush and country rock. The equigranular topaz granite and marginal pegmatite (stockscheider) crystallized from this evolved melt. Phase relations of the Kymi equigranular topaz granite have been investigated utilizing crystallization experiments at 100 to 500 MPa as a function of water activity and F content. Fluorite and topaz can crystallize as liquidus phases in F-rich peraluminous systems, but the F content of the melt should exceed 2.5 - 3.0 wt % to facilitate crystallization of topaz. In peraluminous F-bearing melts containing more than 1 wt % F, topaz and muscovite are expected to be the first F-bearing phases to crystallize at high pressure, whereas fluorite and topaz should crystallize first at low pressure. Overall, the saturation of fluorite and topaz follows the reaction: CaAl2Si2O8 (plagioclase) + 2[AlF3]melt = CaF2 (fluorite) + 2Al2SiO4F2 (topaz). The obtained partition coefficient for F between biotite and glass D(F)Bt/glass is 1.89 to 0.80 (average 1.29) and can be used as an empirical fluormeter to determine the F content of coexisting melts. In order to study the magmatic evolution of the Kymi stock, crystallized melt inclusions in quartz and topaz grains in the porphyritic and the equigranular topaz granites and the marginal pegmatite were rehomogenized and analyzed. The homogenization conditions for the melt inclusions from the granites were 700 °C, 300 MPa, and 24 h, and for melt inclusions from the pegmatite, 700 °C, 100 MPa, and 24/96 h. The majority of the melt inclusions is chemically similar to the bulk rocks (excluding H2O content), but a few melt inclusions in the equigranular granite show clearly higher F and low K2O contents (on average 11.6 wt % F, 0.65 wt % K2O). The melt inclusion compositions indicate coexistence of two melt fractions, a prevailing peraluminous and a very volatile-rich, possibly peralkaline. Combined petrological, experimental and melt inclusion studies of the Kymi equigranular topaz granite indicate that plagioclase was the liquidus phase at nearly water-saturated (fluid-saturated) conditions and that the F content of the melt was at least 2 wt %. The early crystallization of biotite and the presence of muscovite in crystallization experiments at 200 MPa contrasts with the late-stage crystallization of biotite and the absence of muscovite in the equigranular granite, indicating that crystallization pressure may have been lower than 200 MPa for the granite.

Fretting wear study of Cu-10 wt% TiB2 and Cu-10 wt% TiB2-10 wt% Pb composites

In developing materials with better tribological properties, it is always conceived that the addition of softer phase would result in better frictional behavior. In order to address this issue, we report here the results of fretting wear study on Cu-10 wt% TiB2 and Cu-10 wt% TiB2-10 wt% Pb composites, sintered using spark plasma sintering (SPS) technique. It was found out that the addition of softer phase i.e. 10 wt % Pb to Cu-10 wt% TiB2 composites has not resulted in the lowering of the coefficient of friction (COF). The combination of steady state COF (0.6) and wear rate (10(-3) mm(3)/N-m) was measured and such properties are even better than that obtained with TiB2 coatings reported in the literature. For Cu-10 wt% TiB2 sintered at different temperature, a lower wear resistance with increase in hardness is being measured. An attempt has been made to correlate the observed wear behavior with the surface and subsurface deformation. The formation of a wear-resistant delaminated tribolayer consisting of TiB2 particles and ultrafine oxide debris (Cu, Fe, Ti)(x)O-y was the reason assigned for the observed low wear rate of these composites. (C) 2013 Elsevier B.V. All rights reserved.

Microstructure-hardness-fretting wear resistance correlation in ultrafine grained Cu-TiB2-Pb composites

The retention of the desired combination of mechanical/tribological properties in ultrafine grained materials presents important challenges in the field of bulk metallic composites. In order to address this aspect, the present work demonstrates how one can achieve a good combination of hardness and wear resistance in Cu-Pb-TiB2 composites, consolidated by spark plasma sintering at low temperatures ( < 500 degrees C). Transmission electron microscope (TEM) studies reveal ultrafine grains of Cu (100-400 nm) with coarser TiB2 particles (1-2 mu m) along with fine scale Pb dispersoid at triple junctions or at the grain boundaries of Cu. Importantly, a high hardness of around 2.2 GPa and relative density of close to 90% relative density (rho(theo)) have been achieved for Cu-15 wt% TiB2-10 wt% Pb composite. Such property theo, combination has never been reported for any Cu-based nanocomposite, by conventional processing route. In reference to the tribological performance, fretting wear tests were conducted on the sintered nanocomposites and a good combination of steady state COF (0.6-0.7) and wear rate (10-4 mm(3)/N m) were measured. An inverse relationship between wear rate and hardness was recorded and this commensurates well with Archard's relationship of abrasive wear. The formation of a wear-resistant delaminated tribolayer consisting of TiB2 particles and ultrafine oxide debris, (Cu, Fe, Ti)(x)O-y as confirmed from subsurface imaging using focused ion beam microscopy has been identified as the key factors for the low wear rate of these composites. (C) 2014 Elsevier B.V. All rights reserved.

Características biogeoquímicas da interação atmosfera criosfera na Antártica ocidental

O manto polar antártico retêm informação paleoclimatologica por entres suas camadas de neve e gelo. O gelo antártico tem revelado a base de dados paleoclimática de maior resolução para os últimos 800 mil anos. Os padrões de transporte atmosférico refletem a composição e a fonte do particulado encontrado na neve e no gelo do continente Antártico. Estando relacionado a processos climáticos, as características desse transporte alteram em quantidade e qualidade as espécies químicas que se depositam sobre o manto de gelo. Dessa forma, o estudo dos depósitos de particulado ao longo das camadas de neve/gelo na Antártica pode sugerir mudanças nos padrões de transporte atmosférico. Atualmente a comunidade científica discute as diferenças de padrões climáticos entre o leste e o oeste antártico. Enquanto de forma geral observa-se instabilidade no setor oeste, o clima da antártica oriental demonstra relativa estabilidade climática. Neste estudo, analisamos dois testemunhos de gelo recente de duas regiões com características climáticas diferentes do continente Antártico. No Platô Detroit situado na Península Antártica (6410′S/0600′O), analisamos a variabilidade de Black Carbon (BC) ao longo de 20 metros de neve. O BC encontrado na Península Antártica apresentou baixas concentrações comparáveis as encontradas no gelo do Artico período pré-industrial. Nossos resultados sugerem que sua variabiliade corresponde à sazonalidade dos períodos de queimada nos continentes do Hemisfério Sul. No interior do continente Antártico, analisamos o particulado em geral por um processo de microanálise ao longo de um testemunho de 40 metros extraído em Mont Johns (79o55′S/09423′O). Encontramos uma tendência negativa na deposição de poeira mineral (AlSi) entre 1967 e 2007. Nossos resultados sugerem que esta tendência seja resultado de um crescente isolamento atmosférico da região central do continente antártico pelo aumento da intensidade dos ventos ao redor da Antártica. Este aumento na intensidade dos ventos reflete por sua vez o resfriamento da alta atmosfera no centro antártico causado pela depleção da camada de ozônio na região. Adicionalmente, amostras de diferentes microambientes de Patriot Hills (8018′S/08121′O) foram coletadas de maneira asséptica para análise microbiológica. As amostras foram cultivadas em meio R2 e paralelamente o DNA total extraído foi sequenciado pela técnica de pirosequenciamento. Os resultados preliminares desta analise mostram grande riqueza de espécies dos mais variados grupos. Os resultados deste trabalho caracterizam três diferentes parâmetros relacionados a deposição atmosférica em duas áreas pouco exploradas e de grande interesse científico do continente antártico.

Microfabries of lacustrine sediments to pollutant adsorption from a polluted Eutrophic lake, the Yangtze delta region

Two types of microfabrics relating to pollutant adsorption were studied in the scanning electronic microscope (SEM) in a polluted, eutrophic lake, the Yangtze delta region. Agglutinational texture or the aggregates of small particles are composed of clay minerals and fine organic fragments among the silty grains and the coatings with a thickness about 1 mu m were on the surfaces of the silty grains in the sediments. The chemical constituents of the aggregates and the coatings are K, Na, Ca, Mg, Si, Al, O, Fe, Ti, C, N and P determined in X-ray energy spectrometry connected with the SEM. In some cases, Pb was detected in the aggregates in the top sediment. It is suggested that nutrients and metals are adsorbed to the aggregates, which were formed by electrostatic attraction of physicochemical floes. The coatings on the surface of quartz grains were formed by the interaction of dissociated Al, Si, Fe, etc from silicates with dissolved N, P and C nutrients in interstitial water, which was aroused by human pollution to the lake in recent two decades.

I：新型稀土永磁材料Nd-Fe-B氧化过程及抗氧化新体系研究II：CuO、Y_2Cu_2O_5、BaCuO_2和RBa_2Cu_3O_(7-δ)超导体磁化率及Cu价态研究

本论文由两大部分组成。第一部分是新型稀土永磁材料Nd-Fe-B氧化过程及抗氧化新体系的研究。Nd-Fe-B永磁体是1983年问世的新型稀土永磁材料。和原有的铁氧体及Sm-Co体系相比，具有磁能积高（50MGOe）。价廉源广，制备简单等三大优点；也有居里温度低（310℃），温度系数大（－0.126%/K），易氧化等三大缺点，我们对Nd-Fe-B合金的氧化过程进行研究，发现该材料热稳定性差，容易发生氧化反应，氧化使材料的结构受到破坏，并给材料的磁性造成不可恢复的损失，整个氧化过程是分阶段的。在室温和干燥的空气中材料基本是稳定的。150℃以下材料磁性受到破坏的主要原因是体系中Nd的氧化。230℃以上材料主体成分Fe也开始氧化，温度升高使反应进程大大加快。到800℃左右反应基本结束，最终产物主要为Fe_2O_3, Nd_2O_3·FeNdO_3和NdBO_3。增加体系中B的相对含量和添加某些新的元素均能提高材料的抗氧化能力，新研制的Nd-Fe-B-Si四元体系和原来的Nd-Fe-B体系相比具有下列显著优点：新体系的抗氧化能力大大提高，经过150℃的长期恒温试验，材料的结构，磁性均未受到破坏，某些体系甚至能在更高的温度下使用，另外，新体系的居里温度Tc也大为提高。比原有Nd-Fe-B磁体高40℃左右。因此该体系是一种大有发展前途的新材料。此外，我们用动态热重法研究了Nd-Fe-B合金的氧化动力学过程，但由于我们新合成的体系构相较为复杂，未能达到预期效果。第二部分是CuO，Y_2Cu_2O_5，BaCuO_2和RBa_2Cu_3O_(7-δ)超导体（R稀土元素）磁化率及铜价态研究，铜的氧化物具有复杂的化学计量关系和磁学性质。在对CuO的磁化率研究中，我们发现在低温区（77K－110K）和一定磁场下，CuO由顺磁突变为抗磁。这种转变与磁场强度有很大关系。这一结果与前人的工作有较大的出入。而与超导体的形为极为相似。所不同的是，转变温度与样品的重量也有关系。实验结果重复。由于铜氧性质在R-Ba-Cu-O超导体中起决定作用，因此有必要对CuO的低温磁性作进一步研究。此外，我们对文献尚未报道的Y_2Cu_2O_5的磁化率在77－300K温度区间进行了测量，发现它是顺磁性物质，室温有效磁矩μ_(eff) = 2.13μB。高于Cu~(2+)的理论有效磁矩（1.73μB）。经过碘量法价态分析，发现Y_2Cu_2O_5中有部分Cu~(3+)，这与磁化率的测定相符合。Tc在90K左右的Y-Ba-Cu-O体系是近期才发现的具有超高温超导材料。该体系有着独特的结构和性质。在对R-Ba-Cu-O及R-Ba-Cu-O-Ag超导体的研究中，我们发现此类超导体属II类超导体，在临界温附近该超导体由顺磁转变为抗磁，此种变化与磁场强度有很大关系，当场强大于一定值后，则观察不到这种转变。在对RBa_2Cu_3O_(7-δ) (R = Y, Sm, Eu, Gd, Dy, Ho, Er, Tm)超导体和具有相同配比但由于合成工艺条件不同而不超导的R'Ba_2Cu_3O_(7-δ) (R' = Y, Sm, Eu, Gd)非超导体的铜价态分析中，我们发现此两类化合物中均含有一定量的Cu~(3+)。且超导体中Cu~(3+)的含量高于非超导体中Cu~(3+)的含量（同样比例）。我们还发现Cu~(3+)对水极为敏感，将RBa_2Cu_3O_(7-δ) (除R = Gd, Dy, Er)超导体在未干燥容器中测出的Cu~(3+)量远远低于干燥容器中所测得的值。我们认为这可能是引起超导体不稳定的重要原因。由于尚缺乏用其它手段检测到超导体中Cu~(3+)存在的例证。故对此问题还有待于今后继续作进一步的研究。

以水滑石类化合物为前体的Co-M-Al(M=过渡金属)复合氧化物对催化消除NO_x活性的研究

以共沉淀法制得的水滑石类化合物为催化剂前体,经焙烧可得到一系列尖晶石类化合物Co-M-Al[M=Cr,Mn,Fe,Ni,Cu;n(Co):n(M):n(Al)=3:1:1].通过XRD,比表面测定,化学分析,NO吸附等方法对其进行表征,测定了此系列催化剂对NO催化还原和催化分解的活性,结果发现此系列催化剂对消除NO具有很高的活性.同时对催化消除NO的机理及过渡金属离子中d轨道电子对催化活性的影响进行了一些探讨.

萃取分离电感耦合等离子体原子发射光谱法测定钢中的微量稀土元素

本文采用苯甲酰苯胲(BPHA)-甲基异丁基酮(MIBK)溶剂萃取方法将钢中基体元素Fe,Ti,Mo,V等大量非稀土元素萃入有机相中,稀土元素留于水溶液中.由电感耦合等离子体原子发射光谱(ICP-AES)仪直接测定水溶液中的微量稀土元素La,Ce,Pr,Nd.Sm,Y和Gd,实验结果与推荐值基本相符,方法的回收率为96％～108％,相对标准偏差低于5％.

湖南、广西泥盆纪硅岩地球化学与沉积构造背景

During the Devonian, a complicated carbonate platform-basin configuration was created through transtensional rifting in the context of opening of Devonian South China Sea; extensive bedded chert, commonly interbedded with tuffaceous beds, occurred in the narrow, elongate interplatform basins (or troughs) in South China, where they occurred earlier (Early Devonian) in southern Guangxi and later (early Late Devonian) in northern Guangxi-south central Hunan. In order to unravel the origin and distribution of the bedded chert successions, and their relationships to basement faulting activities during the opening of the Devonian South China Sea, studies of element (major, minor and REE) geochemistry and Rb-Sr, Sm-Nd isotopic systematics are carried out upon the chert deposits. These chert deposits commonly have high SiO2 contents and (average 94.01%) and low TFe2O3 (average 0.55%), together with other geochemical parameters, suggestive of both biogenic and hydrothermal origins. However, Fe/Ti ratio are high along the elongate interplatform basins(troughs) to the northwest along Wuxiangling-Zhaisha-Chengbu, and to the southeast along Xiaodong-Mugui-Xinpu, suggesting relatively intense hydrothermal activities there. They generally contain very low total REE contents (∑REE average 31.21ug/g) with mediate negative Ce anomalies (mean Ce/Ce*=0.83) and low Lan/Cen values (average 1.64), indicating an overall continental margin basin where they precipitated. The northward increases in Ce/Ce* values, particularly along the elongate troughs bounded both to the east and west of the Guangxi-Huanan rift basin, suggest a northward enhancement of terrigenous influences, thereby reflecting a gradual northward propagation of open marine setting. Generally low positive Eu anomalies in the chert, except for the apparently high Eu anomalies in the chert from Chengbu (Eu/Eu* up to 4.6), suggest mild hydrothermal venting activities in general, except for those at Chengbu. The initial 87Sr/86Sr (0) ratios of chert generally vary from 0.712000 to 0.73000 , suggesting influences both from terrigenous influx and seawater. The Nd isotopic model ages (tDM or t2DM) and initial εNd (0) values of chert vary mostly from 1.5 to 2.1 Ga, and from –16 to –21, respectively, implying that the silica sources were derived from the provenances of the Palaeoproterozoic crust relics at depth. The high εNd (0) values of chert (-0.22 to 14.7) in some localities, mostly along the elongate troughs, suggest that silica sources may have been derived from deeper-seated mantle, being channeled through the interplate boundary fault zones extending downwards to the mantle. At Wuxiangling, Nanning, chert occurs extensively from the Emsian through the Frasnian strata, both U/Th ratios and tDM ages of chert reached up to a maximum in the early Frasnian corresponding to the extensive development of chert in South China, pointing to a maximum extensional stage of Devonian South China basin, which is supported by the Ce/Ce* values as is opposed to the previous datasets as the coeval minimum values.

伽马射线谱仪探测月球表面元素的分布——以“嫦娥一号”伽马射线谱仪为例

Apollo和Lunar Prospector(LP) 携带的伽马射线谱仪探测了月球表面的氧（O）、硅（Si）、铝（Al）、铁（Fe）、钛（Ti）、钙（Ca）、钾（K）、镁（Mg）、钍（Th）和铀（U）等10种元素的全球分布，对于了解月球的形成与演化有重要的意义。在我国首颗月球探测卫星“嫦娥一号”上搭载了伽马射线谱仪将进一步探测月球表面14种元素的分布特征。本论文的选题紧密结合“嫦娥一号”伽马射线谱仪数据处理和科学反演工作的工程需求，系统研究了伽马射线谱仪探测数据的处理流程和反演方法，并利用LP的数据开展了月球元素、岩石类型及其分布特征的反演工作，为嫦娥一号卫星伽马射线谱仪的数据处理和反演奠定了技术基础。论文主要包括如下几个方面的内容： （1）概述了伽马射线谱仪探测月球表面元素的发展历程，特别是阐述了伽马射线产生的机理和伽马射线谱仪元素探测的原理； （2）讨论了伽马射线谱仪数据反演及其模型，以及在“嫦娥一号”伽马射线谱仪数据反演中的应用； （3）阐述了“嫦娥一号”伽马射线谱仪性能指标，数据处理流程，地面验证实验（模拟月壤的研制及其试验）和初步的探测成果； （4）以LP伽马射线谱仪探测数据为例，讨论了伽马射线谱仪探测数据科学反演工作，阐述了全球Th的分布特征以及月球化学不均一性的相关性；用LP探测数据首次划分出月球岩石类型的分布，探讨了月球演化对岩石类型分布特征的影响。

高强度瓷绝缘子的矿物组成和显微结构研究

以矿物学理论为基础，采用XRD、AAS、TEM和OM等分析仪器，对国产70kN、日本120kN和210kN高强度瓷绝缘子的化学成分、显微结构等特征进行了分析，找出造成国内外瓷绝缘子性能差异的主要因素。并对贵州地区的高强瓷非金属矿物原料进行了较系统的矿物学研究，确定了6个主要原料基地。在以上研究的基础上，优化设计了420kN和300kN高强度瓷绝缘子的配方及相关生产工艺。并对烧结出420kN高强度瓷绝缘子的化学成分与显微结构进行了研究分析。得到的主要结论如下： （1）对比国内外高强瓷得出，造成国内高强瓷性能差的主要因素是化学成分和显微结构。国内70kN样品含有较高的K2O和TiO2，严重超过了高强瓷标准配方值，而国外配方恰好落在标准值范围内；国内70kN样品晶相含量仅为35%，而国外210kN样品的晶相含量为48%，且晶粒细小分布均匀，玻璃相和气孔相含量也比国内产品少且分布均匀。 （2）采用XRD对贵州地区矿物原料进行分析，最终选定了毕节、大方6个高强瓷原材料产地。这些基地粘土类矿物原料，具有可塑性好，有害矿物含量少，化学成分中Si、Al比适中，Fe、Ti等杂质元素含量低的特点；铝氧类矿物具有含Al2O3含量高且杂质元素少的特点，是制备高强度瓷绝缘子的优质原料。 （3）在主要使用贵州所产的矿物原料基础上，结合国内外高强瓷的性能差异，优化设计了300kN和420kN高强瓷的配方和工艺。其中将坯料的颗粒度组成设定在：≥5µm43-48%，≥10µm25-31%，≥20µm5-12%，并采用合理烧结制度下烧结出420kN高强瓷，其烧结温度范围在13001400℃，最终产品通过IEC检测且显微结构较好。

晋北高岭石及其热产物的矿物物理学研究

通过对晋北地区高岭石及其热产物的研究，笔者主要得到了以下几点结论：1、晋北煤矸石是一种优质的高岭石，Fe、Ti含量低，结晶度高，晶体主要呈片状形态，具有较好的开发前景，应打破仅仅局限于陶瓷工业的局面。而P-1高岭石因Fe、Ti含量高，质量差。2、在高岭石受热脱羟过程中，部分羟基一直到850℃才完全脱失。3、在高岭石-莫来石反应系列中，存在SiO_2与Al_2O_3的分凝，SiO_2与Al_2O_3反应生成莫来石是莫来石的主要形成途径，Al-Si尖晶石与SiO_2反应生成莫来石只是一个次要途径。4、在高岭石热处理产物的研究中首次测到了-70ppm附近的Al-Si尖晶石的~(29)Si MAS NMR谱峰，Al-Si尖晶石是一个不稳定相，存在的温度范围大约为850-1000℃，随着温度升高，它将转变为莫来石。5、高岭石的980℃放热峰归因于在高岭石受热相变过程中，莫来石、方英石、γ-Al_2O_3的晶出。6、在煤矸石中，Fe主要以Fe~(2+)置换Al~(3+)形式存在，其次是部分Fe~(2+)被吸附在高岭石表面；而在P-1高岭石中，Fe主要以Fe~(3+)、Fe~(2+)置换Al~(3+)及杂质氧化物的形式存在。7、以前国内一些学者提出的所谓新矿物—“偏岭石”，笔者认为很可能是高岭石受煤自然烘烤形成的变高岭石。

山东蓝宝石的矿物学研究

本文研究的主要目的在于两个主要方面：一是从理论上阐明蓝宝石的呈色机制，为蓝宝石的改色加工利用提供理论根据；二是基础矿物学方面的研究，重点在其中的包裹体，了解它们的组成成分、形态、分布规律。1、蓝宝石的颜色是由Fe~(2+)—Ti~(4+)、Fe~(2+)—Fe~(3+)、Fe~(3+)以及Cr~(3+)的吸收峰所决定的，但是矿物究竟呈现什么颜色，不仅取决于这些吸收峰本身的强弱，而且更取决于它们之间的相对强弱。这些吸收峰的强弱决定于进入刚玉晶格中的色素离子Fe~(2+)、Fe~(3+)、Ti~(3+)、Ti~(4+)、Cr~(3+)、Mn~(2+)等的含量，而其相对强弱则取决于这些离子的相对含量即Fe~(2+)/Ti~(4+)、Fe~(3+)/Fe~(2+)的比值，对于蓝色而言，Fe、Ti的含量越高，颜色就越深。2、通过热处理可以改变刚玉中致色元素的含量（含色素离子的包体矿物发生溶解，离子通过扩散作用进入刚玉晶格）和混价离子的比值，这是蓝宝石改色的理论基础。3、刚玉中包体矿物的多少直接影响支蓝宝石的透明度，根据其分布特征，进行合理切割，通过热处理可以改变蓝宝石的颜色，提高其质量；但很难使其透明度有在的改观。4、在刚玉众多的包体矿物中，我们新发现了石英、钛铁晶石、刚玉微晶、更长石等矿物以及目前尚不能定名的卤化物和含硫化合物。5、刚玉巨晶是多成因多来源的，主要是从寄主岩浆——玄武岩浆中结晶出来的，其结晶过程十分复杂，也可以作为地幔矿物或捕掳晶而存在。