Lecture 18 Nanominerals

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纳米材料双语翻译

纳米材料双语翻译

姓名:学号:1012100105 班级:化学1001 Photoluminescence properties of LaF3: Eu3+nanoparticlesprepared by refluxing method光致发光性质:铕掺杂的三氟化镧纳米粒子的回流制备方法Rare earth ions-doped nanostructure materials have been widely investigated because of their sharp and intense emission originating from the electronic transitions within the 4f shell of the doping ions and their applications in many fields. In comparison with the conventional oxide-based luminescent materials, fluorides are advantageous as fluorescent host materials owing to their low vibrational energies and the subsequent minimization of the quenching of the excited state of the rare-earth ions[1]. Hence, rare earth ions-doped nanostructural fluorides have attracted extensive interests due to their potential applications in lighting and displays[2,3], upconverters[3−8], magnetic resonance imaging (MRI)[9], biological fluorescent labels[10−14],optical amplifiers[15], transparent glass[16], scintillators[17], photonic crystals[18], etc. Among these fluorides, LaF3 host matrix exhibits the photochemical stability, the biocompatibility, and the relative low crystalline temperature, and its phonon energy is as low as 350 cm−1[19,20]. Rare earth ions (Eu3+, Ce3+, Tb3+, Nd3+, Er3+, Pr3+, Ho3+, Yb3+, Tm3+) doped LaF3 nanoparticles[21−24], LaF3 triangular nanoplates[24,25], and silica-coated[19], or organic ligands[20,26]modified LaF3 luminescent nanoparticles have been reported in literatures.稀土离子掺杂的纳米结构材料已被广泛研究,因为其尖锐和激烈的排放来源于电子跃迁的4f内壳的掺杂离子和其在许多领域的应用。

一流课程建设背景下《矿物岩石学》线上课程建设探索

一流课程建设背景下《矿物岩石学》线上课程建设探索

一流课程建设背景下《矿物岩石学》线上课程建设探索*马莉燕,丁伟*,王葆华,赵义来,白令安,温淑女,杨金豹(桂林理工大学地球科学学院,广西桂林541006)一、概述矿物学、岩石学和矿床学(070901)属于地质学(0709)的二级分支学科,涉及相关的课程包括“晶体光学与造岩矿物”“岩浆岩岩石学”“沉积岩岩石学”“变质岩岩石学”“岩石学”“矿物学与岩石学”“环境矿物学导论”“成因矿物学概论”“岩石显微结构分析”“岩矿物理化学”等10门课程[1]。

其中,矿物学是研究矿物化学组成、内部结构、外表形态、物理性质和化学性质、形成和变化的条件、时间与空间上的分布规律、形成与演化的历史和用途以及它们之间关系的一门学科[2-3]。

岩石学主要研究岩石的矿物成分、结构构造、产状和分布、岩石成因和形成环境等[2-3]。

无论从事地质学基本理论的研究,还是勘探开发利用地下资源或解决实际工程地质问题,都需要有矿物岩石学的基本理论[2]。

因此,在我国本科院校开设的地质类工科专业,包括地质工程、勘查技术与工程、地下水科学与工程等专业,都将“矿物岩石学”课程作为一门重要的专业基础课[4]。

结合矿物岩石学专业性强、知识点多和实践性强的特点,课程以MOOC课的形式在线授课,尽管已有少量矿物岩石学相关课程MOOC的教学改革探索[5]。

然而,截至目前,中国大学MOOC平台上能搜索到《矿物岩石学进展》《岩石学》《结晶学与矿物学》等有些相关性课程,而缺少《矿物岩石学》的在线课程。

2019年国家发布《教育部关于一流本科课程建设的实施意见》中关于一流课程的5类推荐类型中,有2类就是与线上课程有关的,学生线上自主学习与线下面授有机结合开展混合式教学,可以打破学习的时空限制,有效提高教学质量,故此,《矿物岩石学》在线课程建设是本课程改革建设的主摘要:为响应国家一流课程建设要求,深化教育教学改革,将现代信息技术与教学深度融合,我校《矿物岩石学》课程组整合现有教学资源,开展线上教学建设,提升课程建设水平。

中国地质大学(北京)考博专业英复习材料

中国地质大学(北京)考博专业英复习材料

晶) is said to have a porphyritic texture(斑状结构). The classification of fine-grained rocks, then, is based on the proportion of minerals which form phenocrysts and these phenocrysts (斑晶)reflect the general composition of the remainder(残留) of the rock. The fine-grained portion of a porphyritic(斑岩) rock is generally referred to as the groundmass(基质) of the phenocrysts. The terms "porphyritic" and "phenocrysts" are not restricted to fine-grained rocks but may also apply to coarse-grained rocks which contain a few crystals distinctly larger than the remainder. The term obsidian(黑曜岩) refers to a glassy rock of rhyolitic(流纹岩) composition. In general, fine-grained rocks consisting of small crystals cannot readily be distinguished from③ glassy rocks in which no crystalline material is present at all. The obsidians, however, are generally easily recognized by their black and highly glossy appearanceass of the same composition as obsidian. Apparently the difference between the modes of formation of obsidian and pumice is that in pumice the entrapped water vapors have been able to escape by a frothing(起泡) process which leaves a network of interconnected pore(气孔) spaces, thus giving the rock a highly porous (多孔的)and open appearance(外观较为松散). ④ Pegmatite(结晶花岗岩) is a rock which is texturally(构造上地) the exact opposite of obsidian. ⑤ Pegmatites are generally formed as dikes associated with major bodies of granite (花岗岩) . They are characterized by extremely large individual crystals (单个晶体) ; in some pegmatites crystals up to several tens of feet in length(宽达几十英尺)have been identified, but the average size is measured in inches (英寸) . Most mineralogical museums contain a large number of spectacular(壮观的) crystals from pegmatites. Peridotite(橄榄岩) is a rock consisting primarily of olivine, though some varieties contain pyroxene(辉石) in addition. It occurs only as coarse-grained intrusives(侵入), and no extrusive(喷出的) rocks of equivalent chemical composition have ever been found. Tuff (凝灰岩)is a rock which is igneous in one sense (在某种意义上) and sedimentary in another⑥. A tuff is a rock formed from pyroclastic (火成碎 屑的)material which has been blown out of a volcano and accumulated on the ground as individual fragments called ash. Two terms(igneous and sedimentary) are useful to refer solely to the composition of igneous rocks regardless of their textures. The term silicic (硅质 的)signifies an abundance of silica-rich(富硅) and light-colored minerals(浅 色矿物), such as quartz, potassium feldspar(钾长石), and sodic plagioclase (钠长石) . The term basic (基性) signifies (意味着) an abundance of dark colored minerals relatively low in silica and high in calcium, iron, and

纳米材料学英文教学PPT.ppt

纳米材料学英文教学PPT.ppt
2021/3/5
Co/Cu(111) H.C. Monoharan, C.P. Lutz, D.M. Eigler Nature 403 (2000) 512
• Association: the bias was raised to 500 mV for 10 s
• It is not possible to break the C-H and C-C bonds with a single electron process at this voltage, especially as their bond energies are about 2 and 3 times higher than the C-I bond.
Pried them apart into iodine and phenyl (C6H5) by injecting electrons from the STM tip (a).
Used the tip to pull the iodine away (b and c) and draw the phenyl molecules closer together (d).
MIX-AND-MATCH molecule: Atomic engineers eventually hope to create molecules from scratch, adding atoms exactly as needed to perform specific functions. This molecule, with 18 cesium and 18 iodine atoms, was built--one atom at a time--with a STM
2021/3/5

细粒钽铌矿选矿工艺流程

细粒钽铌矿选矿工艺流程

细粒钽铌矿选矿工艺流程英文回答:Tantalum-niobium ore is a valuable mineral resourcethat is widely used in various industries. The ore is typically found in the form of fine-grained tantalum-niobium minerals, such as tantalite and columbite. Extracting tantalum and niobium from the ore requires a complex process known as mineral beneficiation.The beneficiation process for tantalum-niobium ore typically involves several stages, including crushing, grinding, gravity separation, magnetic separation, and flotation. Each stage is designed to remove impurities and increase the concentration of tantalum and niobium minerals in the ore.Firstly, the ore is crushed into small particles using a jaw crusher or a cone crusher. This helps to break down the ore and release the tantalum and niobium minerals. Thecrushed ore is then ground into a fine powder using a ball mill or a rod mill. This grinding process helps to further liberate the minerals and increase their surface area for subsequent separation.Next, gravity separation is employed to separate the heavier tantalum and niobium minerals from the lighter gangue minerals. This is done using techniques such as spiral concentrators, shaking tables, or centrifugal concentrators. The principle behind gravity separation is that the denser minerals will settle to the bottom, while the lighter minerals will rise to the top. By adjusting the parameters of the gravity separation equipment, such as the angle of inclination or the water flow rate, the desired separation can be achieved.After gravity separation, magnetic separation is used to remove any remaining magnetic minerals from thetantalum-niobium concentrate. This is done using high-intensity magnetic separators, which generate a strong magnetic field to attract and separate the magnetic minerals. The non-magnetic minerals are discarded as waste,while the magnetic minerals are collected as a magnetic concentrate.Finally, flotation is employed to further increase the concentration of tantalum and niobium minerals in the concentrate. Flotation involves the use of chemicals, such as collectors and frothers, to selectively separate the valuable minerals from the gangue minerals. The froth flotation process relies on the differences in the surface properties of the minerals, allowing the valuable minerals to attach to air bubbles and float to the surface, while the gangue minerals sink.Overall, the beneficiation process for tantalum-niobium ore is a complex and multi-stage process. It requires careful optimization and control to achieve the desired separation and concentration of tantalum and niobium minerals. However, with the right combination of equipment and process parameters, it is possible to produce a high-quality tantalum-niobium concentrate that can be further processed into valuable products.中文回答:英文回答:钽铌矿是一种有价值的矿产资源,广泛应用于各个行业。

18课课件

18课课件

由于腐蚀具有非常大的作用,不仅要考虑在 空气中的曝光时间还要考虑电蚀作用,高温 氧化和危险的应力腐蚀断裂。

Most properties of materials are temperature sensitive . The principal effect of increasing temperature on metallic fasteners is a decline in their strength properties.
在分析紧固件的用途时,设计人员首先应 该询问的问题之一是:它是在什么样的环 境中使用和是否会遭受腐蚀的侵袭?
Seldom will the answer be no . Any yes answer obligates the engineer to identify the character of the exposure,anticipate the possible consequences,and determine the most effective counter-measures.
当温度在230 ℃以下时,通常用来制造紧固件 的商品等级的中碳钢和合金钢均可以胜任它们 的工作。
From 230 ℃ to about 480 ℃ stainless steels and the chrome-moly steels are adequate. For higher temperature service one of the specially developed heat resistant superalloys must be used.
Selection of Fastener Materials
Lesson 18

学术英语理工详解答案Unit3

学术英语理工详解答案Unit3

第11页/共53页
Unit 3 Listening to Lectures
1 Preparing for listening to a lecture
4 What are the potential effects of global warming?
The effects of global warming may be physical, ecological, social or economic. Evidence of observed climate change includes the instrumental temperature record, an increase of extreme weather events (such as hurricanes, earthquakes, volcanoes, and landslides), rising sea levels, decreased snow cover in the Northern Hemisphere, mass animal extinctions and human migrations.
Unit 3 Listening to Lectures
Unit Contents
1 Preparing for listening to a lecture 2 Paying attention to the introduction 3 Understanding the ideas through examples 4 Following a lecture through signal words 5 Memorizing the points by taking notes
1 What are the definitions of the following terms?

Lecture18-19-Graphene and Nanotubes(ppt)

Lecture18-19-Graphene and Nanotubes(ppt)
equi-potential lines
Science 315, 1379 (2005)
Carbon nanotubes
Iijima 1991 Smalley 1993
STM images of carbon nanotubes T.W. Odom, J.-L. Huang, P.Kim, C.Lieber, Nature 391 (1998)
Angle-resolved photo-emission spectroscopy of heavily doped graphene synthesized on silicon carbide
A. Bostwick et al – Nature Physics, 3, 36 (2007)
high-energy photon ħω~100-1000eV
ε
?
strong covalent bonds
σ
Ultra-thin graphitic films: from flakes to micro-devices
Novoselov & Geim (Manchester) Science 306, 666 (2004)
for references, see the review article A.Geim & K.Novoselov - Nature Materials 6, 183 (2007)
Lectures 18-19 Carbon nanotubes
Physical Properties of Carbon Nanotubes Saitoh, Dresselhaus, Dresselhaus, Imperial College Press 1998
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Perturbation of Interfacial Water Perturbation of Interfacial Water
MD Simulation of Water near Hematite Nanoparticles
• Ordering of water, the intermolecular bonding, and water exchange rates are affected by nanoparticle size and morphology and morphology
γ ≡ (δG / δA)P ,T
G = Gibbs Free Energy, A = surface area • The total free energy of a system then is: gy y Gtot = ∑ μi ni + ∑ γ j A j
i j
Thermodynamic y Properties
Buseck and Posfai (1999) PNAS 96, 3372‐3379 Buseck et al. (2000) Int. Geol. Rev. 42, 577‐593
Unique Aspects of Nanoparticles Unique Aspects of Nanoparticles
Fig. 7. Progression of chain development: (a) single primary crystallite; (b) f i t llit four primary crystallites f i t llit forming i a single crystal via oriented attachment; (c) five primary crystallites forming a single crystal via oriented attachment; (d) single crystal of anatase with magnified inset of the attachment interfaces.
Burns et al. (2005) Angew. Chem. Int. Ed. 44, 2135‐2139
Small Angle X‐ray Scattering (SAXS)
Small‐Angle Scattering g g
Svergun and Koch (2003) Rep. Prog. Phys. 66, 1735–1782
Repulsive Force Depends on Double Layer Thickness, Which Depends on I h k h h d
• Critical Coagulation Concentration (CCC): Ionic strength above which particles aggregate
1 3
1
Figure 10. TEM micrographs of aggregates formed by counterion screening of surface charge. KCl concentration is 39 mmol kg-1.
3 4 2
2
4
Figure 5. Summary of kinetic data. Hydrodynamic diameter of hematite particles after 30 rain coagulation time as a function of (a) KCl and (b) phosphate concentrations. Hematite concentration = 10 mg L-1, pH = 6.0, T = 25°C
General Particle Aggregation Behavior General Particle Aggregation Behavior
Particle Aggregate Structure Affected by Surface Charge, Electrolytes, and Adsorbates Ch El l d Ad b
Chorover et al. (1997) Clays Clay Miner. 45, 690‐708
Oriented Aggregation of Nanoparticles: TiO2 l
Penn and Banfield (1998) Science 281, 969‐971 Penn and Banfield (1999) GCA 63, 1549‐ 1557
Surface Thermodynamics Surface Thermodynamics
• Surfaces contribute to the free energy of a Surfaces contribute to the free energy of a system • This is described by the surface free energy: This is described by the surface free energy:
Surface Restructuring Surface Restructuring
Zhang et al. (2003) Nature 424, 1025‐1029
Domains or Stacking Faults Domains or Stacking Faults
Zhang and Banfield (2009) J. Phys. Chem. C 113, 9681‐9687
Lecture 18: Nanominerals Lecture 18: Байду номын сангаасanominerals
Size Range of Natural Particles Size Range of Natural Particles
Fig. 2. Examples of how ferric iron occurs in the environment, ranging from the molecular to macroscopic scales. (Left) Molecular ferric oxide states, including an octahedrally coordinated monomer [hexaquairon III (53), top] and oligomer [trimer cluster (54), bottom] with Fe3+ (smaller dark red spheres), oxygen (larger light red spheres), and hydrogen (light pink spheres). These molecules are hydrogen‐terminated but should only be considered approximations of actual aqueous/environmental states. (Middle) Polyhedral representations of 1‐ and 5‐nm hematite (Fe2O3) nanoparticles. Each polyhedron represents an Fe3+ in octahedral coordination with oxygen. The thickness of the 5‐nm particle should be typically several (roughly five to seven) octahedral layers (23) and that of the 1‐nm particle should be just a few octahedral layers. (Right) (Top) typically several (roughly five to seven) octahedral layers (23) and that of the 1 nm particle should be just a few octahedral layers (Right) (Top) HRTEM image of hematite nanoparticles from Namibia (Africa) (sample courtesy of the Smithsonian Institution research collection); (Middle) TEM image of an unoriented aggregate of 3‐ to 5‐nm hematite crystals (stippled portion of the image) from an acid mine drainage site in Montana (USA) (55); (Bottom) photograph of macroscopic specular hematite (courtesy of R. Lavinsky). (from: Hochella et al. (2008) Science)
Spagnoli et al. (2009) GCA 73, 4023–4033
Surface Functional Group Reactivity G R i i
Rustad and Felmy (2005) GCA 69, 1405–1411
Nanoparticle Aggregation Nanoparticle Aggregation
Nuclear Test Site Groundwater
Utsunomiya et al. (2009) ES&T 43, 1293‐1298
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