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The Ningqiang carbonaceous chondrite is the first falling carbonaceous chondrite in China, The ge...
宁强碳质球粒陨石是中国第一块降落的碳质球粒陨石。
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The Ningqiang carbonaceous chondrite is the first falling carbonaceous chondrite in China, The geochemical characteristics of the refractory inclusions in the meteorite including petrology, mineralogy and chemical compositions were studied by many kinds of scientific method such as optical microscopy, electron microprobe, and instrumental-activation analysis and so on.
宁强碳质球粒陨石是中国第一块降落的碳质球粒陨石。本工作采用了光学显微镜、电子探针、仪器中子活化分析等多种手段,对这块陨石难熔包体的地球化学特征(包括岩石学、矿物学及化学成份)进行了研究。
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The friction performances of carbon face were investigated with an inertia friction tester. The torque curve of carbon face was ideal, the coefficient of static friction was lower than that of dynamic in 0.28 MPa, the friction coefficient of static and dynamic decreased with the braking pressure increasing. To the fiber face, the coefficient of dynamic friction of carbon face was more stable in cycle braking process, the wear rate was lower, and it was efficient to protect the couple plate not to be worn.
结果表明:碳质层的摩擦力矩在制动初期上升较快,中间过渡区平稳,尾部翘起较小;在制动压力小于0.28 MPa时静摩擦系数小于动摩擦系数,且动、静摩擦系数均随制动压力增加而减小;相对纤维层而言,采用碳质层摩擦时摩擦力矩曲线形态更好,连续制动时摩擦系数波动较小,磨损率低且能够有效保护偶件,是1种静/动摩擦系数比较低且适用于高载荷工况条件下使用的摩擦材料。
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Based on the above research, we analyzed regional metallogenic conditions from geology, geophysics and geochemistry. Considering regional strata, some source beds with ore-bearing strata controlled apparently metallogenesis. The strata contained hydrothermal siliceous rock or siliceous albitite ether formed some favorable source beds and established substantial foundation for later diplogenetic metallogenesis e.g.
从区域地层上来看,含特殊层位的矿源层对成矿有明显的控制作用,其中含热水沉积成因的硅质岩或硅质钠长质岩的地层或形成有利的矿源岩,为后期叠生成矿奠定物质基础,或直接形成工业矿床;另外,区内黑色页岩(包括碳质板岩、碳质泥岩、碳质页岩和含碳钙质板岩等)也是很好的矿源层。
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The sharp difference suggests that they have different origins: the former comes from allochthonous sapropel-type organisms of the lower strata and is the remains of crude oil, and the latter is autochthonous humic-type organic matter of sedimentary rocks between the basalt layers.
玄武岩中铜矿石沥青的δ13CV-PDB为-27.3‰~-33.2‰,平均-31.97‰,沉积岩中铜矿石碳质的δ13Cv-PDB为-20.2‰~-23.2‰,平均-22.11‰,表明二者无明显成因联系,前者属腐泥型,为石油的遗迹,来自下部地层;后者为腐植型,来自原地沉积的陆生高等植物。
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Specifically, itcontains 8 chapters.In chapter 1, the formation, structures, properties and the futureprospect of liposome were thoroughly reviewed;In chapter 2, the stibility and permeability of phopholipid -eleostericacid liposome were studied together with the effect of polymerizationof eleostearic acid. This membrane system was very sensitive to 〓,the effect of 〓 was clarified to increase the aggregation/fusion ofliposomes and made the permeability of mixed liposomes much higher;In chapter 3, two polymerizable conjugated diyne bolaamphiphiles were synthesized. They could form very stable mixed liposome, andthe diyne could be polymerized by UV light in bilayer liposomes, as aresult, the stability of mixed liposome against solvent or surfactantafter polymerization were enhanced. In chapter 4, two kinds of amphiphilic amino acids were synthesized andstable liposomes were formed therefrom After the condensationpolymerization of amino acid in bilayer liposomes, stable polypeptide liposomes were obtained, which had lower phase transition temperatureand higher permeability.In chapter 5, four kinds of glycolipids were synthesized and theiraggregation behavior in water was comparied. When incorporated intophospholipid bilayer membranes, they could increase the phase transitiontemperatures and inhibit the aggregation and fusion of mixedliposomesat lower temperature.In chapter 6 and 7, three kinds of steroidal bolaamphiphiles withdifferent chain lengths were synthesized. Incorporation of steroidalmoiety to the center of lipid bilayer membrane obviously increased themobility of lipid membrane and shifted Tc to lower temperature side incomparasion with cholesterol. The bolaamphiphile which was shorter thanthe hosted lipid bilayer membrane thickness influenced the lipid packingmore obviously.
全文共分8章:第一章对脂质体的形成、结构、性质及展望进行了较为详细的文献综述;第二章研究了磷脂-桐酸脂质体的稳定性,通透能力及桐酸的聚合对这些性质的影响;磷脂-桐酸混合脂质体为一类对〓灵敏的脂质体,〓的作用首先是使脂质体集聚然后使脂质体融合,并加速内包荧光物的释放;第三章通过合成两种可聚合共轭双炔双极性双亲分子DDCA,DDOL,研究了共双炔分子在双分子层脂质体膜上的聚合及对脂质体性质的影响,聚合可以提高脂质体相对于溶剂及表面活性剂的稳定性;第四章合成了两类氨基酸为极性基团的双亲分子,它们均可以在超声下形成稳定的脂质体结构;氨基酸基团可以在脂质体上进行缩聚反应,若聚合后脂质体表面仍有足够的亲水能力,则可得到稳定的多肽型脂质体;聚合后脂质体的相变温度降低,通透能力增加;第五章合成了四种亲水基团为单糖基的双亲分子GL-l,GL-2,GL-3, GL-4,研究了它们在水中的分散情况、集合体形态与分子结构的关系;在DMPC双分子层膜中加入糖脂分子可以使脂质体的相变温度提高,阻止脂质体在低温放置时的集聚与融合;第六章-第七章合成了三种不同碳链长度的双极性含胆甾环双亲分子 CL-1,CL-2,CL-3;它们可以象胆固醇一样与磷脂混合形成稳定脂质体,胆甾环基团位于脂质体双分子层膜的中间;与胆固醇的作用相反,它们可以增加磷脂双分子层膜的流动性,降低混合脂质体的相变温度;三种分子的作用与其碳链长度和磷脂双分子层膜的厚度有关,比膜厚度短的分子影响最大。
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They are most abundant in quartz of pegmatitic leucosomes and granitic rocks, and represent the fluid appearing in their cooling stage. The DL(H2O) of such fluid is 0.93~0.96g/cm3 corresponding to P≈0.6GPa which is compatible with condition when the rapid decompression in this region was ended. 3 CO2-H2O two or three phases inclusions. They are the most widespread, and more frequently in clusters and in intragranular tails in quartz. The relative content of CO2+CH4 and H2O is considerably variable. They are also characterized with lower density (0.6~0.8g/cm3) and low pressure about 0.3~0.4GPa, and may be originated by mixture of carbonic liquid from breaking of most inclusions of peak stage and aqueous liquid of magmatic source. After entrapment, the further decrease of temperature to lower than 330℃ made such fluid separated to two or three phases.
主要集中于伟晶质脉体和花岗岩中,是这期岩浆冷凝过程析出的流体相当时就被封闭所成,密度为0.93~0.96g/cm3,相应压力约0.6GPa,这与峰期后迅速减压过程结束时的条件相符。3CO2-H2O两相和多相包体,分布最广,成簇状和拖尾状包体群,碳质和H2O相对含量很不均匀,整体密度相对最低,一般为0.6~0.8g/cm3,相应压力为0.3~0.4GPa,它们可能是大幅度减压过程中第一类包体大量爆裂析出的碳质流体与第二类H2O溶液流体在各处以不同比例混溶所成,它们被封闭后在降温至330℃以下时分裂成两相或三相包体。
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CNTs were first pre-treated using acid solution (HNO3) to obtain CNTs functionalized with carboxylic groups. Subsequently, the stearyl alcohol was grafted onto CNT with the assistance of dehydrating agent, N,N'-dicyclohexyl-carbodiimide. Excellent dispersion in organic solvents such as acetone, THF, and chloroform was found for the modified CNTs (CNT-C18). In addition, the PBS/CNTs nanocomposites were then prepared through simple melt-blending. Mechanical properties, thermal behavior, conductivity of resultant polymer/CNT composites were investigated. The results show that excellent dispersion of nanotubes in the PBS matrices was achieved.
为了增加多壁奈米碳管在复合材料中的分散性,将碳管表面进行化学修饰,首先将多壁奈米碳管浸入HNO3溶液中,进行酸化,使碳管表面带有羧酸的官能基,然后再加入十八烷醇,在温和的条件下,藉由N,N'-二环己基碳二亚胺(N,N'-dicyclohexyl- carbodiimide,DCC)脱水剂脱水,使碳管和十八烷醇之间产生酯基的化学键结,改质后的碳管可以分散在acetone、THF、chloroform…等有机溶剂中,结果显示成功的利用DCC脱水剂完成碳管的改质。
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The kiln body is divided into two sections of electrical furnace body and dynamic rotation with the kiln body constructed of clayed circular hearth uniformly inserted with 9 silicon carbon rods along the circular axis( one group made up of 3 rods and Y connection for every 3 groups).
窑体部分又分为电炉炉体和动力转动两部分,炉体部分采用粘土质圆形炉膛,沿圆轴向均匀插9根硅碳棒(每三根串联成一组,三组按& Y &接线)高铝质的陶瓷炉管又置于硅碳棒内周,通电后硅碳棒产生高温,加热炉管。
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The Company is an emerging carbon refractories specialized production factory, main products have mixed iron motor aluminum carbon brick kiln, blast furnace with sintering porous aluminum carbon brick, molded carbon bricks, mixed iron and iron tank cars do not burn carbon brick of aluminum silicon carbide composite corundum brick and developed corundum--type silicon carbide carbon brick.
本公司是一个新兴的碳质耐火材料专业化生产厂,主要产品有混铁车用烧成铝碳砖,高炉用烧成微孔铝碳砖,模压碳砖,混铁车和铁水罐不烧铝碳化硅碳砖,复合刚玉砖及研制开发的刚玉-β型碳化硅碳砖。
- 更多网络解释与碳质的相关的网络解释 [注:此内容来源于网络,仅供参考]
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carb carbonaceous:碳质的
kao kaolin 高岭土质 | carb carbonaceous 碳质的 | qtzc quartzitic 石英质
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carbonaceous:碳质的
碳循环 carbon cycle | 碳质的 carbonaceous | 碳质岩 carbonolite
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carbonaceous:碳的,碳質的,含碳的
carbonaceous sediment 碳质沉积 | carbonaceous 碳的,碳质的,含碳的 | capsule-type pressure gauge 囊式压力计
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carbonaceous chondrite:碳质球粒陨石
有些球粒陨石中含有多量的碳,甚至有许多有机物,因而称为碳质球粒陨石(carbonaceous chondrite);另一些富含顽火辉石(enstatite,MgSiO3),而组成顽火辉石球粒陨石;但最常见的是普通(ordinary)球粒陨石,其中又再细分为高铁和低铁两类.
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culmiferous:碳质页岩的
culm 草秆 | culmiferous 碳质页岩的 | culminate 到绝顶
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culmiferous:含有碳质页岩的, 生成空心茎的
culmicolous | 生于茎秆上的 | culmiferous | 含有碳质页岩的, 生成空心茎的 | culminant | 达到顶点的, 绝顶的
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cumulose:碳质堆积的
累加性选种 cumulative selection | 碳质堆积的 cumulose | 楔形的 cuneal
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cumulose deposits:碳质堆积层
cumulophyric 联合斑状的 | cumulose deposits 碳质堆积层 | cumulus 积云
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qtzc quartzitic:石英质
carb carbonaceous 碳质的 | qtzc quartzitic 石英质 | quartzizose 石英质的
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carbonized:碳化的
carbonaceous 碳质的 | carbonized 碳化的 | conchoidal 贝壳状