Tunable left-handed metamaterial based on electrorheological fluids

A tunable left-handed metamaterial consisting of a periodic array of the left-handed dendritic structure units infiltrated with electrorheological fluids is demonstrated. Experimental results show that the passband can move from the original 8.50-10.60 GHz to 7.16- 8.39 GHz after electrorheological fluids are infused. When a dc （direct current） electric field of 666 V/mm is applied, the passband moves toward lower frequency of within 7.08-8.30 GHz. This method provides one convenient way to design adaptive metamaterials.     

S135钢在含CO2聚合物钻井液中腐蚀研究

利用高温高压反应釜研究油田常用的四种S135钢在含CO2聚合物钻井液中腐蚀行为。结果表明,平均腐蚀速率随温度或CO2分压增大而先增大然后降低;随流速增大而升高。S135钢在动态液相中的平均腐蚀速率远大于动态气相,无论在液相还是气相S135钢平均腐蚀严重情况依次为S135（A）＞S135（B）＞S135（C）＞S135（D）。该实验条件下（温度为100℃,CO2分压为3MPa,流速为2m/s,腐蚀时间为96h）,S135钢气相局部腐蚀比较轻微,其点蚀系数介于1.12~1.49,液相局部腐蚀比较严重,其点蚀系数介于1.40~5.22。用聚合物钻井液钻遇高含CO2气层时,建议采用S135（D）钻杆,最好不用S135（A）或S135（B）钻杆。     

立方结构的导电磁球的有效磁导率

用迭代方法研究了磁流变体中体心立方结构、面心立方结构及简立方结构3种立方格子导电球的有效磁导率与磁导率比、趋肤深度及频率的依赖关系.结果发现：3种立方格子结构的导电磁球的有效磁导率为一复数,在临界体积比时,3种结构中,面心立方结构的有效磁导率最大,计算结果与文献[10-12]的实验结果符合较好.     

粘弹性流体的一个爆破准则与存在性结果

我们给出描述粘弹性流体的Oldroyd方程的一个爆破准则,即∫T*0‖(△)u‖L∞dt= ∞.在较弱的条件下,即当初值(φ)0∈W2,q(Ω),3＜q≤6, u0∈H10∩H2时,同样得到了强解的局部存在惟一性,从而改进了林芳华、柳春和张平的一个结果.     

磁流变液管道流模式流动行为的实验研究

通过实时显微观测，描述了磁流变液在管道中的流动行为.从观测到的一系列新的流动现象中可看出目前通用的均匀连续介质模型和管道流测试手段有不合理之处.这一工作为进一步深入理解磁流变液的力学行为和性质，建立新的更合理的理论模型提供了实验依据.     

Electrorheological Effects at High Shear Rate

Introduction Winslow in his patent discovered the electro- rheological (ER) effect[1], which is characterized as the rapid, drastic, and reversible change in the rheological properties of a material upon the application of an ex- ternal electric field. Ma…     

Late Yanshan-Himalayan hydrocarbon reservoir adjustment and hydrotherrnal fluid activity in the central Tarim Basin

The adjustment of primary hydrocarbon reservoirs in marine formations is an important feature of the oil pools in the Tarim Basin. Large-scale hydrocarbon adjustment is related to the strong regional tectonic movements, which is always accompanied by extensive migration of basin fluids including diagenetic and mineralizing fluids. Organic fluid inclusions are well developed in hydrothermal minerals, such as fluorite, which have been found in the dissolution-enlarged fractures or karstification caves in the Ordovician in the central Tarim Basin. Proved by well drilling, the fluorite deposit is good reservoir for oil and gas. So the peculiar accompanied or superimposed relationship between fluorite hydrothermal fluid mineralization and hydrocarbon migration and accumulation exists in the Ordovician in the central Tarim Basin. Considering regional tectonic setting and mineralization condition,through different kinds of analytic methods including electron spin resonance dating, fluid inclusion laser Raman and colonial inclusions hydrocarbon fossil analysis, we proposed that extensive mineralizing fluids and hydrocarbon migration occurred in late Yanshan-Himalayan (110.4-30.8 Ma) period, and Himalayan, especially, is an important period for hydrocarbon accumulation from 34.3 Ma to present.     

强烈蚀变火山岩地层组构及其防塌钻井液研究

在辽东湾、渤海湾及其邻近的冀东油田和大港油田东部的钻遇地层中存在易塌的火山岩地层。为了探寻适用于该地层的防塌措施 ,对冀东油田M2 7- 2 7井岩心的岩石结构、矿物组成、水分含量、线膨胀率、回收率和稳定指数等进行了分析。结果表明 ,该套岩层含有大量蛋白石等粘土矿物 ,且非均质性严重 ,成分复杂 ,裂隙发育。因此 ,在钻进过程中 ,该井段的钻井液需要有强抑制、强封堵、低失水的性能。基于这一认识 ,优选出了多元醇防塌钻井液。现场试验结果表明 ,该钻井液体系有效地保证了玄武岩井段的安全顺利钻进及井眼规则性。     

应用锆石研究铀成矿流体的地球化学特征:以粤北棉花坑铀矿床为例

铀矿中锆石富集Li、P、Ti、Nb、Hf、U、Th、Ta、Y、Rare earth elements(REE)等微量元素,Th/U比值较低,在以大陆上地壳为标准化的模式图上呈现明显的重稀土富集、Ce、Y正异常和Eu负异常的特征。根据锆石/热液间微量元素的分配系数估算了成矿流体的微量元素质量分数。铀成矿流体具有富U,低Th/U比值,高稀土元素质量分数,轻、重稀土分异不明显,显著的Ce、Eu负异常和Y正异常,低Ce~(4+)/Ce~(3+)比值等特征。成矿流体主要来源于岩浆期后热液,并得到流体/岩石反应的改造,流体上升减压导致流体沸腾、气体溢出、碱性增高和还原环境,最终导致铀矿物的沉淀和铀矿床的形成。     

壳幔混染成矿机制的流体包裹体证据—以滇西老王寨金矿为例*

深部地质过程的流体包裹体示踪显示,老王寨金矿床含矿石英中Na Cl-H2O包裹体和CO2-H2O包裹体发育,含矿热液从成矿前阶段→成矿阶段→成矿后阶段,其均一温度、成矿压力、盐度与侵位深度变化依次表现为226.2~374.9℃→173.1~251.1℃→107.2~170.9℃、(827~1 084)×105Pa→(711~736)×105Pa→(410~460)×105Pa、9.208%~9.857%→4.496%~4.651%→2.736%~4.651%和3.19~4.18 km→2.74~2.84 km→1.59~1.78 km。综合研究表明,矿区初始含矿流体主要为含CO2的地幔流体,随着成矿作用的进行,含矿热液温度、压力、盐度和侵位深度不断降低,导致成矿流体由高温熔浆性质向低温热液性质演变,从而表现出壳幔混染特征。这一深部地质演化过程反映,高温高压的含矿地幔流体,在参与成矿过程中,与地壳岩石相互作用,引发交代蚀变及壳幔物质混染叠加成矿。