琉璃的搭配

琉璃与22K金的搭配 金不变色,琉璃永不褪色,两者的搭配代表着天长地久。金的贵重与琉璃的明澈,又是财富与高贵的象征,精致中不失幽雅,是与佩带者心灵相通的桥梁。     

“HY—1A”卫星海洋水色扫描仪像旋转图像校正处理

"海洋1"号("HY—1A")卫星海洋水色扫描仪由于K镜的失效而出现了像旋现象,对获得的卫星图像质量产生直接影响。基于光学反射矢量理论,分析了多元探测器并行扫描方式下45°扫描镜加K镜的扫描轨迹特征,利用图像之间的相关性,首先自动寻找K镜停转的准确角度,然后根据K镜的停转角度与多元并扫理论对像旋图像进行了校正处理,获得了可用的校正图像。     

加味丹参饮通过PTEN/PI3K/Akt信号通路抑制IRI作用的研究

目的：探讨加味丹参饮预处理通过抑瘤基因/磷脂酰肌醇-3激酶/蛋白激酶B（PTEN/PI3K/Akt）信号通路对大鼠心肌缺血再灌注损伤（IRI）的保护作用及机制。方法：将75只雄性远交群（SD）大鼠随机分为5组：假手术组、模型组、加味丹参饮组、加味丹参饮+PI3K/Akt通路抑制剂（LY294002）组、LY294002组,采用结扎大鼠冠状动脉左前降支30min后再灌注60min的方法制备IRI模型。采用酶联免疫吸附测定（ELISA）法检测各组大鼠心肌肌钙蛋白I（cTnI）表达;取心肌梗死边缘区心肌组织,采用脱氧核糖核苷酸末端转移酶介导的缺口末端标记（TUNEL）法检测心肌凋亡指数,采用免疫组化法检测各组大鼠心肌组织Akt、PTEN的表达。结果：与假手术组比较,模型组cTnI水平显著升高,大鼠心肌凋亡指数增加,PTEN、Akt表达均显著升高（P<0.05）;与模型组比较,加味丹参饮组cTnI水平均显著降低,Akt表达升高,心肌凋亡指数和PETN表达降低（P<0.05）;与加味丹参饮组比较,加入抑制剂后,cTnI水平均明显降低,Akt表达降低,PTEN表达升高（P<0.05）。结论：大鼠心肌缺血再灌注时,加味丹参饮可以通过降低PTEN表达,激活PI3K/Akt信号通路,抑制大鼠心肌细胞的凋亡,从而减轻心肌损伤,保护心肌。     

温度、质量浓度对富氟流体中Hf高温高压水解行为的影响

Hf是一种高场强元素,在地壳中的丰度较低,往往以类质同象的形式进入锆石中。以氟铪酸钾(K_2HfF_6)络合物为研究对象,观察它们在富水热液中的水解程度,进而研究Hf元素在地质过程中的迁移行为。结果表明:K_2HfF_6络合物在热液条件下能发生一定程度的水解反应,总体趋势为络合物的初始质量浓度越低且反应的温度越高,其水解程度越剧烈,络合物的稳定性也就越低;获得了高温高压条件下K_2HfF_6络合物的累积水解平衡常数。同时运用实验模拟的方法,根据提取液中Hf元素含量来推测矿物结晶时富氟流体中Hf元素含量,若以K_2HfF_6络合物最高配位的离子团形迁移时,Hf与F元素之间的质量浓度比值为1.6,据此可以计算成矿流体所需的最小F元素含量。     

地磁活动K指数自动计算FMI方法的改进

将Kp指数与国际地磁学与高空物理学协会(International Association of Geomagnetism and Aeronomy,下文简称IAGA)推荐的FMI方法(V1.0)计算的K值对比分析后发现,二者的差值在中国区域内出现"不同台站之间K1~K8两头离散、K值整体高出K_p约0.5个单位、个别日期S_R计算错误、相邻日期S_R频繁出现跨天台阶"现象.针对这些现象,分析了可能产生的原因,并对原FMI算法进行了四处改进.用改进后的FMI算法计算了全球8个台站、中国5个台站在2003-2005年和2009年共4年的K指数数据,并将计算结果分别与Kp指数以及这些台站用其他方法计算的K值进行一致性比较,发现改进后的计算结果与二者更为接近,说明本文对FMI方法的改进是有效的.     

矿井多极距偶极电剖面法及其应用

论述了矿井多极距偶极电剖面法的井下施工方法与技术,并分析了全空间效应和巷道影响问题,提出了矿井多极距偶极电剖面法资料解释的基本原则。应用实例旨在说明其应用效果。      

贵州耕地质量地球化学调查评价工程成果及其意义

基于广义(C,α,ρ,d)K,θ-凸函数,广义(C,α,ρ,d)K,θ-伪凸函数和广义(C,α,ρ,d)K,θ-拟凸函数等,探讨了涉及这些新广义凸性的一类多目标半无限分式规划的Mond-Weir型对偶,得到了相关的弱对偶定理和强对偶定理,并进行了证明。     

伊利石结晶度及其在低温变质研究中若干问题的讨论

文中介绍与伊利石结晶度相关的伊利石矿物新的定名方案;讨论了伊利石结晶度的结晶学基础与Scherrer方程式的关系;讨论了三个重要的伊利石结晶度指数Weaver、K櫣bler和Weber指数的关系,并介绍推导的Weaver、K櫣bler和Weber指数的理论关系式;评价了衍射仪测量条件对结晶度数值的影响和三套伊利石结晶度标样的作用以及成岩带、变质带与葡萄石-绿纤石相、沸石相、绿纤石-阳起石亚相对比的依据。建议(1)停用绢云母一词;(2)建立可供各实验室使用的具有晶体结构和晶体化学参数和多型参数的伊利石结晶度标样;(3)建议多开展规范的可进行国际对比的低温变质研究,划分出与国际上一致的成岩带和近变质带,不仅利于低温变质作用理论的研究,而且由于成岩带到近变质转变带是重要的煤气油的生成带,也利于中国煤气油资源的勘探与开发,利于国民经济的长远持续发展。     

Study on fluid inclusions and features of ore-forming fluids of Diakha gold deposit,Mali, West Africa

The Diakha gold deposit is located in the southeastern margin of the highly prospective/productive Paleoproterozoic( Birimian) Kédougou-Kéniéba Inlier. Gold mineralization is closely associated with a narrow,sub-vertical,NE-trending shear corridor. The corridor is to the east of a sinistrally reactivated D1 west-dipping fault,which emanated from SMSZ( D2 reverse-sinistral regional structure). The mineralization is hosted by fine-grained sandstone and breccias units associated with a moderate to strong hydrothermal alteration,which is dominated by albitization,carbonization,silicification,hematization,and chloritization. Diakha field data and laboratory analysis suggest the existence of two main stages of hydrothermal mineralization,namely stage I and stage II. Stage I is of a breccias type of mineralization and represents the major gold bearing stage. It isassociated with hematite + calcite + ankerite/dolomite and quartz pervasive alteration,controlled by the predominantly brittle-ductile NNE to NE-shearing structures of the main deformation event D2. Stage II is represented by the second minor hydrothermal episode,showing local quartz-tourmaline and tremolite alteration which is structurally controlled by the dipping S3 cleavage formed during D3 deformation. Petrographic and microthermometric studies of fluid inclusions from quartz veins reveal the presence of early dominant carbonic CO2-pure and aqueous-carbonic CO2-rich( LCO2+ VCO2± H2 O) in stage I. The exclusively aqueous H2 O + Na Cl ± CO2 fluid inclusions( L-type) are observed in stage II. Interpretation shows that the ore-forming fluids originated from a homogeneous H2 O-CO2 fluid during phase separation,with trapping temperatures of 250℃ to 280℃ and low salinity( 6 wt % Na Cl equiv),indicating an estimated trapping pressure for the deposit between 610 to 800 bars.     

Effects of salinity on embryonic and larval development of Chinese mitten crab Eriocheir sinensis(Decapoda: Brachyura) and salinity-induced physiological changes

To investigate the effects of salinity on early development of Chinese mitten crab ( Eriocheir sinensis ), and the salinity tolerance mechanism of embryos, different developmental stages of embryos (gastrula, eyespot and pre-hatching stage), and hatched stage I zoea and megalopa, were exposed to a range of salinities (1, 5, 10, 15 (control), 20, 25, 30, 35 and 40). Hatching, survival and molting were monitored. Effects of 24-hour hypersaline (35) and hyposaline (1) stress on egg diameter, water content, Na +/K +-ATPase (NKA) activity, and crustacean hyperglycemic hormone (CHH) gene mRNA expression in embryos and megalopa, are reported. Embryos are more tolerant of low (≤ 5) than high (≥25) salinities, with optimum ranges for gastrula and pre-hatching stage embryos being 5-20, and for eyespot embryo and stage I zoea, 10-20. Most megalopa can molt to the first juvenile instar by day 5 at salinities between 1 and 40, whereas molting of megalopa stages was delayed at 40. Hypersaline conditions resulted in a loss of moisture, reduction of egg volume, and a signifi cant increase in NKA activity and CHH mRNA expression at some developmental stages. Hyposaline conditions did not affect moisture content or egg volume, but resulted in decreased NKA activity and CHH mRNA expression in embryos. For megalopa stages, NKA activity was significantly upregulated following both hypo- and hypersaline stress. Our results suggest high salinity will inhibit development and hatching of E. sinensis embryos, and low salinity will affect the survival of their stage I zoea. Increased NKA activity in embryos and megalopa stages might indicate a hyporegulation response under hypersaline conditions. These findings provide useful information for spawning ground protection of indigenous E . sinensis and enrich the knowledge of embryonic tolerance mechanisms of hyperregulating crustaceans following osmotic stress.