Tissue-specific bioaccumulation and oxidative stress responses in juvenile Japanese flounder (Paralichthys olivaceus) exposed to mercury

To understand mercury (Hg) toxicity in marine fish, we measured Hg accumulation in juvenile Japanese flounder (Paralichthys olivaceus) and assessed the effects on growth and antioxidant responses. After Hg exposure (control, 5, 40, and 160 μg/L Hg) for 28 d, fish growth was significantly reduced. The accumulation of Hg in fish was dose-dependent and tissue-specific, with the maximum accumulation in kidney and liver, followed by gills, bone, and muscle. Different antioxidants responded differently to Hg exposure to cope with the induction of lipid peroxidation (LPO), which was also tissue-specific and dosedependent. As Hg concentration increased, superoxide dismutase (SOD) and catalase (CAT) activities increased significantly, whereas glutathione S-transferase (GST) activity and glutathione (GSH) levels decreased significantly in the gills. SOD and glutathione peroxidase (GPx) activities and the GSH level increased significantly in the liver. SOD activity and GSH levels increased significantly, but CAT activity decreased significantly with an increase in Hg concentration in the kidney. LPO was induced significantly by elevated Hg in the gills and kidney but was least affected in the liver. Therefore, oxidative stress biomarkers in gills were more sensitive than those in the liver and kidney to Hg exposure. Thus, the gills have potential as bioindicators for evaluating Hg toxicity in juvenile flounder.     

湘西—鄂西地区铅锌矿的大范围低温流体成矿作用研究

对湘西—鄂西地区狮子山、李梅、耐子堡、茶田、打狗洞、董家河、唐家寨、冰洞山、凹子岗等典型铅锌矿床中闪 锌矿、方解石、白云石及石英等矿物进行了流体包裹体均一温度、盐度、流体包裹体气相成分、流体包裹体群体液相成分 测定,结果表明:成矿流体温度主要分布在 80~230 °C,总盐度一般>15%,密度多>1g/cm3,成矿压力为 223×105~777× 105 Pa,是以钠和钙氯化物为主的高浓度溶液,属于低温度、高盐度、高密度的地下热卤水性质的含矿热水溶液。成矿流体 阳离子成分主要为 Cl-, Na+, Ca2+, K+, Mg2+,流体包裹体氢氧同位素组成表明成矿流体来源与建造水有关,后期可能有雨水和 少量变质水的渗入。矿物流体包裹体中含有机质,流体包裹体气相成分中 CH4 普遍存在,表明成矿与有机质相关,处在控 矿构造内容矿层中的有机质使矿床中的硫酸盐硫还原为还原硫,促使成矿流体中的铅、锌沉淀形成矿床。相邻的低温成矿 域川滇黔地区典型铅锌矿床成矿温度约为 90~280°C,湘西—鄂西地区铅锌矿与川滇黔铅锌矿相比,具有相同的低温成矿特 征,矿床类型均为 MVT 型,两者可能受控于相同的动力学背景。     

交通工程规划核实测量与管道检测的关键技术

随着“多测合一”的推行,市政交通工程规划核实测量与排水管道检测成果已成为规划管理、建设、施工、养护及馆藏等单位的必备材料。本文通过工程实践,阐述项目的工作内容、技术流程等,并对成果数据进行精度验证,同时,介绍了项目实施中应注意的问题。     

四阵元微带天线阵列试制与测试

将阵列天线放置于射电望远镜焦平面处,结合波束合成网络,可以同时观测一片天区,实现更大的视场覆盖。由于需要对各个阵元的幅度和相位进行调控,阵列天线实际就是一个小型相控阵,因此在做阵列设计时,除了需要结合反射面焦面场分布及望远镜拟实现的视场以外,阵列自身的性能验证可以参照传统相控阵进行。设计并加工了工作在1.27 GHz的2×2矩形排布的微带贴片天线阵列,阵元间距为0.7倍波长。经实测,各端口S11均在-10 dB以下,4阵元合成后波束增益为12.54 dBi,通过为对应阵元添加理论偏移30^°的延时线,实测阵列的波束扫描角度为28.3^°。上述实测数据与仿真结果相比虽略有差异,这和阵列加工及馈电端口焊接有关,但相关工作为之后更多阵元的阵列天线设计、研制及测试积累了经验,尤其对性能验证具有较高的指导意义。     

Otolith shape analysis for stock discrimination of two Collichthys genus croaker(Pieces: Sciaenidae,) from the northern Chinese coast

The otolith morphology of two croaker species(C ollichthys lucidus and C ollichthys niveatus) from three areas(Liaodong Bay, LD; Huanghe(Yellow) River estuary, HRE; Jiaozhou Bay, JZ) along the northern Chinese coast were investigated for species identifi cation and stock discrimination. The otolith contour shape described by elliptic Fourier coefficients(EFC) were analysed using principal components analysis(PCA) and stepwise canonical discriminant analysis(CDA) to identify species and stocks. The two species were well dif ferentiated, with an overall classifi cation success rate of 97.8%. And variations in the otolith shapes were significant enough to discriminate among the three geographical samples of C. lucidus(67.7%) or C. niveatus(65.2%). Relatively high mis-assignment occurred between the geographically adjacent LD and HRE samples, which implied that individual mixing may exist between the two samples. This study yielded information complementary to that derived from genetic studies and provided information for assessing the stock structure of C. lucidus and C. niveatus in the Bohai Sea and the Yellow Sea.     

湖北凹子岗锌矿床流体包裹体研究

凹子岗锌矿床位于鄂西湘西铅锌多金属成矿区带的黄陵-神农架找矿远景区之黄陵背斜东部,该成矿区带是中国地质调查局确定的全国十六处重点矿产资源调查评价地区之一。凹子岗锌矿床含矿层位为震旦系上统灯影组二段中部的一套角砾状白云岩,该套白云岩在黄陵背斜周缘广泛分布,具有良好的找矿前景。     

本溪—集安地区三维地质结构重磁电综合解释

本溪—集安地区的三维地质填图对于该区深部找矿具有重要意义。本文通过对该区5条实测重磁电剖面的数据处理以及对实测物性标本数据的整理分析,结合该区已有地质、地球物理等其它资料,对5条剖面进行了综合地质地球物理解释,初步得到了研究区的三维地质结构。     

车载激光雷达点云与全景影像的自动配准

针对激光雷达点云数据缺乏纹理信息的问题,该文提出一种基于互信息的车载激光雷达点云与全景影像配准方法。该方法使用统一的球面全景成像模型,引入互信息作为相似性测度,将车载激光雷达点云生成的深度图与信息提取后的全景影像进行配准,实现配准参数的自动、高精度解算。同时,对车载激光雷达点云与全景影像配准的精度进行评定与分析。实验结果表明,车载点云与全景影像的配准方案是可行的,具有较高的配准精度。     

湘西花垣铅锌矿田成矿物质来源的C、O、H、S、Pb、Sr同位素制约

花垣地区铅锌矿床有望成为中国最大的铅锌矿床,也是铅锌矿资源储量超过千万吨的世界级超大型矿床之一。文章通过碳、氧、氢、硫、铅和锶同位素地球化学特征研究,探讨了成矿流体和成矿金属来源。测试结果显示,花垣地区铅锌矿床主成矿期方解石样品的δ~(13) CPDB值范围为-2.71‰~1.21‰,δ~(18) OSMOW值范围为16.09‰~22.48‰,该地区铅锌矿床成矿流体中的碳主要来源于海相碳酸盐岩的溶解作用。花垣矿区的围岩的δ~(13) CPDB值范围为0.29‰~1.05‰,δ~(18) OSMOW值范围为21.33‰~23.89‰,为沉积成因海相碳酸盐岩。矿石中硫化物的δ~(34) S变化于24.93‰~34.66‰之间,重晶石δ~(34) S为32.78‰~34.22‰,表明还原硫主要来自地层中海相硫酸盐的还原。矿石硫化物的铅同位素组成均一,~(206)Pb/~(204)Pb、~(207)Pb/~(204)Pb和~(208)Pb/~(204)Pb分别为17.999~18.919、15.554~15.798和38.088~38.576,铅模式年龄为437~534Ma,成矿金属可能主要来源于奥陶系—寒武系。方解石和闪锌矿样品中流体的δD_(SMOW)变化于-91.1‰~-15‰之间,δ~(18) Ofluid变化范围为-4.1‰~8.75‰,矿床成矿流体的主要来源是建造水和大气降水。成矿流体与围岩的水-岩反应是导致该区铅锌矿床中方解石和闪锌矿矿物沉淀结晶的主要机制。成矿流体~(87)Sr/~(86)Sr为0.70906~0.71022,高于赋矿围岩寒武系清虚洞组灰岩锶同位素比值0.70886~0.70921,表明成矿流体流经了清虚洞组下伏地层,并与其中具有高锶同位素比值的碎屑岩、页岩和泥岩等进行了水岩反应及同位素交换。