《京津冀协同航运发展地图集》的制图设计与编制初探

首先简要介绍了《京津冀协同航运发展地图集》的编制背景,然后详细地阐述了图集的总体结构、内容体系、编图资料和编制方法,可为其他同类图集的编制提供参考。     

中国对虾虾苗体表细菌的扫描电镜和病理学观察

从对虾育苗池中任意收集活的虾苗，通过扫描电镜观察发现其体表有大量附生细菌和污着生物，优势菌为弧菌属。这些细菌可分解几丁质，损害甲壳表导并影响蜕皮，为其它生物附着创造了机会。当有病毒感染或其它因素使其抗病力下降时，此类细菌可能乘机进入虾苗繁殖，引发弧菌病，故可称之为条件致病菌。有体表细菌附生的虾苗，肝胰腺内也常发现细小病毒和大量细菌感染，造成肝组织坏死。这是虾苗停止变态、蜕皮和大量死亡的重要原因。     

中国对虾（Penaeuschinensis）核包涵体型杆状病毒装配的电镜观察

９４－９５斫养殖对虾病毒爆发流行期间，对患病中国对虾肝胰上皮细胞和胃肌细胞进行了电镜检测，发现一种核包涵体型杆状病毒（１４０－１６０ｎｍ×２８０－３３０ｎｍ），对其装配机质的超微结构研究表明，核包涵 体型杆状病毒以核内装配为主，部分病毒基质转入胞质进行了装配。     

用电镜观察气功外气效应──体外培养的人体子宫颈癌细胞经气功外气施功的效应

结合细胞培养技术，用电子显微镜，从细胞生物学的角度研究了气功效应。对体外培养的ＨｅＬａ细胞经气功外气施功后的生物效应作了仔细的超微结构观察。     

圆筛藻亚微结构的几种图像显示技术

通过S250MKⅢ型扫描电镜对圆筛藻亚微结构的显示图像,介绍该扫描电镜的几种扫描模式,分析各种图像的特点,对仪器的开发利用和亚微结构的研究、鉴别分析手段作些探索。     

正交设计和方差分析应用于悬浮物和沉积物的EDAX分析条件试验

本文用正交试验和方差分析对悬浮物和沉积物粉末样品的EDAX分析进行了条件试验和数据处理,找出影响试验结果的主要因素和最佳分析条件,提高了分析结果的准确性。     

长牡蛎死因初探

本文对广西北海市海涂养殖的长牡蛎大量死亡的原因作了研究。电镜检测结果表明，在其外套膜、肝脏和中肠组织已吸入与积累了大量的直径为０．１～１．１０μｍ的球状有机化合物，未见微生物病原体感染，故该市海涂长牡蛎大量死亡的原因是其体内积累了大量的球状有机污染物而严重中毒引起的。     

The role of sediments in the phosphorus cycle in Lake Lugano. II. Seasonal and spatial variability of microbiological processes at the sediment-water interface

P, Fe, Mn, and S species were analyzed in water samples from the sediment-water interface collected at four seasonally different times during the course of a year at two sampling sites in the southern basin of Lake Lugano (Lago di Lugano). The results reveal the strong influence of the biogeochemical processes in the sediment on the chemical composition of the lake water above. Consumption of oxygen and nitrate under oxic to microoxic conditions in the water column as well as sequential release of reduced manganese and iron under anoxic conditions was observed as a direct or indirect consequence of microbially mediated degradation of organic matter. The seasonal pattern observed for the release and the retainment of dissolved reduced iron and manganese correlates well with the one for dissolved phosphate. Iron, manganese and phosphorus cycling are coupled tightly in these sediments. Both sediment types act as sinks for hydrogen sulfide and sulfate. An inner-sedimentary sulfur cycle is proposed to couple iron, manganese and phosphorus cycling with the degradation of organic matter. Nutrient cycling at the sediment-water interface might thus be driven by a microbially regulated electron pumping mechanism. The results contribute to a better understanding of the role of sediment processes in the lake's internal phosphorus cycle and its seasonal dynamics.     

Simultaneous operation of opposing reaction mechanisms: The influence of matrix heterogeneity on post-kinematic garnet crystallization in an inverted metamorphic sequence

Metapelites from the inverted Barrovian sequence in the Sikkim Himalaya (northeast India) are shown to be largely continuous with respect to their bulk rock compositions, microstructures and pressure–temperature–time–deformation (P–T–t–D) histories. However, the upper garnet–lower staurolite zone demarcates a region of microstructurally anomalous post-kinematic garnet populations contained within strongly segregated matrices. The different microstructures within samples from this region cannot be attributed to differences in their thermobarometric histories or bulk compositions, but are instead interpreted to represent an otherwise unexposed level of the Daling Group that is now exposed along a post-metamorphic thrust splay. These heterogeneous samples contain several discrete garnet populations that progressively crystallized with increasing P–T. Garnet populations that experienced the most protracted growth now form complex polycrystals that exhibit crystallographically controlled and morphologically irregular interfaces adjacent to micaceous and quartzofeldspathic domains respectively. Electron backscatter diffraction indicates that these polycrystalline garnet structures contain numerous coalesced porphyroblasts that are structurally uncorrelated across their grain boundaries. However, a crystallographically preferred orientation at the polycrystal scale is interpreted to derive from epitaxial crystallization of early-formed garnet porphyroblasts on precursor mica. Later-nucleated porphyroblasts within polycrystals preferentially concentrated towards quartzofeldspathic domains, with the overall nucleation distribution likely controlled by a complex interplay between chemical heterogeneities, strain partitioning and epitaxial crystallization. The subsequent growth of these polycrystals was equally spatially heterogeneous; it was moderated by differences in the efficiency of grain boundary transfer between quartzofeldspathic and micaceous domains that precluded thin section-scale chemical equilibration. In contrast to samples from Sikkim containing more typical porphyroblastic populations in continuous and disseminated matrices, heterogeneous availability of garnet-forming components within this strongly layered matrix is shown to have resulted in grain-scale variations in growth rates and the spatial juxtapositioning of interface-controlled microstructures and locally equilibrated chemical compositions with those that were transport controlled.     

Geological Characteristics and Occurrence of Gold in the Xiling Gold Deposit,Jiaodong Peninsula北大核心CSCD

西岭金矿床是胶东金矿集区内近来新发现的超大型破碎蚀变岩型金矿床(475吨@4.56 g/t),位于著名的三山岛金矿床的东侧。本文在详实的野外地质观察的基础上,系统介绍了西岭金矿床的基础地质特征,并运用光学显微镜和扫描电镜观察,结合电子探针分析,系统研究了西岭金矿床金的赋存状态。西岭金矿床大量金矿物(银金矿和自然金)主要赋存在Ⅱ阶段石英-黄铁矿和Ⅲ阶段灰石英-多金属硫化物脉中。西岭金矿床金矿物主要有晶隙金、裂隙金和包体金三种赋存状态,以晶隙金为主。金的主要载体矿物为黄铁矿,次为石英、黄铜矿和方铅矿等。金矿物粒度大小包括粗粒金、中粒金、细粒金和微粒金,以细粒-微粒为主。金矿物形态有粒状、叶片状、线状、钩状、枝杈状和哑铃状等,以粒状为主。金矿物成分以Au和Ag为主,含微量的Cu、Cr、Fe、Ni、Te、S等元素。金成色为685~831,以银金矿为主,含少量自然金。综合地质和地球化学特征,西岭金矿床为蚀变岩型金矿床,是由早白垩世中温岩浆热液充填-交代形成。