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451.
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Daily rates of gross primary production, net community production and community respiration were determined in spring of 1997
at two stations in a warm streamer off Sanriku, Japan fromin vitro changes in dissolved oxygen. The phytoplankton community was composed of chlorophytes, cryptophytes and prymnesiophytes as
determined by biomarker pigment analysis. Gross production, integrated from the surface to its 1% light level was 52.5 and
80.4 mmol O2 m−2d−1. The difference in gross production is ascribed to variations in photosynthetic activity of the population. Community respiration
was 17.4 and 49.5 mmol O2 m−2d−1, and positive net community production was found within the euphotic zone. The contribution of autotrophic and heterotrophic
respiration to community respiration was estimated on the basis of the observed respiration and the phytoplankton composition.
Heterotrophic respiration was calculated to be highly variable and the observed difference in community respiration was due
to heterotrophic respiration. Heterotrophic respiration was considered to play an important role in the rapid mineralization
of organic materials. 相似文献
454.
单链环状DNA在纳米技术、分子生物学和医药学等领域具有广泛的应用前景,但难以大量制备一直是制约其研究和应用的难题之一。本文针对一种高效大量制备单链环状DNA的方法-逐步添加法,系统地探究了逐步添加法中各主要条件对制备单链环状DNA的影响,确定了逐步添加法中的主要关键条件为:T4DNA连接酶Buffer浓度、单链DNA浓度、添加间隔时间、温度和Splint GC含量。以72nt的核酸链为例,使用逐步添加法将单链环状DNA的制备得率提高至99%,产量与常用的一步法相比提高至4.9倍。本研究为高效、大量制备单链环状DNA提供了指导,为以单链环状DNA为基础的研究奠定了基础。 相似文献
455.
提出一种产生局域空心光束(bottle beam)的新方法,它是在传统的轴棱锥底面上放置一个环形障碍物.平面波入射到带有环形障碍物的轴棱锥底面时,将在轴棱锥产生的最大无衍射距离内形成bottle beam,而在bottle beam的前后仍然保持无衍射贝塞尔光.通过变化障碍物大小及轴棱锥底角实现bottle beam尺寸的控制.利用衍射理论描述了平面波经带有环形障碍物的轴棱锥产生bottle beam的原理,分析和模拟了传输过程中不同位置的截面光强分布及整个过程的三维光强分布,并给出相关的实验结果.研究结 相似文献
456.
Clay mineral diagenesis and quartz cementation in mudstones: The effects of smectite to illite reaction on rock properties 总被引:1,自引:0,他引:1
The Late Cretaceous to Early Tertiary sequence of the Vøring and Møre Basins from the Norwegian Sea has been examined with respect to mineralogy based on 319 cutting samples from five wells. A clear relationship between mineralogy and well log data is demonstrated. A significant change with respect to velocity, porosity and density occurs within the depth interval corresponding to 80–90 °C. At shallow depths/temperatures (<2.0 km/70 °C), compaction is mainly mechanical and the physical properties are similar to what has been measured by experimental compaction of mudstones. At greater depths, however, the log derived velocities and densities are higher than those produced by experimental compaction indicating significant chemical compaction. XRD analyses show a progressive alteration of smectite to illite (S–I) within this depth/temperature interval which results in the release of significant amounts of silica into solution. Detrital silt and fine-grained quartz showed no secondary quartz overgrowths. These grains are isolated within a clay matrix and surrounded by clay minerals, thus limiting the available surface area and pore space for quartz overgrowths. Chemical analyses (XRF) indicate that silica is conserved within this depth interval, and the amount released from S–I alteration was locally precipitated. Field emission gun-scanning electron microscopy (FEG-SEM) and cathode luminescence (CL) identified authigenic micro-crystalline quartz cement within the clay matrix at temperatures above ∼85 °C. This is accompanied by an increase in velocity and density indicating that the S–I reaction and the precipitation of authigenic quartz caused a significant change in the rock stiffness. 相似文献
457.
Characterisation of a Campanian deep-sea fan system in the Norwegian Sea by means of ichnofabrics 总被引:1,自引:0,他引:1
Ichnofabrics are applied in concert with sedimentological data to discriminate sub-environments within a Campanian deep-sea fan system in the Norwegian Sea. Seven ichnofabric types are recognised in the studied cores, which correspond to specific architectural elements of the fan system, including amalgamated channels, lobate sand sheets, proximal and distal overbank, fan fringe, and hemipelagic basin plain environments. A unique observation is an ultra-deep Chondrites ichnofabric, interpreted to result from the activity of a chemosymbiotic tracemaker, possibly utilising hydrothermal vents or hydrocarbon seeps in the near vicinity of an active rift system. Mapping and inter-well correlation of ichnofabrics allow a better control of lateral and vertical facies changes, which are important to exploration and production strategies. This study demonstrates that ichnofabric analysis is proving to be a valuable tool for the characterisation and prediction of reservoir quality, the recognition of potential flow barriers and prediction of lateral depositional trends in deep-sea fan deposits. 相似文献
458.
459.
通过磁学手段以树木年轮为研究对象,通过多参数磁学研究探讨钢铁厂周围环境污染的历史.研究表明:钢铁厂附近树木年轮样品中磁性矿物为准单畴(其中颗粒偏向于多畴)的磁铁矿,磁性矿物形状各异,粒径大小不一;样品中磁铁矿的含量随年份的不同差异很大;通过树木不同方向上磁性参数尤其是饱和等温剩磁(SIRM)值的差异以及扫描电镜(SEM)和X射线能谱(EDX)分析,发现树木木质部中的磁性颗粒来自于树皮,即大气中颗粒被树皮和树叶表面吸附后,在树木的生长季节通过树皮进入形成层的木质部细胞,然后通过木质化作用被固定在当年生长的树木木质部木材中;另外,朝向钢铁厂方向的树干年轮钻芯样品SIRM值与对应年份钢铁厂年生产量之间高度相关,磁性颗粒在年轮之间不存在横向迁移,树干年轮钻芯的磁性参数(SIRM和部分磁滞参数)可指示该区大气环境污染的历史;污染树木钻芯样品的SIRM随时间的变化曲线说明该研究区大气污染日益严重. 相似文献
460.
辽宁永宁地区发育一套闪长质火山岩,该岩石中曾选获金刚石及其指示矿物,因此成为辽宁省金刚石第Ⅳ成矿带。通过对该岩石矿物组成及其显微结构构造特征研究,表明:(1)闪长质岩石中的斑晶斜长石具有环带结构;(2)橄榄石及金云母具有多世代性,且目估橄榄石+金云母含量在10%以上,局部更为富集;(3)出现“橄榄石+金云母+石榴石”与“斜长石+辉石+角闪石”不平衡的矿物组合;(4)发现橄榄石有碎斑结构和金伯利岩角砾。初步认为,永宁地区的闪长质岩浆在上升过程中捕获了早先已形成的金伯利岩并与之发生熔融混合作用,金刚石来自于深部的金伯利岩。这一认识对该地区寻找金刚石原生矿具有启示意义。 相似文献