文蛤副溶血弧菌间接 ELISA检测技术的研究

从患病文蛤组织内分离出一株细菌,回归感染试验证明是文蛤的致病菌,经鉴定为副溶血弧菌,灭活后(56 ℃,1 h)制成菌苗,用该菌苗制备兔抗血清,以辣根过氧化酶标记的羊抗兔血清(HRP-IgG)为酶标二抗,对副溶血弧菌进行间接ELISA快速检测.结果表明:应用间接 ELISA 技术检测副溶血弧菌具有较高的灵敏度,其最低检测极限为 1 × 105 cfu / mL.患病文蛤内脏团中副溶血弧菌的检出率为 80 %,无病症带菌文蛤中的检出率为 15 %,海水中副溶血弧菌的浓度低于最低检测极限.表明间接 ELISA检测法不仅可以用于发病文蛤的快速检测,而且能够检测出无病症的带菌的文蛤,为有效预防副溶血弧菌病的暴发提供了检测手段.     

大黄鱼病原菌——溶藻弧菌的EuSA快速检测研究

以灭活溶藻弧菌(0.05%甲醛,30℃,8h)制成菌苗,注射免疫实验兔获得抗血清.该抗血清经吸附后与副溶血弧菌、河流弧菌等10株对照菌株无交叉反应.用该抗血清进行溶藻弧菌ELISA检测,其最低检测极限为97000cfu/ml.将该方法应用于养殖现场,检测结果为海水中溶藻弧菌浓度均低于最低检测限、外观健康大黄鱼肝脏中溶藻弧菌的阳性检出率为20%、患病大黄鱼的阳性检出率为80%,表明ELISA法不仅可以用于诊断大黄鱼的溶藻弧菌病,也可以检测无病症带菌大黄鱼.     

大黄鱼病原菌──溶藻弧菌的ELISA快速检测研究

以灭活溶藻弧菌（0.05%甲醛，30℃,8h）制成菌苗，注射免疫实验兔获得抗血清。该抗血清经吸附后与副溶血弧菌、河流弧菌等10株对照菌株无交叉反应，用该抗血清进行溶藻水中溶藻弧菌浓度均低于最低检测限、外观健康大黄鱼肝脏中溶藻弧菌的阳性检出率为20%、患病大黄鱼的阳性检出率为80%，表明ELISA法不仅可以用于诊断大黄鱼的溶藻弧菌病，也可能检测无病症带菌大黄鱼。     

大黄鱼病原副溶血弧菌单克隆抗体制备及其应用

用甲醛灭活副溶血弧菌(Vibrio parahaemolyticus)和溶藻弧菌(V.alginolyticus)制成免疫原免疫BALB/c小鼠,利用淋巴细胞杂交瘤技术,获得1株特异的针对副溶血弧菌的单克隆抗体,命名为D6F3H5。腹水及培养上清液抗体的ELISA效价分别为:1∶5 120和1∶1 280,该单克隆抗体与其它细菌没有明显的交叉反应。利用该单克隆抗体和兔抗副溶血弧菌多克隆抗体,建立了检测副溶血弧菌的双抗体夹心ELISA方法。该方法对副溶血弧菌的最小检出量为5×104个/mL。用双抗体夹心ELISA检测大黄鱼(Pseudosciaena crocea)样品,14尾患病大黄鱼中有11尾检出副溶血弧菌,而10尾健康大黄鱼都没有检出副溶血弧菌。由此可见,本试验制备的高特异性的抗副溶血弧菌单克隆抗体,可以用于患病大黄鱼副溶血弧菌的快速诊断。     

副溶血弧菌胶体金快速检测试纸的研制及应用

副溶血弧菌(Vibrio parahaemolyticus)是海水养殖动物弧菌病的主要病原菌之一。为实现对该菌的现场快速检测,本文以制备的兔抗副溶血弧菌多克隆抗体作为金标抗体,提取副溶血弧菌的外膜蛋白、鞭毛蛋白、胞外产物和全菌蛋白,以不同浓度的4种抗原蛋白作为4条检测线(T1~T4),特别在T4线设置全菌蛋白,基于竞争免疫层析原理研制出副溶血弧菌胶体金快速检测试纸。使用该试纸检测了副溶血弧菌(V.parahaemolyticus)、鳗弧菌(V.anguillarum)、溶藻弧菌(V.alginolyticus)、哈维氏弧菌(V.harveyi)和鱼肠道弧菌(V.ichthyoenteri),检测结果表明其能够准确鉴别副溶血弧菌感染,排除其他菌的交叉反应干扰。副溶血弧菌快速检测试纸的最低检测限为5×105 cfu·mL^-1,感染副溶血弧菌的牙鲆组织的检测结果与ELISA结果一致。本文研制的试纸具有较高的特异性与准确性且操作简单,为现场快速检测副溶血弧菌提供了有力工具。     

大黄鱼溶藻弧菌LPS的间接ELISA检测

用酚 水法从20dm3溶藻弧菌培养液中分离得到脂多糖(LPS)97.6mg,以0.5mg cm3的LPS溶液通过耳缘静脉注射免疫实验兔,经过3次加强注射后从颈动脉放血制备抗血清.该抗血清的效价为1∶2560,对副溶血弧菌等10株细菌的交叉反应效价都较低.用免疫吸附过滤法去除血清中的非特异性成分.用吸附后的抗血清进行溶藻弧菌间接ELISA检测,其检测限为97×104个 cm3.以ELISA进行大黄鱼体内溶藻弧菌检测.结果表明:用LPS抗血清可以较为灵敏地检测大黄鱼体内的溶藻弧菌,该方法不仅可以用于诊断大黄鱼的溶藻弧菌病,也可以检测无病症带菌大黄鱼.     

溶藻弧菌的间接荧光抗体快速检测

建立了大黄鱼病原溶藻弧菌的间接荧光抗体检测方法，溶藻弧菌的特异性抗血清由新西兰兔制备，试管凝集法测定抗血清及交叉反应效价，吸附离心法去除交叉反应，荧光抗体为异硫氰酸荧光素标记的羊抗兔免疫球蛋白，现场检测对具典型弧菌病表症大黄鱼病原检出率为100％，表观健康大黄鱼病原检出率为30％，养殖海水检测结果均为阴性，结果表明，间接荧光抗体检测法不仅可以用于已感染发病大黄鱼的快速检测，而且还能用于已感染未发病大黄鱼的检测。     

检测海洋弧菌的酶联免疫吸附试验研究

研究建立中国对虾病原菌┐副溶血弧菌（Ｖｉｂｒｉｏｐａｒａｈａｅｍｏｌｙｔｉｃｕｓ）的间接酶联免疫吸附试验（ＥＬＩＳＡ）快速检测技术。间接ＥＬＩＳＡ技术中的副溶血弧菌的特异抗血清由家兔制备，羊抗兔ＩｇＧ用碱性磷酸酶标记，酶的底物为对磷酸基硝基苯。将该技术标准化后，测定了抗血清与１３株其它副溶血弧菌菌株及２９株其它弧菌标准菌株的交叉反应，并进行了苗期对虾样品中副溶血弧菌的检测     

间接ELISA技术在病原性鳗弧菌SMP1快速检测中的应用

以大菱鲆(Scophthalmus maximus)出血症的病原菌——鳗弧菌(Vibrio anguillarum)SMP1为抗原,制备兔抗血清,测定了抗血清的工作浓度和对抗原的特异性,建立了在大菱鲆肝肾组织中检测SMP1的间接ELISA方法。SMP1人工感染大菱鲆,用建立的间接ELISA对大菱鲆肾脏和肝脏进行检测,结果肾脏的阳性检出率为87.7%,肝脏的阳性检出率为90%。该方法的建立有助于快速准确地鉴定由SMP1引起的大菱鲆疾病。     

中国对虾弧菌病的间接荧光抗体诊断技术研究

于１９９４年８月－１９９５年５建立中国对虾病原菌－副溶血弧菌的间接荧光抗体检测技术，其中副溶血弧菌的特异抗血清由家兔制备，羊抗兔免疫球蛋白用异硫氰酸荧光素标记，并以罗丹明标占血清白蛋白为背影染色。     

Microbial Biomass and Organic Nutrients in the Deep-Sea Sediments of the Central Indian Ocean Basin

In order to assess the impact of deep-sea mining on the in situ benthic life, we measured the microbial standing stock and concentration of organic nutrients in the deep-sea sediments of the Central Indian Ocean Basin in the Indian pioneer area. Sediments were collected using box core and grab samples during September 1996. The total bacterial numbers ranged from 10 10 -10 11 cells per g -1 dry weight sediment. There was a marginal decrease in the number of bacteria from surface to 30 cm depth, though the subsurface section registered a higher number than did the surface. The highest numbers were encountered at depths of 4-8 cm. The retrievable number of bacteria were two orders less in comparison with the direct total counts of bacteria. An almost homogeneous distribution of bacteria, total organic carbon, living biomass, and lipids throughout the depth of cores indicates active microbial and benthic processes in the deep sea sediments. On the other hand, a uniform distribution of total counts of bacteria, carbohydrates, and total organic carbon in all the cores indicates their stable nature and suggests that they can serve as useful parameters for long-term monitoring of the area after the benthic disturbance. Further studies on temporal variability in this region would not only verify the observed norms of distribution of these variables but would also help to understand restabilization processes after the simulated benthic disturbance.     

A Review of Some Environmental Issues Affecting Marine Mining

This article reviews information recently available from existing marine and coastal mining for responses to environmental issues affecting marine mining at different depths. It is particularly but not exclusively concerned with those issues affecting seabed biodiversity impact and recovery. Much information has been gathered in the past 10 years from shallow mining operations for construction aggregate, diamonds, and gold, from coastal mines discharging tailings to shallow and deep water, and from experimental deep mining tests. The responses to issues identified are summarized in a series of eight tables intended to facilitate site-specific consideration. Since impacts can spread widely in the surface mixing layer SML, and can affect the biologically productive euphotic zone, the main issues considered arise from the depth of mining relative to the SML of the sea. Where mining is below the SML, the issue is whether it is environmentally better to bring the extraction products to the surface vessel for processing (and waste discharge), or to process the extraction products as much as possible on the seabed. Responses to the issues need to be sitespecific, and dependent on adequate preoperational environmental impact and recovery prediction. For deep tailings disposal from a surface vessel, there are four important environmental unknowns: (1) the possible growth of "marine snow" (bacterial flocs) utilizing the enormous quantities of fine tailings particles (hundreds or thousands of metric tons per day) as nuclei for growth, (2) the possibility that local keystone plankton and nekton species may migrate diurnally down to and beyond the depth of deep discharge and hence be subjected to tailings impact at depth, (3) the burrow-up capability of deep benthos and their ability to survive high rates of tailings deposition, and (4) the pattern and rate of dispersion of a tailings density current through the deep water column from discharge point to seabed. Actions to obtain relevant information in general and site-specifically are suggested.     

Increased Particle Fluxes at the INDEX Site Attributable to Simulated Benthic Disturbance

Particle fluxes were measured 7 m above the sea bottom during the predisturbance, disturbance, and postdisturbance periods by using time series sediment traps attached to seven deep-sea moorings deployed in the INDEX experiment site in the Central Indian Basin. The predisturbance particle fluxes varied between 22.3 to 55.1 mg m -2 day -1 . Increased and variable particle fluxes were recorded by the sediment traps during the disturbance period. The increase observed was 0.5 to 4 times more than the background predisturbance fluxes. The increases in particle fluxes (~4 times) recorded by the sediment trap located in the southwestern direction (DMS-1) were the greatest, which could be the result of preferential movement of resuspended particles generated during the deep-sea benthic disturbance along the general current direction prevailing in this area during the experimental period. Also, the traps located closer to the disturbance area recorded greater fluxes than did the traps far away, across the Deep Sea Sediment Resuspension System path. This variability in recorded particle fluxes by the traps around the disturbance area clearly indicates that physical characteristics such as grain size and density of the resuspended particles produced during the disturbance had an important effect on particle movement. The postdisturbance measurements during ~5 days showed a reduction in particle fluxes of ~50%, indicating rapid particle settlement.     

Assessing the Validity of Seismo-Acoustic Predictor Equations for Obtaining Seabed and Sub-Surface Sediment Physical Properties

The interdependence between the seismo-acoustic properties of a marine sediment and its geotechnical/physical parameters has been known for many years, and it has been postulated that this should allow the extraction of geotechnical information from seismic data. Though in the literature many correlations have been published for the surficial layer, there is a lack of information for greater sediment depths. In this article, a desktop study on a synthetic seafloor model illustrates how the application of published near-surface prediction equations to subsurface sediments (up to several tens of meters burial depth) can lead to spurious predictions. To test this further, acoustic and geotechnical properties were measured on a number of sediment core samples, some of which were subjected to loading in acoustically-equipped consolidation cells (oedometers) to simulate greater burial depth conditions. For low effective pressures (representing small burial depths extending to around 10 meters subsurface), the general applicability of established relationships was confirmed: the prediction of porosity, bulk density, and mean grain size from acoustic velocity and impedance appears generally possible for the investigated sedimentary environments. As effective pressure increases through, the observed relationships deviate more and more from the established ones for the near-surface area. For the samples tested in this study, in some instances increasing pressure even resulted in decreasing velocities. There are several possible explanations for this abnormal behavior, including the presence of gas, overconsolidation, or bimodal grain size distribution. The results indicate that an appropriate depth correction must be introduced into the published prediction equations in order to obtain reliable estimates of physical sediment properties for greater subsurface depths.     

海上大直径钢管桩打桩过程中桩周土强度弱化研究

海上大直径钢管桩打桩过程中,桩周土体受到强烈扰动而发生强度弱化,掌握桩周土体强度弱化规律对于准确预测打桩过程、保证工程安全具有重要意义。为研究土体强度弱化规律,开展了环剪试验模拟打桩对桩周土体的扰动,测试土体强度随剪切速率的变化规律,建立了描述土体强度弱化规律的拟合公式,引入到打桩分析软件中。研究结果表明：土体的强度折减程度不仅与土体本身的性质有关还受到土体的埋深和剪切速率的影响,埋深越深土体强度折减程度越低,剪切速率越高土体强度折减越高,在打桩分析中可采用这里推荐的线性折减方法来模拟不同深度处土体强度的折减规律。     

Geoacoustic Inversion via Genetic Algorithm and Its Application to Manganese Sediment Identification

An acoustic inversion method using a wide-band signal and two near field receivers is proposed and applied to multiple layered seabed models including a manganese sediment. The inversion problem can be formulated into a probabilistic model comprised of signals, a forward model, and additive noise. The forward model simulates wide-band signals, such as chirp signals, and is chosen to be the source-waveletconvolution plane wave modeling method. The wavelet matching technique, using weighted least-squares fitting, estimates the sediment sound-speed and thickness on which determination of the possible numerical ranges for a priori uniform distribution is based. The genetic algorithm is applied to a global optimization problem to find a maximum a posteriori solution for determined a priori search space. Here the object function is defined by an L 2 norm of the difference between measured and modeled signals. Not only the marginal pdf but also its statistics are calculated by numerical evaluation of integrals using the samples selected during importance sampling process of the genetic algorithm.     

Determination of In Situ Sediment Shear Strength from Advanced Piston Corer Pullout Forces

The advanced piston corer (APC) has been used by the Ocean Drilling Program since 1985 for recovering soft sediments from the ocean floor. The pullout force measured on extracting the core barrel from the sediment is shown to correlate with the average shear strength of the sediment core measured in the ship's laboratory. A simple rule of thumb is derived relating the shear strength of the sediment to the pullout force. Multiple APC holes at individual sites allow the consistency of the pullout measurements to be assessed. The effects of different operational procedures during APC coring are also explored. Although generally applicable, the correlation between pullout force and laboratory measurements of shear strength breaks down for some APC holes, possibly because of the disturbance of some sediment types during the APC coring process. A better understanding of the physical process of APC coring, and its effect on the properties of the sediment both inside and immediately outside the core barrel, would indicate what confidence can be put on the measurement of pullout force as a way of evaluating the in situ shear strength of deep sea sediments.     

Interannual Sea Level Variations and Annual Tides in the Northwestern Pacific

Specific properties of the interannual sea level variations and annual tides in the Northwestern Pacific were studied. Several tide stations were monitored. The monthly mean sea level for the year of 1995 was analyzed at each tide station. A seismic event in 1995, some tectonic activity around the subject area, and the Kuroshio (the oceanic western boundary current) may possibly contaminate results which would have occurred from the astronomical annual tide alone.     

《Acta Oceanologica Sinica》Vol. 33(2014) contents

<正>~~