共查询到20条相似文献，搜索用时 46 毫秒
1.
采用气相色谱法对渤海海上6个不同区块、7个平台的8口油井原油中正构烷烃组分及姥鲛烷植烷进行了定性定量分析,通过原始指纹谱图、正构烷烃组分及姥鲛炕植烷浓度分布比较和特征比值比较对原油进行了鉴别.结果表明,不同区块的原油指纹信息不尽相同,即使同一平台不同油井所产的原油指纹也存在一定差异,采用气相色谱法进行分析可对其进行鉴别.原油的风化对特征比值影响较小,可利用其进行风化油样的鉴别.为确保鉴别的准确性,分析过程中必须实施严格质量控制措施. 相似文献
2.
对两种原油进行混合配比实验,将混合后油样置于人工气候箱进行风化模拟实验,采用气相色谱质谱联用仪(GC-MS)检测风化样品中的生物标志化合物,短期风化作用对混合溢油的油指纹、生物标志化合物诊断指标等的影响。结果表明,混合溢油的正构烷烃总质量变化与单一原油油品的变化规律相近,即前期风化较快,质量减损较多,而后期风化趋缓,不同混合比例的溢油表现差异不明显。常用于短期风化的诊断比值对各混合油样的风化具有指示意义,但难以定性鉴别油品是否发生混合。重复性限法检验只能判定短期风化过程前后的油样为同一油源,而难以反映油样是否为混合油源的特征,各诊断比值的RSD%值较大可能是混合溢油的一个表现。 相似文献
3.
以2种原油和3种溢油分散剂的混合物为对象,借助SPSS统计分析软件,采用主成分分析法研究基于诊断比值的原油分类,旨在判别分散剂对原油的影响。KOM值近似等于0.6、Bartlett球形度检验对应概率P值为0,表明原始数据适合做主成分分析;前两个主成分F1和F2的特征值均大于1,累积贡献率为81.433%,多变量可降至2维。根据F1和F2表达式得到主成分分类图可知:两种原油中加入不同分散剂后还可在图中大致区分,富肯-2号分散剂对两种原油几乎没有影响,GM-2分散剂对渤海原油分类程度有一定影响,但对华北原油却有较大影响;海鸥4号分散剂对两种原油分类程度都有影响。结果表明:主成分分析法可用于添加分散剂的溢油分类辨别,研究发现一些分散剂对原油影响较小,而某些分散剂对原油有复杂的影响。因此,溢油指纹鉴定需考虑分散剂的影响。 相似文献
4.
5.
将胜利和塔西两种原油以不同比例混合后置于人工气候箱进行风化模拟实验,采用气相色谱质谱联用仪(GC-MS)检测风化样品中的生物标志化合物,探讨和揭示短期风化作用对混合溢油常用的甾萜类和多环芳烃诊断指标的影响。结果表明经过15d的短期风化,在混源比例大于10%时,各系列混合油样的甾萜类生物标志物诊断指标与单一油品的相关诊断比值的差异性和混源油品比例值呈明显正相关。各系列混合油样中的常用萘及烷基萘等指标不适宜作为短期溢油来源鉴别的指标,但可以作为溢油是否发生混合的间接判定指标。根据常用的多环芳烃相关诊断指标,可将各系列油样的短期风化模式依据混源油品中塔西油田原油所占比例大致分为3类(20%~50%、10%和0%)。多环芳烃系列诊断指标的相对标准偏差(RSD%)与混源油品比例有关,混源塔西油样的比例越高,PAHs系列指标的RSD%越大,稳定性越差。 相似文献
6.
运用单因子方差分析、主成分分析、聚类分析3种方法,对大连、威海、青岛、嵊泗和南麂5个地区的马粪海胆(Hemicentrotus pulcherrimus)群体(125只)的13个特征进行了比较分析。单因子方差分析结果显示,大连、威海、青岛地区的马粪海胆样品13组数据特征比值参数与另外2个地区的均差异显著(P0.05);主成分分析结果显示,贡献率最大的3种主成份的累计贡献率为75.599%;聚类分析结果显示,大连、威海和青岛地区马粪海胆聚为一支,南麂地区的马粪海胆与嵊泗地区的聚为一支;根据Mayr等提出的75%原则,大连、威海、青岛地区的马粪海胆和南麂、嵊泗地区的马粪海胆的形态差异属种内不同群体间的差异,未到亚种水平。 相似文献
7.
为探明珠江口黑鲷海捕苗种与人工繁殖苗种间的形态差异,作者采用3种多元统计分析和方差分析方法,对采集自珠江口两岸的海捕黑鲷(Acanthopagrusschlegelii)苗种与2个繁殖场的人工繁殖苗种进行形态差异比较,比较了不同样品组的外部形态特征差异。可量性状主成分分析结果表明,前2项主成分的累计贡献率为89.90%,聚类分析结果表明汕头苗场(ST)样品组与另外3个样品组距离最远,判别分析结果同样显示以对该样品组判别准确率最高;可数性状单因素方差分析结果表明,样品组间背鳍鳍条数、鳃耙数、椎骨数存在显著性差异(P0.05)。主成分分析、聚类分析、判别分析和单因素方差分析从不同角度反映了样品组间的形态差异,各分析方法获得结论基本类似,相互印证。该研究结果显示,采集自不同繁殖场的黑鲷苗种与珠江口海域野生苗种存在一定的形态差异,但没有证据显示这种差异已导致黑鲷野生和养殖群体间明显的形态分化。 相似文献
8.
石油污染来源的鉴别主要是借助于石油的性质及其组成的特点，以其固有成分进行直接的比较(passive tagging)，或是以其包含的一些可鉴别标记物进行鉴别(active tagging)。石油的特性和化学分析在石油工业中早已做过详细的研究。但是，石油工业以及海上石油运输漏泄在海洋环境中的石油受到各种因素的影响，诸如溶解、蒸发、阳光曝晒、氧化以及生物降解作用等等，都不可避免地导致石油成份的改变。常规的物性测定与石油成份的分析,作为对环境样品的鉴别(fingerprint)就不起作用了。因此，石油污染来源的鉴别应当依据那些既是石油所具有的特性，而在环境诸因素的影响下又不易改变的参数。如石油的残留部分的气液色谱图，镍、钒的含量及其比值，碳、硫同位素含量及其比值的对比等，均可作为石抽污染来源鉴别的参数。
E.R.Adlard研究了石油的正构烷烃气液色谱的FID(氢火焰离子鉴定器)色谱图和FPD(火焰光度鉴定器)有机硫色谱图，用于石油污染来源的鉴别。M. E. Garze应用气液色谱FID，FPD 相结合的方法分析环境油样，直接比较其色谱图，并对比其典型的相应峰强度比值以鉴别环境的污染油样。最近，Alanp Bentz对环境中溢油的鉴别及使用的各种方法作了较为全面的评述。并对石油在环境中的风化影响，萤光光谱在石油天然萤光成份分析中的应用，以及气液色谱、薄层色谱、红外光谱、质谱等分析手段应用于石油污染来源鉴别，亦作了论述。
对于用来鉴别海洋环境中溢袖来源的各项参数，实际上不可能认为其中某一个参数优越于另一个参数，而必须进行多参数的综合分析对比。本文只是对取自调查区的海上溢油及一些岸边污染抽样和取自可疑来源区油田的原抽样品进行气液色谱分析，对样品中的正构烷烃、有机硫化合物的色谱图作了对比，绘制了正构烷烃碳数分布曲线，并以(C21+C22)/(C28+C29)的比值作为鉴别南黄海北部石油污染来源的参数。 相似文献
9.
本文对渤海海上 2个不同区块所产原油的红外光谱进行小波分析 ,分别获得不同尺度下的光谱信息。通过观察比较不同尺度下的光谱信息 ,包括谱图的大体形状 (谱图的低频部分 )和特征峰信息 (谱图的高频部分 ) ,更好地对 2种原油进行了分辨 ,为提高用红外光谱法进行海上溢油鉴别的准确度探索出 1种新的方法 相似文献
10.
对2种不同地理种群七带石斑鱼进行14项形态性状的测定,采用2种多元统计分析方法和t-检验方法,比较了2个群体的外部形态特征.t-检验结果表明,2群体在14个性状中有12个性状表现出极其显著差异(P＜0.01),1个性状表现出差异显著(P＜0.05).主成分分析构建了3个反映形态特征信息的综合性指标--主成分1、主成分2和主成分3,三者的贡献率分别为29.873%、25.091%和16.875%.三个主成分的累积贡献率为71.804%,2群体之间存在明显的偏离态势,形成两个不同的类群,2群体在主成分l轴上的差异较在主成分2轴上的差异更为明显,主成分1主要由经t-检验差异指标数量多和差异程度大的性状组成.判别分析表明,2个七带石斑鱼群体的形态差异显著(P＜0.0001),建立了2个群体的判别函数,其判别准确率及综合判别率均为100%,可以认为逐步判别法对七带石斑鱼不同群体的初步鉴定是可行的.差异系数(CD)计算的结果表明,尽管2群体在形态上存在一定的差异,但尚未达到亚种水平.主成分分析、t-检验和判别分析的结论基本上是类似的,它们从不同的角度反映了群体间的形态学差异. 相似文献
11.
Chandralata Raghukumar G. Sheelu P. A. Loka Bharathi Shanta Nair C. Mohandass 《Marine Georesources & Geotechnology》2001,19(1):1-16
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. 相似文献
12.
Arne Schnack-Friedrichsen Angela M. Davis Jim D. Bennell Dei G. Huws 《Marine Georesources & Geotechnology》2001,19(4):221-243
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. 相似文献
13.
Derek V. Ellis 《Marine Georesources & Geotechnology》2001,19(1):51-63
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. 相似文献
14.
G. Parthiban 《Marine Georesources & Geotechnology》2000,18(3):223-235
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. 相似文献
15.
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. 相似文献
16.
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。 相似文献
17.
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. 相似文献
18.
Shigehisa Nakamura 《Marine Geodesy》2000,23(1):55-61
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. 相似文献
19.
The effect of different fixation and storage protocols on the flow cytometric (FCM) simultaneous analysis of bacterioplankton and phytoplankton in coastal seawater samples (Mediterranean coastal lagoons) was investigated. FCM measurements (cell number, fluorescence and scatter characteristics) were obtained through DAPI staining. Three fixatives [glutaraldehyde (GA), formaldehyde (FA) and paraformaldehyde (PFA)] and two storage (3 months duration) methods (5 °C and −196 °C) were tested. Two dominant populations were detected in studied samples: bacteria and eukaryotic picophytoplankton. Adding fixatives (2% final concentration) appears necessary to obtain FCM exhaustive counts of all the bacteria and phytoplanktonic cells. This was related to the permeation effect of fixatives which allowed a better DAPI staining of the cells. Maximum fluorescence, i.e. optimal staining of the cells was obtained with FA or PFA, and significant lower fluorescences with GA. Fixed samples stored at 5 °C induced rapid cell loss. Only storage in liquid nitrogen of samples fixed with FA or PFA, allows mid-term (≥4 months) preservation of bacteria or picophytoplankton cell numbers, and limited evolution of DAPI-induced fluorescence and scatter characteristics. 相似文献
20.