凡纳滨对虾(Litopenaeus vannamei)即食虾仁在常温保藏中的货架期预测及品质分析

采用化学分析、质构检测及动力学模型建立等方法, 对凡纳滨对虾(Litopenaeus vannamei)即食虾仁在常温保藏中的细菌总数、TVB-N值、pH值、质构特性、色差值及感官评价等参数进行测定。以挥发性盐基氮TVB-N作为货架寿命的关键指示因子, 利用Arrhenius法预测常温流通高水分即食调味虾仁的货架寿命。计算结果Ea为65.26kJ/mol, k0为6.04×109, 进一步推算得到在20℃和25℃常温流通条件下, 即食虾仁产品的货架期为148.61d和94.1d。在25℃保藏3个月的虾仁虽在细菌总数、TVB-N值、pH值、感官评分、质构、色差值等方面均发生了一些变化, 但都在安全范围之内, 不影响其食用价值。本研究为常温流通的即食虾仁产品开发奠定了理论基础。     

海捕大管鞭虾(Solenocera melantho)调理食品在常温保藏中的货架期预测及产品质量分析

本文测定了海捕大管鞭虾(Solenocera melantho)(又称红虾)调理食品在不同温度保藏中的细菌总数、挥发性盐基氮(TVB-N)值、pH值及感官评价等参数。通过对虾肉色泽、组织质构、风味和外形四个方面的检测,综合各项指标决定将TVB-N作为该产品质量变化和推测货架期时长的关键指标。将各温度下测定的TVB-N值代入线性方程组计算出反应活化能E_a为55.21 k J/mol,指前因子k_0为1.08×10~9。利用Arrhenius方程外推法计算得出在20°C和25°C温度下TVB-N值变化速率常数分别为k_(20°C)=0.1405和k_(25°C)=0.2386,从而进一步确定该条件下保藏的理论货架期分别为153.6d和92.1d。经质构仪分析红虾虾仁的硬度与弹性变化,综合感官评定结果和其它测定值,确定海捕红虾产品在常温贮藏中的货架期为3个月。本研究为常温下红虾调理食品的保藏提供了理论依据。     

低温贮藏罗非鱼微生物学质量变化特性和保藏期

进行了罗非鱼在0,5,10,15℃贮藏过程中的微生物学质量变化特性和高品质期、货架期的研究,并对其特定腐败菌假单胞菌、细菌总数、VBN与感官评价的一致程度进行了探讨。结果表明,罗非鱼在0～15℃温度区域是淡水鱼中鲜度下降慢的鱼种,在0,5,10,15℃贮藏中,罗非鱼的高品质期分别为11,6,3和1.5d,货架期分别为20,9.5,5和2.5d。高品质期和货架期终点的假单胞菌数平均为(6.27±0.23)Log10cfu·g-1和(7.70±0.11)Log10cfu·g-1,显示了假单胞菌计数与罗非鱼的感官鲜度及保藏期具有较可靠的一致性。高品质期和货架期终点的细菌总数平均为(6.84±0.60)Log10cfu·g-1和(8.08±0.41)Log10cfu·g-1,VBN值平均为(11.8±1.38)mg·100-1·g-1和(20.1±1.66)mg·100-1·g-1,均无显著差异(P>0.05),表明细菌总数和VBN作为罗非鱼低温贮藏的鲜度指标与感官鲜度评价有较好的一致性。     

鲫鱼(Carassius auratus)在微冻保鲜过程中的质量变化

该文研究鲫鱼 ( Carassius auratus)在微冻 ( - 3℃ )保鲜过程中的质量变化规律。以感官评价、细菌总数、T- VBN值、p H值、ATPase活性、K值等作为质量指标。实验结果表明 ,微冻可以明显抑制细菌总数的增长 ,维持较低的 T- VBN和 K值。但是 ,微冻条件下鲫鱼的 ATPase活性下降速度较快     

超低温冻藏对金枪鱼肉质构及生化特性机理研究

为探索金枪鱼肉冻藏过程中质构与生化特性变化规律,得到节能低耗的最佳冻藏温度,以黄鳍金枪鱼质构、盐溶性蛋白含量、K值、颜色(a值)、持水率等为指标,研究在不同冻藏温度下(–18,–25,–35,–45,–55,–65°C)冻藏6个月的质构与生化特性变化规律。结果表明:在不同温度下冻藏,肌肉的质构、肌原纤维蛋白的盐溶性含量、鲜度随着冻藏时间的延长,均呈下降趋势;而且质地的变化与肌原纤维中盐溶性蛋白含量的变化呈正向关系,冻藏温度越低,品质变化越小。冻藏温度对金枪鱼的质构、盐溶性蛋白含量、鲜度、颜色的变化均有显著性影响(P0.05)。但在超低温–55°C与–65°C冻藏180d,无明显变化。从低碳环保角度来看,采用–55°C冻藏180d可以最大限度地保持金枪鱼的品质。     

南美白对虾冰温下菌相变化

通过测定南美白对虾的冰点,确定了南美白对虾冰温贮藏温度;分析了冰温贮藏条件下南美白对虾细菌总数的变化情况,并通过生化实验分离鉴定了生鲜状态和达到一级鲜度时南美白对虾的细菌菌相。结果表明,南美白对虾冰点为(-1.4±0.1)℃,冰温贮藏3d后细菌总数达到1.03×105,达到一级鲜度的细菌总数极限值;4 d后细菌总数达到1.75×106,到达货架期终点。生鲜南美白对虾的优势菌为Aeromonas spp.,Chromobacterium spp.和Photobacterium spp.;冰温贮藏条件下达到一级鲜度时,南美白对虾的特定腐败菌(specific spoilage organisms,SSO)为Shewanella spp.,Flavobacte-rium spp.和Acinobacter spp.。     

贮藏温度对中国毛虾(Acetes chinensis)品质变化影响的研究

为探究贮藏温度对中国毛虾品质的影响,通过感官评分,菌落总数和理化指标的测定,分析毛虾虾皮在不同贮藏温度下的品质变化。结果表明:25°C及37°C贮藏期间感官评分、亮度值(L*)显著下降,红度值(a*)、黄度值(b*)、菌落总数显著增加(P0.05),p H值先缓慢增加后趋于稳定,TVB-N和TBA值在贮藏前期均缓慢增加,后期增加显著。4°C贮藏下,感官评分缓慢下降,p H值、菌落总数基本不变,贮藏30 d后,L*、a*、b*、TVB-N及TBA值呈现显著变化(P0.05)。综合分析,不同温度对毛虾虾皮贮藏期的色泽、感官评分、TVB-N、TBA、p H值及菌落总数变化均有显著影响;毛虾皮在25°C和37°C下分别贮藏至15 d及9 d时,已严重发黄并产生异味,菌落总数均大于107CFU/g,已腐败变质。4°C下贮藏至60 d时毛虾虾皮仍未失去食用价值,说明低温能显著延长毛虾虾皮的贮藏时间。     

水产品鲐鱼(Pneumatophorus japonicus)细菌多样性及优势微生物分析

为研究鲐鱼(Pneumatophorus japonicus)在不同冻藏时期的优势微生物,并且得到一个较全面的细菌群落组成结构,采用16SrDNA基因克隆文库及克隆子分析等方法,分别对冻藏1d、8d和20d条件下鲐鱼鳃体系中的细菌种群多样性、优势微生物及其中产组胺菌的变化进行分析。结果表明,不同时期鲐鱼鳃内的细菌多样性均较强;冻藏1天的鳃体系中不动杆菌属(Acinetobacter)占优势为总数的77.5%,产组胺细菌如泛菌属(Pantoea)和肠杆菌属(Enterobacter)较少;第8天优势细菌种群是梭杆菌属(Fusobacteria bacterium)和希瓦氏菌属(Shewanella),而产组胺菌如发光杆菌属(Photobacterium)和弧菌属(Vibrio)较前期数量有所增加;冻藏到第20天的优势种群为哈夫尼菌属(Hafnia)和沙雷菌属(Serratia),它们均是产组胺的菌群。鲐鱼中细菌多样性及其优势微生物的变化等全面信息可为了解鲐鱼水产品组胺发生的微生物机制及其控制方法提供重要依据。     

流化冰对于鲣鱼的保鲜效果研究

以远洋鲣鱼为研究对象,以传统淡水碎冰保鲜为对照,研究流化冰处理对鲣鱼的理化性质及微生物特性的影响。结果表明:(1)–4°C冷藏18d后,流化冰保鲜鱼肉pH值、TVB-N、TBA、a*值和菌落总数依次为5.57、10.2mgN/100g、2.87mg/100g、8.92和2.61lgCFU/g,而淡水碎冰保鲜鱼肉各指标已达6.05、20.3mgN/100g、6.60mg/100g、7.16和3.02lgCFU/g,故可知流化冰保鲜处理效果明显优于碎冰保鲜。(2)在25±1°C室温条件下,将冰与鱼放入保温箱内保鲜8h后,流化冰保鲜鱼肉的a*值、pH值、TVB-N、TBA、菌落总数和汁液流失率均显著低于空白和淡水碎冰保鲜处理组(P0.05)。流化冰保鲜可显著减缓鱼体的腐败进程、延长产品货架期,进而满足冰鲜水产品的远洋及长距离运输要求。     

鱼鲜酱油稀发酵中的糖量变化及其对曲霉活动的影响

在鱼鲜酱油的酿制中 ,研究鱼鲜酱油稀发酵中的糖量变化及其与曲霉生长活动的关系 ,对比了在发酵后期向发酵液中加入与不加入糖化液对曲霉生长活动和发酵效果的影响。结果表明 ,鱼鲜酱油稀发酵过程中仅消耗了以粗淀粉形式出现的糖量 ,在 35℃下 ,开始发酵的第 1天至第 4天为曲霉生长繁殖的高峰期 ,到第 1 3天曲霉活细胞数达到最大值 ,此后则开始衰退。第4天至第 1 0天为糖量消耗高峰期。而在发酵后期 (第 1 9天 )添加糖化液 ,在 32℃下发酵 ,可促使曲霉细胞二次活动高潮的形成 ,并使最终产品的无盐可溶性固形物、全氮及各项感官指标均优于未加糖组。     

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.     

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.     

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.     

Phylogenetic diversity and phenotypic characterization of cultivable bacterioplankton isolated from polar oceans

A set of 27 marine planktonic bacteria isolated from the polar regions was characterized by 16S rDNA sequencing and physiological and biochemical testing. More than half of these bacteria were positive for caseinase, gelatinase and 13-glucosidase, and could utilize glucose, maltose or malic acid as carbon source for cell growth. Twelve isolates expressed nitrate reduction activities. Except for one antarctic isolate BSwlO175 belonging to Actinobacteria phylum, these isolates were classified as γ-Proteobacteria, suggesting that γ-Proteobacteria dominated in cultivable marine bacterioplankton at both poles. Genus Pseudoalteromonas was the predominant group in the Chukchi Sea and the Bering Sea, and genus ShewaneUa dominated in cultivable bacterioplankton in the Prydz Bay. With sequence similarities above 97%, genus Psychrobacter was found at both poles. These 27 isolates were psychrotolerant, and significant 16S rDNA sequence similarities were found not only between arctic and antarctic marine bacteria （ 〉 99% ）, but also between polar marine bacteria and bacteria from other aquatic environments （ ≥ 98.8% ）, including temperate ocean, deep sea, pond and lake, suggesting that in the polar oceans less temperature-sensitive bacteria may be cosmopolitan and have a bipolar, even global, distribution at the species level.     

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.     

Deep-Sea Sediment Compression Curves: Some Controlling Factors, Spurious Overconsolidation, Predictions, and Geophysical Reproduction

Oedometer tests have been carried out on 70 undisturbed surficial clays (at approximately 250 mm below the mudline), mostly collected by free-fall corers from sites widely scattered throughout the deep-sea North Atlantic. Acoustic measurements were also made, initially on contiguous samples and ultimately on the same sample using a geophysically instrumented oedometer which also collected electrical resistivity data. Apart from those quiescent areas below the carbonate compensation depth, such as north of the West Indies where very fine clays exist, most of the samples are silty clays whose geotechnical-geophysical properties are dependent on the type of clay minerals present (and their ability to take in moisture), the sand-size fraction, and the quantity of carbonate present. Thus the pure clays have high compressibilities which decrease on the addition of coarse particles, while the converse is true for the acoustic parameters, these increasing with the sand fraction. Using the notion of the intrinsic compression line for all samples, and comparison to it of the measured compression curves, it is clear that, contrary to some previously held ideas, most deep-sea clays are normally consolidated; the addition of carbonate has the effect of creating an open, stronger sediment skeleton. Interestingly, where information is available, the variation with depth of a sample's acoustic velocity follows the void ratio pressure relationship of the compression curve. This allows the construction of an in-situ sediment compression curve using the in-situ geophysical observations.