动物蛋白酶1058水解ti鱼可溶性蛋白质

研究了动物蛋白酶 1 0 58水解鱼是鱼蛋白时 ,酶量、温度、作用时间对鱼是鱼蛋白质水解率和苦味的影响。结果表明 :酶浓度的提高 ,水解时间的延长 ,均使鱼是鱼蛋白水解率明显提高。最适水解温度为 50℃ ,当温度高于 50℃时 ,水解率逐渐下降 ,蛋白酶开始失活。苦味值随水解率提高而增加。用正交试验的方法 ,经综合分析和试验得出 ,该蛋白酶水解鱼是鱼的最佳条件是酶量与底物之比为 1 .5∶ 1 0 0 0 ;温度为 50℃ ;水解时间为 4h。     

双酶分步水解金枪鱼(Eleotridae)碎肉制备高F值酶解液的工艺研究

以金枪鱼碎肉为原料, 采用双酶分步水解法制备高F值酶解液, 通过Box-Behnken试验设计, 分别确定两步酶解的最佳条件, 酶解液经活性炭静态吸附去除游离芳香族氨基酸, 对脱芳后的酶解液进行氨基酸组成分析并测定F值。结果表明, 胃蛋白酶为第一步水解用酶, 酶解的最佳工艺条件为酶用量650U/g, 料水比1∶7(g/mL), 温度35.9℃; 风味蛋白酶为第二步水解用酶, 酶解的最佳工艺条件为酶用量50700U/g, pH 6.51, 温度51℃, 最终水解度达到36.87%±0.54%; 酶解液在pH 3.0, 温度35℃条件下, 经5%(质量体积分数)的活性炭吸附时间3h后, 脱芳率达到63.18%, F值为30.33, 符合高F值肽的要求。     

黄海西部沿岸冷水在夏季南黄海西部底层冷水形成和季节演变过程中作用的化学水文学分析

以金枪鱼碎肉为原料, 采用双酶分步水解法制备高F值酶解液, 通过Box-Behnken试验设计, 分别确定两步酶解的最佳条件, 酶解液经活性炭静态吸附去除游离芳香族氨基酸, 对脱芳后的酶解液进行氨基酸组成分析并测定F值。结果表明, 胃蛋白酶为第一步水解用酶, 酶解的最佳工艺条件为酶用量650U/g, 料水比1∶7(g/mL), 温度35.9℃; 风味蛋白酶为第二步水解用酶, 酶解的最佳工艺条件为酶用量50700U/g, pH 6.51, 温度51℃, 最终水解度达到36.87%±0.54%; 酶解液在pH 3.0, 温度35℃条件下, 经5%(质量体积分数)的活性炭吸附时间3h后, 脱芳率达到63.18%, F值为30.33, 符合高F值肽的要求。     

酶解蓝圆鲹蛋白制备降血压肽的工艺研究

以蓝圆(Decapterus maruadsi)鱼肉蛋白为原料,选用6种蛋白酶在各自适宜的条件下酶解制备鲹降血压肽,通过检测酶解产物对血管紧张素转化酶(ACE)的体外抑制活性,筛选出木瓜蛋白酶为制备蓝圆降血压肽的最佳用酶。考察了不同水解度的酶解产物对ACE抑制效果,当水解度为13.7%时,产物对ACE的最高抑制活性可达67.4％。在此基础上,分别了考察酶解时间、初始酶用量、初始底物浓度、酶解温度和 pH 值对酶解工艺的影响,鲹得到制备蓝圆降血压肽的适宜酶解工艺为：初始酶用量鲹为7000 U/g,初始底物浓度为25 g/L,酶解温度为45℃, pH为7.0,酶解240 min。采用超滤技术对酶解产物活性组分进行分离富集,发现产物中高活性部分均可富集于10 kDa和5kDa渗透液中,且高活性组分分子量主要集中在5 kDa以下,该组分对ACE的活性抑制率为88.47%。     

鹌鹑蛋蛋清蛋白酶解工艺条件的研究

以鹌鹑蛋蛋清蛋白作为原料,探讨酶解鹌鹑蛋蛋清蛋白生成小分子活性肽的加工工艺。采用单因素和响应面分析试验,优化出蛋清蛋白酶解的最佳工艺条件为:选用胰蛋白酶,固液比1∶3,加酶量187.5 U/g底物,水解时间5 h,pH 8.07,酶解温度51.76℃,水解度可达到91.37%,且得到的酶解液风味良好。采用高效液相色谱法分析酶解液中游离氨基酸的组成及含量,结果表明:酶解液含有7种人体必需氨基酸,其中赖氨酸含量达16.22%,是1种天然优质的水解制品,可精制成富含多种氨基酸的蛋白溶液,应用于新型产业的开发。     

酶解糙刺参内脏团蛋白制备抗氧化肽的工艺研究

为了能够有效利用糙刺参内脏蛋白,以水解度为主要指标,对酶解蛋白酶进行了筛选,并系统研究了酶解温度、p H、加酶量和水解时间等单因素对水解度的影响。在此基础上,利用响应面中心组合设计实验,对酶解工艺进行了优化,得到以温度、p H、加酶量及水解时间为因子的二次方程,通过方差分析和验证性实验得出,此二次方程能较好反应海参内脏团蛋白水解度的变化规律,得到最佳水解条件为:温度52.66℃,p H 6.71,加酶量2.5%(质量分数),酶解时间10 h,预测最高水解度为49.58%。最佳酶解条件下所得多肽74%以上分子质量小于500 Da。利用DPPH法测定最佳条件酶解所得多肽的抗氧化活性,3 g/L的抗氧化率达到了24.8%,利用ABTS法测定最佳条件酶解所得多肽的抗氧化活性,3 g/L的抗氧化率达到了0.255μmol/g。为海参内脏蛋白的利用提供了参考。     

绿侧花海葵(Anthopleura anjunae)寡肽制备的关键技术与抗前列腺癌作用研究

本文探讨绿侧花海葵(Anthopleura anjunae)抗前列腺癌酶解寡肽制备与工艺优化。以绿侧花海葵肉为原料进行酶解,筛选最佳蛋白酶,通过正交实验优化酶解条件,并通过超滤、阴离子交换层析、G-25凝胶过滤和反相高效液相色谱(RP-HPLC)分离纯化,通过LC-MS和氨基酸序列测定鉴定寡肽的氨基酸序列,并以MTT法检测产物对前列腺癌细胞系DU-145增殖抑制率,以确定活性最强组分,最后通过倒置显微镜观察纯化肽的抗前列腺癌活性。结果表明,碱性蛋白酶为最佳酶种;工艺条件为:最适料液比1︰5、最适p H=11、最适加酶量2000U/g、最适温度35oC、最适酶解时间6h;经高效液相纯化得到由五个氨基酸组成的绿侧花海葵抗前列腺癌寡肽,其氨基酸序列为:Tyr-Val-Pro-Gly-Pro(AAP-H);倒置显微镜结果显示经AAP-H作用24h后的DU-145细胞具有明显的凋亡形态学特征。结论:采用碱性蛋白酶酶解并通过超滤和色谱分离技术能从绿侧花海葵肉中制备抗肿瘤活性肽;且AAP-H对DU-145细胞的增殖抑制作用呈时间与剂量依赖关系,作用后细胞出现了凋亡的形态学特征。因此,AAP-H能明显抑制前列腺癌细胞DU-145增殖,可以诱导其发生凋亡而发挥抗肿瘤作用。     

酶解马氏珠母贝肉制备降血压肽工艺条件优化

以马氏珠母贝（Pinctada martensii）肉为原料，选用6种蛋白酶在各自适宜的条件下进行酶解，采用HPLC法分析酶解产物对血管肾张素转换酶（ACE）的抑制活性（IP），筛选出碱性蛋白酶为其制备的最佳酶种类，并确定了水解度为21％时，产物具有较好的抑制活性。在此基础上，分别考察了加酶量，底物浓度，酶解温度及pH对水解度的影响。结果表明：当加酶量为0．175g／L，底物浓度为35g／L，温度为45℃，pH为9．5，水解时间240min为酶解最适宜工艺条件。通过SDS-聚丙烯酰胺凝胶电泳测定分子质量分布，表明酶解产物中主要为14．4ku以下的多肽分子。     

鳀鱼水解蛋白脱苦方法的研究

蛋白质水解产物常带有苦味，鱼蛋白经过酶水解后也产生强烈的苦味［４，６］。苦味来自水解过程中产生的含疏水基团的短肽和疏水性氨基酸［５］，其中，带有疏水基团的短肽比疏水性游离氨基酸的苦味大［２］。短肽的苦味与其疏水基团的多少、种类及其排列顺序有直接关系。大多数苦味肽的链端都有亮氨酸（Ｌｅｕ）［３］。水解蛋白的脱苦方法大致有５种［１～３］；水解法、类蛋白合成法、有机溶剂法、吸附法、掩盖法。鱼（Ｅｎｇｒａｎｌｉｓｊａｐｏｎｉｃｕｓ）属于中上层低值鱼类，在我国沿海蕴藏量很大。随着大多数经济鱼类资源的日益匮…     

南美白对虾副产物酶解工艺优化及其蛋白肽活性评价

为高质化利用南美白对虾加工副产物蛋白资源,本研究以南美白对虾加工副产物虾头虾壳为原料,蛋白水解度为考察指标,采用单因素和响应面试验优化酶解工艺。检测虾蛋白肽分子量的分布范围,评价其抗氧化能力及免疫调节作用。结果表明,碱性蛋白酶与虾头内源酶自溶酶解具有较好的协同作用,最佳酶解工艺参数值为：酶添加量4%、酶解时间6.5 h、酶解温度40 ℃、料液比1∶5。经蛋白层析仪检测,分子质量分布在75~1 355 Da的蛋白肽占比达到76.35%。虾蛋白肽的羟自由基清除率IC₅₀为4.64 mg/mL、DPPH自由基清除率IC₅₀为3.08 mg/mL,提示其具有一定的抗氧化能力。虾蛋白肽中剂量组（10 mg/kg）能显著促进淋巴细胞增殖,并提高免疫低下模型小鼠的免疫器官指数和吞噬指数,表明虾蛋白肽具有显著的免疫调节作用。     

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.     

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.     

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.     

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。     

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.     

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.     

Flow Cytometric Analysis of Coastal Lagoon Bacterioplankton and Picophytoplankton: Fixation and Storage Effects

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.     

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.