氟苯尼考3种不同给药方式在中国明对虾体内的药代动力学研究

用高效液相色谱法研究静注、肌注和口服氟苯尼考在中国明对虾(Fenneropenaeuschinensis)体内的药代动力学特征,所得数据用MCP-KP程序分析。结果表明,3种给药方式的血药经时过程均符合二室开放模型,符合一级吸收二项指数方程,血窦注射、肌肉注射、口服药饵的时间对药物质量浓度的理论方程分别是:C血注=16.38e-2.58t 0.32e-0.1t,C肌注=18.7e-2.57t 0.26e-0.12t,C药饵=15.08e–1.49t 0.65e-0.09t–15.74e–10.38t。主要药物代谢动力学参数分别是:吸收半衰期(t(1/2)α)为0.269,0.270和0.465h,消除半衰期(t(1/2)β)为6.921,6.494和7.903h,表观分布容积(Vβ)为1.287,1.293和2.421L/kg,总体清除率(Cs)为0.129,0.138和0.213L/(h·kg),药时曲线下总面积(Au,c)为0.755,0.681和0.666L/(h·kg)。肌肉注射和口服给药的生物利用度(F)分别是90.20%和97.58%。     

诺氟沙星2种不同给药方式在中国对虾体内的残留及消除规律

在水温(28±1)℃条件下,诺氟沙星药浴给药(10 mg·L-1)和药饵给药(30 mg·kg-1)连续5 d后,利用反相高效液相色谱法(RP-HPLC)分析诺氟沙星在中国对虾体内的残留及消除规律。结果表明,2种给药方式下,诺氟沙星在中国对虾肝胰腺、肌肉等组织中的分布和消除差别较大。药浴给药后中国对虾肝胰腺和肌肉中药物达峰时间分别为9和24 h,药峰浓度分别为1.36,0.25μg.g-1,消除半衰期分别为29.87和40.19 h;药饵给药后中国对虾肝胰腺和肌肉中药物达峰时间均为4 h,药峰浓度分别为0.79,0.113μg.g-1。2种给药方式下药物在对虾肌肉中的消除曲线分别为C(t)浴=0.2449e-0.4138t和C(t)饵=0.4066e-0.5364t;消除半衰期分别为40.19和31.01 h。根据诺氟沙星在水产品中的残留限量标准(50μg·kg-1),2种给药方式下,肌肉中诺氟沙星浓度均在给药后24 h低于此残留限量;肝胰腺中浓度经药浴给药后216 h低于此残留限量,药饵给药后96 h低于此残留限量。药浴给药和药饵给药后,肌肉中药物浓度达到此残留限量的休药期分别为3.84和3.90 d。     

肌注和口服药饵麻保沙星在日本对虾体内的药代动力学比较

在水温(25±0.6)℃条件下,分别以10、10和30 mg/kg剂量给健康日本对虾血窦注射、肌注和口服药饵麻保沙星后,用高效液相色谱法测定药物浓度,采用DAS2.0药动学软件对血药浓度进行分析,主要比较了肌注和口服药饵两种给药方式下麻保沙星在日本对虾体内的药代动力学差异。结果显示,血窦注射给药后,麻保沙星在日本对虾体内药物动力学最佳模型为无级吸收二室开放模型,表达方程为:C血窦注射=13.373e–1.396 t+8.28e–0.062 t;肌注和口服药饵麻保沙星后,在日本对虾体内的代谢过程均符合一级吸收二室开放模型,表达方程为C肌肉注射=15.521e–1.153t+7.90e–0.059t-23.421e–11.73t,C口服药饵=17.486e–0.33t+3.01e–0.051t-20.496e–0.408t。与口服药饵给药后药代动力学参数比较,肌注给药后的tmax(0.25 h)、t1/2Ka(0.059 h)、t1/2α(0.601 h)和t1/2β(11.769 h)均小于口服药饵给药的tmax(0.5 h)、t1/2Ka(1.697 h)、t1/2α(2.103 h)和t1/2β(13.535 h),且Cmax(20.7858 mg/L)和F(99.56%)均大于口服药饵给药Cmax(12.4774mg/L)、F(69.68%)。结果表明,肌注麻保沙星在日本对虾体内的吸收、分布和消除均快于口服药饵给药,且比口服给药吸收较完全。本实验将药动学参数与抗菌后效应(PAE)和最小抑菌浓度(MIC)相结合来探讨麻保沙星的给药方案,建议在治疗日本对虾细菌性疾病时,肌注14.30 mg/kg,每隔13.6 h一次;口服19.17 mg/kg,每隔11.8 h一次。     

氟苯尼考在三疣梭子蟹(Portunus trituberculatus)疾病模型内的代谢动力学

为了解健康和疾病条件下药物在三疣梭子蟹(Portunus trituberculatus)体内的代谢差异,在构建三疣梭子蟹溶藻弧菌疾病模型的基础上,按25mg/kg剂量分别给健康和患病三疣梭子蟹单次口灌氟苯尼考后,采用高效液相色谱法测定了其肝胰腺、肌肉和血浆中的药物浓度,药时数据应用3P97药代动力学软件拟合。结果显示:氟苯尼考在健康和患病条件下三疣梭子蟹相同组织中的药时曲线形态相似,三种组织的药时数据均符合带时滞的一级吸收二室开放模型;肝胰腺吸收药物最快,肌肉次之,血浆最慢;与健康组相比,患病蟹肝胰腺、肌肉、血浆三种组织对氟苯尼考的吸收和消除速度明显减慢,达峰时间推迟,半衰期延长,清除率减低,最高药物浓度下降,表观分布容积和药时曲线下总面积变大。说明疾病使氟苯尼考在三疣梭子蟹体内的吸收、分布、代谢和消除均发生了显著变化,建议患病三疣梭子蟹口服氟苯尼考的休药期至少10d。     

噁喹酸在大菱鲆体内的药代动力学研究

采用高效液相色谱法,研究了(24.5±0.2)℃水温条件下单次静注和口服给药后噁喹酸在健康大菱鲆体内的代谢动力学规律.结果显示,大菱鲆单次口服嗯喹酸(20mg/kg)后,药物在血浆中经时过程符合一级吸收二室开放模型,表达方程为C口服 =2.059e-0.062t +0.645e-0.023t-2.704e-0.202t,单次静注嗯喹酸(10mg/kg)后,药物在血浆经时过程符合无级吸收二室开放模型,表达方程为C静注=12.284e-0.144 +0.284e-0.027t.血浆中的主要药动学参数,静注的t1/2α (4.813 h)、t1/2β(25.441h)、tmax(0.083 h)均小于口服给药(11.26、30.212、6h).结果表明,静注嗯喹酸在大菱鲆体内的吸收、消除速度,达峰时间均快于口服给药.根据本实验的结果,嗯喹酸的合理给药方案为:建议口服给药按鱼体重21.41mg/kg,每日1次给药,连用5～7 d.     

恩诺沙星在菲律宾蛤仔体内的消除规律研究

以5mg/L恩诺沙星浸浴菲律宾蛤仔(Ruditapes philippinarum)24h,取血液、鳃、内脏团、足、闭壳肌5种组织,反相高效液相色谱法测定其中的药物浓度。结果表明,恩诺沙星按一级动力学过程从体内消除,在5种组织中消除速率快慢不一,其在菲律宾蛤仔血液、鳃、内脏团、足、闭壳肌中的消除曲线方程分别为c=6.995e-0.0853t,c=2.7957e-0.1177t,c=1.539e-0.1013t,c=1.7015e-0.1535t,c=2.010e-0.1414t,消除半衰期T1/2分别为6.284,5.889,6.483,4.516,3.679h。恩诺沙星在水产品中的最大残留限量为50μg/kg,在本实验条件下,建议临床休药期不小于2d。     

黄芩苷在中国对虾体内的代谢及残留消除规律研究

在(24±1)℃下,中国对虾连续7 d给予100 mg/kg黄芩苷药饵,用高效液相色谱法(HPLC)测定对虾血液及其它组织中的黄芩苷含量,建立适合中国对虾体内黄芩苷含量的测定方法,研究黄芩苷在中国对虾不同组织中的残留消除规律.结果表明,HPLC法黄芩苷与杂质分离良好,4个浓度水平的黄芩苷在不同组织中的平均回收率在80.57%～96.25%之间,日内精密度在3.26%～5.85%之间,日间精密度在3.88%～5.73%之间.与其它给药方式相比,黄芩苷药饵给药吸收较慢,在血液、肝胰腺、肌肉、鳃中的达峰时间(Tmax)依次为6,3,6,3 h;黄芩苷在不同组织中的分布为肝胰腺>鳃>血液>肌肉.黄芩苷在肝胰腺、鳃、肌肉、血液中的消除半衰期(t1/2β)分别为29.62,27.50,25.20,23.73 h,消除速率从快到慢依次为血液>肌肉>鳃>肝胰腺;黄芩苷残留较少,在肌肉和血液中5 d已降到检测限以下,肝胰腺及鳃7 d降到检测限以下.本试验为含黄芩苷的药物的应用提供参考.     

甲基睾丸酮在尼罗罗非鱼(Oreochromis niloticus)肌肉中的代谢和消除规律研究

在实验水温(28±2)℃条件下,以60mg/kg单剂量甲基睾丸酮对尼罗罗非鱼混饲口灌给药后,采用超高效液相色谱-串联质谱联用(UPLC-MS/MS)法测定尼罗罗非鱼肌肉中的药物水平,研究甲基睾丸酮在尼罗罗非鱼肌肉中的代谢及消除规律。结果表明,肌肉中药物浓度时间数据符合一级吸收二室开放模型,主要药代动力学参数达峰时间T(peak)为3.04h,质量浓度C(max)为33.331ng/g,消除半衰期T(1/2)β为23.073h。肌肉中甲基睾丸酮浓度24h内呈指数型下降,具有较高的消除速率,其后消除得较缓慢,消除方程符合C=46.18e0.101t。29d后罗非鱼肌肉中甲基睾丸酮水平在美国FDA的检测限0.8ng/g以下,给药120d后肌肉中检测不到甲基睾丸酮残留。     

凡纳滨对虾摄食诺氟沙星强化卤虫的药代动力学研究

应用高效液相色谱法研究了凡纳滨对虾(Litopenaeus vannamei)摄食诺氟沙星强化卤虫(Artemia)的药物代谢动力学。结果表明:强化4~8 h,卤虫体内的药物质量浓度达到最高,此后卤虫体内药物摄入和排除达到一个动态平衡;温度影响诺氟沙星在卤虫体内半衰期:体长3mm和6 mm的卤虫,在4,16,28℃时的半衰期分别为51.33,19.29,18.64 h和39.67,13.26,12.6 h。对虾摄食诺氟沙星强化的卤虫后,对虾组织中药物质量浓度经时过程符合一级吸收二室开放模型;投喂剂量对Tmax和Cmax影响较大,当对虾给药质量分数分别为800,400,200mg/kg时,肌肉中给药后出现最高血药的时间或达峰时间分别为0.403,0.540,0.481 h;肝胰脏中给药后出现最高血药的时间或达峰时间分别为0.826,1.839,1.469 h;肌肉中给药后的最高血药质量浓度分别为98.943,46.752,10.887 mg/L;肝胰脏中给药后的最高血药质量浓度分别为738.267,597.352,415.268 mg/L。药物在对虾肌肉的消除半衰期(约26.688 h)明显长于肝胰脏中消除半衰期(约13.988 h)。     

黄芩苷在中国对虾体内对诺氟沙星消除及细胞色素P450 酶的影响

对照组中国对虾(Fenneropenaeus chinensis)连续投喂不含药物饵料,诺氟沙星组和联合用药组以50 mg/kg体质量剂量连续投喂含诺氟沙星药饵5 d后,诺氟沙星组投喂不含药物饵料10 d,联合用药组以100 mg/kg体质量剂量投喂含黄芩苷饵料10 d。从投喂诺氟沙星药饵时开始,在不同时间点采集中国对虾血液、肝胰腺、鳃和肌肉组织进行药物残留和肝药酶活性测定。结果表明:与诺氟沙星组相比,联合用药组各组织中诺氟沙星消除较快,血淋巴、肝胰腺、鳃和肌肉的理论休药期比诺氟沙星组分别缩短了23.92%、22.73%、25.92%和21.92%;与对照组相比,诺氟沙星对中国对虾CYP1A(ECOD)和CYP2(APND)酶活性有一定的抑制作用,但随着诺氟沙星的消除抑制作用逐渐减弱,最后恢复至对照水平;黄芩苷在加速诺氟沙星在中国对虾体内消除的同时,对中国对虾CYP450酶也有较强的诱导作用。因此,药物使用应注意药物之间的相互作用,以免造成药物中毒或疗效下降现象。     

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.     

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.     

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.     

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.     

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.     

INFORMATION FOR AUTHORS

<正>Acta Oceanologica Sinica(AOS)is a comprehensive academic journal edited by the Editorial Committee of Acta Oceanologica Sinica and is designed to provide a forum for important research papers of the marine scientific community which reflect the information on a worldwide basis.The journal publishes scholarly papers on marine science and technology,including physics,chemistry,biology,