Species composition and distribution of marine nematode community in the North Taiwan Strait

I~IOW~ne nelnatode is a ban gIOup of benthic OrgAnsrns. Abbot 5 000 spotes Of free-livingnelnatedes have ben dedbo so far, and it has ho estimated that abbot 20 (XX) are as yetunknoWn. Chinese bothologist has Paid attention to marine nelnatodes in China seas in yare. The spatial distribution and shoes commotion of marine nelnatedes in the HUanghe EstUary, Qinhuangdao waters, QingdaO Bay and Xiamen ~ have ho reported (Zhang etal., 1990, 1991, 1993; ac and Li, 1998). ~ new shoes in the…     

南海地区海气环境场的季节和年际变化

本文对南海地区(0—20°N,105—135°E)海气环境场进行EOF分析。其结果除了深入了解南海地区气候的基本场外,还揭示了叠加在基本场上的各种扰动场与热带天气系统的联系,为研究南海ITCZ等热带天气系统以及南海环境场对EL—Ni(?)o现象的反映提供了研究依据。     

有风浪太湖水体的光照传输模式

根据辐射传输方程的近似解方法和光照传输的累加原理,建立了包括水面风浪效应、水中悬浮粒多次散射和底泥反射的垂直分层水体的光照传输数值模式。利用该模式和太湖悬浮粒实测资料,计算和讨论了太湖水体中光照随水深的变化以及悬浮粒浓度、风浪和太阳高度的影响。结果表明,悬浮粒的多次散射所形成的漫射光是湖水中光照不可忽视的重要部分。在水体的下层,漫射光甚至是光照的主要构成部分。风浪对水中光照的影响则主要在天顶角大于70°时才明显地表现出来,此时风浪水体对太阳直接辐射和全辐射的反射率比平静水面都有明显的减小。     

南海深海盆地沉积柱样中的浊流沉积

本文根据南海深海盆地三个沉积柱样的粒度结构、地球化学、微体古生物等特征分析,深讨了南海深海盆地细粒沉积物的浊积现象。结果表明,位于南海北部陆架斜坡上KL37孔的浊流沉积现象并不明显;位于陆架斜坡和深海盆地交界处的KL29孔存在着大量的浊积层,属于浊流沉积和半远洋沉积环境;位于南海盆地中部的KL91孔虽然已属于远洋性沉积环境,但除出现火山灰沉积外,浊流沉积作用仍然是相当活跃的。     

The impact of several chemical poisons on the absorbing 45Ca by the Arca granosa

The impact of several chemical poisons on the Arca granosa absorbing 45Ca was studied. The results showed that the absorption of 45Ca in the blood and the soft tissue by Arca granosa was inhibited by the inorganic compounds of Cu, Zn, Pd, Cd, Hg and so on, among which the inhibition of Cd was the strongest, next was that of Cu and Hg. But the inhibition of the absorption of 45Ca in the shell of Arca granosa was little. The impact of three kinds of energy metabolism inhibitory substances on the absorption of 45Ca by the Area granosa showed that the absorption was an active transfer process.     

Estimation of Contamination of ERS-2 and POSEIDON Satellite Radar Altimetry Close to the Coasts of Australia

It is broadly acknowledged that the precision of satellite-altimeter-measured instantaneous sea surface heights (SSH) is lower in coastal regions than in open oceans, due partly to contamination of the radar return from the coastal sea-surface state and from land topography. This study investigates the behavior of ERS-2 and POSEIDON altimeter waveform data in coastal regions and estimates a boundary around Australia's coasts in which the altimeter range may be poorly estimated by on-satellite tracking software. Over one million 20 Hz ERS-2 (March to April 1999) and POSEIDON (January 1998 to January 1999) radar altimeter waveform data were used over an area extending 350 km offshore Australia. The DS759.2 (5'resolution) ocean depth model and the GSHHS (0.2 km resolution) shoreline model were used together to define the coastal regions. Using the 50% threshold retracking points as the estimates of expected tracking gate, we determined that the sea surface height is contaminated out to maximum distance of between about 8 km and 22 km from the Australian shoreline for ERS-2, depending partly on coastal topography. Using the standard deviation of the mean waveforms as an indication of the general variability of the altimeter returns in the Australian coastal region shows obvious coastal contamination out to about 4 km for both altimeters, and less obvious contamination out to about 8 km for POSEIDON and 10 km for ERS-2. Therefore, ERS-2 and POSEIDON satellite altimeter data should be treated with some caution for distances less than about 22 km from the Australian coast and probably ignored altogether for distances less than 4 km.     

The CANALES experiment (1996-1998). Interannual, seasonal, and mesoscale variability of the circulation in the Balearic Channels

Repeated hydrographic casts, mooring time series and satellite sea surface temperature collected during the CANALES experiment (1996–98) are used to describe the thermohaline circulation in the Balearic Channels (western Mediterranean) and to analyze its variability. Mass transports are estimated by inverse calculations. The role played by each channel in the meridional water exchange is clarified: the Ibiza Channel funnels southward cool, saline, northern waters whereas the Mallorca Channel appears as the preferred route for the northward progression of warm, fresh, southern waters. A neat interannual trend is revealed by the continuous decrease of the amount of Western Mediterranean Intermediate Waters (WIW) brought by the Northern Current, reflecting the increase in temperature of the winter mixed layer in the northern Mediterranean that occurred each year between 1996 and 1998. A clear seasonal signal was also seen in the transport of the Northern Current which decreased from 1 to 1.4 Sv in winter to < 0.5 Sv in summer. The current intensified again in fall. A number of mesoscale eddies, from 20 to 70 km in size, most of them anticyclonic vortex eddies were brought by the unstable Northern Current, these eddies strongly perturbed the water exchange in the Ibiza Channel forcing retroflections of northern waters back to the north-east into the Balearic Current. These eddies either stayed stalled for several months in the Gulf of Valencia to the north of the channel, or were slowly funnelled southward through the channel narrows. A decreasing trend was observed in the mesoscale activity of the Northern Current between 1996 and 1998. Conversely, large, anticyclonic eddies, 150-km diameter, progressively invaded the Algerian Basin to the south of the channels in 1997–98 and forcing northward inflows (up to 0.75 Sv) of fresh and warm waters of Atlantic origin (AW) into the Mallorca Channel. The marked interannual differences observed in both northern and southern eddy activity may be linked to the interannual variability of the large scale thermohaline circulation.     

生物制氢研究进展

目前, 世界上利用的能源90%以上都是“化石能源”(如石油、煤炭和天然气等)。随着人类不断利用这些不可再生的“化石能源”, 它将会逐渐枯竭, 且其燃烧形成的产物(如CO2和SO2等)造成的严重环境污染(如温室效应和酸雨), 也有害于人类健康。因此, 人类正面临着能源紧缺和环境污染的双重压力。为满足能源需求量日益增长和环境保护的需要, 我们必须寻找环保型的可再生能源来替代“化石能源” 以满足人类对能源的需求。 在各种可再生能源中氢能将有可能替代“化石能源”,成为未来能源利用的主要形式。氢能具有许多优点:①氢能燃烧时只生成水, 不产生任何污染物, 甚至连CO2也不会产生, 实现真正的“零污染” 和“零排放”;②氢能的能量密度高, 放热高达122 kJ/g, 是焦炭放热的4.5倍, 汽油的2.68倍;③氢能可经济有效的输送和储存, 可以利用已有的天然气管道输送, 输送成本低, 甚至优于输电, 因为输送氢能不会产生如电能输送过程中所产生的能量损耗;氢能的存储也比较简便, 其中储氢合金材料就是一种非常理想的储氢方法, 该方法储氢能力强、运输方便、操作容易, 且安全可靠。在利用储氢合金进行储氢时, 还可用以进行制冷或采暖(Kulkova et al., 2006), 因为储氢材料在吸氢时放热, 在放氢时吸热。正因为氢能具有如此多的优点, 许多大的跨国公司开始对制氢技术高度关注, 如主要汽车制造商(通用、福特、戴姆勒-克莱斯勒等)对开发以氢能作为燃料的汽车投入大量的人力和物力;宝马公司从20世纪70年代就开始研制以氢能为能源的汽车, 宝马公司现在已拥有了时速达240km的氢能汽车(Munro,2003)。同时, 一些发达国家的科研院所的科学家们对氢能的制备方法、制氢机制以及提高产氢量等进行了大量的研究。     

Methane-dominated thermochemical sulphate reduction in the Triassic Feixianguan Formation East Sichuan Basin, China: towards prediction of fatal H2S concentrations

New sour pools have recently found in the Lower Triassic Feixianguan Fm carbonate reservoirs in the East Sichuan Basin in China with H₂S up to 17.4% by volume. A recent blowout from a well drilled into this formation killed hundreds of people as a result of the percentage concentrations of H₂S. In order to assess the origin of fatal H₂S as well as the cause of petroleum alteration, H₂S concentrations and the isotopes, δ³⁴S and δ¹³C have been collected and measured in gas samples from reservoirs. Anhydrite, pyrite and elemental sulphur δ³⁴S values have been measured for comparison. The high concentrations of H₂S gas are found to occur at depths >3000 m (temperature now at 100 °C) in evaporated platform facies oolitic dolomite or limestone that contains anhydrite nodule occurrence within the reservoirs. Where H₂S concentrations are greater than 10% its δ³⁴S values lie between +12.0 and +13.2‰ CDT. This is within the range of anhydrite δ³⁴S values found within the Feixianguan Fm (+11.0 to +21.7‰; average 15.5±3.5‰ CDT). Thus H₂S must have been generated by thermochemical sulphate reduction (TSR) locally within the reservoirs. Burial history analysis and fluid inclusion data reveal that the temperature at which TSR occurred was greater than about 130–140 °C, suggesting that the present depth-temperature minimum is an artifact of post-TSR uplift. Both methane and ethane were actively involved in TSR since the petroleum became almost totally dry (no alkanes except methane) and methane δ¹³C values become significantly heavier as TSR proceeded. Methane δ¹³C difference thus reflects the extent of TSR. While it is tempting to use a present-day depth control (>3000 m) to predict the distribution of H₂S in the Feixianguan Fm, this is an invalid approach since TSR occurred when the formation was buried some 1000–2000 m deeper than it is at present. The likelihood of differential uplift across the basin means that it is important to develop a basinal understanding of the thermal history of the Feixianguan Fm so that it is possible to determine which parts of the basin have been hotter than 130–140 °C.     

中国对虾人工诱导雌核发育的研究 Ⅱ.紫外线辐射对精子顶体反应和受精能力的影响

研究了 36 5 nm波长紫外线辐射中国对虾精子对其顶体反应和受精能力的影响。结果表明 ,低剂量紫外线辐射促进精子发生顶体反应 ,大剂量辐射使精子丧失发生顶体反应的生理机能并死亡。 36 5 nm波长紫外线能够透过精荚和纳精囊盖 ,对其内精子起到杀伤作用。精液稀释液在紫外线下辐射 5～ 8s,仍有部分精子具有受精能力 ,但胚胎在早期阶段即死亡。人工诱导雌核发育的过程中 ,紫外线辐射精液稀释液 5～ 8s,可获得遗传物质失活的精子 (激活源 )。经透射电镜观察分析 ,紫外线对精子遗传物质的损伤是一种使染色质变性的化学作用。