臭氧处理海水生成氧化物对扁藻生长的影响海水养殖

研究了臭氧处理海水生成氧化物对扁藻(Tetraselmis chuii)生长的影响.臭氧生成氧化物浓度在0.736mg/L以下不产生毒害作用,在1.113mg/L 以上观察到了毒害作用,并且浓度越高毒性越强.实验发现扁藻对臭氧生成氧化物的毒害有抵抗能力.     

真鲷仔,稚,幼鱼期消化酶活性的变化

本文研究了真鲷仔，稚，幼鱼不同发育期三种消化酶活性的变化，结果表明，蛋白酶活性两个极低点分别出现在受精后５日龄和２５日龄，２５－４４日龄蛋白酶活性上升明显，之后活性上升稍缓；淀粉酶从受精后到５日龄活性急剧下降，５－４４日龄变化很小，４５日龄后活性略有提高；脂肪酶活性从受精后至５日有所提高，４０日龄活性到最低点，之后上升较快。     

射阳县“十一五”期间沿海经济发展构想

21世纪被誉为海洋开发世纪,江苏省委、省政府正在加快建设沿海产业带,“十一五”期间沿海县面临着难得的战略机遇期。射阳地处江苏沿海的中心区域,拥有103km海岸线和2090km2管辖海域,是同时拥有国家二类对外开放口岩和国家级中心渔港的县,拥有江苏面积最大的1.3万hm2国有未利用     

An Engineering Computational Method of Calculating Wave Forces on the Mat and Platform''''s Sit-on-Bottom Stability

- In this paper, an engineering method is employed to calculate the horizontal and vertical wave forces on the mat of the submersible platform under Froude-Krylov hypothesis. According to some model tests, appropriate diffraction coefficients are selected. And the results of the formulae given in the paper agree satisfactorily with those experimental data now available. The proposed computational method is effective and convenient to use in evaluating the horizontal and vertical wave forces on the mat. An exmaple is also given in this paper. Finally, the effects of the vertical wave force on the platorm's sit-on-bottom stability are analyzed.     

长江口及邻近海域水体中痕量金属的分布

长江是我国第一大河,流域面积达180万平方公里,占全国土地总面积的五分之一；长江平均年人海流量近9240亿立方米,平均年总输沙量约4.68亿吨(张法高等,1987)。调查研究长江口及部近海域水体中痕量金属的分布变化情况,对进一步了解河水入海的转移过程、环境质量和研究河口化学界面交换过程以及对舟山渔场的生态影响等,都将起到积极作用。 1985年8月、11月及1986年1月,由中国科学院海洋研究所分三个航次按标定站位(图1)对长江口及邻近海域的痕量金属进行了调查。水样用 Niskin全塑采水器(美国)采集。     

钝顶螺旋藻的硝酸还原酶与氢酶之间的电子竞争

于1994年6－11月，运用生物化学方法以钝项螺旋藻为材料制备整体细胞和无细胞提取物。测定表明，整体细胞硝酸还原酶与氢酶活性的相互关系和无细胞提取物氢酶与硝酸还原酶的（对还原甲基紫精）Km值，分别为2．299×10－7mol／L和1．098×10－7mol／L；证实在硝酸还原酶与氢酶之间存在着电子竞争。     

三门湾的悬沙分布和输移特性

本文根据实测资料,通过悬沙浓度ρ、流速v和水深H的对应分析,得出了三门湾的悬沙浓度分布遵循着ρ∝f(v~2/H)的规律;同时发现湾外海域有着良好的将悬沙输移入湾的动力条件,是三门湾悬沙来源的主要场所;经全潮单宽净输沙量计算表明:进出海域的悬沙净输移量不大,全湾的悬沙输移具有深槽输向边滩、南进北出的趋势,与口外海域的泥沙存在着活跃的交换。通过摩阻流速计算得到三门湾变化的总趋势是:深槽略受冲刷,滩涂缓慢淤涨,入湾通道处于动态平衡中。     

Some observational results of sea storm current

INTRODUCTIONDr. Hollister, a marine geologist of the Woods Hole Oceanographic Institution, firstpointed out that there was ocean storm current in the ocean. He found out the wavy texture inthe seabed core samples, and suggested that this wavy texture was caused by the high speedsea current in remote antiquity. He then suggested a bold hypothesis that there existed a benthic storm current near the ocean bottom, and presented this hypothesis at the IUGG confer-ence held at San Francisco…     

Modern Undersea Tunneling Technology and the Undersea Tunnel across Taiwan Strait

It is necessary to construct the undersea tunnel across the Taiwan Straits because it would help strengthen communication between Taiwan and the mainland, promote economic and cultural exchanges, and uphold national unification and territorial integrity. Nowadays, there are many undersea tunnels in the world; the English Channel Tunnel and the Seikan Tunnel are two of the most famous. Rich experience has been obtained during the exploration, surveying, design, construction and operation of these undersea tunnels. So, technologically, it is completely feasible to construct the undersea tunnel of the Taiwan Straits. The total length of the undersea Taiwan Straits tunnel is about 220 km; however, water along most of the proposed tunnel site, is less than 50 m deep and the geological condition of the site is relatively good. Although technical difficulties exists in design and construction, there are some favorable aspects. It is, therefore, necessary to start a study by launching some exploration surveys and collecting related data.     

Nitrate in groundwater of China: Sources and driving forces

Identifying the sources of reactive nitrogen (N) and quantifying their contributions to groundwater nitrate concentrations are critical to understanding the dynamics of groundwater nitrate contamination. Here we assessed groundwater nitrate contamination in China using literature analysis and N balance calculation in coupled human and natural systems. The source appointment via N balance was well validated by field data via literature analysis. Nitrate was detected in 96% of groundwater samples based on a common detection threshold of 0.2 mg N L^?1, and 28% of groundwater samples exceeded WHO's maximum contaminant level (10 mg N L^?1). Groundwater nitrate concentrations were the highest beneath industrial land (median: 34.6 mg N L^?1), followed by urban land (10.2 mg N L^?1), cropland (4.8 mg N L^?1), and rural human settlement (4.0 mg N L^?1), with the lowest found beneath natural land (0.8 mg N L^?1). During the period 1980–2008, total reactive N leakage to groundwater increased about 1.5 times, from 2.0 to 5.0 Tg N year^?1, in China. Despite that the contribution of cropland to the total amount of reactive N leakage to groundwater was reduced from 50 to 40% during the past three decades, cropland still was the single largest source, while the contribution from landfill rapidly increased from 10 to 34%. High reactive N leakage mainly occurred in relatively developed agricultural or urbanized regions with a large population. The amount of reactive N leakage to groundwater was mainly driven by anthropogenic factors (population, gross domestic product, urbanization rate and land use type). We constructed a high resolution map of reactive N source appointment and this could be the basis for future modeling of groundwater nitrate dynamics and for policy development on mitigation of groundwater contamination.