海水中铜(Ⅱ)-固体粒子-氨基酸相互作用的红外光谱研究

本文测定了“氨基酸一CU(Ⅱ)-氧化物、粘土、碳酸钙”体系的红外光谱。结果表明:(1)对于“氨基酸-固体粒子”体系,吸附态氨基酸通过其-NH_3~+基团,而不是-COO~_,与表面羟基缔合。(2)对于“氨基酸-Cu(Ⅱ)”表面络合物,氨基酸之-NH_3~+与表面羟基缔合,而-COO~-与Cu(Ⅱ)络合,形成S-AA-Cu表面三元络合物。(3)随着Cu(Ⅱ)交换量增加,固体粒子-氨基酸-Cu(Ⅱ)之间的相互作用使表面缔合羟基发生分级变化。     

对虾白斑综合症病毒基因组同源重复区结合蛋白的筛选

对对虾白斑综合症病毒（WSSV）基因组序列分析发现，基因组3％的区域均匀分布有与昆虫杆状病毒类似的9个同源重复区，很可能具有昆虫杆状病毒同源重复区参与病毒复制起始或转录调控的功能．以WSSV基因组同源重复区中一个包含高度保守结构域的小重复片断DNA（210bp）作为配体，利用WSSV基因组噬菌体展示库，经过5轮淘选出一个可与DNA特异结合的重组噬菌体克隆，包含的外源DNA片断长度为306bp．通过与WSSV基因组序列对比，发现该序列为WSSV的ORFs中wsv 021的5’端部分．推测wsv 021是一个可能与病毒复制或调控相关的重要功能基因．     

冰排在锥面上的断裂长度

依据简化的窄锥冰力模型给出了冰排在锥面上弯曲断裂长度的分析解和无量纲参数（长厚比k)形式给出的结果。由此方法可得到与现场观测结果大体吻合的理论预测值。根据分析解，相关影响因素主要是冰排爬坡的阻力；取决于坡角和接触表面性质；其次是极限破坏时的接触宽度，与相互作用的过程相关，与相近分析模型的解及国外模型试验结果进行比较，说明提出的方程适用的主要范围是窄锥结构，并应满足弯曲变形的小挠度条件。     

寿南小沙丁鱼鳞片表面结构及轮纹特征的扫描电镜观察

运用扫描电镜技术对寿南小沙丁鱼鳞片形态结构及轮纹特征进行了观察。研究结果表明：寿南小沙丁鱼鳞片属圆鳞，与鲱形鳞相似。鳞片上有多少不一呈断裂状的辐射沟，环片呈山嵴状，与辐射沟基本平行，环片脊顶上有许多大小不同的卤状粒突。鳞片侧区的年轮和副轮清晰，在与年轮相交处，环片明显呈下凹弯曲，少数发生断裂。     

Characteristics of nitrogen forms in the southern Huanghai Sea surface sediments

The distributions of different forms of nitrogen in the surface sediments of the southern Huanghai Sea are different and affected by various factors. The contents of IEF-N, SOEF-N and TN gradually decrease eastward, and those of SAEF-N northward, while those of WAEF-N westward. Around the seaport of the old Huanghe (Yellow) River, the contents of both SOEF-N and TN are the highest. Among all the factors, the content of fine sediment is the predominant factor to affect the distributions of different forms of nitrogen. The contents of IEF-N, SOEF-N, and TN have visibly positive correlation with the content of f‘me sediments, and the correlative coefficient is 0.68, 0.58 and 0.71 respectively, showing that the contents of the three forms of nitrogen increase with those of f-me sediments. The content of WAEF-N is related to that of fine sediments to a certain extent, with a correlative coefficient of 0.35; while the content of SAEF-N is not related to that of fine sediments, showing that the content of SAEF-N is not controlled by fine grain-size fractions of sediments. In addition, the distributions of different forms of nitrogen are also interacted one another, and the contents of IEF-N and SOEF-N are obviously affected by TN, while those of inorganic nitrogen (WAEF-N, SAEF-N and IEF-N) are not affected by SOEF-N and TN obviously, although they are interacted each other.     

Nitrogen and Phosphorus Diffusive Fluxes Across the Sediment-Water Interface in Estuarine and Coastal Tidal Flats

Nitrogen and phosphorus contents are analyzed in the overlying waters and pore waters taken from the Changjiang Estuary and Shanghai coastal tidal flats in this study. In addition, the diffusion fluxes of nitrogen and phosphorus across the sediment-water interface in tidal flats are estimated according to the nutrient concentration gradients at the interface. It has been indicated that the concentrations of ammonium, nitrite, nitrate and dissolved phosphorus in overlying waters range from 0.0082～2.56, 0.03～0.58, 0.69～5.38 and 0.035～0.53 mg/L, respectively, while 0.0025 ～ 1.35 mg/L for NH4+-N, 0. 0055 ～ 0.20mg/L for NO2--N, 0.61～1.14 mg/L for NO3--N and 0.11～0.53mg/L for DP insurface pore waters.The findings have revealed that ammonium, nitrite, nitrate and dissolved phosphorus diffusion fluxes across the sediment-water interface are between -0.024～0.99, -0.39～ -0.0019, -3.09～the source of phosphorus and an important sink for nitrogen in the waters.