ω-超广义函数的卷积运算

讨论ω-超广义函数间中的卷积运算，并且给出了一些超广义函数卷积运算的公式。     

6种凤仙花属(Impatiens L.)植物叶表皮特征的微形态学研究

应用扫描电子显微镜技术首次研究了6种凤仙花属(Impatiens L.)植物的叶表皮微形态学特征,结果表明:6种凤仙花属植物叶片上表皮纹饰为网状、不规则细波状或曲叉状,其中曲叉状纹饰为一种较特殊的纹饰特征;气孔仅分布在叶片的下表面,呈不规则排列,形状为椭圆形或宽椭圆形,长度在10.5-25.6μm之间,气孔外拱盖内缘平滑或近平滑,多数种类气孔的保卫细胞两极具“T”型加厚.叶表面纹饰,气孔的形状、大小及气孔保卫细胞两极“T”型加厚等特征在种间具有一定的差异,可作为该属植物分类的重要特征之一.文中还探讨了叶表皮微形态学特征在凤仙花属分类中的意义及有关紫花黄金凤的分类学地位问题.     

Mo/HZSM-5催化剂上甲烷脱氢芳构化反应——催化剂蒸汽处理的影响

对机械混合法制备的Mo/HZSM-5催化剂进行蒸汽后处理,利用XRD、XPS等表征催化剂的晶相结构、Mo物种的分散度,在关联催化剂活性评价基础上,研究了催化剂的蒸气处理过程对Mo物种的分散度及其芳构化反应性能的影响.结果表明,机械混合法制备的催化剂上,Mo物种主要以微晶的形式分布在分子筛的外表面,由于缺少分子筛孔道择形保护,便于积炭副反应的发生.经高温蒸气处理后,催化剂上Mo物种的分散度显著提高,有较多的Mo物种迁移至分子筛的孔道内,并与B酸发生强相互作用生成钼氧二聚体,有效地增强了催化剂的抗积炭能力.因此,蒸气处理的Mo/HZSM-5催化剂的芳烃选择性和催化稳定性较传统机械混合法制备的催化剂有明显提高.     

Taylor中值函数的若干分析性质

文献[1-6]对微分中值定理及Taylor定理"中间点"的渐近性质进行了研究,作者在此基础上给出了"Taylor中值函数"的定义,对Taylor中值函数的分析性质进行了系统的讨论,证明了Taylor中值函数的单调性、可积性、连续性、可微性等分析性质.     

蚕豆根尖微核技术检测金属冶炼厂废水污染状况

以滇东某金属冶炼厂废水出水口、距出水口2公里处和8公里处水样,并参照已测定的该厂所排废水中铜、锌、锰、铅和镉5种金属离子的含量配制溶液再稀释100和1000倍后的水样,共5个水样处理蚕豆根尖,用微核技术检测该厂废水污染状况.结果表明:该厂排放废水污染程度随着与出水口距离的增加有所减轻;此外,除稀释1000倍水样外,其他水样均为重污染或中度污染,单因素方差分析和多重比较结果显示,除稀释1000倍水样外,其他测试水样处理结果与对照均有极显著差异(P<0.01).     

三角形并联微通道换热特性研究

基于Navier-Stokes方程的传统理论,把整个实验硅晶片上的所有并联微通道纳入计算区域,通过FLUENT商业软件对其进行数值模拟.计算得到的温度场和实验结果的红外成像数据对比,吻合得很好,从而验证了数值计算的正确性.对并联通道中的不同通道计算结果表明,不同微通道中流量几乎没有差异,但是不能完全忽略热流密度的差异.此外,通过三角形微通道在壁面上的热流密度分布很不均匀,与矩形通道截然相反;轴向导热对热流密度的分布有很大影响.在进出口温差较大时,用进出口平均温度作定性温度计算的结果与变物性计算的结果相比,误差很小.     

珠江口桂山岛沉积物甲烷厌氧氧化作用研究

系统分析了珠江口桂山岛沉积物间隙水甲烷和硫酸盐、pH和溶解无机碳(DIC)以及δ13C-CH4和δ13C-DIC的垂直剖面分布.结果显示:间隙水硫酸盐浓度呈线性梯度减小,至沉积物SMI(sulfate-methane interface)附近,硫酸盐几乎全部消耗而甲烷浓度急剧增大,与此同时,间隙水pH和DIC在该深度位置明显升高.间隙水地球化学特征揭示了沉积物发生了甲烷厌氧氧化(AOM)作用.在AOM过程中,由于12CH4氧化速率较13CH4快,故引起沉积物间隙水剩余甲烷的碳同位素偏重,而δ13C-DIC值变为极负.由扩散公式计算结果可知,AOM消耗沉积物间隙水硫酸盐占总硫酸盐的比例为58.6%,该过程产生的DIC占间隙水总DIC的比例为41.4%.沉积物有机质的活性及含量大小对AOM作用的发生及其强度有重要的影响,该研究区沉积物活性有机质(主要为海洋来源)在沉积物表层通过矿化分解作用消耗,从而导致进入沉积物硫酸盐还原带底部的活性有机质数量减少,在该条件下,部分硫酸盐将转为与甲烷反应消耗,从而引发AOM.     

Pseudo-particle modeling for gas flow in microchannels

The velocity profiles and temperature distributions of gas flow in microchannels, for Knudsen numbers ranging from 0.01 to 0.20, are investigated with pseudo-particle modeling (PPM). It has been found that the velocity profiles are mainly affected by Knudsen number and the external force fields applied. When Knudsen number was increased, the slip velocities on the walls increased at the beginning, and then decreased. The temperature distributions were also significantly affected by the external force. The Darcy friction factor increased with increasing Knudsen number, and its variation with Mach number under increased Knudsen number was similar to the so-called premature laminar-turbulent transition observed in experiments.     

Study on peptide-peptide interaction using high-performance affinity chromatography and quartz crystal microbalance biosensor

The specific interaction between sense and antisense peptides was studied by high-performance affinity chromatography （HPAC） and quartz crystal microbalance （QCM） biosensor. Fragment 1-14 of human interferon-β （hlFN-βwas chosen as sense peptide and its three antisense peptides （AS-IFN 1, AS-IFN 2, and AS-IFN 3） were designed according to the degeneracy of genetic codes. The affinity column was prepared with sense peptide as ligand and the affinity chromatographic behavior was evaluated. Glu-substituted antisense peptide （AS-IFN 3） showed the strongest binding to immobilized sense peptide at pH 7.5. A quartz crystal microbalance-flow injection analysis （QCM-FIA） system was introduced to investigate the recognition process in real-time. The equilibrium dissociation constants between sense peptide and AS-IFN 1, AS-IFN 2 and AS-IFN 3 measured 2.08×10^-4, 1.31×10^-4 and 2.22×10^-5 mol/L, respectively. The mechanism study indicated that the specific recognition between sense peptide and AS-IFN 3 was due to sequence-dependent and multi-modal affinity interaction.     

Authigenic sulfide minerals and their sulfur isotopes in sediments of the northern continental slope of the South China Sea and their implications for methane flux and gas hydrate formation

This is a report of the study of the authigenic sulfide minerals and their sulfur isotopes in a sediment core (NH-1) collected on the northern continental slope of the South China Sea, where other geo-physical and geochemical evidence seems to suggest gas hydrate formation in the sediments. The study has led to the findings: (1) the pyrite content in sediments was relatively high and its grain size relatively large compared with that in normal pelagic or hemipelagic sediments; (2) the shallowest depth of the acid volatile sulfide (AVS) content maximum was at 437.5 cm (>2 μmol/g), which was deeper than that of the authigenic pyrite content maximum (at 141.5-380.5 cm); (3) δ 34S of authigenic pyrite was positive (maximum: 15‰) at depth interval of 250-380 cm; (4) the positive δ 34S coincided with pyrite enrichment. Compared with the results obtained from the Black Sea sediments by Jorgen-sen and coworkers, these observations indicated that at the NH-1 site, the depth of the sulfate-methane interface (SMI) would be or once was at about 437.5-547.5 cm and the relatively shallow SMI depth suggested high upward methane fluxes. This was in good agreement with the results obtained from pore water sulfate gradients and core head-space methane concentrations in sediment cores collected in the area. All available evidence suggested that methane gas hydrate formation may exist or may have existed in the underlying sediments.