三七总皂苷对海马CA1区长时程增强效应的影响

三七总皂苷(Panax notoginseng saponins,PNS)是从传统中药三七的根中提取的主要有效成分,具有改善血液循环、耐缺氧、改善记忆力、抗衰老等多方面的生理活性.本研究采用"盲法"全细胞膜片钳技术观察PNS对大鼠海马CA1区锥体神经元长时程增强效应(LTP)的影响,以分析其增强学习记忆功能的神经电生理机制.以断头法分离Wistar大鼠(3～4 周)海马半脑,用切片机切出400 μm厚度的海马脑片,以全细胞电压钳制方式记录CA1区锥体细胞的兴奋性突触后电流(EPSCs),给予高频刺激HFS(100 Hz)诱导LTP,分析PNS对大鼠海马CA1区EPSCs和LTP的影响.结果表明,PNS(0.1～0.4 g·L-1)能显著抑制EPSCs(P＜0.05),且对海马CA1区LTP无易化作用;但PNS(0.04～0.05 g·L-1)不影响CA1区的EPSCs基础突触传递(P＞0.05),却可以增强HFS诱发的LTP(P＜0.05).上述结果提示,PNS(0.04～0.05 g·L-1)能易化海马CA1区锥体神经元的长时程增强效应,该作用应是其增进学习记忆力的神经电生理机制.

工艺流程中高浓定影液酸度的流线分析方法研究

每种酸碱指示剂在其变色PH范围内都有一个明显的颜色变化，在其相应的PH-A曲线上总存在一段直线部分，通过选择一定PH变色范围和适当浓度的指示剂，就能使各指示剂PH-A曲线上的直线部分相互迭加成一条新的直线，从而加宽了混合指示剂的表现变色PH范围，依此原理，本论文以二种流动注射分析方法独立地完成了工艺流程中高浓定影液酸度的在线分析。并对这二种方法做了简单的对比。（一）工艺流程中高浓定影液酸度的在线分析方法研究（1）我们选择了内含0.08%溴甲酚紫，0.04%溴百里酚兰，0.02%甲酚红组成的混合指示剂的6%稀释液作为试剂，以C-41CX定影浓缩液作载流，用F2A-分光光度法完成了高浓度定影液酸度的在线测定，相对标准偏差在50.2%以内，采样频率为100次/h，分析周期很短（25秒），在5.5～8.0PH范围内，PH-A工作曲线具有很好的线性关系，相关系数0.9996，斜率即灵敏度达到：0.198A/PH。（二）工艺流程中高浓定影液酸遮掩在线分析方法研究（2）我们造反了0.005%的溴甲酚紫，0.009%的溴百里酚兰和0.025%的甲酚红作为混合酸碱指示剂，以蒸馏水作载流，通过选择最佳测定条件用流动注射-分光光度法（F2A-Spectrophotometry）在线测定了不宜用其它分析法测定的高浓溶液的酸度。该分析方法还可以推广到其它高浓溶液的酸度的在线测定。相对误差在±0.2%以内；分析周期为30秒；采样体积为60μL。在5.2～8.5PH范围内，混合指示剂的PH-A工作曲线具有良好的线性关系，相关系数达到0.9991，工作曲线斜率即是灵敏度达到0.376A/PH。

金硅面垒~8Be探测器的研制

介绍了金硅面垒8Be探测器的制造工艺和测试结果。有效面积157~570mm2,厚度为280μm,工作电压100~150V时,其漏电流0.04~0.12μA。对于8.78MeV α粒子的能量分辨率为0.54%~0.80%,用该探测器通过对8Be带电粒子的角关联测量确定高激发能级的宇称及自旋。

Nd~(3+)掺杂对LiFePO_4结构及电化学性能的改善

采用两步加热高温固相法合成了掺杂Nd3+的LiFe1-xNdxPO4/C复合材料(x=0,0.01,0.02,0.04,0.06,0.08)。用TG-DSC对前驱体进行分析和SQUID(超导量子干涉仪)对样品中Fe3+的磁性测定,优化了合成工艺条件;采用XRD、FE-SEM、EDS等方法分析了样品的结构并对其电化学性能进行了测试。结果表明:LiFe1-xNdxPO4/C复合材料具有橄榄石型结构;当Nd3+的掺杂量6%(物质的量分数)、煅烧温度700℃、煅烧时间16 h时,样品在0.2C(1C=170.0 mA.g-1)电流密度下的最大放电比容量可达165.2 mAh.g-1,循环100次后的容量保持率仍为92.8%,在1C、2C、5C下的最大放电比容量分别为146.8、125.7和114.8 mAh.g-1。通过测定样品在不同较低倍率下的放电比容量,采用外推法得出制备样品的实测理论比容量为168.7 mAh.g-1。

Electrooxidative polymerization of phenothiazine derivatives on screen-printed carbon electrode and its application to determine NADH in flow injection analysis system

The electrooxidation polymerization of phenothiazine derivatives, including azure A and toluidine blue 0, has been studied at screen-printed carbon electrodes in neutral phosphate buffer. Both compounds yield strongly adsorbed electroactive polymer with reversible behavior and formal potentials closed to 0.04 V at pH 6.9. The modified electrodes exhibited good stability and electrocatalysis for NADH oxidation in phosphate buffer (pH 6.9), with an overpotential of more than 500 mV lower than that of the bare electrodes. Further, the modified screen-printed carbon electrodes were found to be promising as an amperometric detector for the flow injection analysis (FIA) of NADH, typically with a dynamic range of 0.5-100 muM.

黄海纤毛虫的丰度和生物量

海洋浮游纤毛虫是在海洋中浮游生活的一类单细胞原生动物，主要是指寡毛类纤毛虫(Oligotrich ciliates)，隶属原生动物界(Protozoa)、纤毛门(Ciliophora)、寡毛纲(Oligotrichea)，分属于Oligotrichina 和Tintinnina两个亚纲。它们个体微小，粒径在5-200 µm之间，是微型浮游动物和海洋微食物环(Marine Microbial Food Web)的重要组成部分。 2006年4月至2007年12月，在黄海(包括胶州湾)采样分析海洋浮游纤毛虫的种类组成(砂壳纤毛虫)、丰度和生物量，分析纤毛虫在这一海区的季节变化和空间变化。 纤毛虫丰度和生物量的研究方法为：Rosette采水器(胶州湾用Niskin采水器)采集水样，取1 L水样，加Lugol’s试剂固定(终浓度1%)，Utermöhl方法100倍镜检。测量虫体的体长、体宽，按最接近的几何形状(圆柱体、球体和圆锥体)计算体积。生物量由体积乘转换系数(0.19 pgC/µm3)得到，砂壳纤毛虫的肉体体积按照壳体积的1/3近似。 本文的结果表明，胶州湾各站纤毛虫平均丰度于6月达到全年最高值6065 ind./L，12月为全年丰度最低值843 ind./L。平均生物量8月达全年最高值(18.5 µg C/L)，6月为全年最低值(0.6 µg C/L)。砂壳纤毛虫种丰富度于8月达到最高值，共发现25种砂壳纤毛虫，1月种类最少(6种)。湾内站位的纤毛虫平均丰度比湾外的高(6月和8月除外)。砂壳纤毛虫在纤毛虫总丰度中的比例较小，平均为25%，范围为8-57%，分别于1月和8月达到最低和最高值。 两次冷水团大面调查结果表明，4月表层纤毛虫平均丰度(1490 ind./L)要高于10月(972 ind./L)。10月表层纤毛虫生物量0.14-5.33 µg C/L，14194站、15694站和15894站生物量较高，为4.08-5.33 µg C/L。无壳纤毛虫优势种Laboea strobila在两个航次中均呈现斑块分布，4月航次丰度0-10000 ind./L，10月航次丰度11-350 ind./L；砂壳纤毛虫优势种Ptychocylis obtusa仅在4月航次发现，最大丰度2895 ind./L，10月航次未发现。4月航次砂壳纤毛虫有百乐拟铃虫(Tintinnopsis beroidea)，丰度为0-1920 ind./L；卡拉直克拟铃虫(Tintinnopsis karajacensis)，丰度很小(10-93 ind./L)。10月航次砂壳纤毛虫优势种Tintinnidium primitivum，丰度为35-700 ind./L；也出现了尖底类瓮虫(Amphorellopsis acuta)和网纹虫(Favella spp.)，但丰度不大(0-210 ind./L)；运动类铃虫(Codonellopsis mobilis)、筒状拟铃虫(Tintinnopsis tubulosoides)和Eutintinnus sp.丰度也较低(35-105 ind./L)；Craterella torulata丰度为0-120 ind./L，主要分布于15694站。10月航次已经出现了温跃层，位于30 m左右水层，纤毛虫主要分布于温跃层之上。 六次黄海断面航次表明：温跃层在5月已经出现，到12月消失。在有温跃层的5月、6月、8月、9月，纤毛虫主要分布于温跃层(30 m左右)之上。其中8月份航次纤毛虫丰度最高，表层平均丰度3103 ind./L。12月份纤毛虫丰度最低，表层平均丰度406 ind./L。纤毛虫生物量春夏季为0.02-5.5 µg C/L，冬季为0.04-1.99 µg C/L。小型无壳纤毛虫占优势，砂壳纤毛虫东方拟铃虫(Tintinnopsis orientalis)、筒状拟铃虫、运动类铃虫、Craterella torulata和Tintinnidium primitivum几乎在各个航次均有分布。

西江流域环境河水地球化学研究

River is a major component of the global surface water and CO2 cycles. The chemistry of river waters reveals the nature of weathering on a basin-wide scale and helps us understand the exogenic cycles of elements in the continent-river-ocean system. In particular, geochemical investigation of large river gives important information on the biogeochemical cycles of the elements, chemical weathering rates, physical erosion rates and CO2 consumption during the weathering of the rocks within the drainage basin. Its importance has led to a number of detailed geochemical studies on some of the world's large and medium-size river systems. Flowing in the south of China, the Xijiang River is the second largest river in the China with respect to its discharge, after the Yangtze River. Its headwaters drain the YunGui Plateau, where altitude is approximately 2000 meters. Geologically, the carbonate rocks are widely spread in the river drainage basin, which covers an area of about 0.17xl06 km2, i.e., 39% of the whole drainage basin. This study focuses on the chemistry of the Xijiang river system and constitutes the first geochemical investigation into major and trace elements concentrations for both suspended and dissolved loads of this river and its main tributaries, and Sr isotopic composition of the dissolved load is also investigated, in order to determine both chemical weathering and mechanical erosion rates. As compared with the other large rivers of the world, the Xijiang River is characterized by higher major element concentration. The dissolved major cations average 1.17, 0.33, 0.15, and 0.04 mmol I"1 for Ca, Mg, Na, and K, respectively. The total cation concentrations (TZ+) in these rivers vary between 2.2 and 4.4 meq I'1. The high concentration of Ca and Mg, high (Ca+Mg)/(Na+K) ratio (7.9), enormous alkalinity and low dissolved SiO2/HCO3 ratio (0.05) in river waters reveal the importance of carbonate weathering and relatively weak silicate weathering over the river drainage basin. The major elements in river water, such as the alkalis and alkaline-earths, are of different origins: from rain water, silicate weathering, carbonate and evaporite weathering. A mixing model based on mass budget equation is used in this study, which allows the proportions of each element derived from the different source to be calculated. The carbonate weathering is the main source of these elements in the Xijiang drainage basin. The contribution of rainwater, especially for Na, reaches to approximately 50% in some tributaries. Dissolved elemental concentration of the river waters are corrected for rain inputs (mainly oceanic salts), the elemental concentrations derived from the different rock weathering are calculated. As a consequence, silicate, carbonate and total rock weathering rates, together with the consumption rates of atmospheric CO2 by weathering of each of these lithologies have been estimated. They provide specific chemical erosion rates varying between 5.1~17.8 t/km2/yr for silicate, 95.5~157.2 t/km2/yr for carbonate, and 100.6-169.1 t/km2/yr for total rock, respectively. CO2 consumptions by silicate and carbonate weathering approach 13><109and 270.5x10 mol/yr. Mechanical denudation rates deduced from the multi-year average of suspended load concentrations range from 92-874 t/km2/yr. The high denudation rates are mainly attributable to high relief and heavy rainfall, and acid rain is very frequent in the drainage basin, may exceed 50% and the pH value of rainwater may be <4.0, result from SO2 pollution in the atmosphere, results in the dissolution of carbonates and aluminosilicates and hence accelerates the chemical erosion rate. The compositions of minerals and elements of suspended particulate matter are also investigated. The most soluble elements (e.g. Ca, Na, Sr, Mg) are strongly depleted in the suspended phase with respect to upper continent crust, which reflects the high intensity of rock weathering in the drainage basin. Some elements (e.g. Pb, Cu, Co, Cr) show positive anomalies, Pb/Th ratios in suspended matter approach 7 times (Liu Jiang) to 10 times (Nanpan Jiang) the crustal value. The enrichment of these elements in suspended matter reflects the intensity both of anthropogenic pollution and adsorption processes onto particles. The contents of the soluble fraction of rare earth elements (REE) in the river are low, and REE mainly reside in particulate phase. In dissolved phase, the PAAS-normalized distribution patterns show significant HREE enrichment with (La/Yb) SN=0.26~0.94 and Ce depletion with (Ce/Ce*) SN=0.31-0.98, and the most pronounced negative Ce anomalies occur in rivers of high pH. In the suspended phase, the rivers have LREE-enriched patterns relative to PAAS, with (La/Yb) SN=1 -00-1 .40. The results suggest that pH is a major factor controlling both the absolute abundances of REE in solution and the fractionation of REE of dissolved phase. Ce depletion in river waters with high pH values results probably from both preferential removal of Ce onto Fe-Mn oxide coating of particles and CeC^ sedimentation. This process is known to occur in the marine environment and may also occur in high pH rivers. Positive correlations are also observed between La/Yb ratio and DOC, HCO3", PO4", suggesting that colloids and (or) adsorption processes play an important role in the control of these elements.

贵州喀斯特高原湖泊物质循环过程中的铜锌同位素地球化学－以红枫湖、阿哈湖为例

近年来铜、锌同位素地球化学研究已经进入了快速发展时期。作为新兴的同位素技术手段，铜锌同位素工具已普遍应用于地球化学、矿床学、古海洋学和生物学等多种领域，然而铜、锌同位素在湖泊生态系统中的研究却相对较少。湖泊生态系统中，重金属的迁移、循环与转化一直是地球科学家们关注的焦点，但研究手段仅局限于含量与形态的测定。因此本论文旨在通过对湖泊生态系统中铜、锌同位素的研究，揭示影响铜、锌同位素组成的主要因素，为铜、锌同位素成为湖泊系统中新的重金属示踪工具奠定基础。 本论文通过一系列条件实验，确定了用于MC-ICP-MS测定环境样品中铜、锌同位素时最佳的化学分离条件。随后选取红枫湖和阿哈湖为主要研究对象，用此实验流程对湖泊水体及其主要支流悬浮物中的铜、锌同位素的季节及剖面变化进行了初步研究。除此之外，对水体中重金属如Cu、Zn、Mn、Ni、Co、Cr、Cd和Pb的形态分布特征及物质循环进行了研究。主要得出以下几点认识： 1、环境样品中铜锌的最佳分离条件是，采用AG MP-1(100-200目)阴离子交换树脂，分别以7 mol/L HCl + 0.001% H2O2，2 mol/L HCl+ 0.001% H2O2，0.5 mol/L HNO3作为淋洗液，并分别在适当的体积接收淋洗液，可以有效地分离沉积物、植物和悬浮物等样品中的铜和锌。化学分离过程中回收率接近100％，同位素比值的变化均在误差范围以内。 2、红枫湖、阿哈湖水体及主要支流悬浮物和红枫湖生物样品中的δ65Cu分布范围为-2.64‰~1.11‰，可达到3.75‰的变化。红枫湖夏季水体悬浮物的δ65Cu变化为-0.08‰~0.25‰，入湖河流水体悬浮物δ65Cu的变化范围为0.13‰~ 1.11‰；阿哈湖夏季水体悬浮物δ65Cu的变化范围为-0.62‰~0.37‰，入湖河流水体悬浮物δ65Cu的变化范围为-1.08‰~0.60‰。两湖冬季水体悬浮物的δ65Cu值均较负。红枫湖生物样品中δ65Cu较负（-1.54‰~ 0.03‰）。 红枫湖水体悬浮物中δ65Cu的随水深的变化趋势主要受到藻类吸收作用的控制，而阿哈湖δ65Cu的随水深的变化趋势主要受到其物源的控制。说明在贫营养化湖泊中，铜同位素组成可以示踪物源；而在富营养化湖泊中，铜同位素组成则可以示踪生物活动。同时水温的垂直变化也可能是其影响因素之一。 3、红枫湖水体及其主要支流水体悬浮物中的δ66Zn变化范围分别为-0.29‰~0.26‰和-0.04‰~0.48‰，阿哈湖水体及其主要支流水体悬浮物中的δ66Zn变化范围分别为-0.18‰~0.27‰和-0.17‰~0.46‰，均表现出支流中的锌同位素组成较重的趋势。而生物样品中的δ66Zn变化范围较大，为-0.35‰~0.57‰。说明湖泊生态系统中各端元的锌同位素组成存在明显差异。 红枫湖夏季δ66Zn随着湖水深度的变化，与Chla（叶绿素）呈极显著的正相关(R=0.97)。说明锌同位素组成与藻类生物量有一定的响应关系，主要是藻类对锌的有机吸附或是吸收过程改变了锌同位素组成。阿哈湖的锌同位素组成主要受到其源区的控制作用，从而可利用锌同位素示踪源区；此外，红枫湖和阿哈湖悬浮物中的锌同位素比值均表现出夏季小于冬季，说明大气的干湿沉降可能是一个较负的锌同位素源。生物样品中的δ66Zn变化范围较大，说明由于生物作用过程导致的锌同位素分馏大于非生物过程。 4、红枫湖重金属Mn、Ni、Co、Cr、Cd和Pb的含量在南湖高于北湖，主要是羊昌湖的输入所导致；重金属入湖通量的季节性变化，直接导致了重金属含量的季节性变化。沉积物－水界面在冬夏季节，由于“富氧”和“贫氧”状态的改变，导致了溶解态Mn、Ni和Cr的季节性变化；水粒相互作用过程中，溶解有机碳（DOC）、氧化铁胶体、氧化锰胶体和水生藻类的生长繁殖，影响了重金属不同结合形态的变化。

Kinetic measurements of cell surface E-selectin/carbohydrate ligand interactions

Selectin/ligand interactions initiate the multistep adhesion and signaling cascades in the recruitment of leukocytes from circulation to inflamed tissues and may also play a role in tumor metastasis. Kinetic properties of these interactions are essential determinants governing blood-borne cells' tethering to and rolling on the vessel wall. Extending our recently developed micropipette method, we have measured the kinetic rates of E-selectin/ligand interactions. Red cells coated with an E-selectin construct were allowed to bind HL-60 or Colo-205 cells bearing carbohydrate ligands. Specific adhesions were observed to occur at isolated points, the frequency of which followed a Poisson distribution. These point attachments were formed at the same rate with both the HL-60 and Colo-205 cells (0.14 +/- 0.04 and 0.13 +/- 0.03 mum(2) s(-1) per unit density of E-selectin, respectively) but dissociated from the former at a rate twice as fast as did from the latter (0.92 +/- 0.23 and 0.44 +/- 0.10 s(-1), respectively). The reverse rates agree well with those measured by the flow chamber. The forward rates are orders of magnitude higher than those of Fc gamma receptors interacting with IgG measured under similar conditions, consistent with the rapid kinetics requirement for the function of E-selectin/ligand binding, which is to capture leukocytes on endothelial surfaces from flow.

Viscosity, Surface Tension, and Atomization of Water-Methanol and Diesel Emulsions

This article is the result of experimental studies of the rheologv, viscosities, surface tensions, and atomization of water-methanol and diesel emulsions. The Span 80 and Tween 60 are employed to make three emulsifying agents, Y01, Y02, and Y03, with viscosity of 1.32-1.5 Pa s and HLB values of 5.36, 4.83, and 4.51, respectively. In the water-in-oil emulsions, the aqueous phase is between 10% and 50%; the agent concentration added is 0.8-8.0%. The viscosity of the emulsions is 0.003-0.02 Pa s, and the surface tens ion is 0.04-0.1 N/m. The types and concentrations of agents significantly influence the viscosity of the emulsions, and the higher concentration of the aqueous phase (<50%) in creases the viscosities of the emulsions, especially for higher agent concentration. Interfacial membrane and HLB values of the agents can explain all these phenomena. Higher aqueous phase concentration and agent viscosity results in larger Sauter mean diameter.

Experimental Investigation Of Particle Velocity Distributions In Windblown Sand Movement

With the PDPA (Phase Doppler Particle Analyzer) measurement technology, the probability distributions of particle impact and lift-off velocities on bed surface and the particle velocity distributions at different heights are detected in a wind tunnel. The results show that the probability distribution of impact and lift-off velocities of sand grains can be expressed by a log-normal function, and that of impact and lift-off angles complies with an exponential function. The mean impact angle is between 28 degrees and 39 degrees, and the mean lift-off angle ranges from 30 degrees to 44 degrees. The mean lift-off velocity is 0.81-0.9 times the mean impact velocity. The proportion of backward-impacting particles is 0.05-0.11, and that of backward-entrained particles ranges from 0.04 to 0.13. The probability distribution of particle horizontal velocity at 4 mm height is positive skew, the horizontal velocity of particles at 20 mm height varies widely, and the variation of the particle horizontal velocity at 80 mm height is less than that at 20 mm height. The probability distribution of particle vertical velocity at different heights can be described as a normal function.

三相交流工频等离子体冶炼高锡钨中矿制取钨铁

简单地介绍了寻求新的冶炼钨铁工艺的现实意义,着重复述了用三相交流工频等离子体冶炼高锡钨中矿制取钨铁的冶炼原理、冶炼过程、工业扩大试验得到的结果及放料的情况。用WO_3为46.54％、Sn含量超标61倍、Cu为8.3倍、As为0.6倍的不合标准的钨中矿为原料,冶炼出钨铁达到:W含量为78％,Sn为0.02％～0.03％、Cu0.03％～0.06％、As小于0.04％、其它杂质也低于标准,W的直收率为95％～98％。依据工业扩大试验的结果,每吨钨铁盈利为6300元以上。

爆炸焊接飞板运动的研究

本文通过量纲分析指出,爆炸焊接飞扳运动是几何相似的。不过,由于起爆端端部稀疏波的作用,飞板运动存在着非稳定运动段,在该段内确定飞板极大动态弯折角的相似参数有两个:一个是R;一个是炸药厚度与爆轰波波阵面距起爆端距离之比he/VDt。在稳定运动段内,确定飞板极大动态弯折角的相似参数只有一个R。试验结果证明,最纲分析的结论是正确的;并确定了he/V_(Dt)=0.04是稳定运动和非稳定运动的分界,它是制定大厚度扳焊接方案的依据之一。

风沙流中沙粒速度分布的实验研究

采用相位多普勒粒子分析仪(phase Doppler particle analyzer,PDPA)测量了风沙两相流动中沙床面上沙粒碰撞和起跳速度概率分布以及不同高度处沙粒速度概率分布.结果表明,沙床面上沙粒碰撞和起跳速度概率分布均可用对数正态分布函数描述,碰撞和起跳角度均可用指数分布函数描述.沙粒平均碰撞角度为28°～39°,平均起跳角度为30°～44°,平均起跳速度为平均碰撞速度的0.81～0.9倍,向后碰撞沙粒占总碰撞沙粒的比例为0.05～0.11,向后起跳沙粒占总起跳沙粒的比例为0.04～0.13.沙粒水平速度概率分布在4mm高度处表现为正偏斜类型,在20mm高度处沙粒水平速度的变化范围更加广泛,在80mm高度处沙粒水平速度变化范围小于20mm高度处的变化范围.沙粒垂直速度概率分布在不同高度处均可表示为正态分布函数.