牡蛎低分子活性肽对人肺腺癌A549细胞形态与超微结构变化的影响

以牡蛎（Saccostrea cucullata）体内分离提取出的牡蛎天然低分子活性多肽（BPO-L，Bioactive Peptides of Oyster in Peak L）为效应物，观察研究BPO-L对人肺腺癌细胞形态和超微结构的影响．光镜观察显示经0．1mg／mL BPO-L处理后的A549细胞体积增大，趋于扁平铺展状态，细胞核质比例变小，核仁数量减少．透射电镜观察显示经0．1mg／mL BPO-L处理后的A549细胞核形态较规则，细胞核内异染色质减少，常染色质增多；细胞质内线粒体数量增多，结构较为一致，高尔基体呈较为典型发达状态，并出现粗面内质网增多和多聚核糖体减少等变化．结果表明，BPO-L能有效改变人肺腺癌细胞的恶性形态与超微结构特征，对肺癌细胞具有一定的诱导分化作用．     

某大型金-铜矿对环境的重金属污染及生态影响

对某金-铜矿山矿山的自然植被、矿区内外的土壤和水系进行金属污染分布特征及其迁移转化进行了系统地研究．结果表明：该矿的开采对矿区环境造成严重的重金属环境污染，水体污染程度要大于土壤污染程度，该矿区水体造成的是重污染，多金属复合污染，综合污染指数PI为12．084～83．848，不同重金属对地表水造成的污染程度分别为：As〉Cu〉Zn〉Cr，分别为国家Ⅲ类地表水标准的45．06、30．95、7．16和3．88倍．该矿区的土壤已造成轻等污染，其综合污染指数PI为1．038～1．856，平均为1．4515，其Cu和As分别是土壤环境质量三级标准（GB 15618-1995）11．406倍和2．774倍．矿区的植物也已经受到重金属污染，其Cu和As的含量分别是背景植物的5．21倍和3．90倍．     

花(鱼骨)胚胎发育及卵黄囊仔鱼形态的初步观察

运用多种处理方法对花的胚胎发育进行连续观察,并对其卵黄囊仔鱼形态变化进行初步观察与测量。观察结果显示:(1)花胚胎发育可以划分为22个明显的时期,包括7个主要的发育阶段;(2)在(20±1)℃条件下,仔鱼在出膜后的第3天开口摄食,卵黄囊在第7天基本消失,此阶段仔鱼的全长平均日增长率为4．67％,而以第4天增长最快。该实验结果将为花的人工繁殖及苗种培育,特别是为仔鱼在营养转换阶段的培育提供了理论参考。     

多参数通讯设定型力矩限制器的设计

为了设计适应多种型号起重机和提高现有工作精度的新型力矩限制器,采用了起重机多元参数调整,拟合计算曲线和实际工作曲线的方法,并结合通讯方式设定力矩限制器的工作参数,实现了适应不同型号起重机和不同量程范围传感器工作的新的力矩限制器系统。介绍了传感器性能选择、硬件系统框图和软件流程图。该系统已经在实际应用中取得良好的效果,工作精度提高到±4%。     

电场场量在真空和介质中表述的转化

处于静电场中的介质要被极化,极化产生的束缚电荷要产生束缚电场,该电场叠加到原来的电场中,构成静电平衡时的总电场.本文讨论了电场场量在真空中和在介质中表述的转化,说明当把场量中的介电常数0ε从换为ε时,其中已考虑了束缚电荷对场量的贡献,对场量无需作进一步处理即得到介质中场量的表述.     

高密度LiMn0.4 Ni0.4 Co0.2 O2正极材料的合成与研究

用一种改进的氢氧化物共沉淀法制备了粒径均一、近球形的Mn0.4Ni0.4Co0·2(OH)2,再通过高温固相合成法制备了高密度的LiMn0.4Ni0.4Co0·2O2正极材料。结果表明,在沉淀体系中加入F-,可以在较为宽松的条件下制备出振实密度为2·3g·cm-3的LiMn0.4Ni0.4Co0·2O2正极材料。对产物进行了XRD、SEM和充放电测试。SEM测试结果表明,产物具有良好的形貌;XRD测试表明,产物具有良好的层状结构,无杂质相存在。在充放电电压区间为3·0~4·4V,电流密度为30mA·g-1时,首次充电和放电容量分别为185和164mAh·g-1,经过50次循环,放电容量仍能保持90%。     

Lithostratigraphy and faunal aspects of marine Jurassic rocks in Thailand

Thai marine Jurassic rocks are well exposed in the Mae Sot, Umphang, and Phop Phra areas, less extensively near Mae Hong Son, Kanchanaburi, Chumphon, Nakhon Si Thammarat and Krabi. Generally they rest unconformably on Permian and Triassic, and are overlain by Quaternary strata. Fourteen lithostratigraphic units are defined (in ascending order): Pa Lan, Mai Hung, Kong Mu formations of the Huai Pong Group-Mae Hong Son area; Khun Huai, Doi Yot, Pha De formations of the Hua Fai Group-Mae Sot area; Klo Tho, Ta Sue Kho, Pu Khloe Khi, Lu Kloc Tu formations of the Umphang Group-Umphang area; and Khlong Min Formation-Chumphon, Nakhon Si Thammarat, and Krabi areas. Dominant widespread mudstones, siltstones and sandstones; limestones are confined to the Mae Sot, Phob Phra, Umphang, Kanchanaburi and Mae Hong Son areas; marls are found only in Mae Sot. Sequences are approximately 900 m thick (Mae Sot), 450 m thick (Umphang) and thinner elsewhere, especially the south. Based on ammonites, brackish to marine bivalves, and foraminifera, the beds are dated mainly as ToarcianEarly Bajocian.     

Depositional environments of Bathonian sediments from the Jaisalmer Basin, Rajasthan, western India

The pericratonic sedimentary Jaisalmer Basin, west of the Aravalli Ranges, on the westerly dipping eastern flank of the Indus Shelf, is a principal structural element of Rajasthan. Jurassic sediments in the SE comprise non-marine sandstones and conglomerates to nearshore, brackish to marine sands, silts, clays and carbonates, grouped lithostratigraphically into the Lathi, Jaisalmer, Baisakhi, and Bhadasar formations. The Late Bajocian to Oxfordian Jaisalmer Formation is divided, in ascending order, into the Hamira, Joyan, Fort, Badabag, Kuldhar, and Jajiya members. Fossil records providing a Bajocian to Bathonian age for the lower and middle parts of the formation include: a Late Bajocian coral Isastraea bernardiana (d’Orbigny) in the uppermost Joyan Member; Bathonian ammonite Clydoniceras in the basal part of the Badabag Member; Bathonian foraminiferal/bivalve assemblages in the Fort Member. The topmost bed of the Joyan Member represents the peak of first marine transgression of the Jaisalmer Basin, probably contemporaneous with the Late Bajocian one in the neighbouring Kachchh Basin. Based on faunal studies Bajocian to Bathonian sediments of the Jaisalmer Basin can be broadly correlated with those of the Kachchh Basin. The Fort and Badabag members represent the following depositional environments, in chronological order: (a) brackish to shallow fully marine; (b) fully marine with rapidly fluctuating water energy and sedimentation rates; (c) near-shore to lower shoreface with fluctuating energy conditions, salinity and sedimentation rates; (d) near-shore to shoreface channels and storm-dominated marine above fair-weather wave-base; (e) lagoon with fluctuating low to moderate energy, salinity and sedimentation rates; (f) stormdominated shelf to lower shoreface.     

Cs3ZnCl5:Co2+精细结构、EPR参量和磁化率研究

基于完全对角化方法和Zhao的半自洽场d轨道理论,从Cs3ZnCl5:Co2+的杂质局部结构对其光谱精细结构作了解释,在此基础上进一步计算了电子顺磁共振(EPR)g因子、零场分裂(ZFS)D值和顺磁磁化率,计算结果与实验值符合.     

基于模糊集μRX的α-截集和强β-截集的粗近似

研究了基于模糊集μRX的α-截集和强β-截集的粗近似问题,提出了(α,β)-粗糙集模型,讨论了粗糙近似算子的一些重要性质,给出了粗糙度和近似精度的定义和性质,证明了该模型比Pawlak粗糙集模型具有更好的精度.