Clifford半群的平坦性刻划

半群Ｓ称为Ｃｌｉｆｏｒｄ半群,如果它是群的强半格．利用左Ｓ１系的平坦性给出了Ｃｌｉｆｏｒｄ半群的特征刻划．     

一种改进的树形矢量量化编码算法

矢量量化中的一个最严重的问题是在一本码本中搜索最近码字的高计算复杂度。本文在研究树形矢量量化的基础上提出了一种改进的树形矢量量化编码算法。实验结果表明,本文提出的编码算法相对于树形矢量量化算法可大大改善峰值信噪比（ＰＳＮＲ）。     

一些基本图的〔强〕自同态摹群

确定了一些基本图的〔强〕自同态摹群的基数,并在证明过程中实际上确定了这些摹群的全部元素,同时发现确定一些极其简单的图之自同态摹群却是极其困难的事情,有时甚至导致一些一般的组合难题．     

与星（m,r）——正交的（g,f）——因子分解

设ｇ和ｆ是定义图Ｇ的顶点集Ｖ（Ｇ）上的整值函数。本文证明了如下结果：设ｒ是一个正整数,Ｇ是一个（ｍｇ＋ｍ－１,ｍｆ－ｍ＋１）—图,且ｇ（ｘ）≥ｒ－１,对ｘ∈Ｖ（Ｇ）。若Ｈ是Ｇ的一个有ｍｒ条边的星,则Ｇ有（ｇ,ｆ）—因子分解与Ｈ（ｍ,ｒ）—正交。     

苯甲醛缩氨基硫脲Cu(I)、Zn(Ⅱ)配合物的直接电化学合成

用电化学金属阳极氧化法在非水溶剂中合成了苯甲醛缩氨基硫脲（ＨＬ）与Ｃｕ（Ｉ）、Ｚｎ（Ⅱ）配合物,通过元素分析、红外光谱、紫外光谱、磁矩、摩尔电导等对配合物进行了表征。     

海芋凝集素的理化性质鉴定

采用葡聚糖凝胶１００（ＳｅｐｈａｄｅｘＧ－１００）从天南星科植物海芋（Ａｌｏｃａｓｉａｏｄｏｒａ（Ｒｏｘｂ）Ｃ．Ｋｏｃｈ）中分离出了一种凝集素（简称ＡＯＬ）．ＡＯＬ对兔血有较强的凝集效果,而对各类型人血的凝集活力较弱,在３种糖蛋白中,猪甲状腺球蛋白对ＡＯＬ的凝血活力抑制最强;ＡＯＬ对培养人外周血白细胞的转化率高达７９％,超过对照ＰＨＡ的转化率;用ＳｅｐｈａｄｅｘＧ－２００柱测得ＡＯＬ的相对分子质量为３１５００;用癌细胞体外培养的方法证明了ＡＯＬ对肺腺癌细胞株Ｐ１８具有较强的直接杀伤能力．此外还发现ＡＯＬ对温度（８０℃以下）、变性剂（盐酸胍和脲）有较高的稳定性,在ｐＨ６～１０的范围内相当稳定．     

盐胁迫下Na^＋,K^＋,Cl^—对碱蓬和玉米离子的吸收效应

用ＮａＣｌ、ＫＣｌ、ＮａＮＯ３和ＫＮＯ３处理碱蓬（Ｓｕａｅｄａｓａｌｓａ）和玉米（Ｚｅａｍａｙｓ）幼苗,发现ＮａＣｌ胁迫引起Ｋ＋、Ｃａ２＋、Ｍｇ２＋、Ｆｅ２＋、Ｚｎ２＋、ＮＯ－３等必需元素的含量降低．认为ＫＣｌ和ＫＮＯ３处理引起碱蓬幼苗幼叶黄化的主要原因是Ｎａ＋的缺乏;ＫＣｌ处理引起玉米和碱蓬幼苗的干枯死亡主要是由于植物体内高浓度Ｃｌ－引起的;Ｎａ＋是引起盐生植物碱蓬叶片肉质化的重要因子;Ｃｌ－是刺激碱蓬生长的重要因子     

Stability of the Sarcin/Ricin domain of 28S RNA in rat ribosome under hydrostatic pressure

Under 2 100 bar of hydrostatic pressure, KNA N-glycosidase can still cleave the N-C bond of adenosine at position 4324 in R/S domain of 28S RNA in rat ribosome, demonstrating that high pressure has no effect on the tertiary structure of S/R domain.     

High-precision timing of the Quaternary standard samples with thermal ionization mass spectrometry (TIMS) U-series method

Two national stalagmite standard (GBW04412, GBW04413) and one international coral standard (RKM_4) have been determined by using thermal ionization mass spectrometry (TIMS) method. The values of ( 234 U/ 238 U) act , ( 230 Th/ 234 U) act and age are all consistent in error range with the standard values obtained by using α spectrometry.     

New evidence for the Qinghai-Xizang (Tibet) Plateau as a pilot region of climatic fluctuation in China

Over 40 a observed temperature data in 172 stations in China and historical proxy data were analyzed. Evidence suggested that during 1980–1994, the warmest year appeared first in southeastern part of the Qinghai-Xizang (Tibet) Plateau (henceforth SETP) and then gradually spread northwards and eastwards to eastern China. The climatic change on century time scale in recent 600 a shows 3 relatively warm and clod stages in China. Each warm and cold stage appeared first in Tibet Plateau (henceforth TP) and then in the Qilian Mountains, then in the eastern parts of China. The warm and cold stages in TP were 10–60 a earlier than in the eastern China. The facts show that TP is a pilot region of climatic fluctuation in China on the time scale shorter than 10³a.