The in vivo expression of the globin genes of theβ cistron in γ-,δ-, andδβ-thalassemia heterozygotes

There is considerable evidence suggesting that the switch from to and chain production after birth is due, in part, to silencing of the genes by stage-specific factors which bind to their promoters and to the competition from the adult ( and ) genes for a common enhancer element located in the locus control region. As a consequence one can expect that the increased Hb F production in adults with hereditary persistence of fetal hemoglobin or -thalassemia is directed mainly by -globin genes in cis to the deletion(s) responsible for these conditions. Here we review data on heterozygotes with -, -, or -thalassemia, who also had an^AT mutation, in cis or in trans, which was used as a marker of gene expression. The results show that a deletion affecting adult genes favors the expression of genes in cis, while the deletion of a single gene does not affect the expression of the gene in cis but leads to a faster switch postnatally.     

一类一阶线性非齐次方程组的解法

利用二阶线性微分方程的可解定理,给出一阶线性非齐次方程组的一种新解法     

有间隙系统自激振动的近似解析解

对有间隙系统自激振动非线性方程的解析解进行了分析,通常平均法产生误差的重要原因在于假设平均法的解时未考虑间隙的影响,从而提出一种新的方法,即加权平均法。经验证,计算精度符合工程要求,为某些非线性方程提供了一条求其近似解析解的途径。     

Critical slope gradient for compulsory abandonment of farmland on the hilly Loess Plateau

Scientific evidence for the upper limit of farmland is proposed. Shallow gully erosion is one of erosion types distributed extensively on sloping farmland in the hilly regions of the Loess Plateau. Field observation and aerial photos interpretation, as well as laboratory experiments show that the shallow gully erosion occurring on the steeper farmland in the hilly regions of the Loess Plateau is an important factor leading to intensive erosion on slope, because of its extensive distribution and intensive runoff collection. The data on the formation, development and distribution of shallow gullies on sloping farmland indicate that critical slope gradient for shallow gully initiation ranges from 15 to 20 degrees with an average of 18.2 degrees. Therefore, it is suggested that critical slope gradient for compulsory abandonment of farmland on the hilly Loess Plateau should be kept within the critical slope gradient for shallow gully initiation to prevent shallow gully formation in order to control soil loss more effectively. But as the first step, the cultivation on the slopes with slope larger than 25 degrees where the maximum erosion occurs should be strictly forbidden.     

稳定非线性动力系统周期的计算机分析

提出采用后继函数法来确定非线性动力系统的周期,并编制计算机程序对Ｖａｎ ｄｅｒ Ｐｏｌ方程实例计算周期和绘制相图,结果表明,该方法计算结果准确且实用性强,本方法不但适合于求解保守系统和具 周期解非线性动力系统的周期,也适合于耗散系统和不稳定系统的分析。     

直线电机瞬态特性的场路耦合分析法

运用磁网络法,进行了单边直线感应电动机的性能分析。提出了此种电机的磁网络模型,由电磁场方程导出了磁网络的参数,从而考虑了直线电机边端效应、绕组不对称分布等结构特点。场路耦合及机电耦合法的运用,使文中提供的分析模型更接近实际情况,适合于动态特性的分析     

保守系统的混沌同步

发现保守系统相空间中的一个轨道囚禁区．用闭环控制方法将系统引入囚禁区并在其内实现了同步．     

关于运城地区发展经济林的反思

优越的农业自然条件使运城地区成为山西省重要的粮棉生产基地。但近年来经济林的迅速发展使果树栽植面积几乎占到耕地总面积的1／4。尽管平原地区广种经济林具有一定的经济效益与环境效益,但它却违背了合理利用土地的原则,若不及早采取有力措施加以控制,我国将会潜伏粮食危机,种植业的可持续发展将会受到严重影响。     

AlGaAs／GaAs HBT基区电流的研究

在ALGaAs/GaAs HBT E-M模型直流参数的研究基础上,对HBT的基区电流进行了研究,特别是针对BE结空间电荷区的复合电流和基区表面复合电流,因为在HBT的小偏置情况下,HBT的BE结空间电荷区的复合电流和基区表面复合电流在整个基区电流中占有主导地位。当BE结间外加电压为0.5-1.2V时,ALGaAs HBT的基区电流的计算机模拟值和测试值比较接近,这一研究结果有助于进一步了解HBT的直流特性和1/?噪声特性。     

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.