具粘弹性支承的柔轴弹性盘转子系统的动力学分析

讨论了柔轴弹性圆盘转子系统在粘弹性支承下的临界转速和动力稳定性问题，轴和支承具有不对称的阻尼系数和刚度系数，利用能量法和耗散系统的Lagrange方程推导了系统的运动微分主程，阐述了求解方法，大多数的不稳定区出现在不平衡共振附近，通常可以通过调整轴、支承的阻尼和刚度系数的恰当组合来减小不稳定区域。     

离子选择电极法测定NBPG与银、镉、汞的配合物组成和稳定常数

本文用离子选择电极法测定了N,N—二甲基膦酸基甘氨酸(NBPG)与银、镉、汞的配合物组成和稳定常数。结果表明,NBPG与Ag~ 、Cd~(2 )、Hg~(2 )均生成组成为1:1的多齿质子型配合物。其lgK_稳值分别为:AgL5.28、CdH_3L3.63、CdH_2L5.16、CdHL7.30、CdL11.56、HgH_3L6.06、HgH_2L7.55、HgHL8.24、HgL12.58。     

黑米天然黑(紫)色素的研究

特种稻黑米品种的糙米果皮中,含有大量的稀有天然黑(紫)色素。本文研究了这种色素的提取与分离方法、化学结构及其稳定性,并对其药理作用和应用前景作了简要分析。     

Using antisense nucleic acid technology to study the influence of POLκ on genetic stability

AIM:To establish cell line FL-POLκ^- and to study the role ofPOLκ(polymerase kappa) on genetic stability.METHODS:A mammalian expression vector expressing antisense POLκ gene fragment pMAMneo -amp^--POLκ was constructed by cloning the 1 690-1 918 fragment of POLκ gene into the mammalian expression vector pMAMneo-amp^- in antisense orientation. FL cells were fransfected with this antisense RNA expressing vector and selected by G418. Based on the shuttle-plasmid pZ189, the mutation assay was made.RESULTS:The spontaneous mutation frequency of supF tRNA gene in the plasmid replicated in the FL- POLκ^- was 11.2×10^-4, while it was 4.9×10^-4 and 3.7×10^-4 in the control cells FL and FL-M, respectively.CONCLUSION: POLκ playes an important role in maintenance of genetic stability.     

赤峰市松山区土地利用动态变化及其原因分析

以TM遥感资料为信息源 ,利用 3S技术手段 ,对内蒙古自治区赤峰市松山区 1987,1993,2 0 0 0年的土地利用变化进行了分析。结果表明 ,在不同年度内 ,其主要的土地利用类型为耕地、草地和林地。土地利用类型的总量变化也以这 3种土地利用类型和建设用地变化最大。而从年变化速率看 ,1987- 2 0 0 0年 ,以建设用地的增加和未利用土地类型的减少最为快速。从土地利用类型转化的方向看 ,以耕地、草地和林地相互之间的转化最为频繁。从土地利用类型的空间稳定性看 ,耕地的稳定性最高 ,其次为草地 ;而最不稳定的土地利用类型为未利用土地。利用相关分析所作的土地利用变化动因显示 ,该地区土地利用变化的驱动因素主要是社会与经济因素 ,其中以总人口、农业总产值、粮食作物产量总计、农牧民人均纯收入、化肥使用面积和化肥实物量等因子的作用最大 ,而自然因素对该地区土地利用变化的影响极小。     

天山北麓的水资源利用与绿洲稳定性-以玛纳斯河流域为例

玛纳斯河是天山北麓最大的河流流域 ,玛纳斯流域拥有天山北麓最大的绿洲 ,以玛纳斯河流域绿洲为研究对象 ,来分析天山北麓水资源的利用对流域绿洲稳定性的影响。天山北麓自然环境体现为山地 -绿洲 -荒漠复合生态系统。绿洲是干旱区所特有的一类景观 ,它是一个人工与自然的复合生态系统 ,它作为发育在干旱气候大背景下的隐域性的自然景观 ,水分条件是决定其存在和发展的基础。天山北麓地区人类活动历史悠久 ,对水资源利用的影响较大 ,也是引起天山北麓绿洲演变、分布变化及其稳定性的重要因子。处于不同地貌位置的绿洲 ,由于其水资源特点不同 ,绿洲的稳定性以及绿洲演变规律也有所区别。总的来说 ,绿洲的稳定性由其内部与外部生态系统的结构、功能及生态过程决定 ,直接关系到区域社会经济的持续发展 ,水资源状况及利用是关系到天山北麓绿洲稳定性的关键性因素。合理利用水资源 ,可保持绿洲面积的稳定性 ,绿洲分布的稳定性 ,以及绿洲生态系统结构、功能的稳定性 ;水资源利用不当会导致绿洲内部土地发生大面积次生盐渍化 ,绿洲外围则由于生态用水不足加之人为破坏 ,使作为绿洲屏障的过渡带转变成生态断裂带 ,威胁绿洲的稳定性。利用工程技术方法和工程管理方法解决好灌区水利工程存在的问题 ;实施高新技术?     

Plantago ovata in broiler chicken nutrition: Performance,carcass criteria,intestinal morphology,immunity, and intestinal bacterial population

In this experiment, the effect of dietary Plantago ovata (PO) on performance, carcass criteria, intestinal morphology, immunity, and intestinal bacterial population of broiler chickens was evaluated. A total of 250 one‐day‐old male broiler chicks (Ross 308) were randomly assigned to five treatments containing 0, 5, 10, 15, or 20 g/kg of PO with five replicate pens and 10 birds in each replicate. Dietary PO increased body weight gain and decreased feed conversion ratio in the finisher period, improving the performance index (p < .05). Dietary treatments had no effects on carcass criteria, but breast meat percentage showed an increasing trend with incremental levels of PO in the diet (p = .069). The length of small intestine, especially jejunum section, as well as the villus height, villus width, villus area, and goblet cell numbers were significantly increased with supplemental PO (p < .05). Humoral and cellular immunity parameters, and oxidation stability of meat were improved due to use of dietary PO (p < .05). Dietary PO decreased the CFU of Escherichia coli, whereas the Lactobacilli population was increased (p = .001). Broken‐line regression revealed that dietary PO at the rate of 10 g/kg may results in the best performance in broiler chickens. This study showed that PO at the level of 10 g/kg could be considered as a beneficial feed additive in broiler diet.     

径向谐和激励下圆形隧道衬砌的动力稳定性

对径向谐和激励下圆形隧道的动力稳定性进行了研究，从动荷载下衬砌结构的振动方程出发，得到了隧道衬砌动力失稳临界频率计算公式，对可能影响隧道衬砌动力稳定性的因素进行了参数分析，探讨了系统参数，如地基土的性质、衬砌径厚比、外激励的性质以及系统的阻尼对衬砌动力稳定性的影响，计算结果表明：隧道周围土体的性质以及系统阻尼对衬砌的动力稳定性影响不大；相反，衬砌的厚度和外激励特性对衬砌的动力不稳定区域影响较大     

Evaluating biodegradability of soil organic matter by its thermal stability and chemical composition

The stability of soil organic matter (SOM) as it relates to resistance to microbial degradation has important implications for nutrient cycling, emission of greenhouse gases, and C sequestration. Hence, there is interest in developing new ways to quantify and characterise the labile and stable forms of SOM. Our objective in this study was to evaluate SOM under widely contrasting management regimes to determine whether the variation in chemical composition and resistance to pyrolysis observed for various constituent C fractions could be related to their resistance to decomposition. Samples from the same soil under permanent pasture, an arable cropping rotation, and chemical fallow were physically fractionated (sand: 2000-50 μm; silt: 50-5 μm, and clay: <5 μm). Biodegradability of the SOM in size fractions and whole soils was assessed in a laboratory mineralization study. Thermal stability was determined by analytical pyrolysis using a Rock-Eval pyrolyser, and chemical composition was characterized by X-ray absorption near-edge structure (XANES) spectroscopy at the C and N K-edges. Relative to the pasture soil, SOM in the arable and fallow soils declined by 30% and 40%, respectively. The mineralization bioassay showed that SOM in whole soil and soil fractions under fallow was less susceptible to biodegradation than that in other management practices. The SOM in the sand fraction was significantly more biodegradable than that in the silt or clay fractions. Analysis by XANES showed a proportional increase in carboxylates and a reduction in amides (protein) and aromatics in the fallow whole soil compared to the pasture and arable soils. Moreover, protein depletion was greatest in the sand fraction of the fallow soil. Sand fractions in fallow and arable soils were, however, relatively enriched in plant-derived phenols, aromatics, and carboxylates compared to the sand fraction of pasture soils. Analytical pyrolysis showed distinct differences in the thermal stability of SOM among the whole soil and their size fractions; it also showed that the loss of SOM generally involved preferential degradation of H-rich compounds. The temperature at which half of the C was pyrolyzed was strongly correlated with mineralizable C, providing good evidence for a link between the biological and thermal stability of SOM.