Gd_(1-x)Zn_xMnO_3系列化合物Rietveld结构分析

利用标准的固相反应法在1 350 ℃烧结了Gd(1-x)ZnxMnO3(x=0,0.2,0.4,0.6,0.8)样品.利用X射线衍射(XRD)对其晶体结构进行了研究.X射线衍射测量表明样品的单胞仍然具有正交结构.用Rielveld方法进行了结构精修,结果表明,随着Zn掺杂浓度的变化,导致A位原子半径的变化,样品的晶格常数、晶胞体积Mn-O键长、Mn-O-Mn键角随之变化.在Zn掺杂浓度x=0.4时,这种变化达最大.     

黑鱾（Girellaleonina）淀粉酶与蛋白酶的活力研究

通过测定1＋龄黑鱾的胃、盲囊、肝脏和肠道4个消化组织中蛋白酶和淀粉酶活性,并研究其与温度及pH值的关系,可以为黑纪的合理投饵提供理论依据．实验设9个温度梯度（10～50℃）和14个pH缓冲液梯度（pH2．0～9．0）,用淀粉-碘显色法测淀粉酶活力,用福林-酚试剂法测蛋白酶活力．结果表明：黑纪盲囊、肠道中淀粉酶和蛋白酶活力均较高,最适温度为35℃,淀粉酶最高活力为每克鲜组织46．02U和42．61U蛋白酶最高活力为每克鲜组织156．52u和147．79U;胃中酶的最适温度为40℃,肝脏中淀粉酶温度要求稍低,最适温度为30℃,酶活力值也最低;胃淀粉酶和胃蛋白酶最适pH值分别为6．5和3．5,盲囊、肠道和肝脏组织中的最适pH值相近,为7．0-8．0．可以认为黑鲍胃中主要存在着酸性蛋白酶,胃是食物蛋白质初步分解消化的场所;Q10值充分反映了温度对消化酶活力的影响,当温度从10℃上升至20℃时。2种消化酶活力增幅显著,可作为开始投饵的温度指标．     

用PCR技术检测生物硝化池污水中硝化细菌(Nitrobacteria)的研究

从生物硝化池污水水样中分离了硝化细菌ＤＮＡ,以其为模板,针对其１６ＳｒＲＮＡ基因及２３ＳｒＲＮＡ基因而设计合成了两对引物并分别进行了ＰＣＲ扩增,扩增产物的２％琼脂糖凝胶电泳结果显示,硝化细菌ＤＮＡ模板得到了特异性扩增．参照分子量标准（Ｍａｒｋｅｒ）的电泳结果,被扩增的ＤＮＡ条带大小分别约为４００ｂｐ和７３０ｂｐ．实验结果表明ＰＣＲ技术可用于污水中硝化细菌的快速检测     

Burgers方程新的多孤波解

在Backlund变换的基础上,通过改进准解的求解方法,给出了Burgers方程一批新的多孤波解．     

地下室外墙裂缝的成因分析与预防措施

针对地下室外墙易产生各种形式的裂缝, 分析了地下室外墙裂缝的主要特征, 讨论了地下室外墙混凝土裂缝产生的主要原因, 并针对性地提出了裂缝控制措施和与混凝土裂缝有关的见解, 以确保构件的耐久性, 保证结构的使用安全.     

二氢卟吩e~6-6-酰胺衍生物的合成

首次报道了以蚕沙叶绿素初提物为基础原料,经酸降解得到含焦脱镁叶绿酸a和脱镁叶绿酸a的混合物,不经分离直接与胺类反应使脱镁叶绿酸a的戊酮环(V)裂开,合成得11种二氢卟吩e~6-6-酰胺衍生物。提供了一种合成二氢卟吩酰胺的新方法。     

Measurements of climatic parameters and ground-level ozone at Terra Nova Bay in Antarctica

Summary The results of local meteorology, solar radiation and ground-level ozone measurements taken in Antarctica during the second Italian expedition (December 86–February 87) at Terra Nova Bay are presented. During the summer months the site of the Italian base camp is characterized by a thin strip of deglaciated ground, along which the temperature measurements close to the ground and up to 6 m high show a strongly superdiabatic profile. This irregular trend of the temperature in the surface layer is mainly due to the notable incoming amounts of radiation and to the extreme transparency of the atmosphere. This is also shown by the low values of the ratio between total radiation and diffuse radiation. The ground is thus subjected to intense heating, especially in the warmer hours of the day, while the surface layer of the atmosphere will be characterized by strong upward heat fluxes and by turbulent convective movements. Vertical-temperature-profile measurements show an almost forced persistence in the superdiabatic trend, which tends towards isothermic values only as a resultof rapid variations in the direction and intensity of the wind, connected to the downward flux of cold air masses, shown also by the simultaneous increases in ground-level ozone concentrations which would support the presence of dry-deposition processes in the lower layer. However, the complex local orography and the horizontal discontinuity (sea, deglaciated coast, snow-covered surfaces) do not permit a correct application of profile flux relations, normally used in studies on groundlevel dry-deposition. Paper presented at the IV Congresso del Gruppo Nazionale per la Fisica dell'Atmosfera e dell'Oceano, June 22–24, 1987, Rome.     

Infrared spectrum and vibrational potential function of thionylimide (HNSO)

The ir absorption of gaseous HNSO, DNSO and H¹⁵NSO is recorded in the range 300–4100 cm^?1 at medium resolution. Besides the fundamental vibrations, overtones and combination bands are measured and assigned. From these data, combined with the ir absorptions of four more isotopic species of thionylimide, and with the centrifugal distortion constants of HNSO and DNSO, a harmonic force field, with 11 constants was derived.     

关于Cp,q圆型域的酉曲率

先用级数法得到圆型域Cp，q=E｜a｜z1｜^2/p＋b｜z2｜^2/q〈1，0〈a，b≤1，p，q为正整数｜的Bergman核函数显表达式，然后计算了它的Bergman度量，酉曲率和Ricci曲率。     

Boltzmann-Poisson方程组初边值问题的整体弱解

§ 1.　Introduction　　LetΩ R3beasmoothboundedopenset,f(t,x ,v)bethedistributionfunctionofcar riersattimet >0 ,positionvectorx∈Ωandvelocityvectorv∈R3.Theforcefieldactingonthecarriersisdenotedbythe3 dimensionalvectorfunctionE(t,x) ,thepotentialcorespondingtoE(t,x)isdenotedbyu(t,x) ,then (f,E)satisfythefollowingBoltzmann Poissonsystem tf +v· xf +E· vf =Q(f) ,　 (t,x ,v)∈R+ ×Ω×R3,(1 .1 )E =- xu ,-Δxu =ρ ,　 (t,x) ∈R+ ×Ω ,(1 .2 )whereρ(t,x) =∫R3 f(t,x ,v)dvisthecarriernum…