用静息细胞培养法研究L－谷氨酸氧化酶的生物合成

建立了静息细胞培养系统，并以此研究了Ｌ－谷氨酸氧化酶生物合成的影响因素。结果表明，发酵１６ｈ的菌体在有诱导物情况下有酶的合成，无诱导物则无酶的合成，发酵４０ｈ的菌体在有、无诱导物的条件下均有酶的合成。对发酵１６ｈ的菌体研究表明：β－丙氨酸（Ⅰ）、α－酮戊二酸（Ⅱ）、丙酮酸钠（Ⅲ）是酶合成的诱导物，谷氨酸（Ⅳ）则不是。而对发酵４０ｈ菌体而言：ＭｇＣｌ＿２，ＣａＣｌ＿２能促进酶的合成；Ⅰ不能作氮源利用；Ⅰ～Ⅳ均具有高浓度抑制产酶、低浓度促进产酶的双重作用。     

B位元素掺杂对Y-Ba-Cu-O系ABO_3化合物超导电性影响的研究

自高T_c氧化物超导陶瓷出现以来,已提出了许多可能与超导电性相关的因素。为探讨这些因素对超导性的影响,对元素掺杂的研究有着重要的意义。按照容许因子公式的要求,我们选择了满足ABO_3化合物中B位要求条件下的过渡族元素,将它们掺入(YBa)CuO_3中时,能部分取代Cu的位置而处于B位上。这样利用B位元素的少量掺杂,可以作为“结构探针”引出与周围O的2P电子、氧缺位及Cu、稀土离子等相互作用信息的变化,有助于对超导微观机理的了解;又因为ABO_3化合物     

发酵代谢物对葡萄糖氧化酶生物合成的影响

用膜透析技术和静息细胞系统，对影响葡萄糖氧化酶（ＧＯＤ）发酵的控制因素进行了研究。静息细胞系统显示：鸟氨酸、谷氨酸、甘氨酸、丙氨酸、丝氨酸和胱氨酸等氨基酸对ＧＯＤ的合成有促进作用；葡萄糖酸和丙酮酸对ＧＯＤ的合成有阻遏作用，１．５ｍｍｏｌ／Ｌ的丙酮酸使酶活降低４６．２４％；２０ｍｍｏｌ／Ｌ的葡萄糖酸使酶活降低２１％左右，但葡萄糖酸浓度增大，有被菌体作为碳源利用的可能。利用膜透析技术可除去部分发酵过程中产生的葡萄糖酸和丙酮酸等阻遏物，减少它们对ＧＯＤ合成的分解代谢物的阻遏作用，与分批发酵相比．提高酶活４０％左右。     

Radiolarian record to paleoecological environment change events over the past 1.2 MaBP in the southern South China Sea

This note studies the Radiolarian fossil groups since 1.2 MaBP in ODP leg 184 site 1143, the southern South China Sea (SCS). The result shows that radiolarian abundance experienced a significant variation: before 0.9 MaBP it remained at the extremely low level, but increased with low extent between 0.9–0.65 Ma, which corresponded to the Mid-Pleistocene Transition stage, and it increased rapidly after 0.65 MaBP. During the whole process, the average abundance became higher and higher in each stage, and showed regularly periodic fluctuations. The obvious increase after 0.65 MaBP is inferred to result from the enhanced upwelling in this region, which was induced by the intensified monsoon circulation after the “Mid-Pleistocene Transition”. An outstanding result of the spectral analyses is that a long oscillation of ∼ 0.2 Ma cycle was found in the records of radiolarian abundance and complex diversity, which corresponds well to the result of other paleoceanographic indexes. This probably indicated a special cycle characteristic of paleoecological environment evolution in this area. In addition, all of the radiolarian indexes show an obvious boundary in about 0.47 MaBP, indicating the abrupt variation of the community structure and radiolarian abundance level before and after 0.47 MaBP. So we suppose that there existed a distinct change event of oceanic ecology environment during that period.     

Behavior of argon gas release from manganese oxide minerals as revealed by <Superscript>40</Superscript>Ar/<Superscript>39</Superscript>Ar laser incremental heating analysis

Manganese oxides in association with paleo- weathering may provide significant insights into the multiple factors affecting the formation and evolution of weathering profiles, such as temperature, precipitation, and biodiversity. Laser probe step-heating analysis of supergene hollandite and cryptomelane samples collected from central Queensland, Australia, yield well-defined plateaus andconsistent isochron ages, confirming the feasibility dating very-fined supergene manganese oxides by 40Ar/39Ar technique. Two distinct structural sites hostingAr isotopes can be identified in light of their degassing behaviors obtained byincremental heating analyses. The first site, releasing its gas fraction at thelaser power 0.2-0.4 W, yields primarily 40Aratm, 38Aratm, and 36Aratm (atmospheric Ar isotopes). The second sites yield predominantly 40Ar* (radiogenic 40Ar),39ArK, and 38ArK (nucleogenic components), at ～0.5-1.0 W. There is no significant Ar gas released at the laser power higher than 1.0 W, indicating the breakdown of the tunnel sites hosting the radiogenic and nucleogenic components. The excellent match between the degassing behaviors of 40Ar*, 39ArK, and 38ArK suggests that these isotopes occupy the same crystallographic sites and that 39ArK lossfrom the tunnel site by recoil during neutron irradiation and/or bake-out procedure preceding isotopic analysis does not occur. Present investigation supports that neither the overwhelming atmospheric 40Ar nor the very-fined nature of the supergene manganese oxides poses problems in extracting meaningful weathering geochronological information by analyzing supergene manganese oxides minerals.     

晋北山地樟子松人工林生长及立地质量的研究

介绍了晋北山地樟子松人工林生长及立地质量研究的材料及研究方法，对研究结果进行了分析，最后为樟子松速生丰产林基地选择和经营规划提供了科学依据。     

软弱夹层土对软土场地地震效应的影响

本文以来自天津某工程的一场地为原型,对软夹层的埋深和厚度对软土场地地震效应的影响进行了数值分析.为了分析软弱夹层的埋深和厚度对地表地震动参数的影响,分别对原剖面进行了以下处理：软弱夹层的埋深从2 m增加到62 m,构造了16个剖面;软弱夹层的厚度从2 m增加到10 m,构造了5个剖面.选用Taft、ElCentro和Northridge地震记录作为输入地震动,利用程序SHAKE91对不同的构造剖面、不同的输入地震波及不同的峰值加速度水平,进行了场地地震反应分析,结果表明：对于给定的输入地震动和峰值加速度水平,随着软弱夹层埋深的增加,地表加速度峰值和放大系数λ都有减小的趋势,当埋深超过一定值后,地表加速度放大系数小于1.0;软弱夹层厚度对地表加速度峰值的影响与软弱夹层所处位置有关.     

Discovery of the budding phosphatized globular fossils from the Neoproterozoic Doushantuo Formation at Weng’an, Guizhou Province, China

There is much debate on biological affinities of the phosphatized globular fossils from the Neoproterozoic Doushantuo phosphorites at Weng’an, Guizhou Province. Here we report for the first time the budding structures of some of these globular fossils, which have previously been interpreted as the resting eggs and early cleavage embryos of metazoans. The budding structures are similar to the germinating tubes of the spore and zygote of living algae, suggesting that some globular fossils from the Doushantuo phosphorites bear affinity with algae. The present new information indicated various biological affinity of the phosphatized globular fossils from the Doushantuo phosphorites.     

CBA与NBA球队主客场赛防守技战术运用的比较研究

用观察和统计法,对CBA和NBA球队主客场赛防守技战术运用效果进行比较.结果发现:CBA球队客场全场紧逼战术和第1阶段主场防守效果好于NBA球队;第3阶段主场防守篮板球的效果与NBA球队存在差距,两者在防守技战术运用效果的稳定性上也存在差距.