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。     

GaN/Al_xGa_(1-x)N量子点中类氢杂质位置对激子态的影响

利用有效质量方法和变分原理,考虑内建电场效应和量子点(QD)的三维约束效应,研究类氢杂质对GaN/AlxGa1-xN量子点中激子态的影响.结果表明:量子点中心的类氢杂质使激子的结合能升高,基态能降低,QD系统的稳定性增强,发光波长红移.杂质位于量子点上界面时,激子的基态能最小,结合能最大,系统最稳定.随着杂质从量子点的上界面沿着Z轴移至下界面,激子基态能增大,结合能减小,带间发光蓝移.     

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.     

Ⅲ族氮化物量子点中类氢施主杂质位置对束缚激子结合能的影响

在有效质量近似下，运用变分方法，考虑内建电场效应和量子点（QD）的三维约束效应的情况下，研究了类氢施主杂质在量子点中的位置对Ⅲ族氮化物量子点中束缚激子结合能的影响。结果表明：当类氢施主杂质位于量子点中心时，对于InxGa1-xN／GaN量子点，量子点高度和In含量存在临界值，当参数大于临界值时，约束在QD中束缚激子的结合能升高，激子态的稳定性增强，提高了激子的离解温度，使人们能在较高的温度条件下观察到半导体量子点吸收谱中的激子峰。而类氢施主杂质总是使束缚在GaN／AlxGa1-xN量子点中激子的结合能升高，载流子被更强的约束在量子点中。说明对GaN／AlxGa1-xN量子点，杂质使人们能在更高温度下观察到量子点中的激子。类氢施主杂质位于量子点上界面时，束缚激子的结合能最大，系统最稳定；随着施主杂质下移，激子结合能减小，激子的离解温度下降。     

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.     

新型箱状组合压型钢板承载力研究

箱状组合压型钢板是压型板发展的一种新的结构形式，为进一步研究其性质，介绍了它的现场载荷实验情况，描述了建立有限元模型的过程，结合实验数据比较了3种模型，分析了两种因素对构件性质的影响，并通过实验数据对不同厚度的3种构件的性质做了对比。     

平均场加邻近轨道相互作用对力模型对超铀区大形变核的应用

利用严格可解的平均场加邻近轨道相互作用对力模型来描述大形变核 .将该模型应用于超铀区的核素 .计算了2 2 6 2 3 4 Th ,2 3 0 2 40 U及2 3 6 2 43 Pu同位素的结合能和对激发能 ,并与实验结果进行比较 .     

Abnormal overpressure distribution and natural gas accumulation in foreland basins,Western China

Shizitan in Jixian County, Shanxi Province, is a site of transitional period from Paleolithic to Neolithic. The dating and the sporopollen analysis show that the middle reaches of the Yellow River where the site is located had been maintaining a steppe environment during 35.1-9.4 kaBP, in which, 35.1-17 kaBP belonged to the last glacial. With cold and dry climate, this period featured a desert steppe environment. In the late of this period, the area had a cold and half-humid steppe environment. The 17.0-11.9 kaBP belonged to the early- and mid-period of the last deglaciation. Mild and half-arid steppe alternates with mild and half-arid steppe, with a small amount of deciduous broadleaf species. During the period of 11.9-10.5 kaBP, cold and dry glacial climate appeared once more, featuring a desert steppe environment. During 10.5-9.4 kaBP, it is mild and half-arid, and later transited toward warm and half-humid. The early phase of this period featured a steppe environment and the later transited into a steppe environment with fairly more deciduous broadleaf species. Microlith, a mark of a transitional period from Paleolithic to Neolithic, was distributed mainly in 17.0-11.9 kaBP. The relatively warm, half-arid and fluctuating steppe environment in the early and medium period of the last deglaciation made a contribution to the appearance and development of Microlithic culture.