浅析二阶齐次线性变系数微分方程的一个可积类型

本文讨论了二阶齐次线性变系数微分方程的特殊形式，给出了这种微分方程的一个可积类型．     

Global well-posedness for the 3-D MHD equations with partial diffusion in the periodic domain

In this paper, we prove the global well-posedness of the 3-D magnetohydrodynamics(MHD) equations with partial diffusion in the periodic domain when the initial velocity is small and the initial magnetic field is close to a background magnetic field satisfying the Diophantine condition.     

Evolution of the South China Sea and monsoon history revealed in deep-sea records

As the third summary report of ODP Leg 184 to the South China Sea (SCS), this paper discusses the evolution of the East Asian monsoon and the SCS basin. A multi-proxy approach, involving geochemistry, micropale-ontology, pollen and other analyses, was adopted for reconstructing the evolutionary history of the East Asian monsoon, which was characterized by a series of paleo-climate events especially at 8, 3.2, 2.2 and 0.4 Ma. The new record indicates similar stages in the development of the East and South Asian monsoons, with an enhanced winter monsoon over East Asia being the major difference. The rich spectrums of monsoon variability from the southern SCS also reveal other characteristic features of the low latitude ocean. Evidence for the evolution of the SCS includes the hemipelagic Oligocene sediments, implying the existence of deep water environments during the early seafloor spreading stage of the SCS basin. The four major unconformities and some remarkabl ediagenetic features in upper Oligocene deposits indicate the strongest tectonic events in the region. From a careful comparison of lithologies and sedimentation rates, we conclude that the prominent differences in sedimentary environments between the southern and northern SCS were established only by ～3 Ma.     

西藏日喀则地区恰布林组物源分析

长期以来，沿西藏雅鲁藏布江南岸呈东西向展布的恰布林组砾岩，被认为是造山期后磨拉石的产物，而被置于第三纪。由于在屯穷紫色泥岩底部灰绿色粉砂质灰岩中发现腹足类化石Ｋａｔｏｓｉｒａｓｐ．，并结合其他地质证据，可以确定该组时代属于早中侏罗世。结合岩石学特征、典型砾岩中砾石的岩石地球化学和物源区分析表明，恰布林组砾岩的砾石有相当一部分来自蛇绿岩，其特征明显不同于现今的雅鲁藏布江蛇绿岩。因此认为雅鲁藏布江存在早中侏罗世之前的古蛇绿岩。     

古新世—始新世界线全球构造事件在沉积学中的反映

最新研究成果表明，古新世—始新世界线是全球构造事件的结果。这一事件在沉积学中表现为：岩性上从海绿石石英砂岩变化到粘土；粘土矿物组合从伊利石／蒙脱石为主到高岭石为主；大陆植物群的绝灭和迁移；钙质超微化石物种更新速度增长；底栖有孔虫绝灭和分异度降低；碳、氧同位素强烈负异常；大陆哺乳动物演化发生变化。     

敏感及抗性棉铃虫不同龄期幼虫神经细胞Na+通道电生理特性的比较研究

用膜片钳技术分析了棉铃虫三氟氯氰菊酯抗性品系(R)及其同源对照品系(S)不同龄期幼虫神经细胞电压门控Na^ 通道的电生理特性．结果表明，S幼虫神经细胞Na^ 通道的激活电压介于-50～-30mV，约70％细胞的Na^ 通道在-40mV左右激活．Na^ 通道电流(1Na)的峰值电压介于-30～0mV，约72％细胞的1Na在-20mV左右达峰值．R幼虫Na^ 通道的激活电压介于-50～-20mV，约60％细胞的Na^ 通道在-40mV左右激活，约30％的在-30～-20mV激活．2龄幼虫(R2)约76％细胞的1Na在-20mV左右达峰值．R3和R4均有60％以上细胞的INa在-10～OmV达峰值，即R3和R4多数细胞1Na的峰值电压向正电位方向移动．上述结果表明R幼虫神经细胞Na^ 通道功能发生了变异，同时也提示R幼虫在不同发育阶段其Na^ 通道的表达不同．     

Deep-water Earliest Oligocene Glacial Maximum （EOGM） in South Atlantic

The most prominent cooling event of the Earth surface during Cenozoic in the long-term transition from a non-glaciated planet, or “green-house world”, to a polar, glaciated planet, or “ice-house world”, is the Earliest Oligocene Glacial Maximum (EOGM) above the Eocene/Oligocene boundary at about 33.7 Ma. Planktonic and benthic foraminiferal oxygen and carbon isotopes, carbonate content, and coarse fraction, along with high-resolution color reflectance and magnetic susceptibility records during 35-30 Ma, from deep-water Sites 1262 and 1265, Ocean Drilling Program (ODP) Leg 208 in South Atlantic, reveal the global cooling event occurring in both surface and deep oceans. The results show that the earliest Oligocene δ^18O values during 33.5-33.1 Ma represent the magnitude of continental ice sheets on east Antarctica and indicate the large decrease in both surface and deep water temperatures of worldwideoceans. The δ^13C records show the large excursion during the period of EOGM event and indicate some types of shift in global carbon reservoir, probably demonstrating the sudden increase in organic carbon burial rates and the changes in the distribution and timing of production. At the same time, lithologic composition, carbonate content, color reflectance, and coarse fraction brought about significant changes close to the Eocene/Oligocene boundary, reflecting the abrupt deepening in the carbonate compensation depth (CCD). Changes in carbonate content were revealed from the color reflectance identify periodicities associated with eccentricity of the Earth‘s orbit (100 and 400 ka), further indicating orbitally forced global climate variations in the Early Oligocene.     

Well-Posedness of the Ericksen–Leslie System

We prove the local well-posedness of the Ericksen–Leslie system, and the global well-posedness for small initial data under a physical constraint condition on the Leslie coefficients, which ensures that the energy of the system is dissipated. Instead of the Ginzburg–Landau approximation, we construct an approximate system with the dissipated energy based on a new formulation of the system.     

Non-isothermal crystallization behaviors and spherulitic morphology of poly(lactic acid) nucleated by a novel nucleating agent

Journal of Thermal Analysis and Calorimetry - The effect of cadmium phenylmalonate (PMA-Cd) as a novel nucleating agent on the crystallization behaviors and spherulitic morphology of poly(lactic...     

Design and Synthesis of Lipidic Organoalkoxysilanes for the Self‐Assembly of Liposomal Nanohybrid Cerasomes with Controlled Drug Release Properties

This paper reports the facile design and synthesis of a series of lipidic organoalkoxysilanes with different numbers of triethoxysilane headgroups and hydrophobic alkyl chains linked by glycerol and pentaerythritol for the construction of cerasomes with regulated surface siloxane density and controlled release behavior. It was found that the number of triethoxysilane headgroups affected the properties of the cerasomes for encapsulation efficiency, drug loading capacity, and release behavior. For both water‐soluble doxorubicin (DOX) and water‐insoluble paclitaxel (PTX), the release rate from the cerasomes decreased as the number of triethoxysilane headgroups increased. The slower release rate from the cerasomes was attributed to the higher density of the siloxane network on the surface of the cerasomes, which blocks the drug release channels. In contrast to the release results with DOX, the introduction of one more hydrophobic alkyl chain into the cerasome‐forming lipid resulted in a slower release rate of PTX from the cerasomes due to the formation of a more compact cerasome bilayer. An MTT viability assay showed that all of these drug‐loaded cerasomes inhibited proliferation of the HepG2 cancer cell line. The fine tuning of the chemical structure of the cerasome‐forming lipids would foster a new strategy to precisely regulate the release rate of drugs from cerasomes.