冲绳海槽北部PC-1岩芯24 cal.kaBP 以来孢粉记录的古环境信息

东海陆架是世界上最宽阔的陆架之一，面积达770 000 km2左右。在末次冰盛期（LGM），东海海平面下降120～130 m左右，绝大部分陆架暴露出海面。而冲绳海槽是第四纪以来一直保持海洋环境的东海深海区。本文以冲绳海槽北部PC-1岩芯为材料，通过分析该孔的孢粉，加上详细的AMS 14C测年，恢复了周边地区24 cal.kaBP以来的古植被，并推测古环境和古气候变化，重点讨论了LGM时期出露大陆架上发育的植被。 PC-1孔（31°27.5′N，128°24.8′E）位于黑潮支流对马暖流东侧，水深590 m，柱长812 cm。孢粉分析按间隔8 cm取样，个别为4~6 cm，共分析了103个孢粉样品。利用9个AMS 14C数据建立年龄标尺，用Calib5.1.0软件进行年龄校正。通过相邻样品深度的线性内插获得每个样品的年龄，采用外延法得到顶部和底部的校正年龄分别为351cal aBP、24 280 cal aBP，孢粉样品的时间分辨率平均为230 a。 根据孢粉百分比和沉积率的变化，可划分出四个带：Ⅰ带（812～715 cm，24.2～21.1 cal. kaBP）、Ⅱ带（715～451 cm，21.1～15.2 cal. kaBP）、Ⅲ带（451～251 cm，15.2～10.8 cal. kaBP）、Ⅳ带（251～0 cm，10.8～0.3 cal. kaBP），分别对应MIS 3末期、末次冰盛期、冰消期和全新世。末次冰盛期草本植物花粉占优势，孢粉沉积率较高，此时草本花粉主要来源于出露的大陆架，其上发育了以蒿属为主的草地植被，气候比较寒冷干燥；冰消期海平面开始回升，松属花粉含量升高，草本植物花粉含量下降；全新世以木本植物花粉占绝对优势，栗属－栲属花粉迅速增加，蕨类孢子含量升高，草本植物花粉含量锐减，孢粉沉积率降低，由于海平面回升，大陆架被淹没，此时孢粉主要来源于日本岛，九州地区生长了以栲属、栎属为主的常绿阔叶与落叶阔叶林，气候温暖湿润。 叶枝杉属花粉在整个岩芯中零星出现。叶枝杉属植物分布于菲律宾吕宋北部至塔斯马尼亚和新西兰气候潮湿的山地林中，该属花粉在岩芯中的出现，可能暗示了黑潮的影响或者是较强的夏季风。 草本植物与松属花粉百分比变化很好的反映了海平面的升降，松属花粉含量较高指示海平面较高。对岩芯中主要类型的花粉百分比进行了频谱分析，显示存在千年尺度的准周期变化，有明显的6.8，3.8，2.2，1.6 ka的周期。 孢粉样品中的炭屑统计表明，末次冰消期炭屑含量最高，可能因为末次冰消期降雨量增加，炭屑可被降水带到沉积地点沉积下来；全新世的炭屑浓度较高，尤其在晚全新世，出现了一个峰值，究其原因可能与气候变化和人类活动有关。

吡唑和1-甲胺酰基吡唑类化合物的紫外吸收光谱及其应用

研究了吡唑类化合物和1-甲胺酰基吡唑类化合物的紫外吸收光谱。结果表明,3位和5位的取代使吡唑的最大吸收波长红移3~4 nm,而4位的取代能够引起较大的红移(>10 nm)。甲胺酰基的引入可使吡唑类化合物的最大吸收波长红移20~26 nm,最大消光系数提高2~3倍。基于此,建立了快速测定吡唑类化合物含量的紫外分光光度法,并测定了长效尿素中3,4-二甲基吡唑磷酸盐(DMPP)的含量为尿素-N的1.15%,1-甲胺酰基-3-甲基吡唑(CMP)在水溶液中水解的半减期在20,25和30℃下分别为48,30和16 h,应用不同提取剂对三种土壤中硝化抑制剂3-甲基吡唑磷酸盐(MPP)的提取率为63.2%~89.2%。

Halogenated Terpenes and a C-15-Acetogenin from the Marine Red Alga Laurencia saitoi

Seven parguerane diterpenes: 15-bromo-2,7,19-triacetoxyparguer-9(11)-en-16-ol (1), 15-bromo-2,7,16,19-tetraacetoxyparguer-9(11)-ene (2), 15-bromo-2,19-diacetoxyparguer-9(11)-en-7,16-diol (3), 15-bromo-2,16,19-triacetoxyparguer-9(11)-en-7-ol (4), 15bromo-2,16-diacetoxyparguer-9(11)-en-7-ol (5), 15-bromoparguer-9(11)-en-16-ol (6), 15-bromoparguer-7-en-16-ol (7), two polyether triterpenes: thyrsiferol (8) and thyrsiferyl 23-acetate (9), and one C15-acetogenin, neolaurallene (10), were isolated from a sample of marine red alga Laurencia saitoi collected off the coast of Yantai. Their structures were established by detailed NMR spectroscopic analysis and comparison with literature data.

Palaeoenvironmental changes from pollen record in deep sea core PC-1 from northern Okinawa Trough, East China Sea during the past 24 ka

A pollen record of core PC-1 from the northern Okinawa Trough, East China Sea (ECS), provides information on vegetation and climate changes since 24 cal. kaBP. A total of 103 samples were palynologically analyzed at 8 cm intervals with a time resolution of 230 a. Four pollen zones are recognized: zone I (812-715 cm, 24.2-21.1 cal. kaBP), zone II (715-451 cm, 21.1-15.2 cal. kaBP), zone III (451-251 cm, 15.2-10.8 cal. kaBP), zone IV (251-0 cm, 10.8-0.3 cal. kaBP), corresponding to Late MIS 3, Last Glacial Maximum (LGM), deglaciation and Holocene, respectively. The LGM is characterized by the dominance of herbs, mainly Artemisia, and high pollen influx, implying an open vegetation on the exposed continental shelf and a cool and dry climate. The deglaciation is a climate warming stage with Pinus percentage increased and Artemisia percentage decreased and a rapid sea-level rise. The Holocene is characterized by predominance of tree pollen with rapid increase in Castanea-Castanopsis indicating the development of mixed evergreen and deciduous broad-leaved forest and a warm, humid climate. Low pollen influx during the Holocene probably implies submergence of the continental shelf and retreat of the pollen source area. The vegetation indicated by pollen assemblage found in this upper zone is consistent with the present vegetation found in Kyushu, Japan. Originating from the humid mountain area of North Luzon of the Philippines, Tasmania and New Zealand, Phyllocladus with sporadic occurrence throughout PC-1 core probably suggests the influence of Palaeo-Kuroshio Current or intense summer monsoon. The observed changes in Pinus and Herbs percentage indicate fluctuations of the sea level, and high Pinus percentage corresponds to high sea level. Spectrum analysis of the pollen percentage record reveals many millennial-scale periodicities, such as periodicities of 6.8, 3.85 2.2, 1.6 ka.

黔北早寒武世缺氧事件：生物标志化合物及有机碳同位素特征

本文首次报道了黔北早寒武世黑色岩系的生物标志化合物，并结合有机碳同位素组成特征，探讨该时期所发生的重大地质事件。所有样品均检出了丰富的正构烷烃、类异戊二烯烃、萜类化合物以及甾类化舍物。在GC谱图上，正构烷烃显示明显的单峰型分布特征，碳数分布范围为nC14-nC31主峰碳为nC18、nC19或nC20，nC17／nC31为1．15～50．17，显示轻烃组分占绝对优势，OEP值为0．84～1．11，CPI值为0．92～1．16，接近平衡值1．0，无明显的奇偶碳数优势分布。Pr／Ph值为0．24～0．79，具有明显的植烷优势。萜烷化合物以C30藿烷占优势，其相对丰度三环萜烷〉五环三萜烷〉四环萜烷，并且检出少量的γ-蜡烷。规则甾烷C27-C28-C29呈“V”字型分布，∑（C27＋C28）〉∑C29，其比值为1．25～1．99，∑C27／∑C29为0．78～1．22，重排甾烷C27／规则甾烷C27值为0．21～0．47。4-甲基甾烷普遍存在，但丰度相对较低。在地层剖面上，有机碳含量（TOC（％））从0．05～7．91％，平均为2．52％；有机碳同位素组成（δ^13Corg）从-29．49‰～-34．41‰（PDB），发生负偏移，偏移量达到4．3‰，代表该期海平面处于上升阶段，底层水处于严重缺氧状态，底栖生物缺乏。本文根据生物标志化合物特征参数，结合有机碳同位素组成变化，详细分析了黔北早寒武世这套黑色岩系的有机质来源、成熟度、沉积环境以及古海洋意义，将为我国南方早寒武纪古地理重建、地质事件记录提供可靠依据。

Microstructure and mechanical properties of slowly cooled Cu47.5Zr47.5Al5

Cu47.5Zr47.5Al5 was prepared by arc melting and solidified in situ by suction casting into 2-5-mm-diameter rods under various cooling rates (200-2000 K/s). The microstructure was investigated along the length of the rods by electron microscopy, differential scanning calorimetry and mechanical properties were investigated under compression. The microstructure of differently prepared specimens consists of macroscopic spherical shape chemically inhomogeneous regions together with a low volume fraction of randomly distributed CuZr B2 phase embedded in a 2-7 nm size clustered "glassy-martensite" matrix. The as-cast specimens show high yield strength (1721 MPa), pronounced work-hardening behavior up to 2116 MPa and large fracture strain up to 12.1-15.1%. The fracture strain decreases with increasing casting diameter. The presence of chemical inhomogenities and nanoscale "glassy-martensite" features are beneficial for improving the inherent ductility of the metallic glass.

Kinetic Assessment of Measured Mass Flow Rates and Streamwise Pressure Distributions in Microchannel Gas Flows

Measured mass flow rates and streamwise pressure distributions of gas flowing through microchannels were reported by many researchers. Assessment of these data is crucial before they are used in the examination of slip models and numerical schemes, and in the design of microchannel elements in various MEMS devices. On the basis of kinetic solutions of the mass flow rates and pressure distributions in microchannel gas flows, the measured data available are properly normalized and then are compared with each other. The 69 normalized data of measured pressure distributions are in excellent agreement, and 67 of them are within 1 +/- 0.05. The normalized data of mass flow-rates ranging between 0.95 and 1 agree well with each other as the inlet Knudsen number Kn (i) < 0.02, but they scatter between 0.85 and 1.15 as Kn (i) > 0.02 with, to some extent, a very interesting bifurcation trend.

Reconstructing The Vertical Distribution Of The Aeolian Saltation Mass Flux Based On The Probability Distribution Of Lift-Off Velocity

The probability distribution of lift-off velocity of the saltating grains is a bridge to linking microscopic and macroscopic research of aeolian sand transport. The lift-off parameters of saltating grains (i.e., the horizontal and vertical lift-off velocities, resultant lift-off velocity, and lift-off angle) in a wind tunnel are measured by using a Phase Doppler Particle Analyzer (PDPA). The experimental results show that the probability distribution of horizontal lift-off velocity of saltating particles on a bed surface is a normal function, and that of vertical lift-off velocity is an exponential function. The probability distribution of resultant lift-off velocity of saltating grains can be expressed as a log-normal function, and that of lift-off angle complies with an exponential function. A numerical model for the vertical distribution of aeolian mass flux based on the probability distribution of lift-off velocity is established. The simulation gives a sand mass flux distribution which is consistent with the field data of Namikas (Namikas, S.L., 2003. Field measurement and numerical modelling of acolian mass flux distributions on a sandy beach, Sedimentology 50, 303-326). Therefore, these findings are helpful to further understand the probability characteristics of lift-off grains in aeolian sand transport. (c) 2007 Elsevier B.V. All rights reserved.

Damage analysis of tetragonal perovskite structure ceramics implicated by asymptotic field solutions and boundary conditions

Cracking of ceramics with tetragonal perovskite grain structure is known to appear at different sites and scale level. The multiscale character of damage depends on the combined effects of electromechanical coupling, prevailing physical parameters and boundary conditions. These detail features are exhibited by application of the energy density criterion with judicious use of the mode I asymptotic and full field solution in the range of r/a = 10(-4) to 10(-2) where r and a are, respectively, the distance to the crack tip and half crack length. Very close to the stationary crack tip, bifurcation is predicted resembling the dislocation emission behavior invoked in the molecular dynamics model. At the macroscopic scale, crack growth is predicted to occur straight ahead with two yield zones to the sides. A multiscale feature of crack tip damage is provided for the first time. Numerical values of the relative distances and bifurcation angles are reported for the PZT-4 ceramic subjected to different electric field to applied stress ratio and boundary conditions that consist of the specification of electric field/mechanical stress, electric displacement/mechanical strain, and mixed conditions. To be emphasized is that the multiscale character of damage in piezoceramics does not appear in general. It occurs only for specific combinations of the external and internal field parameters, elastic/piezoelectric/dielectric constants and specified boundary conditions. (C) 2002 Published by Elsevier Science Ltd.

On dispersion-controlled principles for non-oscillatory shock-capturing schemes

The role of dispersions in the numerical solutions of hydrodynamic equation systems has been realized for long time. It is only during the last two decades that extensive studies on the dispersion-controlled dissipative (DCD) schemes were reported. The studies have demonstrated that this kind of the schemes is distinct from conventional dissipation-based schemes in which the dispersion term of the modified equation is not considered in scheme construction to avoid nonphysical oscillation occurring in shock wave simulations. The principle of the dispersion controlled aims at removing nonphysical oscillations by making use of dispersion characteristics instead of adding artificial viscosity to dissipate the oscillation as the conventional schemes do. Research progresses on the dispersion controlled principles are reviewed in this paper, including the exploration of the role of dispersions in numerical simulations, the development of the dispersion-controlled principles, efforts devoted to high-order dispersion-controlled dissipative schemes, the extension to both the finite volume and the finite element methods, scheme verification and solution validation, and comments on several aspects of the schemes from author's viewpoint.

一维含气多孔介质突然卸载破坏引起渗流变化的实验研究

利用煤激波管进行了一维含气多孔介质在突然卸载条件下的破坏实验,并对破坏的形态(层裂和层松)以及破坏前后气体渗流特性的变化进行了实验研究。实验结果表明:试样的破坏存在层裂和层松两种典型的破坏形式,破坏后煤样渗透率的变化本质上是由层松引起的;渗透率的分布与破坏应变直接相关,而充气压力是决定总体变化的参数;试样开裂破坏后的渗透率是原始渗透率的1～2倍;随充气压力增加.破坏深度按某一特征厚度的倍数增加。

A high order accurate difference scheme for complex flow fields

A high order accurate finite difference method for direct numerical simulation of coherent structure in the mixing layers is presented. The reason for oscillation production in numerical solutions is analyzed, It is caused by a nonuniform group velocity of wavepackets. A method of group velocity control for the improvement of the shock resolution is presented. In numerical simulation the fifth-order accurate upwind compact difference relation is used to approximate the derivatives in the convection terms of the compressible N-S equations, a sixth-order accurate symmetric compact difference relation is used to approximate the viscous terms, and a three-stage R-K method is used to advance in time. In order to improve the shock resolution the scheme is reconstructed with the method of diffusion analogy which is used to control the group velocity of wavepackets. (C) 1997 Academic Press.

Mn注入n型Ge单晶的特性研究

采用离子能量为100keV,剂量为3×1016cm-2的离子注入技术,室温下往n型Ge(111)单晶衬底注入Mn+离子,注入后的样品进行400℃热处理。利用X-射线衍射法(XRD)和原子力显微镜(AFM)对注入后的样品进行了结构和形貌分析,俄歇电子能谱法(AES)进行了组分分析,交变梯度样品磁强计(AGM)进行了室温磁性测量。结果表明原位注入样品的结构是非晶的,热处理后发生晶化现象。没有在样品中观察到新相形成。Mn离子较深的注入进Ge衬底,在120nm处Mn原子百分比浓度达到最高为8%。热处理后的样品表现出了室温铁磁特性。