莱州湾海湾扇贝养殖区海水中悬浮颗粒的动态变化

1997年10月和1998年6月，在莱州湾两个主要海湾扇贝养殖区－芙蓉岛海区和金城海区，各定点进行了24h连续观测和取样，并在实验室内分析了总颗粒物（TPM）、颗粒有机物（POM）和叶绿素α的含量。结果表明，6月份金城海区的颗粒有机物和叶绿素α的含量均高于荚蓉岛海区；在10月份，芙蓉岛海区颗粒有机物的含量高于金城海区，但其叶绿素α的含量却低于金城海区，表明金城海区颗粒有机物的质量高于芙蓉岛海区。     

A Primary Observation on Palynofacies of the Chuangde Section (Late Jurassic-Cretaceous), Gyangzê, Southern Tibet

A primary study on palynofacies, which concerns the paleoenvironments from the sight of association of sedimentary organic matter preserved in sedimentary rocks, is conducted for a Late Jurassic-Cretaceous succession at Gyangzê, southern Tibet. Two palynofacies are recognized, which are formed in different sedimentary environments. The one in the pelagic is infertile in organic productivity and monotonous in component and is dominated by AOMA, while the other, being closely bound up with the slope, is characterized by abundant black phytoclasts that are possibly of algal origin and contains much AOM. The influence of terrestrial input is clear in the latter, for particles generated from terrestrial plants are common. A number of fossil spores and pollen together with some dinocysts are discovered, but they are normally in a bad condition of preservation. Nevertheless, this convinces us that the late Jurassic-Cretaceous succession in the Gyangzê area has a potential for palynological stratigraphy. We have also proved that the volume of PM can achieve similar results in presenting the productivity of organic matter as the weight of TOC does. This technique is much easier in the laboratory than that we do with TOC.     

烟台四十里湾海区栉孔扇贝同化率周年变化及其与环境的关系

于１９９７年６月－１９９８年５月用现场方法测定了烟台四十里湾海区总颗粒物质（ＴＰＭ）、颗粒有机物（ＰＯＭ）现存量和栉孔扇贝同化率（ＡＥ）周年变化,并分析栉孔扇贝同化率与海区温度、盐度、ＴＰＭ和ＰＯＭ的关系。结果表明,（１）整个海区ＴＰＭ现存量秋季最高,其次为春季和冬季,夏季最低;海区ＰＯＭ含量变化不大,在１．３４－１．６５ｍｇ／Ｌ之间;栉孔扇贝同化率在春、夏、秋三了较高,冬季较低,其中在秋末冬初（     

Transient dynamic response of fluid-saturated soil under a moving cyclic loading

Based on the Theory of Porous Media (TPM), a mathematical model of a two-dimensional incompressible fluid-saturated elastic soil is established, and the periodic boundary conditions are presented to analyze the transient dynamic response of this soil under a moving cyclic loading. The differential quadrature method (DQM) and the second-order backward difference scheme are applied to discretize the governing equations on the spatial and temporal domains, respectively. As application, a typical two-dimensional wave-induced transient problem with a seabed of finite thickness is analyzed, and the numerical results are compared with the analytical results presented in the present work. In addition, a transient dynamic response of fluid-saturated soil under limit moving vehicle loadings is studied. The effects of the velocity of vehicle and the volume fraction on the settlement and the pore water pressure are studied.     

The dynamic response of fluid-saturated porous materials with application to seismically induced soil liquefaction

The numerical simulation of liquefaction phenomena in fluid-saturated porous materials within a continuum-mechanical framework is the aim of this contribution. This is achieved by exploiting the Theory of Porous Media (TPM) together with thermodynamically consistent elasto-viscoplastic constitutive laws. Additionally, the Finite Element Method (FEM) besides monolithic time-stepping schemes is used for the numerical treatment of the arising coupled multi-field problem. Within an isothermal and geometrically linear framework, the focus is on fully saturated biphasic materials with incompressible and immiscible phases. Thus, one is concerned with the class of volumetrically coupled problems involving a potentially strong coupling of the solid and fluid momentum balance equations and the algebraic incompressibility constraint. Applying the suggested material model, two important liquefaction-related incidents in porous media dynamics, namely the flow liquefaction and the cyclic mobility, are addressed, and a seismic soil–structure interaction problem to reveal the aforementioned two behaviors in saturated soils is introduced.     

可信密码模块软件栈兼容方案设计

提出了可信密码模块软件栈的兼容性设计方案,采用软件工程中的策略模式,在软件栈TSS基础上内置兼容解释器,对应用和TCM的交互进行数据流解析以及数据结构和授权协议的转换,为上层应用提供统一的服务接口。该方案使得基于TPM开发的可信应用不需修改或只需少量修改就可以应用于TCM。测试表明,可信密码模块软件栈完成了应用层调用可信功能的透明转换,实现了应用兼容。     

Probabilistic assessment of one‐step‐ahead rainfall variation by Split Markov Process

In this paper, Split Markov Process (SMP) is developed to assess one‐step‐ahead variation of daily rainfall at a rain gauge station. SMP is an advancement of general Markov Process and specially developed for probabilistic assessment of change in daily rainfall magnitude. The approach is based on a first‐order Markov chain to simulate daily rainfall variation at a point through state/sub‐state transitional probability matrix (TPM). The state/sub‐state TPM is based on the historical transitions from a particular state to a particular sub‐state, which is the basic difference between SMP and general Markov Process. The cumulative state/sub‐state TPM is represented in a contour plot at different probability levels. The developed cumulative state/sub‐state TPM is used to assess the possible range of rainfall in next time step, in a probabilistic sense. Application of SMP is investigated for daily rainfall at four rain gauge stations – Khandwa, Jabalpur, Sambalpur, and Puri, located at various parts in India. There are 99 years of record available out of which approximately 80% of data are used for calibration, and 20% of data are used to assess the performance. Thus, 80 years of daily monsoon rainfall is used to develop the state/sub‐state TPM, and 19 years data are used to investigate its performance. Model performance is assessed in terms of hit rate (HR), false alarm rate (FAR), and percentage captured. It is found that percentage captured is maximum for Khandwa (70%) and minimum for Sambalpur (44%) whereas hit rate is maximum for Sambalpur and minimum for Khandwa (73%). FAR is around 30% or below for Jabalpur, Sambalpur, and Puri. FAR is maximum for Khandwa (37%). Overall, the assessed range, particularly the upper limit, provides a quantification possible extreme value in the next time step, which is a very useful information to tackle the extreme events, such as flooding, water logging and so on. Copyright © 2011 John Wiley & Sons, Ltd.     

SmartMK：基于TPM的可信多内核操作系统架构

提出了一个多内核架构SmartMK来支撑不同安全等级和类别的应用.基于TPM和新的CPU安全技术,实现了多内核之间的强隔离与安全通信机制,以软硬件协同保护的方式实现安全的操作系统运行环境.在SmartMK架构上提出了分层次的强制访问控制方模型,进一步降低复杂环境中的访问控制复杂度.性能测试和实际应用都表明,SmartMK能够有效加强系统的安全性,同时很好地保证了系统的运行效率.     

A Primary Observation on Palynofacies of the Chuangde Section (Late Jurassic-Cretaceous), Gyangzê, Southern Tibet

A primary study on palynofacies, which concerns the paleoenvironments from the sight of association of sedimentary organic matter preserved in sedimentary rocks, is conducted for a Late Jurassic-Cretaceous succession at Gyangzê, southern Tibet. Two palynofacies are recognized, which are formed in different sedimentary environments. The one in the pelagic is infertile in organic productivity and monotonous in component and is dominated by AOMA, while the other, being closely bound up with the slope, is characterized by abundant black phytoclasts that are possibly of algal origin and contains much AOM. The influence of terrestrial input is clear in the latter, for particles generated from terrestrial plants are common. A number of fossil spores and pollen together with some dinocysts are discovered, but they are normally in a bad condition of preservation. Nevertheless, this convinces us that the late Jurassic-Cretaceous succession in the Gyangzê area has a potential for palynological stratigraphy. We have also proved that the volume of PM can achieve similar results in presenting the productivity of organic matter as the weight of TOC does. This technique is much easier in the laboratory than that we do with TOC.     

A Primary Observation on Palynofacies of the Chuangde Section(Late Jurassic-Cretaceous),Gyangz■,Southern Tibet

A primary study on palynofacies,which concerns the paleoenvironments from the sight of association of sedimentary organic matter preserved in sedimentary rocks,is conducted for a Late Jurassic-Cretaceous succession at Gyangz(?),southern Tibet.Two palynofacies are recognized,which are formed in different sedimentary environments.The one in the pelagic is infertile in organic productivity and monotonous in component and is dominated by AOMA,while the other,being closely bound up with the slope,is characterized by abundant black phytoclasts that are possibly of algal origin and contains much AOM.The influence of terrestrial input is clear in the latter,for particles generated from terrestrial plants are common.A number of fossil spores and pollen together with some dinocysts are discovered,but they are normally in a bad condition of preservation.Nevertheless,this convinces us that the late Jurassic-Cretaceous succession in the Gyangz(?)area has a potential for palynological stratigraphy.We have also proved that the volume of PM can achieve similar results in presenting the productivity of organic matter as the weight of TOC does.This technique is much easier in the laboratory than that we do with TOC.