扩展的解释学和文本的世界 --伊德与解释学的关系

伊德的技术哲学奠基于现象学和解释学的背景之中,他运用现象学和解释学来分析技术。在解释学问题上。他提出了“物质化的解释学”论题,要求把解释学扩展到非文本的范围内。这一论题在他的“扩展的解释学”中得到了充分的展开。但是伊德所理解的“文本”远离了传统解释学的文本,从“文本”的范畴就可以看出他的扩展是一种误读。     

Cellular responses to mild heat stress

Since its discovery in 1962 by Ritossa, the heat shock response has been extensively studied by a number of investigators to understand the molecular mechanism underlying the cellular response to heat stress. The most well characterized heat shock response is induction of the heat shock proteins that function as molecular chaperones and exert cell cycle regulatory and anti-apoptotic activities. While most investigators have focused their studies on the toxic effects of heat stress in organisms such as severe heat stress-induced cell cycle arrest and apoptosis, the cellular response to fever-ranged mild heat stress has been rather underestimated. However, the cellular response to mild heat stress is likely to be more important in a physiological sense than that to severe heat stress because the body temperature of homeothermic animals increases by only 1–2°C during febrile diseases. Here we provide information that mild heat stress does have some beneficial role in organisms via positively regulating cell proliferation and differentiation, and immune response in mammalian cells.Received 14 May 2004; received after revision 2 August 2004; accepted 16 August 2004     

阻尼振子的起伏频谱及扩散系数

本文讨论一个最简单的耗散系统，即一个谐振子与热库耦合的系统。给出Ｌａｎｇｅｖｉｎ力Ｇ（ｔ）及算符ａ（ｔ），ａ￣＋（ｔ）的定义，由此算出阻尼振子的起伏频谱及扩散系数。其结果与Ｗｉｇｎｅｒ－ｗｅｉｓｓｋｏｐｆ近似下求得结果完全一致。     

LM_2钢恒温超塑性及其显微组织的变化

LM_2钢经1050℃快速加热淬火后,基体晶粒尺寸可细化至4.2μm 以下,碳化物平均截线长小于0.32μm。处理后的钢在830～850℃,■=(1.0～2.3)×10~(-2)min~(-1)变形时均可获得较好的超塑性,其最大延伸率为183%,而流变应力仅55.2MPa。在超塑变形中,碳化物长大倾向比单纯温度作用下要大,但不明显。由于该铜原始组织中存在一定数量的一次碳化物,直接影响其超塑性的较好发挥。     

关于切比雪夫递推方程组的若干研究

应用第一类切比雪夫多项式的递推关系及初始值定义了第一类二元一阶切比雪夫递推方程组和多元一阶切比雪夫递推方程组,运用代数变换法和归纳演绎法得到各数列的通项公式,研究了第一类多元一阶切比雪夫递推方程组通项公式的结构及规律.     

山区河流河床结构对推移质输沙率的影响

河床结构是山区河流河床在洪水过程中达到较强阻力及较高河床稳定性时床面大颗粒的组合,对山区河流的推移质输沙起重要影响．引入河床结构强度S对山区河流河床结构进行定量化研究,使用河床结构测量设备对河床强度进行测量,采用类似于坑测法的子母双槽进行推移质输沙率实测,对云南小江流域的15条主要支流河床结构及推移质输沙进行野外实测,发现推移质输沙强度至少受单宽水流能量与河床结构发育程度共同影响,在同等级水流能量条件下,河床结构的发育程度越高的河流（或河段）其推移质输沙强度越小,河床强度值越小的河流（或河段）推移质输沙强度越大．单宽水流能量小于50kg／（m·S）、河床结构强度大于0.35时,推移质输沙率接近零．     

Types and biotic successions of Ordovician reefs in China

Ordovician reefs are located in the South China,Tarim,and North China blocks,in low-latitude epicontinental marine regions and mostly consist of large-scale carbonate platforms.During the Paleozoic,faunal radiation reef biota diverged and thrived in diverse paleogeographic settings.Algal reefs of the Early Ordovician,Calathium-lithistid sponge-algal reefs of the late Early Ordovician to early Middle Ordovician,and coral-stromatoporoid-algal reefs of the early Late Ordovician,indicate change from Cambrian to Paleozoic biota.Coral-stromatoporoid-algal reefs were the basic communities after 100 Ma.The macroevolution of biotic struc-tures generally shows increased complexity;the evolution of China’s reef biota parallels that worldwide.Important aspects are:(1) The Calathium-algal reefs from the early Tremadocian Nantzinkuan Formation,Zhangjiajie,western Hunan are the pioneer reefs,and the Darriwillian Yijianfang Formation,Bachu are the relic reefs.(2) The bryozoan-dominated reefs of the late Tremadocian Fenhsiang Formation,Middle Yangtze Platform are unique.(3) The early coral-stromatoporoid-algal reefs are highly restricted in China.(4) The algal reefs from the latest Katian on the western margin of the Yangtze Platform,represent an abnormal reef-building environment during the initial stages of Gondwanan glaciations.     

A novel method for solving the multiple traveling salesmen problem with multiple depots

Multi-traveling salesman problem(MTSP) is an extension of traveling salesman problem,which is a famous NP hard problem,and can be used to solve many real world problems,such as railway transportation,routing and pipeline laying.In this paper,we analyze the general properties of MTSP,and find that the multiple depots and closed paths in the graph is a big issue for MTSP.Thus,a novel method is presented to solve it.We transform a complicated graph into a simplified one firstly,then an effective algorithm is proposed to solve the MTSP based on the simplified results.In addition,we also propose a method to optimize the general results by using 2-OPT.Simulation results show that our method can find the global solution for MTSP efficiently.     

An efficient scheme for multi-party quantum state sharing via non-maximally entangled states

We present a new scheme for investigating the usefulness of non-maximally entangled states for multi-party quantum state shar-ing in a simple and elegant manner.In our scheme,the sender,Alice shares n various probabilistic channels composed of non-maximally entangled states with n agents in a network.Our protocol involves only Bell-basis measurements,single qubit measurements,and a two-qubit unitary transformation operated by free optional agents.Our scheme is a more convenient realiza-tion because no other multipartite joint measurements are needed.Furthermore,in our scheme various probabilistic channels lessen the requirement for quantum channels,which makes it more practical for physical implementation.     

SHRIMP zircon U-Pb ages and tectonic implications for Indosinian granitoids of southern Zhuguangshan granitic composite,South China

The large southern Zhuguangshan granitic batholith composite consists of granites with ages varying from the Caledonian through Indosinian to Yanshanian. Based on K-Ar dating data, the ages of the major parts of this composite were previously regarded as Yanshanian. In this study, the SHRIMP zircon U-Pb dating method has been adopted for six plutons, Ledong, Longhuashan, Dawozi, Zhaidi, Baiyun and Jiangnan, in the southern Zhuguangshan composite, in which the four plutons other than Baiyun and Jiangnan were previously regarded as Yanshanian granites. Magmatic zircons from these six plutons, dated by this study, have yielded ages of 239±5 Ma (MSWD = 2.5), 239±5 Ma (MSWD = 2.5), 239±2 Ma (MSWD = 1.7), 239±4 Ma (MSWD = 3.2), 231±2 Ma (MSWD = 0.81) and 231±3 Ma (MSWD = 1.8), respectively. The results indicate that these plutons were formed by early Indosinian magmatism. Geochemical characteristics suggest that these granites were formed in an extensional tectonic environment. Therefore, the Indosinian period granites in the southern Zhuguangshan composite were formed by partial melting of the Paleo-Mesoproterozoic crustal components during the collapse of thickened lithosphere after the collision between the South China and Indosinian plates.