基于车辆动力学的轨迹跟踪器设计

轨迹跟踪是移动机器人导航中的核心问题之一。针对非完整运动约束车辆,利用反馈线性化方法设计了轨迹跟踪器,仿真研究了跟踪算法的鲁棒性。最后,介绍了工程实现中参数观测器设计等相关问题。     

叶燮以"变"为核心的辩证的理性主义诗学观

叶燮的《原诗》针对当时文坛的复古主义思潮和追求偏僻怪戾的形式主义倾向．提出了以“变”为核心,以“因创”“正变”“源流”的艺术辩证观为内容,以“温柔敦厚”的儒家诗教为指归的理性主义诗学观。     

基于纹理基元与颜色的室外自然场景分类

为解决算法生成纹理地图时时间耗费量大的问题,提出采用KD-tree算法对数据结构进行划分、减小KNN算法搜索复杂度、提高搜索速度的方法.针对基于纹理基元的分类算法无法准确检测室外某些纹理相似性较高的自然场景,提出加入颜色特征、设置相应权值构建混合模型的方法.实验结果表明,基于KD-tree的KNN算法可缩短分类时间、满足实时性的要求,基于纹理基元与颜色的分类算法在室外自然场景中能够获得较高的分类精确度.     

核素分布的漂亮三角形

在氘氚结团为坐标的核素图中,边长11核素的核素分布最大三角形的3顶点为361818Ar180,1365838Ce7820,1967838Pt1184,3边为坐标S38,差K18和参量2S-H=36.最大三角形由4个边长10个坐标单位的小三角形组成,还可由3个6×6核素的菱形组成,3个菱形内部的3个4×4核素组合共有36核素1144830Cd6618,1275232Te7220,1305432Xe7622;中心区有2个最小三角形,其3顶点分别为偶偶核素,奇A核素1195031Sn6919,1255231Te7321,1275332I7421.     

适于全断面岩石掘进机的围岩分类方法

为了研究影响全断面岩石掘进机(TBM)掘进速率的地质因素,利用三维离散元程序3DEC建立TBM滚刀破岩三维仿真模型,分析不同的地质条件对TBM掘进速率的影响,根据TBM在围岩中的可钻性对南水北调西线工程中的围岩进行分类。分析结果表明:TBM掘进速率与岩石物理力学性质及岩体中的节理条件密切相关,在一定范围内,围岩强度越低,节理分布越密集,TBM掘进速率越高;而围岩强度越高,节理间距越大,使得TBM掘进速率大大降低。     

在LH模型下研究e~+e~-→τ~+μ~-过程

最小Higgs模型(LH模型)中由于镜像轻子和标准模型(SM)轻子之间存在味改变耦合,会对τ+μ-Z(γ)顶角产生单圈贡献,从而使e~+e~-→τ~+μ~-过程的截面增加,这一效应能被实验探测到.利用LH模型研究了e~+e~-→τ~+μ~-过程,在Mathematica 7.0中通过调用High Energy Physics和Loop Tools,经过复杂计算得到其截面σ.通过这类过程探讨LH模型的效应.     

Sea surface temperature records of core ZY2 from the central mud area in the South Yellow Sea during last 6200 years and related effect of the Yellow Sea Warm Current

Sea surface temperature (SST) records in the South Yellow Sea during the last 6200 years are reconstructed by the unsaturation index of long-chain alkenones (K 37 U ’) in sediment core ZY2 from the central mud area.The SST records varied between 14.1 and 16.5°C (15.6°C on average),with 3 phases:(1) A high SST phase at 6.2-5.9 cal ka BP;(2) A low and intensely fluctuating SST phase at 5.9-2.3 cal ka BP;and (3) A high and stable SST phase since 2.3 cal ka BP.Variation of the SST records is similar to intensity of the Kuroshio Current (KC),and corresponds well in time to global cold climate events.However,the amplitude of the SST response to cooling events was significantly different in different phases.The SST response to global cooling event was weak while the KC was strong;and the SST response was strong while the KC was weak.The difference in amplitude of the SST response is possibly caused by the modulation effect of the Yellow Sea Warm Current which acts as a shelf branch of the KC and a compensating current induced by the East Asia winter monsoon.The warm waters brought by the Yellow Sea Warm Current cushion the SST decrease induced by climate cooling,and both the Kuroshio and East Asian winter monsoon play important roles in the modulation mechanism.The SST records display a periodicity of 1482 years.The same period was found in the KC records,indicating that variation of the SST records in the central South Yellow Sea is strongly affected by KC intensity.The same period was also found in Greenland ice cores and North Atlantic and Arabian Sea sediment cores,showing a regional response of marine environmental variability in the East China Seas to that in the global oceans.     

The methodology of quantitative assess economic output of climate change

A method is introduced in this paper to study the effect of future climatic change on the economy. The researchers determine the economic output of climate change from historical data, and provide a method to quantitatively predict economic output of climate change by an economic-climatic model. A historical reciprocating examination is used to analyze output data for various crops in eight agricultural areas in China and meteorological data from 160 observatories in China from 1980 to 2000. The results show that the methods used are reasonable to a certain extent and good in application.     

Changes in physical features of Glacier No. 1 of the Tianshan Mountains in response to climate change

This study analyzes the changes in glacier zones and snow composition of Glacier No.1 in the Tianshan Mountains of China since 1961,and their possible relations with climate.It is found that precipitation dominated the snow composition and that air temperature and precipitation controlled the distribution of glacier zones,but interannual change in precipitation had a relatively large effect on glacier zones and snow composition during 1963–1981 (P10) and 1963–1989 (P11).However,during 1982–2007 (P20) and 19...     

A high-resolution environmental change record since 19 cal ka BP in Pumoyum Co,southern Tibet

A 380-cm-long sediment core was acquired from the deep water area of Pumoyum Co, southern Tibet. Twenty-five plant residue samples were selected, and organic carbon stable isotopes were obtained using the AMS ¹⁴C chronological method. The ¹⁴C age and carbon reservoir effect were calibrated with surface sedimentation rate measurements using ²¹⁰Pb dating. Results showed that the core sediment deposited over 19 cal ka BP. Based on a multi-proxy analysis of TOC and IC contents, grain size and pollen assemblage data, the palaeoclimatic evolution of Pumoyum Co was reconstructed since the last glacial. Pumoyum Co was a shallow lake prior to 16.2 cal ka BP; although the glacier around the lake began to melt due to increasing temperatures, climate was still cold and dry. In the interval of 16.2–11.8 cal ka BP, the sedimentary environment fluctuated drastically and frequently. Two cold-events occurred at 14.2 and 11.8 cal ka BP, and these may correspond to the Older Dryas and the Younger Dryas events, respectively. After 11.8 cal ka BP, Pumoyun Co developed into the deep lake as it is now. The lake water temperature was relatively lower at that time because of influx of cold water from glacial meltwater entering the lake. As a result, the multi-proxy indicators showed no sign of warm conditions. Comparisons between the sedimentary record of Pumoyum Co with that of other lakes of the same age in southern Tibet indicate a warmer climate following the last deglaciation influenced the southeastern Tibetan Plateau. These results imply that the southwest Asian monsoon gradually became stronger since the deglaciation during its expansion to the inner plateau. The glacial-supplied water of the lake responded sensitively to cold-events. The entire southern Tibet region was dominantly influenced climatically by the southwest Asian monsoon during the Holocene.