基于轮廓插值加权算法的研究

为了进行医学二维图像的三维表面图像重建,最重要的一步就是提取二维图像的轮廓线。文章首先从算法的角度上探讨了诸如线性加权平均的图像插值方法、动态弹性插值方法、方向性插值方法和基于形状的插值算法的基本原理,以及它们的适用范围和局限性。在基于形状的插值方法的基础上,提出了改进的轮廓插值加权算法,采用这种改进算法以后,三维重建的轮廓质量有明显的改善。     

湖滨生态带恢复与重建研究进展

从湖滨带的基本概念入手,简述了湖滨带生态系统恢复与重建的基本内涵、恢复与重建的目标和原则。提出了湖滨带生态系统恢复与重建的几个重要理论,即恢复生态学理论、生态保育理论以及生态系统健康学理论。文中重点介绍了目前国内外所采用的最新的生态系统恢复与重建关键技术及其使用效果,即:1)计算机模拟技术;2)生态工程技术;3)管理技术。文章最后对未来技术研究的方向和思路进行了展望。     

基于轮廓插值加权算法的研究

为了进行医学二维图像的三维表面图像重建，最重要的一步就是提取二维图像的轮廓线。文章首先从算法的角度上探讨了诸如线性加权平均的图像插值方法、动态弹性插值方法、方向性插值方法和基于形状的插值算法的基本原理，以及它们的适用范围和局限性。在基于形状的插值方法的基础上，提出了改进的轮廓插值加权算法。采用这种改进算法以后，三维重建的轮廓质量有明显的改善。     

Holocene lake deposits of Bosten Lake, southern Xinjiang, China

A 9.25-m-long sediment core from Bosten Lake,Xinjiang, provides detailed information about changes in the water budget and biological acticity over the last 8400 cal-endar years. The chronology is constructed from six AMS radiocarbon dates on the terrestrial plant remains. Based onanalyses of TOC, CO3, detrital compounds and biogenic SiO2,lake level fluctuations and periods of remarkably-negative water budget appeared at 8.4-8.2 cal ka, 7.38-7.25 cal ka,5.7-5.5 cal ka, 3.7-3.4 cal ka and 3.3-2.9 cal ka, respec-tively. As they are in-phase with low lake levels at Sumxl Co and Bangong Co in western Tibet Plateau and with paleo-lakes in Inner Mongolia, a climate-induced change to some-what drier and warmer conditions is inferred. A further drop in lake level after 1320 AD of about 200 yr duration may heattributed to a negative water balance prior to the main phase of the Little Ice Age. Deep and stable lake phases of 1500 yr and 1800 yr duration at 7.2-5.7 cal ka and 5.5-3.7cal ka coincide with maximum moisture during the Holocene Megathermai in China. The long term trend towards aridity since about 4.3 cal ka can dearly be recognised. The reduced water budget of Bosten Lake from 640-1200 AD may be attributed to local effects.     

The age of formation of the mirabilite and sand wedges in the Hexi Corridor and their paleoclimatic interpretation

The Hexi Corridor is located at the transition zone of the Asian summer monsoon and westerly airflow, and lies in an important position in terms of its ecological fragility and climatic sensitivity. During a recent field expedition to this region, we found a sedimentary mirabilite layer in a number of localities including Suwushan, Yanchi, Baitujing, Yanchi Gaotai, Huahai, Yumen, Halanuo扙r, and Dunhuang (Fig. 1), which have the potential to provide important information about environmenta…     

Temperature variations on the Tibetan Plateau over the last two millennia

The paleoclimate data recovered from ice cores,tree rings and lake sediments indicate regional features of cfimatic change on the Tibeta n Plateau (TP) during the last 2000 years. The composite temperature reconstructions in-dicate that several main climatic episodes, such as the “LittleIce Age“ between 1400 and 1900, the “Medieval Warm Pe-riod“ in 1150-1400, a less warm period in 800-1100, and an earlier cold period between the 3rd and 5th centuries,occurred in the TP. In addition, temperature varied from region to region. The period from AD 800 to 1100, which waswarm in northeastern TP, was contemporaneous with cool-ing in the western and southern TP. The southern TP ex-perienced warming between 1150 and 1400. For western TP,the δ^18O records of the Guliya ice core indicate that the pe-Hod 1250-1500 witnessed a clear warming. Large-scaletrends in the temperature history from northeastern TP aremore similar to those in eastern China than are the trendsfrom the Guliya ice cap far to the west and southern TP. The most prominent similarities between the temperature varia-tions of the TP and eastern China are such cold phases as 1100-1150, 1500-1550, 1650-1700 and 1800-1850, andthe latter three cold events match with three widespreadg lacial advances which occurred on the TP during the Little Ice A2e.     

Loess-soil sequences in southern Anhui Province： Magnetostratigraphy and paleoclimatic significance

Two parallel loess-soil sequences from Xuancheng and Fanchang in southern Anhui Provinces are dated using geomagnetic and luminescence methods.The Brunhes/Matuyama(B/M) reversal boundary is recognized within the lower part of the so-calles Vermiculated Red Soil (VRS) in the Xuancheng section while the entire Fanchang sequence is of Brunhes age.This indicated that the most recent VRS in southern China,a stratigraphic marker and an indication of extremely warm-humid conditions,was formed during the middle Pleistocene,chronologically correlative with the S4 and S5 soil units in northern China.Microscopic and sedimentologic in vestigations reveal that eolian deposition started in this region at about 0.85 MaBp,roughly synchronous with the well-known Mid-Pleistocene climate change of global significance.The strengthening of both summer and winter monsoon circulations and the consequent river hydrological changes at that time would have provided favorable conditions for sustained eolian deposition in the middle-lower reaches of the Yangtze River since 0.85 MaBP.     

基于凸集投影和线过程模型的超分辨率图像重建

为了改善超分辨率重建图像的效果，提出了一种基于线过程模型的凸集投影方法。根据先验信息在图像重建中有重要作用的原理，该方法在数据一致性投影的基础上，将描述边缘信息的线过程模型作为图像的一个先验知识，用于重建过程中的平滑性约束投影，从而达到既保存图像的高频分量，又在一定程度上降低平滑区域噪声的效果。实验结果表明，该方法重建结果的视觉效果好于原方法，且信噪比有所提高，尤其是在高抽取率的情况下可以明显减少振铃效应。     

非细胞体系核重建的原子力显微镜观察

非细胞体系是研究有丝分裂中核重建过程的重要方法. 原子力显微镜以其高分辨成像的功能已成为观察生物体系的有力工具, 但目前原子力显微镜在非细胞体系研究中的应用还未见报道. 提出了一种适用于原子力显微镜观察的空气干燥样品制备方法, 利用原子力显微镜观察了非细胞体系核重建过程, 得到了高分辨、高质量的非细胞体系核重建过程的形貌像, 并且清晰地分辨出直径为100 nm的膜泡和它在接近染色质表面的形态变化. 为进一步了解核膜的重建机理提供了方向.     

西藏喜马拉雅冷杉年轮δ13C与气候意义

对采自青藏高原东南部林芝地区的喜马拉雅冷杉进行交叉定年后,分析了喜马拉雅冷杉年轮δ13C序列与气候要素之间的关系.去除大气CO2浓度升高导致大气CO2中δ13C下降和生长趋势的影响后,建立树轮δ13C值的残差序列△13C.利用附近林芝气象站的气象资料,分析了树轮△13C序列对气候要素的响应.结果表明: 冷杉δ13C的高频振荡与该地区前一年的9～11月降水和相对湿度存在较好的相关性,并存在强的滞后效应.通过建立回归方程重建了该区域的秋季(9～11)月相对湿度序列,解释方差达37.9%.重建相对湿度序列表明1800年前相对湿度变化周期较短、变幅较小,1800～2000年则相反.