西南丘陵山地区农村居民点土地整理模式——以重庆渝北区为例

通过对样本区域农村居民点布局及土地利用特点的研究 ,从丘陵山地区的自然环境条件和社会经济发展水平的实际出发 ,提出两种土地整理模式 :一是农林综合开发整理模式 ,即居民点闲置土地的复垦利用与抛荒地利用结合 ,与山地区退耕还林等生态建设工程结合 ,进行退宅还林 ;二是新村建设整理模式 ,即由政府对新村统一规划 ,供给道路等基础设施 ,引导农民集中建房的“政府引导型”农村居民点整理模式 ,并对重庆市渝北区新春村的新村建设的运作和效益进行了实证分析。     

气候模式对北冰洋地区气候变化模拟评估和未来预估

正在全球气候变化研究中,北冰洋地区(包括北冰洋海水和海冰区以及周边陆地和岛屿积雪冻土区)受到极大的重视,因为在全球变暖中,北冰洋的变暖和海冰融化是最引起注意的问题之一。因此,气候模式对北冰洋地区气候变化的模拟评估以及对未来的预估,受到极大的重视,本文将综述近些年这方面的研究~([1-4])。     

重庆大学危岩锚固工程简介

重庆大学18层高层建筑物拟建在嘉陵江高陡斜坡脚下,斜坡上部陡崖为侏罗系上沙溪庙组巨厚层砂岩,岩石原生及岸剪裂隙发育,危岩直接威胁着建筑物。川地208队采用锚杆加固及涂抹砂浆水泥护坡综合防治工程,效果明显。     

堆叠降噪自编码器的影像特征融合变化检测

提出一种基于堆叠降噪自编码器的影像特征融合变化检测方法.首先在影像分割对象的像素级特征和对象级特征分析、设计与提取基础上,通过像素级特征主成分分析与特征优选处理算法,实现遥感影像多类型特征融合并构建分割对象的多维特征向量;其次利用堆叠降噪自编码器的高维复杂数据处理能力,实现遥感影像多维融合特征的变化检测.实验结果表明,...     

储层原始含油饱和度计算方法研究

储层原始含油饱和度是评价储层的重要指标 ,它的计算方法有 :岩心直接测定方法、间接确定法和毛管压力曲线计算方法。简要地讨论了这几种方法 ,重点探讨了利用毛管压力曲线计算储层原始含油饱和度的方法 ,针对该方法目前使用中存在的问题进行了改进 ,并在该方法的理论基础上 ,结合新疆塔里木盆地北部的实例 ,提出一种便于利用毛管压力曲线计算储层原始含油饱和度的适用方法     

绿片岩力学性质的实验研究

绿片岩的力学实验表明 ,在围压 45 0MPa条件下 ,岩石约于 45 0℃开始塑性变形。温度升至 5 5 0℃时变形加剧 ,原来直径为 10mm、高 2 0mm的均匀圆柱体变成直径为 10 8mm、高 17 4mm、中部变粗的不规则柱体。这一结果为解释青藏高原的地壳加厚提供了一定的实验依据     

1993年3月20日拉孜、昂仁间6．6级地震与西藏南北向地震构造带

本文在野外实地考察资料的基础上，结合前人工作成果，对１９９３年３月２０日拉孜、昂仁间６．６级地震等震线重新进行了校定并探讨其发震构造．通过对笔者近十年在青藏高原地震地质工作的总结，对西藏最新南北向地震构造带的成生、活动性及其最大地震潜在能力进行了讨论。     

正交矩阵的若干性质

通过对正交矩阵的深入研究，得到正交矩阵的一系列常用性质。     

High-resolution climate simulation of the last glacial maximum

The climate of the last glacial maximum (LGM) is simulated with a high-resolution atmospheric general circulation model, the NCAR CCM3 at spectral truncation of T170, corresponding to a grid cell size of roughly 75 km. The purpose of the study is to assess whether there are significant benefits from the higher resolution simulation compared to the lower resolution simulation associated with the role of topography. The LGM simulations were forced with modified CLIMAP sea ice distribution and sea surface temperatures (SST) reduced by 1°C, ice sheet topography, reduced CO₂, and 21,000 BP orbital parameters. The high-resolution model captures modern climate reasonably well, in particular the distribution of heavy precipitation in the tropical Pacific. For the ice age case, surface temperature simulated by the high-resolution model agrees better with those of proxy estimates than does the low-resolution model. Despite the fact that tropical SSTs were only 2.1°C less than the control run, there are many lowland tropical land areas 4–6°C colder than present. Comparison of T170 model results with the best constrained proxy temperature estimates (noble gas concentrations in groundwater) now yield no significant differences between model and observations. There are also significant upland temperature changes in the best resolved tropical mountain belt (the Andes). We provisionally attribute this result in part as resulting from decreased lateral mixing between ocean and land in a model with more model grid cells. A longstanding model-data discrepancy therefore appears to be resolved without invoking any unusual model physics. The response of the Asian summer monsoon can also be more clearly linked to local geography in the high-resolution model than in the low-resolution model; this distinction should enable more confident validation of climate proxy data with the high-resolution model. Elsewhere, an inferred salinity increase in the subtropical North Atlantic may have significant implications for ocean circulation changes during the LGM. A large part of the Amazon and Congo Basins are simulated to be substantially drier in the ice age—consistent with many (but not all) paleo data. These results suggest that there are considerable benefits derived from high-resolution model regarding regional climate responses, and that observationalists can now compare their results with models that resolve geography at a resolution comparable to that which the proxy data represent.     

辽东湾近岸堆积冰表面形态特征分析

2005 年 1 月在辽东湾盘锦市附近的海滨进行了堆积冰表面形态的现场调查.使用全站仪测量了 5 条不同起伏程度的堆积冰表面轮廓剖面,利用表面起伏高度数据和表面轮廓线在平均高度处的切角数据分析了堆积冰表面形态特征.对堆积冰区内的 3 个冰脊进行了内部层状结构观测,外部破碎冰块尺寸测量和 1 个冰脊涨、落潮时表面高度变化测量.利用这些数据,描述了冰脊内的分层结构;统计分析了冰脊外表层的破碎冰块尺寸并得到描述它们的主要参数值.此外,对冰脊涨、落潮时的表面形态进行了三维仿真绘图并计算了其表面形态参数.