土地分离与共享框架的研究现状及应用拓展

“土地分离”与“土地共享”是2种不同的土地利用思维方式,反映人类土地利用的决策选择。中国有大量包含土地分离和共享思维的实践,但缺乏将这些实践案例纳入统一体系的研究范式。土地分离与共享框架最初用来探索粮食生产与生物多样性保护的权衡关系。经过10多年的发展,其理论内涵和研究内容不断丰富,是地理资源与环境领域重要的研究议题。论文在解析土地分离与共享框架内涵的基础上,综述土地分离与共享框架的相关研究成果,探讨土地分离与土地共享的策略选择。研究发现土地分离与共享相关研究存在从农业环境主题向城市管理主题转化的趋势,而且除了强调单一生物多样性保护和农业生产外,还有少数研究开始关注碳储存、土壤保持等其他生态系统服务类型;尽管土地分离与土地共享策略各有其优势和局限,但在目前的研究和实践中,土地分离比土地共享更受青睐。论文基于土地的多功能性进一步扩展该框架在城市用地管理中的应用,可为复杂社会—生态系统可持续发展提供路径指导。     

内蒙古苏尼特左旗古人类遗存点的发现及意义

内蒙古中北部是一个重要的古人类活动区，从１９９２年至１９９４年笔者在该区发现了１３处古人类遗存点，获得了大量的石器，包括３７７３件打制石器和１５８件磨制石器。这些材料具有十分重要的研究价值。本文对石器进行了分类，并对石器的时代及当时的环境特点进行了探讨。     

An Overview of Passive and Active Dust Detection Methods Using Satellite Measurements

In this paper, the methods to detect dust based on passive and active measurements from satellites have been summarized. These include the visible and infrared (VIR) method, thermal infrared (TIR) method, microwave polarized index (MPI) method, active lidar-based method, and combined lidar and infrared measurement (CLIM) method. The VIR method can identify dust during daytime. Using measurements at wavelengths of 8.5, 11.0, and 12.0 μm, the TIR method can distinguish dust from other types of aerosols and cloud, and identify the occurrence of dust over bright surfaces and during night. Since neither the VIR nor the TIR method can penetrate ice clouds, they cannot detect dust beneath ice clouds. The MPI method, however, can identify about 85% of the dust beneath ice clouds. Meanwhile, the active lidar-based method, which uses the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) data and five-dimensional probability distribution functions, can provide very high-resolution vertical profiles of dust aerosols. Nonetheless, as the signals from dense dust and thin clouds are similar in the CALIOP measurements, the lidar-based method may fail to distinguish between them, especially over dust source regions. To address this issue, the CLIM method was developed, which takes the advantages of both TIR measurements (to discriminate between ice cloud and dense dust layers) and lidar measurements (to detect thin dust and water cloud layers). The results obtained by using the new CLIM method show that the ratio of dust misclassification has been significantly reduced. Finally, a concept module for an integrated multi-satellites dust detection system was proposed to overcome some of the weaknesses inherent in the single-sensor dust detection.     

An experimental study on controlling post-earthquake debris flows using slit dams

Post-earthquake debris flows often break out in groups frequently, which are usually caused by the abundant loose solid materials that produced by earthquake. Slit dams represent a practical and effective kind of countermeasure for controlling the post-earthquake debris flow. Flume experiments were carried out to study the interaction mechanism and the effect of slit dams on the post-earthquake debris flows. The results showed that affected by the slit dams, some certain types of deposits formed on the upstream. The steeper the flume slope, as well as the greater the width and the density of slits, the easier the lateral deposit became “V” shaped. Otherwise, the lateral deposit was more likely to be “–?” shaped. When the flume slopes were 12°, 16° and 20°, the profiles of the deposits would be long-shallow type, short-thick type and short-shallow type, respectively. The slope of the deposition first decreases and then increases with the flume slope increasing within a certain range. The slit dam can trap the coarse sand and discharge the fine sand. The maximum attenuation rate can reach 44.4%. The effect of this capacity gradually weakens as the flume slope is increased. When the width or the density of slits is smaller, the greater the rate of decrease in peak sand discharge and the greater the effect of peak cutting will be. The reduction in the sediment storage rate is likely due to the increase in the width and the density of the slits. With the increase in flume slope, the sediment storage rate first increases, then decreases, which reaches a maximum value when the flume slope is 16°.     

污染大气边界层的长波冷却率模式

考虑大气气溶胶在长波窗区的散射和吸收作用以及水汽的连续吸收作用，建立了一个适用于污染大气边界层的长波冷却率模式。计算结果表明：当单位面积气柱中气溶胶含量为７８５．９ｍｇ／ｍ２时，气溶胶的作用可使到达地面的长波向下辐射增大３９Ｗ／ｍ２。在大气窗区，大气气溶胶和水汽的连续吸收对长波冷却率的影响是同等重要的。在水汽含量和气溶胶浓度较大的大气边界层内，水汽连续吸收的冷却率最大时可达１．３Ｋ／ｄ，气溶胶的冷却率最大时可达到１．６６Ｋ／ｄ，二者对长波冷却率的贡献均不容忽视     

《难溶性含钾岩石工业生产钾肥的不可行性再分析》的商榷

本文从我国可溶性含钾资源现状、难溶性含钾岩石的工作进展到几十年来我国可溶性找钾事业的坎坷历程,联系现行的含钾岩石分解最新科研成果,通过已有中试数据进行计算,阐述了含钾岩石资源产业化的途径、社会效益、经济效益和环境效益几方面的问题.     

Wintertime meso-scale horizontal distribution of large tintinnids in the southern Yellow Sea

Spatial distribution of some large tintinnid species (nominally > 76 μm) is investigated on samples vertically towed in the southern Yellow Sea in winters of 2001 to 2004. Nine tintinnid species are recorded: Codonellopsis morchella, Stenosemella pacifica, S. steini, Tintinnopsis schotti, T. radix, T. karajacensis, Eutintinnus tenuis, Parafavella sp., Leprotintinnus neriticus, of which C. morchella and T. radix dominated in the warm tongue-shaped zone of the Yellow Sea Warm Current (YSWC), and S. pacifica i...     

延龙图地区城市生态用地生态重要性空间识别与保护

采用加权指数求和法,从生态服务功能、景观生态空间格局以及生态敏感性3方面建立生态重要性空间识别指标体系,通过专家咨询和层次分析法确定各评价指标分级赋值标准和权重,结合GIS空间分析功能对“延龙图”（延吉-龙井-图们）地区生态用地的生态重要性进行空间识别,将其划分为3个级别：极重要、重要和一般重要,以反映不同生态用地保护级别和建设管制要求。结果表明,延龙图地区极重要生态用地占生态用地面积的25.720%,主要为耕地、林地和水域;重要生态用地占生态用地面积的39.500%,主要为林地和耕地;一般重要生态用地占生态用地面积的34.780%,以林地为主。     

华北联网中心的短波天线：华北地区遥测地震台网联网论文续五

对华北联网中心北京中心短波天线的设计，功能，安装方案作了较为详细的介绍。