清代东蒙农业开发的消长及其气候变化背景

利用档案史料、建置沿革史研究成果等提取信息,建立历史代用指标序列,对清代（1644～1911）内蒙古东部地区农业开发的时空进程进行描述,结合当地农业气候资源条件（温度、降水）及清代气候变化（温度）探讨其中的气候因素。结果显示：（1）清代东蒙农业开发集中在现代年均≥10℃积温2500℃、降水量400mm以上区域之内;（2...     

镇江圌山绍隆禅寺“活地”成因

"活地"是宗教的传奇,而由于以往知识与技术的限制以及宗教圣地的"不可侵犯性","活地"也成了大自然的千年未解之谜。通过现场考察和资料调研,明晰了"活地"所在地区的地质构造特征。采用高频率表面波监测、分析技术,通过现场试验,研究了"活地"附近地表浅层岩土体分布情况。采用图像分析技术,经室内试验研究得出了"活地"及周围地区出露岩石的矿物组成。最终,对于"活地"的成因提出以下看法:1.否定了地下深层生长性岩脉诱发"活地"现象的观点;2.膨胀岩及膨胀土吸水膨胀对"活地"的隆升有一定作用,但这不是"活地"的主要诱因;3.提出"活地"是岩石风化作用及特殊地理环境综合作用结果的观点:风化作用使岩体疏松、体积增大,地面隆起;两侧山体运动对其交界处岩石产生挤压作用,为"活地"的持续隆升提供动力源。     

基于耗费场的最优路径算法研究

在GIS中,有一类应用是基于连续分布耗费场的最优路径计算问题,如公路选线等。该文首先采用规则格网对耗费场进行建模,进而基于规则格网表现,分别建立网络实现模型和元胞自动机实现模型,并探讨了基于元胞自动机模型的最优路径算法,通过实例研究,说明了算法的正确性。     

苏鲁豫皖省际边界区经济发展空间特征与类型划分

边界区类型划分与经济发展水平密切相关,对省际边界区经济协调发展具有参考价值.该文以苏鲁豫皖省际边界区为研究对象,利用空间自相关分析、产业差异度等方法,分析该地区经济发展的时空特征,并从产业结构视角划分边界区类型和边界线类型.主要结论如下:1)苏鲁豫皖省际边界区经济集聚特征明显且不断增强,并出现地域分化现象,各省域内县域经济发展水平差异不断减小,而省域间经济差异在扩大;2)经济发展水平高值区和低值区集聚趋势明显,省际边界效应带来的经济差异呈现显著的地域特征;3)根据省际边界两侧相邻地区的产业结构差异,将边界区划分为"桥梁型"和"切变型",将省际边界线划分为"桥梁型""切变型"和"中间型".     

基于因子分析法的河西走廊五市旅游竞争力分析

在对河西走廊五市旅游业发展情况进行研究的基础上,从旅游产业发展规模、产业增长潜力和产业环境等3个方面选取了28个指标,通过因子分析法对每个指标数据进行加权,然后通过定量分析法比较各城市旅游竞争力.结果 表明:河西五市中,旅游竞争力顺序依次为酒泉、武威、张掖、嘉峪关、金昌.最后对河西走廊各市旅游竞争力进行了比较分析,并针...     

Estimation of Elastic Stress-Related Properties of Bottom Sediments via the Inversion of Very- and Ultra-High-Resolution Seismic Data

Izvestiya, Atmospheric and Oceanic Physics - This paper provides an overview of several seismic inversion approaches and their application to very- and ultra-high-resolution marine seismic...     

Morphology of Dune-Like Relief in Rivers

Water Resources - Linearized equations of two-dimensional hydraulics have been analyzed by the method of small perturbations within a wide range of alluvial features sizes at large values of Froude...     

The Structure and Formation Conditions of the Callovian–Oxfordian Deposits of Sudak Bay (Crimea)

The composition and origin of the Callovian–Oxfordian deposits of the Sudak Bay were characterized on the basis of the generalization and analysis of our own results, as well as published and unpublished data. The botanical future was first implemented for the geological mapping of the Oxfordian deposits.     

A micro–macro investigation of the capillary strengthening effect in wet granular materials

Wet granular materials are three-dimensionally simulated by the discrete element method with water bridges incorporated between particles. The water bridges are simplified as toroidal shapes, and the matric suction is constantly maintained in the material. A comparison with experimental tests in the literature indicates that the toroidal shape approximation may be one of the best choices with high practicability and decent accuracy. Mechanical behaviours of wet granular materials are studied by triaxial tests. Effects of particle size distributions and void ratios are investigated systematically in this study. The hydraulic limit of the pendular state is also discussed. It gives the capillary cohesion function which is not only determined by the degree of saturation but also positively correlated to relative density and particle size polydispersity and inversely proportional to mean particle size. Furthermore, the capillary strengthening effect is also analysed microscopically in aid of the Stress–Force–Fabric relationship, mainly in fabric anisotropy, coordination number and stress transmission pattern, which revealed the micro-mechanisms of the additional effective stress induced by capillary effect.     

Clay Minerals in Basalt Sills from the Sediment Cover,East Pacific Rise

Clay minerals in basalt sills from the northern East Pacific Rise, covered by Upper Pleistocene clayey–sandy–silty sediments (turbidites, hemipelagites, and diatom oozes) sampled from DSDP Holes 477, 478, and 481A, were studied by X-ray methods based on the modeling of diffraction patterns. Trioctahedral smectites formed in thin (0.1–0.5 and 1.8–4 m) fissured sills that are well permeable for water delivered from the water-saturated host sediments heated by the sills. Smectites in basalts are found in the interstices (20–40 vol % in the rock and up to 50–80 vol % in hyalobasalts). They replace olivine and fill cracks and vesicles. Plagioclase and clinopyroxene are generally unaltered. The structure of smectites is characterized by different height of layers depending on the composition of cations in the interlayers and the degree of their hydration. The different-height layers either make up individual smectite phases or alternate in different proportions and with a high degree of segregation in the mixed-layer structures. Under conditions of a prolonged cooling, thick (43 m) sills are distinguished from the thin varieties by the formation of trioctahedral minerals (smectite–chlorite, chlorite, defective chlorite, and talc). They are found mainly in the interstices that make up 3–7 vol % of the rock.