中国县域城镇化的道路交通影响因素识别及空间协同性解析

本文基于人口普查数据和路网数据,利用空间滞后回归模型和耦合协调度模型等,对中国县域城镇化率的道路交通影响及其空间耦合协同性进行分析,研究表明：①中国县域低城镇化水平的县(区)主要集中在传统农区、集中连片贫困山区、高寒经济欠发达区。经济发展水平与人力资源空间上的错位,致使经济欠发达地区的人口倒挂,异地城市化特征显著;②中国县(区)道路交通优势度宏观上呈现出东西部区域差异和交通枢纽与外围区域的差异,“点—轴”地域结构特征显著,县域道路交通优势度数值呈现偏正态分布;③道路交通是城镇间和城镇与区域间联系的核心纽带和产业转型升级发展的传输廊道,开放式的道路系统增强了农村生产要素非农化转型的市场可介入性,对县域城镇化发展有积极作用。高速公路出口、火车站的布局对城镇化影响和带动农村要素非农化作用较为明显;④中国县域交通优势度与城镇化率耦合协调度分级分布为偏正态分布,城镇化发展与交通优势度相互影响显著,呈一定的双向耦合性。     

Petrophysical and geochemical constraints on alteration processes in granites

The hydrothermal alteration of granites has large influence on their petrophysical properties. To reveal the impact of alteration on magnetic and porosity properties of granites we have conducted a complex study of effects of two largely independent alteration processes, related to chemically different fluids, in granites of the Vysoký Kámen stock (the Krudum granite body, Czech Republic). It includes the whole-rock geochemical, magnetic and pore-space characterization. The alkali feldspathization resulted in decomposition of Li-mica, quartz removal, depletion in mafic cations and growth of new alkali feldspars (albite, K-feldspar), decreasing the overall magnetic susceptibility and disrupting the pore space by its discontinuation. The preservation of the orientation of the principal susceptibility axes is likely related to insignificant influence of the feldspathization process on the paramagnetic and diamagnetic phases orientation acquired during the magma emplacement. The greisenization, on the other hand had considerably more significant effects on microstructure and physical properties of the granite. The microstructure was modified by the growth of large amounts of new phases (Li-mica, quartz and topaz). This changed the mineral density of the rock, the porosity, size and character of pores to larger, flatter and probably more connected. This led also to the complete reworking of the original anisotropy of magnetic susceptibility during the greisenization.     

早第三纪济阳湖盆的形成和演变

在构造和气候的综合作用下,本区在早第三纪成为一个大型裂谷湖盆,并在沙四、沙三和沙一期因受古太平洋海泛影响而具有"近海"湖盆的特征,其演变经历了初始形成-强烈扩张-晚期扩张-收缩干涸四个阶段,构成一个完整的湖侵-湖退旋回和湖泊早期形成-中期扩张-晚期收缩三个亚旋回。     

中国西北半干旱区土地景观变化成因--以榆林市为例

1 Introduction Landscape change is a result of the complex interactions between physical, biological, political, economic and social driving forces (Moody and Woodcock 1995; Apan et al., 2002). Landscape in arid and semi-arid China is extremely vulnerabl…     

Effect of galvanic distortions on the series and parallel magnetotelluric impedances and comparison with other responses

The series and parallel impedances of the magnetotelluric tensor are appraised in relation to their relative immunity to galvanic electric distortions. The distorted responses are modeled using the Groom-Bailey decomposition of the tensor in terms of twist, shear, statics and strike direction. These four parameters and the undistorted responses are normally considered as unknowns, and are obtained from field data through the solution of an inverse problem. In the present work we use the decomposition as a forward model to simulate distorted sounding curves. Starting with undistorted 2-d te and tm responses, the tensor is distorted by assuming arbitrary values of twist, shear, static and strike direction. By default, both series and parallel responses are immune to the strike direction because they are invariants under rotation. In addition, series responses are immune to twist and shear and parallel responses only to twist. The dependence of the latter on shear is in the form of a real factor that shifts downwards the amplitude curves. On the other hand, the effect of statics on both series and parallel responses is more complicated than that on the impedance tensor because it cannot be accounted for by a simple shift of the curves. On the whole, there is a positive balance on the part of the series and parallel impedances over the te and tm responses because some of the distortions are filtered out by the invariants. It is shown that invariance is not sufficient to be immune to any of the distortions. The example chosen is Eggers’ eigenvalues, which are immune only to the by-the-fault strike direction. Invariance is not necessary either, as evidenced by the phase tensor, whose elements depend on strike but are immune to all distortions. The derivations are illustrated using soundings from the synthetic coprod2s1 and field-recorded coprod2 and bc87 data sets.     

Rural settlement spatial patterns and effects: Road traffic accessibility and geographic factors in Guangdong Province,China

Journal of Geographical Sciences - Based on land use classification data of remote sensing images, using kernel density, the minimal cumulative resistance model of road traffic accessibility, and a...     

1995—2010年间中国入境旅游客源国结构动态研究

拓展入境旅游外国市场规模、改变中国入境旅游市场的"二八"结构是中国旅游业发展面临的重要任务。运用标准差、变异系数和市场竞争态理论分析了1995—2010年间我国23个入境旅游客源国结构的变化过程、规律和趋势。研究表明:①中国入境旅游客源国结构不均衡且相对稳定。②12个主要入境旅游客源国规模位序呈现出3个组团。③1995—2010年间,日本、韩国、俄罗斯和美国等明星市场演化为金牛市场的同时,幼童市场数量增加。提出了恢复日本、韩国、俄罗斯和美国等国家的明星市场地位和重点拓展马来西亚、新加坡、澳大利亚和加拿大等幼童市场以及改善中国入境旅游客源国结构、拓展中国入境旅游外国市场规模的对策性建议。     

Multiscale geographically and temporally weighted regression: exploring the spatiotemporal determinants of housing prices

Understanding scale effects is important and indispensable for geography studies. However, spatial and spatiotemporal statistical tools for measuring the operational scales of different processes are rather limited. This article extends the popular geographically and temporally weighted regression (GTWR) model to consider operational scale effects by proposing multiscale GTWR (MGTWR), which offers a flexible and scalable framework for identifying and analysing multiscale processes by specifying flexible bandwidths for various covariates. Then, MGTWR is employed to explore spatiotemporal variations and how influential factors are associated with housing prices in Shenzhen. This article attempts to extend GTWR to MGTWR in consideration of scale effects, thereby highlighting the importance of different levels of spatiotemporal heterogeneity. Furthermore, the empirical results of this study can provide valuable policy implications for real estate development in areas where urban planning should address multiscale effects in both temporal and spatial dimensions.     

冬春季黄海温度锋面的多时间尺度变化及主控因素分析

海洋锋面强度变化对陆源物质输运和全球物质循环有重要作用。冬春季节,中国东部陆架区西太平洋边界流分支与沿岸流之间形成了海洋温度锋。为探究冬季风暴和陆架环流双重影响下温度锋面的多时间尺度变化及主控因素,本文以黄海为研究区,分别在年代际尺度和天气尺度,利用信号分解和可解释深度学习方法,研究了低纬度驱动的环流系统和高纬度驱动的冬季风暴对锋面变化的耦合作用。在年代际尺度,通过使用经验正交函数分解和集合经验模态分解的方法,将北黄海的温度变化与黄海暖流强度相联系。研究结果表明,黄海的海表温度经验正交函数（EOF）分解第一模态的空间分布有明显的黄海暖流—沿岸流体系特征;海表温度EOF第一模态时间序列与黄海暖流强度指标的相关性良好,且受低频率厄尔尼诺‒南方涛动信号调控。在天气尺度,对卷积神经网络−长短时记忆网络（CNN-LSTM）模型进行训练并使用可解释性指标进行分析,结果发现无风或弱风条件下,海洋锋面主要由压力梯度力和科里奥利力的地转平衡维持;但在冬季风暴条件下,受开尔文波传播和切变锋破碎的影响,流场的低频波动成为导致锋面强度变化的主因。本文研究结果表明,大数据及机器学习方法是在众多海洋参数间建立联系,并发现一些独特物理海洋过程的重要手段,具有广阔的应用前景。     

Geodynamic evolution of a forearc rift in the southernmost Mariana Arc

The southernmost Mariana forearc stretched to accommodate opening of the Mariana Trough backarc basin in late Neogene time, erupting basalts at 3.7–2.7 Ma that are now exposed in the Southeast Mariana Forearc Rift (SEMFR). Today, SEMFR is a broad zone of extension that formed on hydrated, forearc lithosphere and overlies the shallow subducting slab (slab depth ≤ 30–50 km). It comprises NW–SE trending subparallel deeps, 3–16 km wide, that can be traced ≥ ∼30 km from the trench almost to the backarc spreading center, the Malaguana‐Gadao Ridge (MGR). While forearcs are usually underlain by serpentinized harzburgites too cold to melt, SEMFR crust is mostly composed of Pliocene, low‐K basaltic to basaltic andesite lavas that are compositionally similar to arc lavas and backarc basin (BAB) lavas, and thus defines a forearc region that recently witnessed abundant igneous activity in the form of seafloor spreading. SEMFR igneous rocks have low Na₈, Ti₈, and Fe₈, consistent with extensive melting, at ∼23 ± 6.6 km depth and 1239 ± 40°C, by adiabatic decompression of depleted asthenospheric mantle metasomatized by slab‐derived fluids. Stretching of pre‐existing forearc lithosphere allowed BAB‐like mantle to flow along the SEMFR and melt, forming new oceanic crust. Melts interacted with pre‐existing forearc lithosphere during ascent. The SEMFR is no longer magmatically active and post‐magmatic tectonic activity dominates the rift.