多元权力主体实践下民族村寨的旅游空间再生产——以贵州肇兴侗寨为例

以贵州肇兴侗寨为案例地,运用列斐伏尔的空间生产理论,采用田野调查与深度访谈结合的方法,从物理空间、社会空间、意义空间3个维度审视多元权力主体的“物质－关系－情感”联结以及与旅游发展的自洽性。结果表明：1）物理空间在权力主体的更迭下得以重新规划,有助于劳动力的回流。村寨的原真性在规制的约束下得以维护,但建构的景观符号是对民族村寨的错位表达。2）对于社会空间中的冲突,当地居民采取退让不退出的策略与管理者达成空间错时使用与管理默契。威权人物寨老成为消解分歧、推动社会关系巩固与凝聚的代表。对游客及外来经营户的让渡与周全,体现了当地居民开放包容的待客之道与处事哲学。3）意义空间通过当地居民对节事、文化的情感注入,对文化惯习的传承、对乡约的承继、对怀旧物的回忆与想象得以再生产。对于处在发展上升期的民族村寨而言,多元权力主体会基于利益的共同性与社会关系的粘连性考虑,做出符合当地旅游发展与自身容纳限度的调适与让步,来适应旅游发展带来的空间变化。     

“水-能源-粮食”视角下粤港澳大湾区生态安全格局的构建及优化

从“水－能源－粮食”3个维度对粤港澳大湾区的生态系统服务进行评价,利用珞珈一号夜光数据修正生态阻力面,运用最小累积阻力模型构建并优化湾区的生态安全格局。结果表明：1）粤港澳大湾区生态源地总面积为9 626.1 km²,主要分布在研究区东部和西部的山地、丘陵地区,对应位于江门市、惠州市中部和肇庆市;2）生态廊道共计38条,总长度为2 023.09 km,其中最短为11.76 km,最长为304.99 km,集中于植被覆盖较好的山地丘陵地区,中部无廊道分布;3）生态源地辐射区面积为28 929.5 km²,达到湾区总面积的51.88%,若要实现60%的覆盖率,则需要至少新增生态源地辐射面积4 524.856 km²;4）为了更好地优化粤港澳大湾区生态安全格局,提出在惠州市北部和南部新增两处生态源地辐射区,并构建以“一带、一轴、四组团”为核心的生态安全格局优化模式。     

The functional evolution and system equilibrium of urban and rural territories

Journal of Geographical Sciences - The coordinated development of urban and rural territorial systems has long been a scientific issue of concern in geography and socioeconomic development in...     

Mapping Wetland Areas Using Landsat-Derived NDVI and LSWI: A Case Study of West Songnen Plain,Northeast China

Increasing interest in wetlands for environmental management requires an understanding of the location, spatial extent, and configuration of the resource. The National Wetlands Inventory is the most commonly used data source for this information. However, its accuracy is limited in some contexts, such as agricultural and forested wetlands. An large number of studies have mapped wetlands worldwide from the perspective of land use and land cover change. However, information on the actual wetland planting areas annually is limited, which greatly impacts ongoing research. In this case study of the West Songnen Plain, we developed a simple algorithm for the quick mapping of wetlands by utilizing their unique physical features, such as annual display of phenological land-cover change of exposed soils, shallow flooding water, and plants from multi-temporal Landsat images. Temporal variations of the Normalized Difference Vegetation Index (NDVI) and Land Surface Water Index (LSWI) derived from Landsat images in 2010 for wetlands at different growth stages were analyzed. Results show that during the ante-tillering phase, the NDVI value (above zero) is lower than the LSWI value of paddies because of flooding of shallow water; during the reproductive and ripening phases, the NDVI value is higher than the LSWI value (above zero); and during the post-harvest wetland planting phase, the NDVI value is still higher than the LSWI value, but the LSWI value is negative. Wetland areas can be detected using one or two images in the optimum time window. The algorithm based on the difference of NDVI and LSWI values derived from Landsat images was used to extract the actual wetland planting area. Validated alongside statistical data, the algorithm showed high accuracy. Therefore, this algorithm highlights the unique features of wetlands and can help in mapping the actual wetland area annually on a regional scale. Results further indicate that the new method has a classification accuracy of 92 %. In comparison, two traditional methods based on Landsat-7/ETM registered accuracy rates of only 83 % and 87 % respectively.     

以地理国情监测为契机改造地理科学专业——以滁州学院为例

在当前社会经济发展形势下,传统地理科学专业人才培养模式存在着诸多不足,实践能力弱、就业范围窄、学无所用等。结合当前学科发展趋势,对传统地理科学专业进行改造,以滁州学院为例,在充分分析总结地科专业发展现状的基础上,阐述了该专业应紧紧抓住地理国情监测这一契机确定专业改革方向,并对改革的可行性与发展目标进行了详细论述和讨论,认为以地理国情监测为契机改造地理科学专业是可行的。可为地方院校地理科学专业向地理国情监测方向转型提供参考。     

The lower limit of the Doppler factor for a Fermi blazar sample

We selected 457 blazars(193 flat spectrum radio quasars, 61 lowsynchrotron peaked blazars, 69 intermediate-synchrotron peaked blazars and 134high-synchrotron peaked blazars) from the second Fermi-LAT catalog(2FGL) of γ-ray sources, which have X-ray observations. We calculated the lower limits for their Doppler factors, δγ, and compared the lower limits with the available Doppler factors and the apparent superluminal velocities in the literature.     

10颗近赤道弱源MK2VLBI观测结果

本文给出利用中国、意大利、南非射电望远镜对一个近赤道源样本在５ＧＨｚ频率上进行ＭＫ２ＶＬＢＩ普测中１０颗弱源的相关流量和其中部分源用ＨａｒｔＲＡＯ望远镜观测的总流量值，作为进一步的ＭＫ３或ＶＬＢＡ记录系统的ＶＬＢＩ观测依据．     

宏观生态环境遥感监测系统总体设计与关键技术

宏观生态环境遥感监测系统是基于环境遥感监测应用技术的软件实现.本文重点介绍了宏观生态环境遥感监测系统的总体结构设计、业务流程设计和核心功能设计,以及模型转换与实现技术、实时投影转换技术与以文件和数据库相结合的数据管理技术、基于XML的数据实时交换技术、产品自动化生产技术等关键技术,并给出了系统的应用实例.系统应用结果表...     

Ray-based modeling of reverberation in subsurface circular cylindrical void

Ray representation of electromagnetic resonance (reverberation) mode in subsurface circular cylindrical dielectric resonator (including void) is proposed. The modal ray path must be regular polygon or polystar. Travel time formulas for fundamental resonance multiples and the detecting conditions for non-exact-backscattering rays are derived. Simulation of time–distance curves of a modal hollow concrete block is generally concurred to the measured ground penetrating radar signal pattern. The proposed modeling method can be generalized to other resonant cavities with different profiles and provide a sound base for further applications of other more complicated geophysics science and engineering fields, particularly in ray-based tomography.     

Oil source analysis of Upper Tertiary Shawan Formation in Chepaizi area,in the northwest margin of Junggar basin

Well che89, located in the Chepaizi area in the northwest margin of Junggar basin, acquires high production industrial oil flow, which is an important breakthrough in the exploration of the south foreland slope area of Junggar basin. The Chepaizi area is near two hydrocarbon generation depressions of Sikeshu and Shawan, which have sets of hydrocarbon source rock of Carboniferous to Jurassic as well as Upper Tertiary. Geological and geochemical parameters are proper for the accumulation of mixed source crude oil. Carbon isotope, group composition and biomarkers of crude oil in Upper Tertiary of well Che89 show that the features of crude oil in Upper Tertiary Shawan Formation are between that of Permian and Jurassic, some of them are similar to these two, and some are of difference, they should be the mixed source of Permian and Jurassic. Geochemical analysis and geological study show that sand extract of Lower Tertiary Wulunguhe Formation has the same source as the crude oil and sand extract of Upper Tertiary Shawan Formation, but they are not charged in the same period. Oil/gas of Wulunguhe Formation is charged before Upper Tertiary sedimentation, and suffered serious biodegradation and oxidation and rinsing, which provide a proof in another aspect that the crude oil of Upper Tertiary Shawan Formation of well Che89 is not from hydrocarbon source rock of Lower Tertiary.