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211.
Simulation of landscape spatial layout evolution in rural-urban fringe areas: a case study of Ganjingzi District 总被引:2,自引:0,他引:2
In recent years, the rapid expansion of urban spaces has accelerated the mutual evolution of landscape types. Analyzing and simulating spatio-temporal dynamic features of urban landscape can help to reveal its driving mechanisms and facilitate reasonable planning of urban land resources. The purpose of this study was to design a hybrid cellular automata model to simulate dynamic change in urban landscapes. The model consists of four parts: a geospatial partition, a Markov chain (MC), a multi-layer perceptron artificial neural network (MLP-ANN), and cellular automata (CA). This study employed multivariate land use data for the period 2000–2015 to conduct spatial clustering for the Ganjingzi District and to simulate landscape status evolution via a divisional composite cellular automaton model. During the period of 2000–2015, construction land and forest land areas in Ganjingzi District increased by 19.43% and 15.19%, respectively, whereas farmland, garden lands, and other land areas decreased by 43.42%, 52.14%, and 75.97%, respectively. Land use conversion potentials in different sub-regions show different characteristics in space. The overall land-change prediction accuracy for the subarea-composite model is 3% higher than that of the non-partitioned model, and misses are reduced by 3.1%. Therefore, by integrating geospatial zoning and the MLP-ANN hybrid method, the land type conversion rules of different zonings can be obtained, allowing for more effective simulations of future urban land use change. The hybrid cellular automata model developed here will provide a reference for urban planning and policy formulation. 相似文献
212.
The initial modeling method based on TTI anisotropy can provide an initial model for the fine modeling of tomographic inversion, and the quality of the initial model directly affects the efficiency and accuracy of tomographic inversion. It is necessary to study the accurate initial modeling method of TTI anisotropy. Based on the conventional flow of the initial modeling method of TTI anisotropic, in this paper the anisotropic parameter extraction formula was perfected, a local tomography method to optimize the flow of the initial modeling method of TTI anisotropy was introduced, and the accuracy of the initial model was further improved, which is more consistent with the actual geological conditions and conducive to the fine modeling of the later tomographic inversion. The processing results of model and filed data show that the initial modeling method of TTI anisotropy based on local tomography is effective and practical. 相似文献
213.
三角洲感潮河段洪潮水位频率分析方法的初步研究 总被引:3,自引:0,他引:3
根据珠江三角洲感潮河段年最高洪潮水位存在长期上升趋势的事实,提出了河口区感潮河段洪潮水位频率分析一种新的计算方法,新方法的分析结果表明,未来不同年代同频率的设计洪潮水位各不相同,也存在相应的长期变化趋势。以灯笼山站为例,新方法计算的2030年和2050年的百年一遇设计洪潮水位分别为3.12m和3.28m,比传统频率分析方法计算的结果分别高出0.24m和0.40m。建立有关部门在制定河口区的防洪标准时,根据洪潮水位的长期变化趋势作相应的动态调整,以适应河口区洪潮水位变化的实际情况。 相似文献
214.
基于泰尔指数和GIS地图分析技术,对河南区域经济和区域金融空间结构变化做对比分析.结果表明:金融业的空间集聚度远大于一般产业,在强大的金融集聚经济作用下,区域经济发展与区域金融发展会表现出显著差异.2000年以来,河南省辖市市区经济实力相对下降,而金融集聚功能上升;县域经济显著发展,而金融发展普遍滞后,郑州市日益成为全省金融服务业的集聚地.金融空间流动带来现代城市的快速成长、功能彰显和激烈竞争,而此种努力的结果往往会抑制一些区域的金融发展,特别是县域和农村地区,需要统筹区域金融中心和乡村普惠金融建设. 相似文献
215.
216.
1932年昌马地震构造力学特征探讨郭万武,张范民,邢成起,温增平(国家地震局兰州地震研究所,兰州)DISCUSSIONONTHETECTONOMECHANICFEATURESOF1932CHANGMAEARTHQUAKEMs7.6¥GuoWanwu;... 相似文献
217.
乌和尔楚鲁图钼矿床位于国内重要的二连东乌旗钼矿成矿带中,为近几年新发现的斑岩型钼矿床.本次就该矿床成矿岩体的地球化学及其U-Pb年代学开展相关研究.结果表明: 矿区中的成矿岩体属过铝质、高钾钙碱性系列;富集大离子亲石元素(LILE)、亏损高场强元素(HFSE),具有与南岭型花岗岩相似的地球化学特征.锆石LA-ICP-MS U-Pb定年显示,与乌和尔楚鲁图钼矿床成矿有关的花岗斑岩形成于中侏罗世((160 ± 1)Ma).因此,可推测乌和尔楚鲁图钼矿床斑岩型钼矿的成矿时代为燕山早期.综合研究认为乌和尔楚鲁图斑岩型钼矿床形成于后碰撞的构造环境. 相似文献
218.
郭遂红 《广东海洋大学学报》2002,22(2):78-81
随着我国改革开放的进展 ,跨国度、跨文化之间的交往越来越频繁。由于文化因素上的差异 ,交际行为在不同的文化中往往产生不同的意义 ,语用迁移难免会造成理解失误或交际失败。因而外语教学在培养学生整体语言技能的同时 ,应注意文化因素的渗透 ,提高学生的跨文化交际能力 相似文献
219.
220.
Zhen Guo Yuliang Cao Xianguang Wang Y. John Chen Jieyuan Ning Weiguang He Youcai Tang Yongge Feng 《地震科学(英文版)》2014,27(3):265-275
P-wave and S-wave receiver function analyses have been performed along a profile consisted of 27 broadband seismic stations to image the crustal and upper mantle discontinuities across Northeast China. The results show that the average Moho depth varies from about 37 km beneath the Daxing’anling orogenic belt in the west to about 33 km beneath the Songliao Basin, and to about 35 km beneath the Changbai mountain region in the east. Our results reveal that the Moho is generally flat beneath the Daxing’anling region and a remarkable Moho offset (about 4 km) exists beneath the basin-mountain boundary, the Daxing’anling-Taihang Gravity Line. Beneath the Tanlu faults zone, which seperates the Songliao Basin and Changbai region, the Moho is uplift and the crustal thickness changes rapidly. We interpret this feature as that the Tanlu faults might deeply penetrate into the upper mantle, and facilitate the mantle upwelling along the faults during the Cenozoic era. The average depth of the lithosphere-asthenosphere boundary (LAB) is ~80 km along the profile which is thinner than an average thickness of a continental lithosphere. The LAB shows an arc-like shape in the basin, with the shallowest part approximately beneath the center of the basin. The uplift LAB beneath the basin might be related to the extensive lithospheric stretching in the Mesozoic. In the mantle transition zone, a structurally complicated 660 km discontinuity with a maximum 35 km depression beneath the Changbai region is observed. The 35 km depression is roughly coincident with the location of the stagnant western pacific slab on top of the 660 km discontinuity revealed by the recent P wave tomography. 相似文献