珠海北斗CORS系统建设的实现及精度分析

珠海北斗ZHBDCORS系统建设已实现,新建了8个基准站,可利用省级GDCORS已有站进行设备和网络升级,实现与省级GDCORS互联互通,资源共享。ZHBDCORS在系统兼容性、基准站升级、数据通信技术、数据安全性等方面得到了较好的解决,积累了经验;首次实现了北斗网络RTK/RTD 10秒级的快速定位;利用珠海优于1 cm似大地水准面成果,可实现三维精确定位,其精度可满足四等水准要求。这将改变传统的平面和高程测量分离的作业模式,实现平面和高程同步一体化测量的现代化方法。ZHBDCORS可满足城市发展建设和导航的需要,是数字城市和智慧城市建设的基础。     

基于MapGIS的农村集体土地所有权确权方法研究

以全国第二次土地调查数据、地理国情普查数据为背景,全国正如火如荼地开展农村集体土地所有权确权工作。目前,农村集体土地所有权确权工作涉及面广、任务繁琐复杂、技术人员稀缺,确权工作面临着巨大挑战。鉴于此,本文根据四川某地区实际确权情况,浅析基于MapGIS的农村集体土地所有权确权方法,以便按时按质全面摸清农村集体土地产权状况,提高农村土地管理水平,优化土地结构,为国家和地方政府城镇化发展过程提供数据支撑。     

面向对象灾害遥感判读知识库设计与实现

灾害遥感研究与应用中积累的判读知识是灾害应急中灾情信息快速、准确提取的重要依据,为了重复利用专家所掌握的不可多得的判读知识,需要通过知识库将其存储管理起来,以实现共享和利用。本文采用面向对象和模糊加权产生式规则的知识表达方法,研制了灾害遥感判读知识库,实现了知识获取、管理与推理,为判读人员提供了学习灾害判读知识和灾害应急应用的平台,对自动化和智能化的灾害遥感信息提取研究将起到推动作用。     

GPCAD在矿山地质环境治理工程土石方计算中的应用

规划总图设计软件GPCAD是基于AUTOCAD软件开发的,用于城市总体规划、控制性详细规划,主要功能有地形处理、地形分析、土石方量计算等。GPCAD软件采用方格网法进行土石方量计算,本文介绍了规划总图设计软件GPCAD计算土石方的基本原理,介绍了方格网划分、零点位置计算和工程量计算公式。矿山地质环境问题主要包括地形地貌破坏、土地资源占压和生态破坏等,矿山开采过程中形成的大量废弃土石方是造成上述问题的根源。因此,矿山地质环境治理工程项目设计、施工通常涉及到大面积的地形整治工程和大规模土石方量的计算,本文结合矿山地质环境治理工程设计实例,通过计算范围确定、方格网布设、自然标高采集、设计标高设定,介绍了各步骤的操作方法,运用GPCAD进行大规模土石方量计算,计算得出区块土石方挖、填方量和净方量。     

旅游消费空间的建构与游客感知——以拉萨玛吉阿米餐厅为例

随着社会研究的"空间转向"以及地理研究的"文化转向",城市消费空间成为城市社会研究与文化地理学研究的热点;然而在全球化推进过程中,地方化也在悄然兴起,玛吉阿米餐厅正是地方化催生的产物,并且自其开业以来就受到中外游客的青睐。基于这种背景,本文从经营者的空间建构和游客的感知两个角度,运用质性的研究方法对玛吉阿米进行研究,发现:经营者运用各种景观符号及名人轶事对空间进行建构与重构,使其成为一个极具民族风情与有故事的空间;而作为消费的游客,通过对实体空间、名人轶事的感知获得一种深刻的消费体验,而对餐厅的功能价值的感知程度较差,这也说明旅游消费也具有符号消费的倾向。     

城乡建设用地增减挂钩项目拆旧地块选址适宜性评价模型研究

由于我国人口众多、人均资源相对不足,后备资源十分稀缺,人多地少的矛盾突出,因此开展城乡建设用地增减挂钩项目的意义重大。但由于目前关于选择拆旧地块要遵守的原则以及适用的方法尚不明确,因此这项工作在开展时存在着很强的随意性。本文以灵川县为实例,研究城乡建设用地增减挂钩拆旧地块选址的适宜性评价模型,并较客观地评价出该县最适宜拆旧区,为全国开展增减挂钩项目提供理论与实证支持。     

滨海CORS建设的实现与精度分析

滨海新区连续运行卫星定位综合服务系统(Bin Hai New Area Continuously Operating Reference Station System,简称BHCORS)已建成实现,系统建设由8个基准参考站、数据处理与控制中心、数据通信子系统、用户应用子系统4部分组成。BHCORS较好地解决了基准站改造与新建、数据通信技术、设备完好性、系统兼容性及系统精度等方面的问题。该系统不仅向测绘用户提供统一的、动态的、连续的、高精度的地理空间数据及时间和空间基准,还可以向社会各需求部门提供各种地理空间信息数据服务,满足各行业多种现代信息化管理的社会需求。     

浅析石灰粉煤灰稳定土的施工

对高速公路工程石灰粉煤灰稳定土路面底基层施工进行总结，并对石灰粉煤灰稳定土路面底基层施工提出了一些质量建议。     

A harmonic approach to global ocean tide analysis based on TOPEX/Poseidon satellite

The constant and harmonic parts of the global ocean tide are modeled by up to nine major tidal constituents, namely, S2, M2, N2, K1, P1, O1, Mf, Mm, and Ssa. Our computations start with the Fourier sine and cosine series expansion for the tidal constituents, including the constant Mean Sea Level (MSL). Although the frequencies of the tidal constituents are considered known, the coefficients of the sine and cosine functions are assumed to be unknown. Subsequently, the coefficients of the sine and cosine functions, as well as the constant part of the Fourier expansion, were expanded into spherical harmonics up to degree and order n, where n corresponds to the number of linearly independent spherical harmonic base functions needed to model the tidal constituents, determined via independent columns of the Gram matrix. The unknown coefficients of the spherical harmonic expansions are computed using sea level observations within cycles #1–#350 of the TOPEX/Poseidon satellite altimetry over 11 years of its mission. A set of orthonormal base functions was generated for the marine areas covered by TOPEX/Poseidon observations from the spherical harmonics using a Gram-Schmidt orthogonalization process. These were used for modeling the dominant tidal constituents. The computed models based on orthonormal base functions for the nine tidal constituents and the constant part of the Fourier expansion, were tested numerically for their validity and accuracy, proving centimeter accuracy.     

Gravity anomalies and deep structure of the Ninetyeast Ridge north of the equator,eastern Indian Ocean — a hot spot trace model

The Ninetyeast Ridge north of the equator in the eastern Indian Ocean is actively deforming as evidenced by seismicity and its eastward subduction below the Andaman Trench. Basement of the ridge is elevated nearly 2 km with respect to the Bengal Fan; seismic surveys demonstrate continuity of the ridge beneath sediment for 700 km north of 10° N where the ridge plunges below the Fan sediment. The ridge is characterised by a free-air gravity high of 50 mgal amplitude and 350 km wavelength, and along-strike continuity of 1500 km in a north-south direction, closely fringing (locally, even abutting) the Andaman arc-trench bipolar gravity field. Regression analysis between gravity and bathymetry indicates that the ridge gravity field cannot be explained solely by its elevation. The ridge gravity field becomes gradually subdued northwards where overlying Bengal Fan sediments have a smaller density contrast with the ridge material. Our gravity interpretation, partly constrained by seismic data, infers that the ridge overlies significant crustal mass anomalies consistent with the hot spot model for the ridge. The anomalous mass is less dense by about 0.27 g cm^–3 than the surrounding oceanic upper mantle, and acts as a cushion for isostatic compensation of the ridge at the base of the crust. This cushion is up to 8 km thick and 400–600 km wide. Additional complexities are created by partial subduction of the ridge below the Andaman Trench that locally modifies the arc-trench gravity field.