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961.
962.
随着5G网络、物联网、云计算、大数据分析、地理信息系统等新技术的兴起,探索更具包容性和创新潜力的参与式治理,引导高效的技术研发与运用,实现城市“以地方现实为基础、以社会需求为导向”的智慧化转型,已成为国内外城市地理学的重要与前沿议题。人本主义视角下的智慧城市研究,为地理学者介入这一领域提供了理论工具。不同于技术中心主义将智慧城市视作由数字技术构成的物理空间集合,人本主义强调特定情境下的技术、社会(人文治理)与空间的互动。该视角呼吁对多方行动者参与技术研发、基础设施建设与治理决策的合作互动开展微观研究,以揭示智慧城市的共建过程与地方性驱动机制。论文梳理了国内外人本主义研究的最新进展,认为该视角下的研究仍然沿袭“技术中心”或采用与之对立的“知识中心”立场,而缺少技术—社会互动的视角来理解城市智慧化转型。论文提出未来值得深入探讨的议题,即技术与社会(治理)的共生性、围绕技术研发的社会关系互动复杂性、技术研发与关系互动的语境化分析。探讨以上议题有助于理解智慧城市如何作为一个复杂地域系统,在人与技术的持续互动中发生转型,也可为未来中国相关研究提供理论借鉴。 相似文献
963.
利用GPS水准代替繁重的几何水准测量工作,必须确定高精度、高分辨率的似大地水准面。本文分别介绍了函数模型算法、随机模型算法和综合模型算法,并基于试验区域的GPS水准数据,通过各种算法的分类计算比较,验证了这几种模型算法的有效性和可靠性,结果证明最小二乘配置算法精度较高,并对实验结果进行三维仿真,可视化的分析似大地水准面的变化。 相似文献
964.
965.
陆明勇 《大地测量与地球动力学》1995,(4)
在国内外现行的主要孕震模式的基础上,得出了一个较为合理的详细阐述孕震过程的模式。该模式由(Ⅰ)弹性变形、(Ⅱ)扩容、(Ⅲ)前兆蠕动、(Ⅳ)地震、(Ⅴ)震后调整等阶段组成,主要强调液体(水)存在;发生大小地震的断层均由积累单元和调整单元组成,余震是大震后构造剪切应力重新调整以及主断层未破裂区和位于它两侧尺度小、长度短的断层未破裂区共同破裂的结果。最后,运用断裂力学理论对该模式的孕震过程进行了比较圆满的解释。 相似文献
966.
NNR������ITRF��ȫ�����˶�ģ�� 总被引:1,自引:0,他引:1
????????ITRF2000???????????????????????????ITRF2000??1 mm/a????????????NNR??NUVEL1A?????????????NNR????;??????????????????????????????????ж?ITRF??????????NNR?????? 相似文献
967.
根据实际应用研制制冷控制系统,该系统采用温度测量、PID控制及PWM脉宽调制等技术实现了对目标对象的制冷处理,具有一定的应用价值。 相似文献
968.
Extreme waves caused by tsunamis and storm surges can lead to soil failures in the near‐shore region, which may have severe impact on coastal environments and communities. Multiphase flows in deformable porous media involve several coupled processes and multiple time scales, which are challenging for numerical simulations. The objective of this study is to investigate the roles of the various processes and their interactions in multiphase flows in unsaturated soils under external wave loading, via theoretical time‐scale analysis and numerical simulations. A coupled geomechanics–multiphase flow model based on conservation laws is used. Theoretical analysis based on coupled and decoupled models demonstrates that transient and steady‐state responses are governed by pore pressure diffusion and saturation front propagation, respectively, and that the two processes are essentially decoupled. Numerical simulations suggest that the compressibility of the pore fluids and the deformation of the soil skeleton are important when the transient responses of the media are of concern, while the steady‐state responses are not sensitive to these factors. The responses obtained from the fully coupled numerical simulations are explained by a simplified time‐scale analysis based on coupled and decoupled models. Copyright © 2010 John Wiley & Sons, Ltd. 相似文献
969.
Yeli Yuan Lei Han Fangli Qiao Yongzeng Yang Ming Lu 《Dynamics of Atmospheres and Oceans》2011,51(1-2):55-74
A linearized instability analysis model with five unknowns was proposed to describe disturbance motions under general oceanic background conditions, including large-scale current shear, density stratification, frontal zone, and arbitrary topography. A unified linear theory of wavelike perturbations for surface gravity waves, internal gravity waves and inertial gravity waves was derived for the adiabatic case, and the solution was then found using Fourier integrals. In this theory, we discarded the assumptions widely accepted in the literature concerning derivations of wave motions such as the irrotationality assumption for surface gravity waves, the rigid-lid approximation for internal gravity waves, and the long-wave approximation for inertial gravity waves. Analytical solutions based on this theory indicate that the complex dispersion relationships between frequency and wave-number describing the propagation and development of the three types of wavelike perturbation motions include three components: complex dispersion relationships at the sea surface; vertical invariance of the complex frequency; and expressions of the vertical wave-number (phase). Classical results of both surface waves and internal waves were reproduced from the unified theory under idealized conditions. The unified wave theory can be applied in the dynamical explanation of the generation and propagation properties of internal waves that are visible in the satellite SAR images in the southern part of the China Seas. It can also serve as the theoretical basis for both a numerical internal-wave model and analytical estimation of the ocean fluxes transported by wavelike perturbations. 相似文献
970.
Vegetation changes can significantly affect catchment water balance. It is important to evaluate the effects of vegetation cover change on streamflow as changes in streamflow relate to water security. This study focuses on the use of statistical methods to determine responses in streamflow at seven paired catchments in Australia, New Zealand, and South Africa to vegetation change. The non‐parametric Mann–Kendall test and Pettitt's test were used to identify trends and change points in the annual streamflow records. Statistically significant trends in annual streamflow were detected for most of the treated catchments. It took between 3 and 10 years for a change in vegetation cover to result in significant change in annual streamflow. Presence of the change points in streamflow was associated with changes in the mean, variance, and distribution of annual streamflow. The streamflow in the deforestation catchments increased after the change points, whereas reduction in streamflow was observed in the afforestation catchments. The streamflow response is mainly affected by the climate and underlying vegetation change. Daily flow duration curves (FDCs) for the whole period and pre‐change and post‐change point periods also were analysed to investigate the changes in flow regime. Three types of vegetation change effects on the flow regime have been identified. The relative reductions in most percentile flows are constant in the afforestation catchments. The comparison of trend, change point, and FDC in the annual streamflow from the paired experiments reflects the important role of the vegetation change. Copyright © 2011 John Wiley & Sons, Ltd. 相似文献