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71.
为解决工程中建筑结构不均匀沉降的监测问题,以连通器作为基本理论,使用嵌入式实时操作系统(FreeRTOS),设计一种基于LTE Cat-1的无线静力水准仪系统。系统分为数据采集终端、数据基站和客户端3个部分,其中数据采集终端主要由压强传感器、ZigBee终端及Cortex-M3微控制器等组成,利用ZigBee终端建立多个数据采集节点;数据基站由ZigBee协调器、Cortex-M3微控制器、Wi-Fi模块及LTE Cat-1等组成,ZigBee协调器收集多个终端的数据,用户可通过PC端或移动端连接设备Wi-Fi对数据进行现场查看,LTE Cat-1模块将数据上传至服务器;客户端主要是针对质检中心或从事市政工程行业的人员设计的,方便查看现场监测结果。现场测试结果表明,该系统能够完成沉降数据的采集与稳定上传,测量精度达到mm级。 相似文献
72.
73.
74.
Bi Yu Chen Donggen Wang Shih-Lung Shaw Hui-Ping Chen 《International journal of geographical information science》2017,31(4):783-804
Travel time uncertainty has significant impacts on individual activity-travel scheduling, but at present these impacts have not been considered in most accessibility studies. In this paper, an accessibility evaluation framework is proposed for urban areas with uncertain travel times. A reliable space-time service region (RSTR) model is introduced to represent the space-time service region of a facility under travel time uncertainty. Based on the RSTR model, four reliable place-based accessibility measures are proposed to evaluate accessibility to urban services by incorporating the effects of travel time reliability. To demonstrate the applicability of the proposed framework, a case study using large-scale taxi tracking data is carried out. The results of the case study indicate that the proposed accessibility measures can evaluate large-scale place-based accessibility well in urban areas with uncertain travel times. Conventional place-based accessibility indicators ignoring travel time reliability can significantly overestimate the accessibility to urban services. 相似文献
75.
76.
地磁低点位移异常类型特征与地震活动 总被引:2,自引:0,他引:2
通过对大量的地磁低点位移异常震例研究,结果表明: ① 地磁低点位移异常的形态、空间展布有明显的地区特征。异常大致可分为: 大范围异常和区域性异常二大类, 还可细分为 5个类型 ; ② 地磁低点位移异常与我国的地质活动构造有较密切的联系。 异常范围的大小、形态与异常所在地区的活动构造的规模、展布形态特征,以及这一地区即将发生的地震强度有关。 相似文献
77.
Yu Liu Hiroki Kurokawa Chang Liu David H. Brooks Jingping Dun Takako T. Ishii Hongqi Zhang 《Solar physics》2007,240(2):253-262
Vector magnetograms taken at Huairou Solar Observing Station (HSOS) and Mees Solar Observatory (MSO) reveal that the super
active region (AR) NOAA 10486 was a complex region containing current helicity flux of opposite signs. The main positive sunspots
were dominated by negative helicity fields, while positive helicity patches persisted both inside and around the main positive
sunspots. Based on a comparison of two days of deduced current helicity density, pronounced changes associated with the occurrence
of an X10 flare that peaked at 20:49 UT on 29 October 2003 were noticed. The average current helicity density (negative) of
the main sunspots decreased significantly by about 50%. Accordingly, the helicity densities of counter-helical patches (positive)
were also found to decay by the same proportion or more. In addition, two hard X-ray (HXR) “footpoints” were observed by the
Reuven Ramaty High Energy Solar Spectroscopic Imager (RHESSI) during the flare in the 50 – 100 keV energy range. The cores
of these two HXR footpoints were adjacent to the positions of two patches with positive current helicity that disappeared
after the flare. This strongly suggested that the X10 flare on 29 October 2003 resulted from reconnection between magnetic
flux tubes having opposite current helicity. Finally, the global decrease of current helicity in AR 10486 by ∼50% can be understood
as the helicity launched away by the halo coronal mass ejection (CME) associated with the X10 flare.
Electronic Supplementary Material The online version of this article () contains supplementary material, which is available to authorized users. 相似文献
78.
A. F. Morozov B. N. Khakhaev O. V. Petrov V. I. Gorbachev G. V. Tarkhanov L. D. Tsvetkov Yu. M. Erinchek A. M. Akhmedov V. A. Krupenik K. Yu. Sveshnikova 《Doklady Earth Sciences》2010,435(1):1483-1486
A thick (200 m) rock salt mass covering Late Archean granitoids was exposed for the first time in the Early Proterozoic volcanogenic-sedimentary
formations in the Onega trough of the east Baltic Shield by the Onega parametric well. The mineral composition of salts, their
geochemical features, and the isotopic composition of carbonate carbon and oxygen have been studied. After fluid inclusions
present in salts, their metamorphism temperature and isotopic composition of helium and argon were determined. The obtained
results give evidence of the fact that rock salts and magnesites associated with them were formed in an evaporate basin with
participation of deep crustal processes. The age of the underlying granitoids (2.716 ± 9 Ma) is determined using the Pb—Pb
method. 相似文献
79.
Byurakan Astrophysical Observatory. Translated from Astrofizika, Vol. 33, No. 2, pp. 271–281, September–October, 1990. 相似文献
80.