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简要对比DDN、SDH光纤、卫星和无线CDMA等几种通讯方式的优缺点,介绍重庆区域测震台网所使用的传输方案,即以SDH光纤传输为主、无线CDMA为辅的双链路备份传输方案。重点介绍该传输方案的原理和实施方法,详细讲述台站及台网中心的路由配置和相关说明。通过在重庆市区域测震台网的运行,结果发现,传输效果较理想,测震台网台站运行率均达到98%以上,证明了该方案应用的可行性。 相似文献
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以江苏省测震台网为例,介绍灾备处理中心数据传输方法、系统框架、子系统建设关键以及存在的问题和解决方案,并对运行效果给予评价。江苏省测震台网采用SDH/MSTP有线专线和4G无线网络同步实时传输方式建立备份信道,原主信道数据由数采以太网口采集,备份信道数据由数采串口采集,从而实现测震数据的实时备份。现已建成溧阳地震台灾备处理中心,部署实时波形汇集交换、数据存储备份、自动速报、人工速报和信息发布、运行监控5个子系统,确保地震监测系统安全稳定运行。 相似文献
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以四川省数字测震台网台站数据通信为例,详细分析了致使台站数据通信质量严重下降的具体原因,发现了CDMA 1x数据通信网络在应用中存在的问题,原因是台站无线数据通信链路实际通信带宽不足,当地震记录数据特有的数据量瞬间爆发式增长时容易造成无线段网络拥塞、挂死。在通信网络进行3G升级后,根据无线数据通信日常需求,注重单个数据包较小、总量较大时的快速数据包交换量,对特大数据包支持降低,易丢包。针对CDMA 1x数据通信网络的先天不足,引入3G(CDMA2000 EV-DO)技术完成台站通信系统升级,能够有效提高台站数据通信质量。 相似文献
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为了提高测震台站运维工作效率,设计一套视频监视系统,实现地震台网中心对测震台站的远程、实时视频监视,数据流监视与中断告警,入侵侦测与告警以及市电中断告警等功能。系统分为台站端子系统和中心端子系统,其中,台站端子系统集成萤石网络摄像机、市电监控装置和4G路由器等设备,可以将台站视频截图通过4G信道近实时传输至中心端子系统;中心端子系统是一套应用程序,基于萤石云API开发。该系统为无人值守台站的视频监视提供了完整解决方案,在承德中心台的应用证明,可提高台网运维工作效率。 相似文献
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通过测震台网网络技术平台,分析其系统构成及虚拟台网、3G无线传输、远程网络监控等技术在陕西测震台网的应用.该平台的建成,提高了测震台网运行质量及流动测震台网的快速响应能力,实现省、市测震台网观测数据的实时共享,对进一步提升地震部门地震响应能力、完善监测体系,具有重要意义. 相似文献
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《地震地磁观测与研究》2015,(6)
为提高数字化地震监测台站的数据连续率及可用率,在综合考虑传输成本、建设难度、运维管理等因素基础上,提出测震台站双链路传输方案。经验证,该方案能有效提高测震台站数据传输连续率及可用率,为测震台站高效稳定的数据传输提供保障。 相似文献
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“十五”网络项目中测震台站CDMA数据传输方式浅析 总被引：1，自引：1，他引：0
中国数字地震观测网络项目建设的一个重要特点是"网络到台站,IP到仪器",从台站数据的采集到数据传输,台网中心数据的接收与实时处理,全部建立在网络化的平台上.因此,保证数据传输的连续性是一个重要的前提,本文从CDMA数据传输方式的特点出发,详细分析了数字地震项目建设过程中测震台网试运行的数据特点,研究表明:测震台站CDMA数据传输模式的连续率较低,在条件许可的情况下,地震数据的传输应尽量采用专用信道. 相似文献
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In this paper, the changes in sediment transport over 51 years from 1955 to 2006 in the Kuye River in the Loess Plateau in China are assessed. Key factors affecting sediment yield and sediment transport, such as precipitation depth, discharge, and human activities are studied. To investigate the changes in sediment yield in this watershed, a trend analysis on sediment concentration, precipitation depth, and discharge is conducted. Precipitation depths at 2 Climate Stations （CSs）, as well as discharge and sediment transport at 3 Gauging Stations （GSs） are used to assess the features of sediment transport in the Kuye River. The rtmoff modulus （defined as the annual average discharge per unit area, L/（s·km^2）） and the sediment transport modulus （defined as the annual suspended sediment transport per unit area, t/（yr km^2）） are introduced in this study to assess the changes in runoff and sediment yield for this watershed. The results show that the highest average monthly discharge during the study period in the Kuye River is 66.23 m^3/s in August with an average monthly sediment concentration of 88.9 kg/m^3. However, the highest average monthly sediment concentration during the study period in the Kuye River is 125.34 kg/m^3 and occurs in July, which has an average discharge of 42.6 m^3/s that is much less than the average monthly discharge in August. It is found that both the runoff modulus and sediment transport modulus at Wenjiachuan GS on the Kuye River has a clear downward trend. During the summer season from July to August, the sediment transport modulus at Wenjiachuan GS is much higher than those at Toudaoguai and Longmen GSs on the Yellow River. The easily erodible loess in the Kuye River watershed and the sparse vegetation are responsible for the extremely high sediment yield from the Kuye River watershed. The analyses of the grain size distribution of suspended load in the Kuye River are presented. The average monthly median grain size of suspended load in the Kuye River is largest in February and then decreases until June. In July, the average monthly median grain size of suspended load approaches another peak and decreases until September. Then, the median grain size of suspended load starts to increase until February of the following year. However, the average monthly median grain size of suspended load in the Yellow River at Toudaoguai and Longmen GSs is the smallest between early summer and late fall The median grain size in the Yellow River starts to increase in November and approaches the largest size in January. 相似文献
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Observations of trace gases (SO2, NH3, NO2 and O3) were made during the period 1981 to 1984 at 6 different locations representative of urban industrial, urban, nonurban, thermal power plant and marine environment. Diurnal variations of the trace gases were studied in an urban environment. Except in the urban industrial environment, the concentration of NH3 was found in the range of background values. Also, the average concentrations of NO2 and O3 at the different environments were in the order of background values. However, the concentrations of SO2 were substantially higher by about 7 times, in urban industrial and thermal power plant environments. The diurnal variations of SO2, NH3 and NO2 showed anitphase relationship with surface temperature at the urban environment station which is relatively free of industrial pollution. Discussion is centred on trace gas variations in different environments in India together with the values reported for various countries in the world. 相似文献
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Ingvar B. Fridleifsson 《Pure and Applied Geophysics》1978,117(1-2):242-252
In an active spreading area like Iceland, where the regional geothermal gradient is in the range 50–150°C/km, it is normally not a problem to find high enough temperature with deep drilling, but the difficulties arise with finding permeable layers at depth within the strata. Various volcanological methods can be applied in the search for aquifers and geothermal reservoir rocks. The flow pattern (as deduced from deuterium studies) indicates that the thermal water flows preferentially along high porosity stratiform horizons and dyke swarms from the recharge areas in the highlands to the hot spring areas in the lowlands. The primary porosity of the volcanic strata is dependent on the chemical composition and the mode of eruption of the volcanic units. Both the reservoir rocks and the flow channels forming the geothermal plumbing system are thought to vary from the Tertiary to the Quaternary provinces due to environmental conditions at the eruptive sites. 相似文献
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3He/4He ratios up to 3.5 times the ratio of atmospheric He were found in groundwater samples. The3He enrichment can be attributed to radiogenic3He produced by in-situ beta-decay of3H. This shows that tritiogenic3He is accumulating in confined waters. From tritiogenic3He and3H concentrations, ages of groundwaters can be calculated. Detection of tritiogenic3He gives a tool to trace a tritium contamination which occurred in the past and cannot be assessed only by the3H counting method. 相似文献
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The aim of this study is to estimate likely changes in flood indices under a future climate and to assess the uncertainty in these estimates for selected catchments in Poland. Precipitation and temperature time series from climate simulations from the EURO-CORDEX initiative for the periods 1971–2000, 2021–2050 and 2071–2100 following the RCP4.5 and RCP8.5 emission scenarios have been used to produce hydrological simulations based on the HBV hydrological model. As the climate model outputs for Poland are highly biased, post processing in the form of bias correction was first performed so that the climate time series could be applied in hydrological simulations at a catchment-scale. The results indicate that bias correction significantly improves flow simulations and estimated flood indices based on comparisons with simulations from observed climate data for the control period. The estimated changes in the mean annual flood and in flood quantiles under a future climate indicate a large spread in the estimates both within and between the catchments. An ANOVA analysis was used to assess the relative contributions of the 2 emission scenarios, the 7 climate models and the 4 bias correction methods to the total spread in the projected changes in extreme river flow indices for each catchment. The analysis indicates that the differences between climate models generally make the largest contribution to the spread in the ensemble of the three factors considered. The results for bias corrected data show small differences between the four bias correction methods considered, and, in contrast with the results for uncorrected simulations, project increases in flood indices for most catchments under a future climate. 相似文献
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This paper briefly summarizes the works in the processing of strong ground motion data, the factors affecting strong ground motion, the modeling of strong ground motion and the calculating of broad-band response spectrum which have been done recent years by engineering seismologists and seismologists of China. In addition, we think back to the international cooperation in strong ground motion of the recent years and make some expectations for the future. 相似文献