共查询到17条相似文献，搜索用时 375 毫秒
1.
为了更好地开展人工地震测深工作,研制了携带式多道数字化观测系统,由拾震器、前置放大滤波器、对时装置和多道数字化数据采集记录器SCJ-8等组成。主要性能是:有1-8个输入通道;带宽为2-30Hz;动态范围约110db;A/D和D/A皆为12位;非线性失真约0.5％;串音约-90db;等待功耗约2W;记录功耗约6W;能同时输出数字和模拟数据,可直接与计算机接口;时间服务用晶控数字钟;有多种控制与监测功能。实验观测表明,该系统性能好,功能全,工作基本可靠,已达到原设计要求,为人工地震测深增添了新的观测记录仪器。 文中对系统的主机SCJ-8作了较详细地介绍,给出了系统在野外试验观测时记录到的地震波形。 相似文献
2.
DZSS-1型深层数字地震仪由三分量检波器CDJ-6B、数据采集单元、磁带机、编码钟和回放装置组成。它采用循环浮点放大-A/D转换技术、低噪音运算放大器、CMOS器件,使仪器噪音小于0.3μV（折合到前级放大器输入端,均值）,动态范围大于96dB,采用调相制、串码、单轨盒式数字磁带记录。仪器频带范围1-30Hz,浮点72dB。有钟差显示（±1ms）、噪音和误操作显示。仪器主要技术指标（道间一致性、漂移、噪音、串音、误码率、主放台阶精度）可用微机进行检测,能满足地震测深和其它低频数字测量之用。 相似文献
3.
采集系统是电磁法仪器的重要组成部分,设计出高精度、低功耗的分布式采集系统是电磁法仪器研制的重点和难点.本文设计的采集系统集成了6个采集通道,每个采集通道的A/D转换器都选用了32位的ADS1282,并通过DAC1282来提供ADS1282校准和自检所需要的外部信号.采集部分的控制中心选用了MachXO2 ZE系列这款功耗极低的CPLD.为了保证同步采集的精度,设计中采用了GPS和OCXO协同授时的方案来提供同步时钟.采集系统具备MT、CSEM、SIP等测量功能.测试结果表明,本采集系统同步精度维持在1E-11以下,待机状态下功耗为0.32 W,运行功耗2.76 W,各通道短路噪声值均在μV级,信噪比在118 dB附近,满足设计要求. 相似文献
4.
Δ调制型A/D转换技术是Δ-ΣA/D转换技术的基础.本文阐述了Δ调制型A/D转换器的基本原理,对信噪比和Δ-ΣA/D转换器的噪声成形作用进行了分析与推导,深入探讨了Δ-ΣA/D阶次、信噪比及采样率之间的关系,并由此得出结论:当代遥测地震仪采用24位四阶Δ-ΣA/D转换器是高分辨率地震勘探精度的基本要求(瞬时动态范围或信噪比为120dB). 相似文献
5.
流动观测台网与固定观测台网的结合是当前地震观测技术系统发展的一个趋势.针对流动观测时地震计与地震数据采集器互相独立、携带不方便、功耗高的问题,自主研发了一款适合流动观测的集地震信号提取、数据采集、记录和服务为一体的数字地震仪.该仪器具有频带宽(60s—80Hz)、动态范围高(140dB)、功耗低(0.6W)、携带方便(整机重量在15kg左右,包括供电系统、GPS天线和包装箱)等特点.详细介绍了该地震仪的外观结构、整体硬件结构、低功耗处理技术和所采用的灵敏度校正、标准方位和正交校正技术.对仪器的主要性能参数指标进行了严格的测试,并给出了具体的测试结果.该仪器研制完成后,投入到了青海玉树MS7.1地震震后流动观测中.从半年的实际使用结果来看,该仪器能够满足流动观测的要求. 相似文献
6.
GDS-1000宽频带通用流动数字地震观测系统主要用于大陆岩石层的人工及天然地震台阵研究、强震观测以及余震观测台网的临时布设。其主要技术指标为:动态范围120dB,前放增益1,16,128倍可调,高端频率6.25,25,45Hz可调,采样率25,100,200Hz可调,1MB固态数据存储器借助地震数据的压缩软件可以存储3MB以上的数据,工作温度范围-10-45℃,功耗小于3W。定时接受的BPM无线电授时信号可保证记录系统时钟校正误差小于10ms。其智能化地震触发系统可处于下列模态:近震触发,远震触发,近震和远震触发,任意地面运动信号触发,以及手动触发和定时触发。DSR-1000数字地震数据回收系统用于GDS-1000的参数预置、地震事件数据的转储和地震图的现场绘制。该系统在野外试验期间已取得大量近震、远震及核爆炸记录。 相似文献
7.
地震数据采集是数字化地震观测的重要环节, 因为模拟数字转换器(A/D)是地震数据采集器的重要部件, A/D的技术水准在很大程度上决定了数据观测质量。 放大器及A/D的漂移和 1/f噪声是数据采集器漂移的主要来源, 对以低频信号观测为主要特征的地震观测有较大影响。 为降低其影响, 本文在算法上对此问题做了一些探讨, 在目前autozero技术上做出一些改进, 即用调制解调技术来降低1/f噪声对信号精度的影响, 并做了相应的算法模拟。 在此基础上, 对算法做了进一步改进, 利用高次谐波加权求和使输出信噪比得到一定程度的提高。 结果表明, 通过优化解调算法, 可以进一步提高信噪比约2 dB, 对试验电路获得的测试数据应用优化解调算法也证实了这一点。 相似文献
8.
通过对地震勘探仪器的主要技术性能的详细分析可以看出,无论是集中式数字地震仪还是24位Δ-∑A/D型遥测地震仪,都还记录不到大动态、高主频、宽频带的地震反射波,它们记录的中深层地震反射信号的瞬时动态范围均在60 dB左右.本文以水平层状介质的吸收衰减特性为依据,给出了智能程控型前置放大器和频谱均衡滤波器的数学模型.用智能程控型前置放大器补偿由于球面扩散所造成的振幅衰减;用频谱均衡滤波器补偿由于地层吸收所造成的振幅衰减.按此设计方案,研制真正具有大瞬时动态和高频提升功能的地震仪,对高分辨率地震勘探技术的进一步发展具有重要意义. 相似文献
9.
10.
根据地震活动参数的数据特征,以2013年内蒙古科尔沁MS5.3地震为例,引入主成分分析和因子分析两种数据挖掘方法,在信息损失尽可能少的条件下,实现对参数变量的约简降维,并提取综合指标W.研究显示,2013年科尔沁MS5.3地震前两年,W值变化显著.在进一步的单因子分析中,从综合后的参数变量信息中重新提取了具有物理意义的多个单因子综合指标,消除了大量信息重叠所造成的不一致,实现了对综合指标的细化分析.在此基础上,对东北华北29次MS≥5.0地震的11个地震活动参数(频次N,b值,η值,A(b)值,Mf值,AC值,C值,D值,E值,Rm值,响应比Y)进行主成分分析,其结果显示,主成分综合指标W在震前1-2年均出现了明显的异常变化,这充分说明综合指标W可以用作地震预报研究的综合异常参考判据. 相似文献
11.
Soluble iron sulfide species in natural waters: Reappraisal of their stoichiometry and stability constants 总被引：4，自引：0，他引：4
William Davison Noel Phillips Brian J. Tabner 《Aquatic Sciences - Research Across Boundaries》1999,61(1):23-43
A wide range of stoichiometries has been previously proposed for soluble iron sulfide species and there is no general agreement on their importance in natural waters. The solubility of Fe(II) in 0.1 M NaClO4 equilibrated at 20 - 0.1°C with various partial pressures of H2S (0.1, 0.001, 0.0001, 0.00001 MPa) was measured in the pH range 3.1-7.9. Equilibrium was established within 1-6 h when amorphous FeS was the solid phase. The results could all be fitted using values for the solubility product constant (I = 0) of p*Ks = 3.00 - 0.12 and of the stability constant for a soluble Fe(HS) 2 species (I = 0) of p#2 = -6.45 - 0.12 where *Ks = aFe2+ · aHS-/aH+ and #2 = aFe(HS) 2/aFe2+ · (aHS-)2. Any soluble species of the form Fex (HS) 2x where x = &gif1; would fit the data equally well. Measurements at different partial pressures are inconsistent with labile species of the form FexSx. There was no evidence for a Fe(HS) + species. When a solution is saturated with respect to amorphous FeS, Fe(HS) 2 will only be a significant proportion of Fe(II) when S(-II) is higher than 0.2mmoll-1. The constants for Fe(HS) 2 or Fex (HS) 2x (x S 2) are consistent with all freshwater data where constant values of measured ion activity products provide no evidence for soluble complex formation. For marine waters with high sulfide concentrations (S 6mmol l-1), measured concentrations of Fe(II) are consistent with there being negligible soluble iron sulfide. The data are better fitted if the dissolved species are polymeric as predicted concentrations of the monomer Fe(HS) 2 are significant. These findings suggest that rather than the dissolved species being Fe(HS) 2, it is probably polymeric, that is Fex (HS) 2x (x S 2). 相似文献
12.
为了进行西藏高原地区的爆炸地震研究,研制了一套模拟磁带记录系统。每台仪器包括三个两周的拾震器（LS-1型）、三个相应的低噪声线性放大器（DDF-5型）、三个调制器、一台低频磁带记录器（DCJ-1型）、石英钟、对时器和收音机。仪器频率范围是2周-20周（对速度）,时间误差小于0.1秒。采用抖动补偿和频率滤波的办法,使系统的信噪比提高到50分贝。系统的幅度误差小于10％。经过野外实地观测和资料整理分析,证明其性能和指标能够满足地壳与上地幔爆炸地震研究的需要。通过模/数转换器,把模拟磁带转录成数字磁带,可以在电子计算机上进行各种数字处理。 相似文献
13.
地球物理勘探在野外进行,测量的电信号振幅范围为n×100 uV～ n×1 V, 对电信号测量精度要求优于0.1%.这就要求相应的隔离放大器增益范围大,档差小, 温漂小.为了满足上述要求,设计的精密隔离放大器由高线性度高精度器件-隔离放大芯片AD202-组成隔离级,3个零漂移运放LT1250组成3级9档放大级,档差为10 dB,增益从0～ 90 dB可控.实际电路的测试结果表明: 基于AD202和LT1250设计的隔离放大器的最大非线性误差为0.23%,19小时内的漂移为27 uV,达到了设计要求. 相似文献
14.
A simple and rapid method for the detection and extraction of oxolinic acid, flumequine, florfenicol and oxytetracycline from marine sediments was developed and validated. The analytes were extracted from the marine sediment using a solution of oxalic acid diluted in methanol with sonication before detection by HPLC using a diode-array detector (florfenicol and oxytetracycline) and fluorescence (oxolinic acid and flumequine). The quantification limits (QL) were 100 ng/g for oxytetracycline and florfenicol and 5 ng/g for oxolinic acid and flumequine. The coefficients of variation of the repeatability and intermediate precision were less than 10% in all of the analytes. The calibration curves were linear between 50 and 500 ng/ml for oxytetracycline and florfenicol and 1 and 20 ng/ml for oxolinic acid and flumequine. The recuperation rate for the analytes was above 86%. 相似文献
15.
AbstractAnnual patterns in climate parameters were studied to evaluate how these influence the quality of reference evapotranspiration (ETo) estimates obtained from the Hargreaves-Samani (HS) equation, since the method only uses the measured temperature directly. The work evaluates how these patterns can be used to improve the HS ETo estimates. Ten-year moving averages from a set of California Irrigation Management Information System (CIMIS) stations were used to evaluate the relationships between solar radiation (Rs), temperature (T) and ETo. The results indicate that T treads behind solar radiation and its value peaks some 25 days later. Thus, the main irrigation season in the Mediterranean climate (1 May–30 September) can be divided into three phases: increasing Rs and T; decreasing Rs with increasing T; and decreasing Rs and T. Non-univocal annual cycles were observed between Rs and T, ETo and Rs, and ETo and T. These annual patterns result in important seasonal changes in the ratio between the HS and Penman-Monteith (FAO PM) ETo estimates. The changes are particularly important during the irrigation season, where the FAO PM initially calculates greater ETo values than the HS methodology, and from the end of May to early September, where the HS equation overestimates the ETo values (by 17 mm, or 3%). These patterns obtained from 2000–2009 data were used to calibrate and improve HS ETo estimates at new sites for the 2010–2011 period. Calibration based on the proposed seasonal region-wide FAO PM/HS ETo ratios improved both the bias (decreased from 0.40 to 0.36 mm d-1) and r2 (increased from 0.67 to 0.87) of the ETo estimates for the irrigation season. The proposed methodology can be easily applied to other regions, even when the existing weather stations are sparse.
Editor Z.W. Kundzewicz 相似文献
16.
Richard M. Worthington 《Annales Geophysicae》1999,17(2):257-272
A simple method is described, based on standard VHF wind-profiler data, where imbalances of echo power between four off-vertical radar beams, caused by mountain waves, can be used to calculate the orientation of the wave pattern. It is shown that the mountain wave azimuth (direction of the horizontal component of the wavevector), is given by the vector
are radar echo powers, measured in dB, in beams pointed away from vertical by the same angle towards north, south, east and west respectively, and W is the vertical wind velocity. The method is applied to Aberystwyth MST radar data, and the calculated wave vector usually, but not always, points into the low-level wind direction. The mean vertical wind at Aberystwyth, which may also be affected by tilted aspect-sensitive layers, is investigated briefly using the entire radar output 1990–1997. The mean vertical-wind profile is inconsistent with existing theories, but a new mountain-wave interpretation is proposed. 相似文献
17.
１９７５￣１９９１年间,广东河源市新丰江水库区发生了５次ＭＬ４．７￣５．１级地震。距震中１０ｋｍ以内的河源黄子洞地电台记录到了震前不同程度的地电阻率异常变化。采用距平法消除年变干扰后异常延续时间一般为３个月左右,电阻率异常下降幅度在１％左右。利用《指南》中的震兆异常信度分析法确认其异常信度后,利用模糊信息处理法对异常判定地震三要素进行了计算,结果与实际基本符合。 相似文献