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1.
塔院井数字化水位观测中的零漂问题   总被引:1,自引:0,他引:1  
通过对塔院井数字化水位观测系统的校测,揭示出水位观测中的仪器零漂现象,分析了零漂的特征,提出了解决零漂问题的对策。  相似文献   

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基于对5口流体观测井使用的3种数字化水位仪的校测对比实验及与气温、气压、供电交流电压等因素的相关性分析,对数字化水位仪的零漂特征及影响因素进行了研究,结果表明:1水位仪的零漂变化呈非线性的特征,每种水位仪、甚至每台水位仪的零漂变动规律均不完全相同,相比较而言,SWY-1A型水位仪的零漂变动更平稳,变幅较小;2水位仪零漂与气温、气压和供电交流电压的相关系数较低,基本可以排除气温、气压和电源电压对水位仪零漂的影响;3水位仪零漂源于探头,主要受探头老化等因素的影响。探头安装时对探头线测量的精准度、探头线因重力作用的拉长、调整探头埋深时对探头线测量的精准度以及水位校测的人为误差等,往往会导致零漂计算结果上的偏差;4数字化水位观测应定期、规范化地进行水位校测并根据零漂变化对观测数据予以校正,以确保观测数据真实、可靠,能更好地发挥地震预测效能。  相似文献   

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采用“水位调和分析(M2波计算)”程序,对天津张道口地震台张道口-1井模拟、数字化水位内在质量变化进行了对比研究。从高频干扰、周围井孔的地下水开采、仪器零漂、探头位置与观测精度变化的关系、仪器自身原因5个方面分析了影响张道口-1井数字化水位内在质量的因素,并提出了数字化水位在日常观测中的注意事项。  相似文献   

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针对投入式水位仪存在稳定性差、零漂大等缺点,研制浮子式JS-1数字水位仪,基于观测原理和仪器结构,在苏18井开展动水位观测实验,结果发现:JS-1数字水位仪在动水位观测中可行,产出数据质量优良,并且在对零漂控制、观测数据质量、观测精度等方面具有一定优势。  相似文献   

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针对目前广泛应用于地下流体水位观测中的投入式水位仪存在稳定性差、零漂大等缺点,研制采用智能型绝对值多圈光电编码器的浮子式数字水位仪,介绍其工作原理和仪器结构,并给出仪器性能的实验测试结果,发现其具有高分辨率、高稳定性和低零漂的特点.  相似文献   

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简要介绍山西孝义地震台晋9-1井的观测概况,对2015年12月数字水位仪校测时发现的测量误差增大的原因进行分析,认为可能存在仪器零漂问题。通过与模拟观测资料对比,明确数字水位仪零漂特征,为今后观测提供参考。  相似文献   

7.
龚永俭 《华南地震》2012,(4):102-108
介绍在静水位井中观测的数字化水位仪探头的两种现场检查方法及结果 ,讨论这两种检查方法的优点及不足,提出现场检查方法的改进意见和允许特殊井孔内观测的数字化水位仪现场检查频率降低和定期消除数字化水位仪零漂影响的建议。  相似文献   

8.
通过对广东各数字化形变观测仪器潮汐因子中误差、相位滞后及仪器零漂等参量的计算,对仪器观测资料的连续性、稳定性及观测质量进行了分析和评价.分析结果认为:各台仪器的观测精度基本达到了中国地震局形变Ⅰ类台的标准;地倾斜类观测仪器精度高,稳定性好,尤其是水管倾斜仪的稳定性及精度较高;垂直摆倾斜仪的漂移较大且资料精度较低.伸缩仪...  相似文献   

9.
对岫岩地震台1号井模拟、数字化水位观测精度变化进行了对比研究,结果表明数字化水位资料观测精度在我台有明显提高,仪器自身运行稳定。为了进一步提高水位观测内在质量,总结了影响数字化水位观测精度的几个因素,提出了数字化水位在日常观测中的注意事项。  相似文献   

10.
对辛集冀21井模拟、数字化水位观测精度变化进行对比研究,结果表明数字化水位资料观测精度高、仪器运行稳定。文章分析并总结了影响数字化水位观测精度的因素,为今后观测资料分析及异常判定提供依据,也为进一步提高水位观测内在质量奠定基础。  相似文献   

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正SCIENCE CHINA Earth Sciences,an academic journal cosponsored by the Chinese Academy of Sciences and the National Natural Science Foundation of China,and published by Science China Press and Springer,is committed to publishing high-quality,original results in both basic and applied research.  相似文献   

16.
正Director:Shangfu Kuang,China Vice-directors:Chunhong Hu,China Duihu Ning,China Guangquan Liu,China The International Research and Training Center on Erosion and Sedimentation(IRTCES)was jointly set up by the Government of China and UNESCO on July 21,1984.It aims at the promotion of international exchange of knowledge and cooperation in the studies of erosion and  相似文献   

17.
Feedback mechanisms, which operate upstream through drawdown and backwater effects and downstream through sediment discharge are responsible for channel evolution. By combining these mechanisms with channel processes it euables a dynamic process-response model to be developed to simulate the initial evolution of straight gravel-bed channels. When erosion commences on a land surface, sediment entrained in the headwater reach by hydraulic action is selectively transported, deposited and reworked. This produces a damped oscillation between degradation and aggradation as the channel and valley respond to spatial and temporal variations in sediment calibre and hydraulic conditions. The initial cut and fill phases are responsible for valley incision and floodplain development while secondary and subsequent activity can produce river terraces. Eventually sediment entrainment in the headwaters declines as slopes are reduced. Subsequent channel evolution is relatively insignificant because it is dependent on local weathering activity producing material that can be transported on declining slopes. Therefore landforms produced during the initial phase of development, when local weathering was non-limiting, dominate the landscape.  相似文献   

18.
Based on relocating the Jiujiang-Ruichang earthquake sequence which occurred on November 26, 2005 in Jiangxi Province with the double-difference (DD) algorithm and master event technique, the paper discusses the focal mechanism of the main shock (MsS.7) and the probable seismo-tectonics. The precise relocation results indicate that the average horizontal error is 0.31kin in a EW direction and 0.40kin in a NS direction, and the average depth error is 0.48kin. The focal depths vary from 8kin to 14kin, with the predominant distribution at 10kin - 12kin. The epicenter of the main shock is relocated to be 29.69^oN, 115.74^oE and the focal depth is about 10.Skin. Combining the predominant distribution of the earthquake sequence, the focal mechanism of the main shock and the tectonic conditions of N-E- and NW-strike faults growth in the seismic region, we infer that the main shock of the earthquake sequence was caused by a NW striking buried fault in the Rnichang basin. The nature of seismic faults needs to be further explored.  相似文献   

19.
Abstract

The western reservoirs represent the principal groundwater system in Morocco. Demographic, industrial and agricultural developments during the last decade have markedly altered groundwater quality. The Mamora coastal aquifer system is among the Atlantic systems which are most heavily threatened by pollution. Agricultural and industrial activities, and rapid urban growth contribute to the pollution of the groundwater. Contamination transport is facilitated by a high permeability of the aquifer formations. In order to assess the actual groundwater quality of the Mamora aquifer and to understand the influence of the factors generating the pollution, an extensive multidisciplinary research programme is in progress, with hydrochemistry and microbiology playing essential roles. The present paper concerns the spatial distribution of physico-chemical parameters in the groundwater, subjected to domestic, industrial and agricultural pollution. Fifty-seven samples were analysed for several parameters (Ca2+, Mg2+, Na+, K+, Cl?, SO4 2?, HCO3 ?, NO3 ?, pH, electrical conductivity and temperature). The microbiological analysis of 143 samples reveals the presence of four kinds of indicator bacteria in the groundwater resources: faecal Streptococci, faecal coliform, Escherichia coli and Clostridium. The physico-chemical results and bacteriological monitoring show that the nitrate and bacteria concentrations exceed the maximum admissible levels, notably around pumping stations in the sectors of Sidi Taibi, Sidi Ahmed Taleb and Aïn Sbaâ. Contamination is generated by uncontrolled anthropogenic activities and accentuated by the high intrinsic vulnerability of the aquifer system. Several parameters appeared to exceed admissibility standards. Measures are recommended to prevent groundwater pollution in the region.  相似文献   

20.
Zinc in the Environment. In 1990 the world production of zinc ammounted to 7 Mio. metric tons. The main areas of application were: galvanization, alloys like brass and zinc metal. The content in the earth crust varies between 10–300 ppm zinc with a mean of 70 ppm. Uncontaminated surface waters contain less than 10 mg/m3 zinc. Apart from civilization air contains 1–10 ng zinc per m3. These background concentrations are exceeded by orders of magnitude in zinc deposit areas and where anthropogenic influences predominate. Accumulation can occur in sediments and sewage sludge. Molluscs and Algae also accumulate zinc. Zinc is essential for live. With normal food the zinc supply of man is just sufficient. Bioaccumulation of zinc towards man or chronic oversupply of man is not known. Zinc has no teratogenic or mutagenic effects, a suspicion on a carcinogenic effect proved wrong. In stockbreeding and plant cultivation a minimum supply of zinc is necessary. Plants are relatively less sensitive against higher soil contents of zinc. Considering the toxicological and ecotoxicological effects of zinc in the environment, the critical organismens are marine invertebratae like tubifex, daphnia, gammarus and algae. But normally only a minor part of the total zinc contest is biologically available, depending on salt content and pH of the waters.  相似文献   

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