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231.
Considering the fact that there is only one pair of fixed potential poles in one direction used to monitor the resistivity
changes under the observatory station which may indicate process of earthquake preparation, based on the precondition that
the resistivity structure is 1-dimensional under the observatory station, and by way of equivalent model put forward by the
authors, this paper suggests a kind of method trying to separate the resistivity changes in deep layers from that of the shallow
layer. Analysis shows that, to obtain the same measured data with the same array, any a multi-layered geo-electrical structure
can be equivalently taken as a two-layered one, we call it equivalent model. In this paper, the resistivity and thickness
of the upper layer of the equivalent model are equal to that of the first layer of the original one, the resistivity of the
lower layer of the equivalent model is obtained with calculation according to the requirement of equivalence, its value is
relevant with the resistivities and thicknesses of all layer of the original model except for the first one, so the resistivity
change of the equivalent layer can indicate the synthetic effect of variation of all layers of the original model except for
the first one. The primary research results show that this method can work well.
Foundation item: Chinese Joint Seismological Science Foundation (100146). 相似文献
232.
An integrated geophysical survey which combines vertical seismic profile method, shallow reflection seismic method, electric
sounding, soil temperature measurement and radioactive gas measurement was used to investigate Zhaoshuling landslide in the
new site of Badong County and to assess the stability of the landslide. By rational use of these methods together with borehole
geological profile and other geological information, the spatial distribution of the landslide body, the formations and structures
within and without the landslide body were determined and the stability of the landslide was also assessed, thus making great
contribution to the successful and rational investigation and assessment of the landslide. 相似文献
233.
Tiexin Gu Zhong Zhang Chunshu Wang Weidong Yan 《Geostandards and Geoanalytical Research》2001,25(1):153-158
Two types of gold deposit with both good homogeneity and a high-grade of gold were selected to prepare four gold ore reference materials (GAu-19,GAu-20,GAu-21 and GAu-22) by the Institute of Geophysical and Geochemical Exploration (IGGE),China.Seven laboratories participated in the certification programme. Volumetric methods for GAu19-21 and atomic absorption spectrometry for GAu-22 were used for the homogeneity testing,the coefficient of variation being found to be less than 3%.After sample digestion and preconcentration,the samples were analysed by flame atomic absorption spectrometry (AAS),colorimetry,neutron activation analysis (NAA)and volumetric analysis. The certified values for the gold concentration in GAu19-22 are 18.3 μg g -1, 32.3 μg g -1, 53.0 μg g -1 and 5.72 μg g -1,respectively. 相似文献
234.
该种方法利用离子色谱仪的电导检测器与电化学检测器串联 ,十几分钟即可连续完成水中S2 - 、SO2 - 3 、SO2 - 4、S2 O2 - 3 的测定 ,方法具有快速、高效、方便、灵敏、选择性好等特点。方法的检出限分别为 :S2 - 12 5 μg/L ;SO2 - 3 2 2 4 μg/L ;SO2 - 45 0 μg/L ;S2 O2 - 35 0 μg/L。相对标准偏差在 1 5 %~ 6 9%之间 ,能够满足水中S2 - 、SO2 - 3 、SO2 - 4、S2 O2 - 3四种阴离子分析测试的需要。 相似文献
235.
通过某工业城市大型一级导线网观测成果的限差检验、观测数据处理,探讨导线网平差时、,边、角验权的合理选择和匹配,及其对平差结果的精度影响,从中得出一些认识和有益的经验。 相似文献
236.
随机地震动场激励下拱坝多点输入的抗震可靠度分析 总被引:5,自引:3,他引:5
本文首次将空间随机地震场输入用于拱坝随机振动分析之中,与拱坝三维动力学有限元法结合,完成了三维拱坝在空间随机地震动场作用下的随机振动分析方法及算法的研究,另外考虑动力和静力的叠加,提出了三维空间随机地震动场的拱坝抗震可靠度分析方法,最后编制了相应的程序,对小湾拱坝进行了抗震可靠度分析,并与随机变量的结果进行了比较。 相似文献
237.
A total of 11 earthquakes with 15 Rayleigh wave paths, recorded at 11 broadband digital PASSCAL seismometers installed in
the Tibet Plateau by the Sino-U.S. joint research group, were used to determine the phase velocity and attenuation coefficient
of surface waves in periods of 10–130 s. The average shear wave velocity and quality factor {ie271-1} structures in the crust
and upper mantle were obtained in this region. The result shows the average {ie271-2} is low and there exists a high attenuation
({ie271-3}=93–141) layer in the crust. The depth range of the low {ie271-4} value layer (16–42 km) is consistent with the
range of low velocity layer (21–51 km) in the crust. Below 63 km in the lower crust, {ie271-5} decreases with depth from 114
to 34 at depth of 180 km. The low shear wave velocity and low value of {ie271-6} at the same depth range in the crust indicate
that the rocks in the range is probably melted or partially melted. According to the shear wave velocity structure, the average
thickness of the crust is about 71 km and a clear velocity discontiniuty appears at the depth of 51 km. The low-velocity zone
(4. 26 km/s) at depth of 96–180 km may be corresponding to the asthenosphere.
Contribution No. 96A0047, Institute of Geophysics, SSB, China.
This study was supported by the National Natural Science Foundation of China. 相似文献
238.
用中国科学院大气物理研究所高分辨率、自由表面热带海洋环流模式对厄尼诺/南方涛动(El/Southern Oscillation)循环中另一重要位相La Niña事件进行了数值模拟研究。模式区域为南北纬30°之间的热带太平洋,经纬圈水平方向分辨率分别为2°和1°,垂直方向分为不等距的14层;模式中考虑了盐度并引入与洋流切变和层结稳定度有关的垂直扩散参数化方案。在观测到的海表风应力、热量和淡水通量(蒸发与降水之差)驱动下,所发展的模式从1984年积分到1989年。本文给出模式对近十几年来最强的1988年La Niña事件进行数值模拟的结果,着重分析La Niña期间热带太平洋海面起伏、流场和温度场时空演变,以及La Niña和El期间变量场时空结构差别。文中还进行了模式结果和一些观测资料间的比较。 相似文献
239.
240.