中国大陆地区地磁场Z分量日变化相位的空间分布特征研究   总被引：1，自引：0，他引：1       下载免费PDF全文

王亚丽  吴迎燕  卢军  余素荣  黎明晓 《地球物理学报》2009,52(4):1033-1040

利用全国52个地磁台站近20年的观测数据,分析我国大陆地磁Z分量日变化相位变化的空间分布特征,得到如下结论：（1）所有台站Z分量低点时间均服从正态分布;（2）Z分量低点时间期望值与经度之间具有很强的负相关关系,反映出显著的地方时依赖性;（3）低点时间标准差与纬度之间具有一定的正相关关系;（4）中国大陆存在两个Z分量低点时间的异常区域,均表现为低点时间比周围地区明显提前,且低点时间的离散度大于周边地区;（5）去除异常区观测点数据之后,低点时间标准差呈现出在30°N（和地磁纬度20°）附近为极小值而向低纬和高纬分别增大的特点,用二次或三次曲线可以在一定程度上描述这种相关关系.  相似文献   

Characteristics of earthquake-triggered landslides and post-earthquake debris flows in Beichuan County   总被引：2，自引：2，他引：0  

Jianqi Zhuang  Peng Cui  Kaiheng Hu  Xiaoqing Chen  Yonggang Ge 《山地科学学报》2010,7(3):246-254

Field investigations and aerial photography after the earthquake of May 12,2008 show a large number of geo-hazards in the zone of extreme earthquake effects.In particular,landslides and debris flows,the geo-hazards that most threaten post-disaster reconstruction,are widely distributed.We describe the characteristics of these geo-hazards in Beichuan County using high-resolution remote sensing of landslide distribution,and the relationships between the area and volume of landslides and the peak-discharges of debris flows both pre-and post-earthquake.The results show:1) The concentration(defined as the number of landslide sources per unit area:Lc) of earthquaketriggered landslides is inversely correlated with distance from the earthquake(DF) fault.The relationship is described by the following equation:Lc = 3.2264exp(-0.0831DF)(R2 = 0.9246);2) 87 % of the earthquake-triggered landslides were less than 15×104 m2 in area,and these accounted only for 50% of the total area;84% of the landslide volumes were less than 60×104 m3,and these accounted only for 50% of the total volume.The probability densities of the area and volume distributions are correlated:landslide abundance increases with landslide area and volume up to maximum values of 5 × 104 m2 and 30 × 104 m3,respectively,and then decreases exponentially.3) The area(AL) and volume(VL) of earthquake-triggered landslides are correlated as described with the following equation:VL=6.5138AL1.0227(R2 = 0.9131);4) Characteristics of the debris flows changed after the earthquake because of the large amount of landslide material deposited in the gullies.Consequently,debris flow peak-discharge increased following the earthquake as described with the following equation:Vpost = 0.8421Vpre1.0972(R2 = 0.9821)(Vpre is the peak discharge of pre-earthquake flows and the Vpost is the peak discharge of post-earthquake flows).We obtained the distribution of the landslides based on the above analyses,as well as the magnitude of both the landslides and the post-earthquake debris flows.The results can be useful for guiding post-disaster reconstruction and recovery efforts,and for the future mitigation of these geo-hazards.However,the equations presented are not recommended for use in site-specific designs.Rather,we recommend their use for mapping regional seismic landslide hazards or for the preliminary,rapid screening of sites.  相似文献   

煤田弯线地震勘探技术及应用     

杨双安  魏书宏 《煤田地质与勘探》2002,30(4):55-57

在黄土塬区或复杂的黄土地形区作煤田地震勘探工作需要进行沿沟弯线地震施工技术的研究。通过项目实施,对弯线技术的应用有所见解,着重分析了弯曲测线在煤田地震勘探中的主要采集参数选择和施工技术措施,并介绍了地震弯线技术的应用效果。   相似文献   

Discussion on the Relationship between Different Earthquake Magnitude Scales and the Effect of Seismic Station Sites on Magnitude Estimation     

Zhang Hongzhi  Diao Guiling  Zhao Mingchun  Wang Qincai  Zhang Xiao  Huang Yuan 《中国地震研究》2008,22(1):24-30

Based on the earthquake catalog reported by the Chinese digital seismic network in recent years, we select the earthquakes with both surface wave magnitude and local magnitude and fit them into a relationship between the two magnitudes. The systematic difference is found from the formula which has been used for 30 years. Because of a large dynamic range and wide frequency range of the current digital observation system, in addition to a larger number of stations and earthquakes being used compared to before, the relation obtained in this paper seems more reliable. Our calculation shows that there is no significant difference before and after magnitude conversion so we suggest the abandonment of magnitude conversion. The site response of a station consists of amplification at different frequencies. The amplification is equal to about 1 and changes little with frequency at stations located on basement rock, and it is greater than 1 at low frequency ranges and less than 1 at high frequency ranges at stations located on sediment layers. The difference between magnitudes from single station located on sediment layer and the average magnitude from the whole network increases from negative to positive with period. It seems that there is no fixed station correction factor and the station correction method does not work to improve the accuracy and magnitude estimates.  相似文献   

海洋重力测量中厄特弗斯改正的优化计算     

张会  柳林涛  梁星辉 《海洋测绘》2011,31(5):1-3

厄特弗斯效应改正值的精度是影响海洋重力测量精度的最主要因素。为了提高其改正精度,提出采用航迹线拟合、合理的航向角和航速计算以及厄特弗斯改正值滤波,并通过理论分析和实例计算证明了该方法的有效性。  相似文献   

深层掏土纠偏法在桩基上多层建筑中的应用研究   总被引：1，自引：0，他引：1  

朱方敏  茜平一  解家毕  徐晗 《岩土力学》2006,27(9):1617-1621

以某栋房屋的倾斜和纠偏为例,采用多高层建筑上部结构-桩基础-地基共同作用分析方法,探讨了深厚软弱地基上大面积地面堆载作用下桩基础建筑物的倾斜、变形形态及桩侧摩阻力的分布情况;了解了桩基础的变形形态及桩端土沉降的成因,进而对掏土纠偏法在桩基础纠偏中的适用性进行研究,为进一步的工程措施提供有效的依据。  相似文献   

定位子台网的选取对定位结果影响研究     

赵英萍  高景春  刘丽  毛国良  常亮  季爱东  王树兴  赵明淳 《地震》2006,26(4):37-44

选取了河北及邻区58个不同区域的地震, 分析“定位子台网”分布对地震定位精度的影响, 研究“定位子台网”的选取规则。 分别探讨了三种台站分布情况下定位偏差、 水平误差、 拟合残差随空隙角、 近台距离、 远台距离的变化; 定位偏差以及水平误差与拟合残差的关系。 结果显示, 速报时选择7～9个分布相对合理的“定位子台网”参加定位结果比较好, 使用水平误差估计定位结果质量比较适合。  相似文献   

三维数值分析在岩土工程应用中的误差问题     

李焕强  李渝生  刘涛  陈智强 《岩土力学》2005,26(12):1945-1948

岩土工程本身的复杂性使岩土工程的三维模型分析结果与实际有一定的误差。利用已有的工程反馈资料,对模型参数进行反演分析。修正易调整的误差因素,来弥补不易调整的误差因素,将模型计算结果的最终误差降到最小。将得到的反演参数用于下一阶段的模型分析,由此获得的三维计算结果更接近真实值。  相似文献   

重力异常反映的郯庐带中南段构造边界与应力场     

朱益民  余腾  王鑫  张鹏 《大地测量与地球动力学》2023,43(1):71-81

为解决传统基于重力场数据一阶导数定义的总水平导数和解析信号振幅存在无法均衡深浅异常振幅的问题,应用重力全张量梯度数据,提出改进的倾斜导数地质体边界识别方法NTD_M。经模型验证,NTD_M在收敛性、抑噪性和边界识别精度方面均有提升。利用NTD_M将郯庐带中南段及邻区划分为14个边界较为清晰的构造单元,借助垂线偏差数据对郯庐带中南段的构造应力场和壳幔密度差进行反演。结果显示,二者在水平方向上存在显著差异,在空间上显著相关,构造应力最大差异值约为16 MPa,壳幔密度差约为0.2 g/cm³,构造应力等值线密集处与构造单元划分的边界以及地震分布情况对应较好。郯庐带中段最大主应力方向为NEE-EW,南段主应力方向以EW-NWW为主,总体呈EW向,与震源机制解、地应力测量和GPS反演结果具有较好的一致性。  相似文献   

2022年8月四川盆地持续性极端高温特征及不同模式预报误差分析     

周秋雪  冯良敏  陈朝平  刘莹 《气象科技》2024,52(2):243-251

本文基于2022年8月四川盆地104站逐时温度、降水数据和1971—2021年历史同期数据,及EC、CMA GFS、CMA MESO模式的2 m气温预报等数据,运用统计学相关方法分析了此次极端高温过程的特征及预报误差。结果表明：①2022年8月四川盆地极端高温过程范围大、强度强、持续时间长,有87.5%站最高气温超过该站历史同期极值,且高温最强盛时段较历史同期明显推后。②2022年8月最高气温分布为东高西低,最高气温与历史同期极值差分布则相反,其中最高气温随站点海拔增大而减小,而极值差则随站点海拔先增大再减小。另外,受热岛效应影响,极值差大值站点主要集中在龙泉山脉附近。③高温期间,最高、最低气温平均值高、距平大,且累计降水量和雨日数也明显低于历史同期。④相较而言,EC模式的预报优势主要在盆地低海拔地区。而CMA MESO模式在盆地周边陡峭地形区域的平均绝对误差则更小。另外,EC模式预报的最高气温峰值出现时间更接近于实况,而CMA MESO模式预报高温持续日数更接近实况。  相似文献