九江-瑞昌5.7级地震余震的S波分裂研究     

汤兰荣  石玉涛  曾新福  郑斌  赵博  吕坚 《中国地震》2012,28(2):179-187

利用在九江-瑞昌MS5.7地震震中附近架设的丁家山台(DJS)、狮子洞台(SZD)和武蛟台(WUJ)的地震波形资料,采用S波分裂系统分析方法,对余震进行了S波分裂分析。结果表明,震中距较小、台站附近断层分布复杂的丁家山台(DJS)的慢波时间延迟相对较大,快波偏振方向不太集中。台站附近断裂分布单一的武蛟台(WUJ)快波偏振优势方向与断裂走向角度相差约35°,与区域主压应力方向也不一致。台站附近无断层通过的狮子洞台(SZD)快波偏振优势方向接近区域主压应力方向。慢波时间延迟大小与震源深度没有明显的规律性关系。  相似文献   

静乐井水位前驱波重现性问题探讨   总被引：1，自引：0，他引：1  

张淑亮  刘瑞春  吕芳 《中国地震》2012,28(2):200-213

以山西静乐井为研究对象,对井水位前驱波重现性问题进行了探讨。结果表明,相似地震前前驱波起始时间和波动周期在一定范围内具有较强的重现性,其比例可达63.1%;部分相似地震前前驱波的波动形态和幅度也存在一定的相似性,但在研究范围内前驱波各项特征均相似的地震尚未发现,其原因可能与前驱波的成因、传播途径、相似地震的震源区特征等因素有关。  相似文献   

太原地震台水位异常分析     

沈晓松  靳玉贞  孟彩菊  冯建琴  吕芳  张淑亮  范雪芳  陈常俊 《地震地磁观测与研究》2012,33(5):178-182

针对太原地震台晋7-1井近年来水位大幅上升情况,进行资料收集和干扰因素分析,结果发现：2009年7月以来的井水位回升,与关闭小煤窑、汾河清水复流工程、关井压采、大量引用黄河水有直接关系。  相似文献   

济南地磁台地磁监测环境分析     

王锋吉  张刚  吕子强 《地震地磁观测与研究》2012,33(Z1)

描述济南地磁台建台以来,周边环境随着城市化进程发生的变化,计算不同重量、距离的铁磁性物质对磁房建筑场地地磁场的影响,应用G856质子旋进磁力仪,采取梯度测量的方法,进行地磁场总强度F测量,对测量结果进行计算和初步分析,以期为其他地磁台的观测环境分析提供参考.  相似文献   

Studies of TLP dynamic response under wind, waves and current     

谷家扬  杨建民  吕海宁 《中国海洋工程》2012,26(3):363-378

Investigated is the coupled response of a tension leg platform (TLP) for random waves. Inferred are the mass matrix, coupling stiffness matrix, damping matrix in the vibration differential equation and external load of TLP in moving coordinating system. Infinitesimal method is applied to divide columns and pontoons into small parts. Time domain motion equation is solved by Runge-Kutta integration scheme. Jonswap spectrum is simulated in the random wave, current is simulated by linear interpolation, and NPD spectrum is applied as wind spectrum. The Monte Carlo method is used to simulate random waves and fluctuated wind. Coupling dynamic response, change of tendon tension and riser tension in different sea conditions are analyzed by power spectral density (PSD). The influence of approach angle on dynamic response of TLP and tendon tension is compared.  相似文献   

Modified Na‐Montmorillonite With Quaternary Ammonium Salts: Application for Removal of Salicylic Acid From Aqueous Solutions          下载免费PDF全文

Zilin Meng  Fengzhu Lv  Yihe Zhang  Qian Zhang  Zhilei Zhang  Shutao Ai 《洁净——土壤、空气、水》2015,43(8):1150-1156

  相似文献   

沧州地区地面沉降现状Sentinel-1A/B时序InSAR监测与分析     

周洪月  汪云甲  闫世勇  吴岳  刘茜茜 《测绘通报》2017,(7):89-93

获取了22景IW模式的Sentinel-1A/B数据,分别采用PS-InSAR和SBAS-InSAR两种时序技术得到了沧州地区2015年11月至2016年11月期间地表平均沉降速率及累计沉降量。经分析,两种时序监测结果具有较高的一致性,其结果表明：献县、沧县、沧州市区地面表现为回升趋势;青县、沧县东部、南皮县西部、东光县等地区地面沉降量较大,其中东光县何庄村累计下沉量达47 mm,而引起这些区域地面沉降的主要原因为农业生产等带来的地下水开采。本文对基于Sentinel-1A/B SAR数据的时序分析方法在城市沉降监测方面的应用进行了探讨,为有关部门提供了重要的参考数据。  相似文献   

Geochemistry, geochronology and mineralization of the rare-metal granites in the Daping Ta-Nb deposit, Fujian Province, South China     

WANG Jinrong  HU Yongbin  HUANG Shufeng  CHEN Bin  YE Yuansheng  LUO Xiaohua  Lv Xinbiao 《《地质学报》英文版》2017,91(Z1):289-290

<正>1 Introduction Rare-metal granites are widely distributed in South China.The Daping porphyritic granitic Ta-Nb deposit,located in the Yongding area of south Fujian province,South China,is a large rare-metal deposit recently discovered.Few studies have been made of its petrology,mineralogy,geochemistry,chronology and metallogeny.In recent years,several exploratory drillings have been done in this deposit.These drilling holes,from 380 to 600  相似文献   

Soil erosion changes over the past five decades in the red soil region of Southern China   总被引：4，自引：0，他引：4  

Yin Liang  Decheng Li  Xixi Lu  Xuan Yang  Xianzhang Pan  Huan Mu  Deming Shi  Bin Zhang 《山地科学学报》2010,7(1):92-99

This paper reports the dynamic changes of soil and water loss in the red soil region of Southern China since the 1950s. The red soil region covers eight provinces: Jiangxi, Zhejiang, Fujian, Anhui, Hubei, Hunan, Guangdong and Hainan. From the 1950s to 1986, the annual rate of soil erosion increased by 3.4%. From 1986 to 1996 and from 1996 to 2000, the annual rates of soil erosion decreased by 2.0% and 0.32%, respectively. Field surveys showed that from 2000 to 2005, the area of soil and water loss decreased annually by 1.2%. This decrease was a result of large-scale erosion control activities across China. Although the eroded soil has been restored, the restoration process is very slow and full restoration will take a long time. Our report suggests that controlling soil and water loss is a challenging task, and additional measures must be taken to effectively control the soil erosion in the red soil region.  相似文献   

The Annual Characteristics of Rainwater HCHO in Guiyang City,Southwest of China     

Xu Gang  Shao HongBo  Lee XinQing  Lv YingChun 《洁净——土壤、空气、水》2010,38(8):726-731

HCHO is ubiquitous and important chemical constitutes in the troposphere. The concentrations of the HCHO (aq) in the rainwater were measured in the Guiyang city, southeastern of China from May 2006 to April 2007 and 153 discrete samples were collected. Rainwater (N = 151) HCHO (aq) concentrations ranged from lower than method detection limit (MDL) to 40.2 µmol/L with a volume weighted mean value of 7.4 ± 8.8 µmol/L. The strong correlations between HCHO (aq) and HCOO^? (r = 0.69, n = 137), HCHO (aq) and nss‐ (r = 0.74, n = 137), HCHO (aq) and (r = 0.67, n = 137), HCHO (aq) and (r = 0.74, n = 133) suggest the significant influence of the anthropogenic input for the HCHO (aq) levels. The concentration levels of rainwater HCHO (aq) was inversely proportional to the amount of rainfall, indicating the below‐cloud process is the most important mechanism for rainwater HCHO (aq) scavenging processes. More than 70% of the HCHO (aq) wet deposition took place during the early stage of the rainfall. According to the air mass back‐trajectory analysis, the rainwater with industrial back‐trajectories coming from the north had the highest levels of HCHO (aq) while the rainwater with the green‐covered or marine back‐trajectories from the southeast had the lowest concentrations, and this indicate the HCHO (aq) originated from urban or industrial regions served as an important source of the rainwater. The annual HCHO (aq) wet deposition flux was calculated as 6.96 mmol/m² per year and the total deposition flux was estimated as 24.35 mmol/m² per year, 71.4% of which was dominated by dry deposition.  相似文献