南极普里兹湾外海大磷虾声学映像的分布分析和生物量的初步估算          下载免费PDF全文

郭南麟  陈雪忠  徐震夷  石承军 《极地研究》1993,5(4):90-103

本文主要根据 1 990 /1 991年度中国南极考察队南大洋调查所获的探鱼仪的磷虾映像资料 ,经 WT- 2图像处理系统处理分析 ,结果表明 ,1 990 /1 991年度南极夏季 ,普里兹湾外海域 (6 2°- 6 9°S,6 8°- 1 0 8°E)的磷虾主要分布在 6 1°- 6 5°S,1 0 3°- 1 0 8°E海区 ,该海区的探鱼仪记录的磷虾群映像的面积占整个调查海区的 92 .3 2 %,磷虾群的分布水层主要在 3 0 - 6 0 m水层 ,在一天 2 4小时中 ,磷虾群映像面积的形心基本在 40 m层上下起伏 ,波动幅度约 1 0 m左右。在调查海区 (6 2°- 6 9°S,6 8°- 1 0 8°E)内 ,估算磷虾资源现存量为 2 2 0 0万吨 ,磷虾分布密度平均为 3 2 .5 t/km2。  相似文献   

张北6.2级地震测震学指标短临判定分析   总被引：4，自引：0，他引：4  

顾瑾平  陈学忠 《地震》1999,19(2):161-167

在对地震学前兆认识的基础上,总结了张北６．２级地震前作出短临判定的可能依据,分析考虑了由场及源、由中国向短临过渡的认识思路。在短临三要素判定中强 空区、条带、平静、震群和中等地震活动及测震学指标异常在时间上的相依性和物理上的关联性。并且对华北近几年发生的５次６级地震的测震学前兆作比较,表明无论是地震活动性或指标参数寂均有共性,但程度各有不同。还非线性理论中的尺度依赖性原理提出一各一范围中的强震进行  相似文献   

福州马尾全新世孢粉组合及其地质意义     

吴学忠 《福建地质》1993,(4)

选择福州马尾青州ZK32钻孔岩芯,作为该地区全新世沉积地层的代表,进行系统的孢粉研究,得出六个孢粉组合,恢复了福州马尾全新世古植被、古气候,探讨了福州马尾全新世地层的划分以及气候与海面变化关系。  相似文献   

时间域航空电磁法在地下空间探测中应用     

梁盛军  李兆亮  何怡原  王明  余学中 《地质论评》2021,67(Z1):67z1215-67z1216

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葫芦岛沿岸海陆风特征及其环境效应     

刘吉敏  黄泓  王学忠 《气象与环境科学》2019,42(1):79-85

利用葫芦岛观测站1980—2009年观测资料,分析了葫芦岛沿岸海陆风风速的季节特征和日变化规律,以及海陆风环流对沿岸环境的影响。结论如下:1)葫芦岛站点在冬季出现海陆风日数最多,其他依次为秋季、夏季和春季。陆风风速从春季到冬季呈现递减趋势;海风在春季最大,其次为秋季的,冬季的最小。总体上,海陆风日中海风要强于陆风。2)对海陆风风速椭圆拟合结果表明,海陆风在10:32由陆风转化为海风,海风在16:32达到最大,在21:42由海风转化为陆风,陆风在04:32达到最大。3)由于海风的存在,沿岸地带在春夏两季日最高气温在12时出现,秋冬季的在13时出现。4)能见度日变化在四季中表现一致,早晨能见度转好的时刻比最低气温出现时刻滞后约2 h,在海风维持较长时间后空气绝对湿度增加导致能见度开始转差。5)冬季静止型海陆风日比例最高,再循环型海陆风日在秋季出现最多,而夏季通风型海陆风日出现最多。  相似文献   

海籍管理系统中用海变化的自动检测方法     

李炳南  蒋雪中  恽才兴 《地球信息科学学报》2013,(5):680-687

彼此相邻的海域之间由于用海类型的不同,经常存在相互的干扰和影响。本文以国家海洋功能区划中规定的海洋功能区分类及海洋环境保护要求为基础,设计了用海变化的自动检测方法。根据不同海洋功能分区的海水水质质量的标准建立缓冲区检测算法和历史用海检测算法,缓冲区检测算法用来检测同一时期不同位置的用海是否存在冲突;历史用海检测算法用来检测同一位置不同时期的用海是否存在冲突。在两种检测算法的基础上,利用地理信息系统开发组件实现了对新加入宗海及原宗海用海变更的自动检测功能,并以上海海洋功能区划数据为测试数据,验证了作为海籍空间信息管理系统的核心功能之一,可以实现用海变化的自动检测,满足对宗海空间变化和时间变化的信息化管理。  相似文献   

河北文安MS5.1地震前首都圈及邻近地区震源动力学参数时空变化特征     

陈学忠  李艳娥  郭祥云 《中国地震研究》2012,26(1):20-32

Source spectra,corner frequency and zero frequency amplitudes in near-source conditions were measured using waveform data from 989 earthquakes with magnitudes larger than ML2.0 observed by the Beijing Digital Telemetry Seismic Network in the Capital Circle Region of China and its surrounding areas from January 2002 to June 2006 by the Brune model.Relevant formulas that were used for the calculation of dynamic source parameters include rupture radius,seismic moment,seismic energy,stress drop,and apparent stress.Scaling relations and characteristics of temporal-spatial variations of these dynamic parameters before the MS5.1 Wenan earthquake in Hebei Province that occurred on July 20,2006 were analyzed.Results show that apparent stress,stress drop,and the ratio of seismic energy to the rupture radius had relatively high values in some areas before the Wenan earthquake.These high-value concentration areas were mainly distributed in the North China Plain seismic zone.As is seen from the time curves,parameters,such as apparent stress,stress drop,and ratio of seismic energy to rupture radius underwent significant ascending processes before the Wenan earthquake,but the variation in the corner frequency showed a descending trend.This result might be related to the enhancement of stress in the North China Plain seismic zone before the earthquake.  相似文献   

北斗/GPS组合伪距单点定位性能测试和分析   总被引：1，自引：0，他引：1  

唐卫明  徐坤  金蕾  文雪中 《武汉大学学报(信息科学版)》2015,40(4):529-533

目的 讨论了北斗/GPS伪距单点定位联合解算的数学模型,并根据北京、武汉两地的北斗/GPS双系统实测数据,在多种模拟遮挡环境下将北斗/GPS联合解算结果与北斗、GPS单系统在可见卫星数、PDOP值、定位精度、定位可用性等方面进行了对比分析。结果表明,相对于单系统伪距单点定位,北斗/GPS组合定位大大增加了可见卫星数,减小了PDOP值,并在观测条件较差的环境下有效地改善了定位精度、显著提高系统定位可用性。  相似文献   

The Focal Mechanism Solutions of the M_S 8.0 Wenchuan Earthquake in Sichuan on May 12,2008 and Some of Its Aftershocks     

Guo Xiangyun  Chen Xuezhong  Li Yan’e 《中国地震研究》2010,24(2):231-243

The focal mechanism solutions of the Wenchuan earthquake(MS8.0) of May 12,2008 and some of its aftershocks occurring up to December 10,2008 are determined with lower semisphere of equal-projection and first motion sign data of P waves from regional and distant stations.The focal mechanism solutions of the MS8.0 Wenchuan earthquake are:Nodal planeⅠ:strike 5°,dip angle 48°,slip angle 39°; Nodal planeⅡ:strike 247°,dip angle 62°,slip angle 131°; P axis azimuth 309°,plunge 8°,T axis azimuth 208°,plunge 54°,B axis azimuth 44°,plunge 35°.Combining geological tectonics and spatial distribution of aftershocks,nodal plane II can be identified as a seismogenic fault.According to focal mechanism solutions,the fault activity that triggered the huge earthquake is reverse thrusting.The main rupture surface is S67° W,basically identical to the fault strike on which the earthquake occurred.The main compression stress P axis is N51°W,which is basically the same as the direction of the regional tectonic stress field.According to the results of focal mechanism solutions of aftershocks,the aftershocks occurring in the southern and northern sections of the Longmenshan fault zone have predominant orientations and are obviously different.For the main shock and the early aftershocks occurring on the southern section of the Longmenshan fault,the rupturing is mainly characterized by reverse-dip slip with some strike-slip,and over time,the aftershocks migrated towards the northern section.The rupturing in the source is mainly characterized by strike-slip with some reverse-dip slips.The stress field is controlled by the main shock stress field in the southern section of the Longmenshan tectonic zone,while it is controlled by the main shock stress field and regional stress field in the northern section of the Longmenshan tectonic zone.  相似文献   

Enhancement of Seismicity Recorded by the Qiaojia Array before the 2013 Lushan and 2014 Ludian Earthquakes     

Li Yan''e  Chen Lijuan  Chen Xuezhong 《中国地震研究》2017,31(4):560-573

A seismic array of twenty four seismometers(Qiaojia array) operated by the Institute of Geophysics,China Earthquake Administration was situated along the Zemuhe fault and the north end of Xiaojiang fault,which is a part of the east boundary of the Chuan-Dian( Sichuan-Yunnan) rhombus crustal mass. The Qiaojia array started operation at the end of February,2012. Since then the April 20,2013 Lushan MS7. 0 earthquake and the August 3,2014 Ludian MS6. 5 earthquake have occurred in the vicinity of the Qiaojia array. The earthquake catalogue recorded by the Qiaojia array since March,2012 is used in this study. The temporal variation of the earthquake count before the Lushan event and the Ludian event is analyzed. The results are as follows:(1) A very clear gradually increasing variation of the count of M ≥ 2. 0 earthquakes within the region,where all earthquakes recorded by the Qiaojia array coverage can be found before the Lushan event and the Ludian event,and the increasing range and duration of the count before the Ludian event are both larger than those before the Lushan event.(2) In the region covered by the Qiaojia array,for earthquakes with depth h ≤10 km a rising process of the count was manifested before both events,along with a nearly same duration of about five and a half months,and for earthquakes with depths h 10 km a rising-dropping process of the count was manifest before the Lushan event,before which the rising-dropping process appeared again. The variation of the count for earthquakes with depth h ≤ 10 km is the reverse of that for earthquakes with depth h 10 km.(3) Within and near the region covered by the Qiaojia array,the variation of the count manifests a rising process for earthquakes with depth h ≤ 10 km or h 10 km before the Lushan event and only for earthquakes with depth h ≤ 10 km before the Ludian event. The variation of the count manifests a weakening process for earthquakes with depth h 10 km before the Lushan event. It is shown from the above results that the seismicity within and near the regioncovered by the Qiaojia array showed a steeply rising change before both the Lushan event and the Ludian event. This phenomenon could be revelatory to understanding the process of seismicity development.  相似文献