从全波段太阳直射辐射确定大气气溶胶光学厚度 II：实验研究   总被引：2，自引：1，他引：2       下载免费PDF全文

邱金桓  杨景梅  潘继东 《大气科学》1995,19(5):586-596

本文通过比较太阳直射表和太阳光度计探测的大气柱气溶胶光学厚度，分析了从太阳直射表探测的全波段太阳直射光强信息确定大气柱气溶胶光学厚度的误差，并应用北京观象台的太阳直射表观测资料，反演得到了 1990—1993年北京大气柱气溶胶光学厚度，分析了该光学厚度月与年变化规律以及1991年菲律宾皮纳图博火山爆发对北京大气气溶胶含量的影响。本文还提出了关于有效水汽含量的一个经验关系式，用于确定水汽对太阳辐射的吸收率。  相似文献   

1987年1月8日甘肃迭部5.9级地震与地形变特征   总被引：1，自引：0，他引：1  

邹明吾  潘颖凌 《地震地磁观测与研究》1995,16(3):35-40

根据１９８７年１月８日甘肃迭部５．９级地震前，该区域的地壳形变中长期背景和定点台站连续观测资料的震反应异常，分析研究了这此异常的变化特征。  相似文献   

硼镁铁矿的新亚种——富锡硼镁铁矿     

杨光明  潘兆橹  彭志忠 《岩石矿物学杂志》1987,6(3):229-235

富锡硼镁铁矿是硼镁铁矿的含锡亚种。它产于湖南常宁县七里坪镁质矽卡岩硼矿床中。矿物中SnO_2变化范围为4.6—12.0%,其分子式为(Mg_1.64Fe~(2+_(0.35))Mn~(2+_(0.01))(Fe~(3+_(0.55))Sn_(0.16)Mg(0.23))BO_5,这是迄今未见详细报导过的。笔者从矿物的光学物理性质、化学成分、X射线晶体学以及晶体化学等方面进行了研究。同时,与它的类似矿物在晶体学方面作了对比讨论。从以上研究中得出结论:Sn~(4+)在结构中占据Fe~(3+)的位置,并以伴随着的Mg~(2+)作电荷补偿。还提出了Sn元素在硼镁铁矿中不仅作为微量元素存在,而且可以作为造种元素存在的新见解。  相似文献   

山东归来庄金矿区g(Au/Ag)的空间信息统计学特征     

肖斌  潘懋  赵鹏大  侯景儒 《地质科学》2001,36(4):500-508

空间信息统计学是一门集数学、空间信息科学及计算机技术于一体,在时空域内对区域化变量的随机性与结构性进行定量研究的技术。以山东归来庄金矿床为例,对其g(AuAg)异常进行空间信息统计学研究。利用指示克立格法研究g(AuAg)的空间变异结构特征,建立空间结构模型。在对结构模型和估计方案进行交叉验证后,对g(AuAg)的空间分布进行估计。根据g(AuAg)的空间分布规律,探讨其与Au空间分布的关系,并对今后该区的找金工作提出建议。  相似文献   

浅谈自动气象站的防雷设计要点   总被引：2，自引：0，他引：2  

李荣迪  潘田凤 《广西气象》2005,26(2):51-52,55

运用当代防雷领域中的有关理论，对自动气象站容易遭受雷击的原因和途径进行分析，提出了自动气象站的防雷设计要点。  相似文献   

中小震近场地震动估计中地震动衰减关系的适用性分析   总被引：9，自引：1，他引：9  

李小军  阎秀杰  潘华 《地震工程与工程振动》2005,25(1):1-7

核工程场地设计基准地震动确定中涉及弥散地震的地震动估计，这导致中小震近场地震动估计成为被关注的研究课题。本文基于一些中小震近场地震动记录资料，分析和探讨了国内外多种地震动衰减关系对中小震近场地震动估计的适用性问题，并结合我国几个核工程地震问题研究工作的实践对中小震近场地震动衰减关系确定的思路和原则提出了建议。  相似文献   

地质科学应用程序从Basic向Visual Basic移植的技巧     

潘孝荣 《福建地质》2005,24(3):193-199

介绍了地质科学应用程序从Basic向Visual Basic（简称VB,下同）移植的基本技巧,并结合实际开发经验对变量定义、数据读取、成果输出和存储等开发、移植过程做了说明.  相似文献   

Cenozoic uplift of West Qinling, northeast margin of Tibetan plateau-a detrital apatite fission track record from the Tianshui basin     

Wang Xiuxi  Li Jijun  Song Chunhui  Zhang Jun  Zhao Zhijun  Gao Junping  Pan Meihui 《Frontiers of Earth Science》2007,1(3):304-308

The Cenozoic sedimentation in the Tianshui basin, which is located at the junction of the liupanshan and West Qinling, northeast margin of the Tibetan plateau, provides a record for the regional tectonism and exhumation history of the surrounding mountains. Thermochronologic study on the detrital apatite grains from sandstones at Yaodian, near Tianshui, has revealed two rapid tectonic uplift-exhumation events of the source area, which happened at 23.7 and 14.1 Ma, respectively. The fast exhumation (0.34 mm/a) at 23.7 Ma, which recorded the tectonic uplift of West Qinling, led to the formation of the Neogene Tianshui basin and initiated the reception of alluvial deposits. This event is most likely in response to the synchronous tectonism of the Tibetan plateau. The source region experienced another rapid exhumation (1.05 mm/a) at 14.1 Ma, when the Tianshui basin began to depress broadly and fluvial-lacustrine sediments dominated the Late Miocene. Translated from Acta Sedimentologica Sinica, 2006, 24(6): 783–789 [译自: 沉积学报]  相似文献   

Crustal structure using receiver function in the east part of A＇nyemaqen suture belt     

段永红张先康  刘志徐朝繁  王夫运潘纪顺 梁国经 《地震学报(英文版)》2007,20(5):513-522

Twenty broadband seismographs were deployed along Hongyuan, Sichuan to Wuwei, Gansu. 81 teleseismic events were recorded in one year. We computed receiver functions from teleseismic waveform data and obtained S wave velocity structure beneath each station along the profile by using receiver function inversion method. The results revealed that the crustal structure is very complex and crustal average S wave velocity is to be on the low side. Low velocity structure generally exists in the depth range of 10～40 km in the crust between Aba arc fault and northern edge fault of Qinling earth＇s axis and it is a tectonic feature of complex geological process such as ancient A＇nyemaqen Tethys ocean from closing and side colliding to subducted plate exhumed or thrust rock slice lifted. The Moho is about 50 km depth along the profile and is slightly deeper in the south than in the north.  相似文献   

Approximation of interfacial properties in multiphase porous medium systems     

J.E. McClure  D. Adalsteinsson  C. Pan  W.G. Gray  C.T. Miller 《Advances in water resources》2007

We investigate the estimation of interfacial areas, curvatures, and common curve lengths in multiphase porous medium systems. Algorithms are developed to obtain estimates of these quantities based upon a variety of potential data sources and estimation approaches. The accuracy of the derived approximations are evaluated as a function of the data type and resolution of the data. The methods advanced improve upon standard approaches now in use and show excellent accuracy at resolutions on the order of five lattice points per minimum radius of curvature of the object being resolved. Finally, we suggest a promising class of extensions that could lead to further improvements in the accuracy of such methods.  相似文献