结构计算的地震荷载模型     

д.  ВМ 李锟 《世界地震工程》1989,(1):50-52,58

  相似文献   

金矿床的热液流体特征研究     

王建国  孙丽娜  赵玉山  侯根群  赵纯福 《国土资源》1993,(4)

通过对中国东部金成矿区域地质特征的分析,根据氢氧同位素及流体包裹体数据特征,表明中国东部金矿床成矿流体主要来自大气降水,其次为变质作用过程释放的水和岩浆分异水;成矿金属组分主要来自太古宙变质岩系。  相似文献   

摩擦作用对西南低涡扰动的影响     

卢敬华  李双林 《成都信息工程学院学报》1990,(4)

西南低涡是对流层下层的中尺度扰动。本文在零级近似条件下,采用p坐标系的基本方程组,在边界层内设计两层模式。通过一定的简化方程组后,得到:当Z≤1/2[kL~2/(μ~2Knu~*)] 时,摩擦效应具有二重性,一方面使扰动减弱;另一方面使扰动增强,而前者的影响略大于后者,最终使扰动消失。频率随高度Z的降低而增加。当Z>1/2[kL~2/(μ~2Knμ~*)]时,摩擦作用甚微,几乎可以忽略不计。频率虽然有两个值,但随高度Z的增加,他们趋于一个常值。  相似文献   

武汉区域气象中心数值预报业务并行计算机系统     

龚贤创  范宏飞  余康庆  王宏记 《成都信息工程学院学报》2002,17(4):236-239

对武汉区域气象中心并行计算机系统进行了详细地介绍，分析了并行计算机体系结构、网络和存储系统特点；给出了在并行计算机SP上实现数值预报业务并行化的部分结果；对数值预报模式在串、并行编程环境下的结果进行了分析比较。  相似文献   

高频VLBI观测射电源的结构     

田文武  张海燕等 《云南天文台台刊》2001,(2):1-9

高频VLBI观测揭示出河外射电源在pc或者亚pc尺度上大都有核-喷流的内部结构，尤其是对平谱致密射电源中毫角秒尺度的子源，能以相当高的概率观测到它的视超光速现象。多频观测可监测到一些新喷流子源的出现，特别在射电激变源中这些新喷流子源的出现与宽带内（从光学到γ射线）的爆发相关。且得到的一些源的核区谱指数分布，为确认源的VLBI核提供了支持。  相似文献   

"活地兴城"看营口     

苏梅 《国土资源》2002,(8):10-19

题记:土地是财富之母城区土地一朝被作为经营城市的资本,那么,多米诺骨牌效应将在这块土地上产生——  相似文献   

维护农民合法权益促进农民增加收入     

杨任远 《江苏国土资源》2002,(2):5-7

国土资源部门是涉农部门。土地是农民的命根子，为“三农”服务特别是维护农民土地权益、促进农民增收，是国土资源部门义不容辞的职责。回顾总结了近年来这方面的工作，指出了今后一个时期国土资源部门为“三农”服务的方向。  相似文献   

1989年8月17日太阳射电尖峰事件的准周期脉动及EFB分析     

张衡  孔勇进  龚元芳  楼恩蕊  尚琼珍 《中国天文和天体物理学报》1994,(1)

本文分析了云南天文台１０ｍ射电望远镜在２ｌｃｍ波段上观测到的一次尖峰辐射事件，这次事件发生在５６２９活动区（Ｓ１６Ｗ１０９），它伴随了Ｘ２·９／ＳＦ耀斑及边缘耀斑环，并且有质子流量的上升和一次罕见的地磁场突然反相脉冲与之对应．我们从耀斑环的Ｈβ照片可以看出，在尖峰辐射发生前，原先存在的耀斑环的顶部开始变亮，而尖峰开始后环顶亮度达到极大，说明这次尖峰辐射与耀斑环顶部增亮有关，辐射很可能来自环顶．从尖峰事件的时间轮廓得到的ＦＦＴ功率谱表明存在１５０ｍｓ的准周期脉动．按照Ｍｃｌｅａｎ等人的模型，即脉动是由俘获在磁通管内的电子的径向振荡引起，可以推断，这次尖峰辐射与Ｆｅｒｍｉ机制激发快速电子有关，且尖峰的发生需要被俘获的电子．此外，我们将这次尖峰事件分解为几百个元耀斑爆发（ＥＦＢ），并且讨论了这些ＥＦＢ的性质．  相似文献   

Comparison of Taste Components between Triploid and Diploid Oyster     

LINHong WANGXiaoxue ZHANGBin TANGHaiqing XUEChanghu XUJiachao 《青岛海洋大学学报(英文版)》2002,1(1):55-58

The main taste components of triploid and diploid oyster (Crassostrea gigas) were compared. Free amino acids, inosine monophosphate, succinate, trimethylamine oxide and betaine in fresh and boiled extractives were analyzed. The protein, lipids, glycogen, moisture and ash, which may affect the flavour, were evaluated. In boiled extractives, the amino acids were 394.1 mg(100g)^-1 in diploid and 183.5 mg(100g)^-1 in triploid. However, in fresh oyster extractives, they were 320.0 mg(100g)^-1 and 147.3 mg(100g)^-1 respectively. The inosine monophosphate in triploid was 44% more than that in diploid, and a little difference existed in the content of trimethylamine oxide between them. The contents of these taste components were the basis for taste flavour pattern determination.  相似文献   

Mantle processes during ocean formation：Petrologic records in peridotites from the Alpine－Apennine ophiolites     

GiovanniB.Piccardo 《《幕》》2003,26(3):193-199

Mantle peridotites were early exposed at the sea-floor of the Jurassic Tethys derived from the subcontinental mantle of the Europe-Adria system. During continental rifting and oceanic spreading, these lithospheric peri-dotites were percolated via diffuse reactive porous flowby melt fractions produced by near-fractional melting of the upwelling asthenosphere. Ascending melts inter-acted with the lower lithosphere, dissolving pyroxenes and precipitating olivine, and crystallized at shallower levels in the mantle column causing melt impregnation.Subsequent focused porous flow formed replacive dunitechannels, cutting the impregnated oeridotites, which were conduits for upward migration of MORB-type liq-uids. Melt migration produced depletionlrefertilization and significant heating of the percolatedlimpregnated mantle, i.e the thermochemical erosion of the litho-sphere. Impregnated and thermally modified lithos-pheric mantle was cooled by conductive heat loss dur-ing progressive lithosphere thinning and was intrudeaby MORB magmas, which formed Mg-rich and Fe-richgabbroic dykes and bodies. Alpine-Apennine ophiolitic peridotites record the deep-seated migration of melts which changed their compositions and dynamics during the rift evolution. The thermochemical erosion of the lithospheric mantle by the ascending asthenospheric melts, which induces significant compositional and rhe-ological changes in the lower lithosphere, is a major process in the evolution of the continent-ocean transi-tion towards a slow spreading oceanic system.  相似文献