吉南老岭地区控矿构造特征分析   总被引：1，自引：0，他引：1  

于城  松权衡  李卫东  黄斌 《吉林地质》2007,26(3):1-5

吉南老岭地区矿产资源丰富,大中型矿床众多,是吉林省的主要成矿区带。本文主要研究大地构造背景和地壳的演化规律及本地区韧性断裂、脆性断裂、韧脆性断裂及变质变形作用等构造类型的特征,进而阐明这些构造对矿产的控制作用。  相似文献   

多年冻土区桩基础桥墩随机地震反应分析   总被引：3，自引：0，他引：3  

虞庐松  严松宏  陈兴冲  高峰 《世界地震工程》2007,23(1):12-16

将随机振动理论、粘弹性边界条件的二维波动法以及结构动力分析有限元法结合起来，考虑场地地震动为零均值的高斯平稳随机过程，对青藏铁路多年冻土区桩基础桥墩进行了随机地震反应分析，计算了9度地震作用下桥墩随机地震响应最大值的均值和均方差，分析了冻土层及桥墩高度对桥墩随机地震响应的影响。  相似文献   

谈谈浑河断裂带的新构造          下载免费PDF全文

何恃松 《地震地质》1981,3(2):65

浑河断裂带在前震旦纪就开始活动,中生代时期活动剧烈,至第三纪和第四纪初、浑河断裂带的构造活动更为频繁强烈。本文主要讨论浑河断裂带自沈阳至清原县草市地段从第三纪以来的新构造活动的一些形迹  相似文献   

西太平洋高压的一些研究   总被引：2，自引：1，他引：2  

黄士松 《气象》1979,5(10):1-3

有关西太平洋高压对我国的雨季、暴雨、旱涝、台风路径等影响问题,近一、二十年来我国广大气象工作者做了大量研究工作,随而对西太平洋高压的活动规律问题更广泛地进行了研究,均取得丰硕的成果。这里我们着重对活动规律的研究结果作一简单的综合介绍。 副热带高压是位于副热带地区的高压系统。在对流圈中层主要位于海洋上,亦有出现在大陆上的。到了高层在200或100mb图上,情况有很大不同,特别在夏季,此时太平洋与大西洋上空变为低槽区,而在  相似文献   

一种泥流擦痕的发现          下载免费PDF全文

李玶  刘行松  潘裕生 《地质论评》1966,24(3):242-244

在湖北丹江口丘陵区出露的基岩面上,发现一些擦痕(在均县习家店一带的丘陵上也有发现)。尤其是张家沟一带,这类擦痕更为多见。有人认为是冰川擦痕,有人怀疑是山洪时水中石子撞击而成,作者试提出另一种看法,即擦痕的形成实系一种泥流缓慢滑动所致。这里特作报道以供讨论。  相似文献   

一九七九年我国东部夏季风系统初步分析(摘要)     

汤明敏  黄士松  陆森娥 《浙江气象》1981,(4)

八月中旬,全国夏季风学术交流会在我省莫干山召开。本刊摘要刊登了南京大学黄士松教授和中山大学陈世训教授的两篇学术报告。我省气象局局长亓汉三同志出席了会议,在开幕式上讲了话,并即兴赋诗一首: 长夏暑炎天,群贤集莫干。将邪双剑在,千古照人间。人工穷造化,季风共磋研。河山锦绣美,气象景万千。  相似文献   

江淮气旋发生发展和暴雨过程及有关预报问题的研究   总被引：3，自引：0，他引：3  

黄士松  林元弼  韦统健 《大气科学》1976,(1):27-41

本文就一次典型过程作为例子,分析了江淮气旋发生发展和暴雨过程的特点,指出有利于江淮气旋发生发展的高空天气形势,地面一些中尺度低压和暴雨核的演变与气旋发展的互相联系。发现气旋区内可存在若干个中尺度低压,这些中尺度低压可先于或后于暴雨核生成而出现,并可增强、减弱或合并。文中计算了潜热释放的加热对涡度制造的贡献,指出潜热加热对气旋发展起着极为重要的作用。作者对于影响气旋发展的因子进行了讨论,并对如何根据湿度场、流场和降水分布(或卫星云图)特征来预报江淮气旋提出建议。  相似文献   

地震时孔隙水压力观测和估算     

石兆吉  郁寿松 《世界地震工程》1990,(4):13-19

  相似文献   

Growth and energy budget of juvenile lenok Brachymystax lenok in relation to ration level     

刘洋  李钟杰  张堂林  苑晶  牟振波  刘家寿 《中国海洋湖沼学报》2015,33(2):347-355

We evaluated the effect of ration level(RL) on the growth and energy budget of lenok Brachymystax lenok. Juvenile lenok(initial mean body weight 3.06±0.13 g) were fed for 21 d at five different ration levels: starvation,2%,3%,4% bwd(body weight per day,based on initial mean values),and apparent satiation. Feed consumption,apparent digestibility,and growth were directly measured. Specific growth rates in terms of wet weight,dry weight,protein,and energy increased logarithmically with an increase in ration levels. The relationship between specific growth rate in terms of wet weight(SGRw,%/d) and RL(%) was characterized by a decelerating curve: SGRw=-1.417+3.166ln(RL+1). The apparent digestibility coefficients of energy exhibited a decreasing pattern with increasing ration level,and there was a significant difference among different RLs. Body composition was significantly affected by ration size. The relationship between feed efficiency rate in terms of energy(FERe) and RL was: FERe=-14.167+23.793RL–3.367(RL)2,and the maximum FERe was observed at a 3.53% ration. The maintenance requirement for energy of juvenile lenok was 105.39 k J BW(kg)-0.80/d,the utilization efficiency of DE for growth was 0.496. The energy budget equation at satiation was: 100IE=29.03FE+5.78(ZE+UE)+39.56 HE+25.63 RE,where IE is feed energy,FE is fecal energy,ZE+UE is excretory energy,HE is heat production,and RE is recovered energy. Our results suggest that the most suitable feeding rate for juvenile lenok aquaculture for wet weight growth is 2.89% bwd,whereas for energy growth,the suggested rate is 3.53% bwd at this growth stage.  相似文献   

在大洋环流模型中对应于惯性内波破碎的垂直混合的一个参数化方案   总被引：1，自引：0，他引：1  

范植松  尚真琦  张善武  胡瑞金  刘海龙 《海洋学报(英文版)》2015,34(1):11-22

Based on the theoretical spectral model of inertial internal wave breaking(fine structure) proposed previously, in which the effects of the horizontal Coriolis frequency component f-tilde on a potential isopycnal are taken into account, a parameterization scheme of vertical mixing in the stably stratified interior below the surface mixed layer in the ocean general circulation model(OGCM) is put forward preliminarily in this paper. Besides turbulence, the impact of sub-mesoscale oceanic processes(including inertial internal wave breaking product) on oceanic interior mixing is emphasized. We suggest that adding the inertial internal wave breaking mixing scheme(F-scheme for short) put forward in this paper to the turbulence mixing scheme of Canuto et al.( T-scheme for short) in the OGCM, except the region from 15°S to 15°N. The numerical results of F-scheme by using WOA09 data and an OGCM(LICOM, LASG/IAP climate system ocean model) over the global ocean are given. A notable improvement in the simulation of salinity and temperature over the global ocean is attained by using T-scheme adding F-scheme, especially in the mid- and high-latitude regions in the simulation of the intermediate water and deep water. We conjecture that the inertial internal wave breaking mixing and inertial forcing of wind might be one of important mechanisms maintaining the ventilation process. The modeling strength of the Atlantic meridional overturning circulation(AMOC) by using T-scheme adding F-scheme may be more reasonable than that by using T-scheme alone, though the physical processes need to be further studied, and the overflow parameterization needs to be incorporated. A shortcoming in F-scheme is that in this paper the error of simulated salinity and temperature by using T-scheme adding F-scheme is larger than that by using T-scheme alone in the subsurface layer.  相似文献