Vertical dynamic response of a disk on a saturated poroelastic half-space

This paper considers the vertical dynamic response of a disk on a saturated poroelastic half-space. Firstly the pressure-solid displacement form of the harmonic equations of motion for a poroelastic solid are developed from the form of the equations originally presented by Biot. These equations are solved by a new method. Then the mixed boundary value problem for the vertical harmonic vibration of a disk on a poroelastic half-space is studied. The two types of drainage conditions at the surface of the poroelastic half-space are considered: (a) the surface of the poroelastic half-space is assumed to be completely pervious both within and exterior to the plate; (b) The interface between the plate and the poroelastic half-space is assumed to be impervious and the exterior region is assumed to be pervious. By using the Hankel transform techniques, the paper develops the governing dual integral equations. These governing integral equations are further reduced to systems of standard Fredholm integral equations of the second kind by Abel transform.     

基于用岛类型和方式的舟山市无居民海岛分类保护应用研究

无居民海岛是舟山市经济、社会和生态发展的重要资源支撑。为促进舟山市无居民海岛的精细化管理和可持续发展,文章分析舟山市无居民海岛开发利用和保护存在的问题,提出无居民海岛分类保护原则,基于国家权益类、自然保护区类、海洋特别保护区类、其他重要保护类、限制开发类和保留类的单岛功能定位分别制定管理方案,基于旅游娱乐用岛等9种用岛...     

太行山地形对“96.8”暴雨影响的数值试验研究

利用ＭＭ４模型,设计了４种模式地形方案,讨论了太行山地形对“９６．８”暴雨降水量的贡献;并利用垂直运动和水汽通量等物理量,探讨了太行山地形对本次暴雨过程增幅作用的机制。结果显示,太行山地形对本次暴雨过程的降水中心强度及位置有显著影响,具有６０％增幅作用。太行山地形对垂直运动及水汽辐合也都具有增幅作用。模式地形越真实,预报结果越好,地形越高,降水增幅作用越明显。     

Geochemical characteristics of trace elements and tectonic setting of sandstones from the Upper Ordovician Pingliang Formation,southwestern margin of Ordos Basin: A case study of the Duanjiaxia profile,Longxian County

Due to the lack of reliable sedimentary provenance data,the geological setting and its provenance of the southwestern margin of Ordos Basin in Late Ordovician is uncertain. In this paper,the sandstone of Upper Ordovician Pingliang Formation in Duanjiaxia profile of Longxian area is selected for a systematic study. Using the methods including the comprehensive analysis on the measured geological profile,analysis of microscopic thin section and trace elements,the following results are obtained: (1)the thin section analysis shows that the sandstone is well sorted but poorly rounded. Clastic grains are dominated by quartz,while the rock fragments are mainly composed of polycrystalline quartz,carbonate sand debris,and a little matrix,which means that the turbidite sandstone has been reworked by obvious traction of deep-water;(2)Rare Earth Element(REE)distribution model shows that the sandstone is rich in LREE and is short of HREE and has the negative Eu-anomaly,indicating that the provenance may derive from the intermediate and acid rock in the upper crust;(3)the provenance discrimination diagrams show that the sandstone of the Pingliang Formation is a mixture of sedimentary rock and granite,while the magmatic component is dominated by intermediate and acid rock;(4)Geochemical data of the sandstone suggests that the geological setting significantly belong to continental island arc and passive continental settings. The study area in Longxian during the Late Ordovician period was located in the back arc basin. At that time,the southwestern margin of the North China Craton with the full trench-arc-basin system was changed from the passive continental margin into the active continental margin.     

苍山5.2Ms级地震前后地震前兆综合危险度的变化

地震前兆综合危险度是以系统论为基础的一种综合地震预报的新方法。利用山东省每年年底的地震会商报告给出的地震前兆异常,而不是取震后的震例总结或论文给出的异常,通过“专家系统”的思想,对每一异常事件进行综合评估,计算出无量纲的、归一化的地震前兆综合危险度,分析了１９９５年９月２０日山东苍山５２Ｍｓ级地震前综合危险度的变化特征。震前综合危险度出现了一次明显的高值异常变化,震后危险度很快下降恢复到正常水平。     

A PRELIMINARY EXPERIMENTAL STUDY ON NON-LINEAR RELATIONSHIP BETWEEN SEDIMENT YIELD AND DRAINAGE NETWORK DEVELOPMENT

1INTRODUCTIONThedrainagenetWorkisoneofimportantcomponentsinafluvialsyStem.Atypicalfluvialsystemiscomposedofthreezones,asSchumm(1977)pointedout,therunoffandsedimentyield,transportationandsettlingzones.Asearlyasinthemiddleofthiscent'Ury,Horton(1945)madeasignificantquantitativeexplanationtohydro-geomorphologyinadrainagenetworksystem,andderivednetworkstatisticslaws.Inthe1970'sSmart(1973)hadtopologicallystudiednetWorkstrUcture.Fromthe1980'sandonst'Udiesoffractalandfractionaldimensioninadra…     

大连地区地震活动性分析及地震概率背景估计

根据统计计算大连地区１９９１年１１月至 １９９９年１月发生的２９９个ＭL≥２．０地震,得出目前该地区的地震活动规律,并对这期间的地震变化趋势进行了理论分析和概率背景估计,认为其间所发生的地震属于１９９３年３月１８日的大连满家滩南海ＭＬ４．３地震序列,从理论值和实测值的结果判断,该地震序列发生 ＭＬ≥５．０的可能性不大, 但不能排除该地震序列仍然存在着发生４．０≤ＭＬ＜５．０地震的概率背景．目前的地震平静期属于该地震序列活动期的尾声和下一地震活动期能量积累的初级阶段．     

完全非线性孤立波的稳态解

报道了应用边界积分方法模拟完全非线性孤立波的传播,给急剧记解的波形,流束和数值计算结果。结果表明,本模型对计算孤立波的传播是有铲的。当ａ／ｈ〉０．３时,自由液面上的水平流速、底部流速和垂向平均流速之间的差别是明显的。三阶Ｂｏｕｓｓｉｎｅｓｑ方程的孤立波解比低阶方程的孤立波解更接近本文完全非线性的数值解。     

湖泊渔业可持续发展的生态学基础及一个范例

从渔业与环境兼顾的角度出发作者认为湖泊渔业可持续发展的生态学理论基础是渔业生态学和渔业湖沼学. 前者是一门较为成熟的学科研究渔业对象的种群生态学渔产潜力最佳放流密度和规格以及科学的捕捞策略等. 后者研究渔业对湖泊生态系统生物多样性和水质的影响并确定最佳的渔业规模和渔业方式但尚未提出令人满意的理论和完善的实验方法今后应予充分重视. 长江中下游草型湖泊因为其优良的水资源和丰富的生物资源而成为我国内陆水体发展优质高效渔业的重要基地. 以湖北一个浅水草型扁担塘渔业实践为例作者着重强调生态学管理的如下方面1) 沉水植被是草型湖泊优质高效渔业持续发展的基础必须在合理利用的同时加以保护优化甚至重建使生物量和覆盖率保持和达到一定水平. 2) 食物链网的基础环节是渔业对象生长和繁衍的物质基础, 必须进行培育保护以提高其生产力从而为提高渔业产量打下物质基础. 3) 合理放养与捕捞策略是湖泊渔业生态系统良性循环的可靠保证应使高价值的种群规模保持较大水平的输出.     

“23·7”河北太行山东麓罕见特大暴雨特征及成因

受台风杜苏芮北上减弱的低压影响,2023年7月29日至8月1日,京津冀地区遭受了历史罕见的特大暴雨,海河发生流域性特大洪水并造成人员伤亡和经济损失。利用高空观测、地面自动站、S波段多普勒天气雷达、风廓线雷达、ERA5再分析资料等,对此次天气过程进行了初步分析。结果表明:特大暴雨过程具有累计降水量大、持续时间长、地形作用明显等特征。台风杜苏芮、卡努提供了极为有利的水汽条件,华北北部形成的高压坝阻挡了台风环流北上,华北地区先后经历了阵性降水、台风倒槽降水和倒槽减弱阶段对流性降水三个阶段,降水落区的叠加效应是形成罕见特大暴雨的主要原因。台风倒槽阶段850 hPa切变线受太行山阻挡移动缓慢,降水持续时间长,初期大气处于近中性状态,雨强整体平稳,30日午后对流开始加强,河北中部降水区冷池出流的偏北风与偏东风形成地面辐合线,使得河北东南部高能区中触发的对流单体发展加强为MCS,移入保定后形成“列车效应”;太行山冷池出流的偏北风与地面东南风形成辐合线触发不稳定能量释放,是30日夜间河北西南部降水维持的原因。31日早晨超过20m·s^-1的东南风急流再次建立,造成北京南部超过110...