木卫二尾迹的数值模拟   总被引：1，自引：1，他引：0       下载免费PDF全文

卢斌  陈出新 《地球物理学报》2014,57(11):3851-3858

木卫二在木星磁层中运动,与快速共转的木星磁场相互作用形成木星极光中木卫二的尾迹,此尾迹反映了连续扰动的磁通量管对木星电离层电流注入的过程.本文应用细丝理论对此过程进行数值模拟,未扰动的上游磁通量管经过大约720 s的时间与木卫二作用形成角度约为4°且相对于木卫二静止的拉伸磁通量管,随后在磁张力的作用下加速运动.在随后大约2160 s的加速时间内,磁通量管的速度逐渐与背景磁力线接近,向木星电离层注入的电流也由9×10⁵A逐渐衰减至0.以1/e初始电流处认为是可观测的木卫二尾迹限度,则木卫二的尾迹仅大约有一至两个经度,这与哈勃望远镜观测到的木卫二尾迹大小大致相同.木卫二尾迹与木卫一尾迹相比,输送的能量约为2.3×10¹³J,仅有木卫一的1/10,导致尾迹长度远小于木卫一的尾迹长度.此外,模拟过程中发现木卫二下游的压力槽对磁通量管运动的影响很小,可以忽略.  相似文献   

沙漠地区风积沙地基输电线路装配式基础真型试验研究     

程永锋  丁士君 《岩土力学》2012,33(11):3230-3236

沙漠风积沙地基输电线路杆塔基础设计是当前我国电网建设中的关键研究课题之一。沙漠风积沙属于特殊土地基,这种地基上的输电线路装配式基础缺少相关设计依据。针对沙漠风积沙地基输电线路基础工程的特点,进行了输电线路装配式基础的真型试验,得到了上拔与水平荷载、下压与水平荷载联合作用下的承载变形特性、基础构件的应变特性、基础底板与风积沙地基之间的接触压力变化规律。根据测试结果,确定了沙漠地区风积沙地基装配式基础的地基承载力和上拔角取值,得到了基础稳定的最不利工况,有助于提高基础设计的可靠性和合理性。试验结果为沙漠地区台远-塔中220 kV输电线路基础工程的设计提供了依据。  相似文献   

�촬���ȿ���ϵͳ������վ������ȡ��λ��Ϣ��һ�ַ���   总被引：2，自引：0，他引：2  

潘国荣  张鹏  孔宁 《大地测量与地球动力学》2010,30(5):121-124

????????????У????????????乤??????????У??????????????λ??????????????????????????????????λ?????????????????????????ε??????λ??????????????????????Matlab GUI?????????????????????????ò??????????????????????????????????á?  相似文献   

组合梁-方钢管混凝土柱框架结构抗震性能的pushover分析   总被引：3，自引：0，他引：3  

刘晶波  郭冰  刘阳冰 《地震工程与工程振动》2008,28(5)

采用考虑组合梁多材料截面引起的正向、负向刚度、强度和承载力不同的截面本构模型,建立了组合梁结构的弹塑性分析模型,对一个15层的钢混凝土组合梁-方钢管混凝土柱框架结构开展了多遇地震、罕遇地震下的pushover分析,为组合框架结构体系的抗震性能分析以及pushover方法在该体系中的应用提供了参考。在此基础上,与钢梁-方钢管混凝土柱框架结构、钢梁-钢筋混凝土柱框架结构进行对比研究,比较了几种结构的动力特性,表明组合梁-方钢管混凝土柱框架结构体系相对于其它两种框架结构体系具有更好的抗震性能。  相似文献   

A fragmentation criterion for highly viscous bubbly magmas estimated from shock tube experiments     

Takehiro Koyaguchi  Bettina Scheu  Noriko K. Mitani  Oleg Melnik 《Journal of Volcanology and Geothermal Research》2008

When a highly viscous bubbly magma is sufficiently decompressed, layer-by-layer fracturing propagates through the magma at a certain speed (fragmentation speed). On the basis of a recent shock tube theory by Koyaguchi and Mitani [Koyaguchi, T., Mitani, N. K., 2005. A theoretical model for fragmentation of viscous bubbly magmas in shock tubes. Journal of Geophysical Research 110 (B10), B10202. doi:10.1029/2004JB003513.], gas overpressures at the fragmentation surface are estimated from experimental data on fragmentation speed in shock tube experiments for natural volcanic rocks with various porosities. The results show that gas overpressure at the fragmentation surface increases as initial sample pressure increases and sample porosity decreases. We propose a new fragmentation criterion to explain the relationship between the gas overpressure at the fragmentation surface, the initial pressure and the porosity. Our criterion is based on the idea that total fragmentation of highly viscous bubbly magmas occurs when the tensile stress at the midpoint between bubbles exceeds a critical value. We obtain satisfactory agreement between our simulation and experiment when we assume that the critical value is inversely proportional to the square root of bubble wall thickness. This fragmentation criterion suggests that long micro-cracks or equivalent flaws (e.g., irregular-shaped bubbles) that reach the midpoints between bubbles are a dominant factor to determine the bulk strength of the bubbly magma.  相似文献   

Phase relations of iron and iron–nickel alloys up to 300 GPa: Implications for composition and structure of the Earth's inner core     

Yasuhiro Kuwayama  Kei Hirose  Nagayoshi Sata  Yasuo Ohishi 《Earth and Planetary Science Letters》2008,273(3-4):379-385

We have investigated the phase relations of iron and iron–nickel alloys with 18 to 50 wt.% Ni up to over 300 GPa using a laser-heated diamond-anvil cell. The synchrotron X-ray diffraction measurements show the wide stability of hcp-iron up to 301 GPa and 2000 K and 319 GPa and 300 K without phase transition to dhcp, orthorhombic, or bcc phases. On the other hand, the incorporation of nickel has a remarkable effect on expanding the stability field of fcc phase. The geometry of the temperature–composition phase diagram of iron–nickel alloys suggests that the hcp–fcc–liquid triple point is located at 10 to 20 wt.% Ni at the pressure of the inner core boundary. The fcc phase could crystallize depending on the nickel and silicon contents in the Earth's core, both of which are fcc stabilizer.  相似文献   

0414号"云娜"台风路径分析   总被引：1，自引：0，他引：1  

周晓英  胡学军  胡得宝  沈全福  陈金龙 《海洋预报》2005,22(3):25-30

通过对0414号“云娜”台风的高空背景场及云图的分析,揭示影响台风移动路径的辛勿理因子。研究结果表明：副高、弱环境场中台风自身内力、台风的非对称结构是影响“云娜”台风移动的主要因素,西风槽对“云娜”台风的移动起着间接作用。  相似文献   

内蒙古东南部中生代构造应力场的多次转换及动力机制探讨   总被引：1，自引：0，他引：1  

方曙  鞠文信  张亚盾 《地质力学学报》2002,8(1):26-34

通过对内蒙古东南部中生代地质构造特征的综合研究,将该区域内中生代构造应力事件划分了8个阶段。构造应力场的压、张应力交替变化,此起彼伏,此消彼长,反映出地壳存在着弹性运动。地壳的发展历史就是在弹性运动过程中不断调整平衡,在调整平衡过程中形成了各种建造和构造。其动力主要来源于地球自转造成的地应力变化。   相似文献   

The inner inner core of the Earth: Texturing of iron crystals from three-dimensional seismic anisotropy   总被引：1，自引：0，他引：1  

Xinlei Sun  Xiaodong Song   《Earth and Planetary Science Letters》2008,269(1-2):56-65

We present a three-dimensional model of the seismic anisotropy and texturing of iron crystals in the inner core. The form of the anisotropy changes suddenly at slightly less than half of the inner core radius. The outer part is composed of iron crystals of a single phase with different degrees of preferred alignment along the spin axis of the Earth. The inner part may be composed of a different phase of crystalline iron or have a different pattern of alignment.  相似文献   

利用湖州台形变观测资料检测地震激发的地球球形自由振荡     

方燕勋  卞根发  惠若愚  孙宗强 《中国地震研究》2016,(4):584-593

By using the digital observations of the pendulum tiltmeter, water tube tiltmeter,extensometer and volumetric strainmeter at Huzhou station and with the power spectrum density estimation method,we acquired the_0S_5-_0S_50 fundamental sphere free oscillations caused by the Japan earthquake on March 11,2011,then compared it with the PREM model. The relative errors are mostly bigger than 1.2‰. The extensometer and volume strainmeter can clearly detect _0S_2,_0S_3and_0S_4,which are closely related to the deep structure and earth's interior.  相似文献