Improving the accuracy of GRACE Earth's gravitational field using the combination of different inclinations

In this paper,the GRACE Earth's gravitational field complete up to degree and order 120 is recovered based on the combination of different inclinations using the energy conservation principle.The results show that because different inclinations of satellite are sensitive to the geopotential coefficients with different degrees/and orders m.the design of GRACE exploiting 89° inclination can effectively improve the accuracy of geopotential zonal harmonic coefficients.However,it is less sensitive to the geopotential tesseral harmonic coefficients.Accordingly.the second group of GRACE exploiting lower inclination is required to determine high-accurately the geopotential tesseral harmonic coefficients and cover the shortage of the single group of GRACE exploiting 89° inclination.Two groups of GRACE individually exploiting 89° (82°-84°)inclinations are the optimal combination of the Earth'S gravitational field recovery complete up to degree and order 120.In the degree 120,the joint accuracy of cumulative geoid height based on two groups of GRACE individually exploiting 89° and 83° inclinations is averagely two times higher than the accuracy of a group of GRACE exploiting 89° inclination.     

Improving the accuracy of GRACE Earth’s gravitational field using the combination of different inclinations

In this paper, the GRACE Earth＇s gravitational field complete up to degree and order 120 is recovered based on the combination of different inclinations using the energy conservation principle. The results show that because different inclinations of satellite are sensitive to the geopotential coefficients with different degrees l and orders m, the design of GRACE exploiting 89° inclination can effectively improve the accuracy of geopotential zonal harmonic coefficients. However, it is less sensitive to the geopotential tesseral harmonic coef- ficients. Accordingly, the second group of GRACE exploiting lower inclination is required to determine high-accurately the geopotential tesseral harmonic coefficients and cover the shortage of the single group of GRACE exploiting 89° inclination. Two groups of GRACE individually exploiting 89° ＋ （82°-84°） inclinations are the optimal combination of the Earth＇s gravitational field recovery complete up to degree and order 120. In the degree 120, the joint accuracy of cumulative geoid height based on two groups of GRACE individually exoloiting 89° and 83° inclinations is averagely two times higher than the accuracy of a group of GRACE exploiting 89~ inclination.     

有挠引力场之能动张量密度及自旋密度的再研究

在有挠情况下对引力场的能动张量密度及自旋密度进行了再研究，肯定了定义Ｔ（Ｇ）μｉｄｅｆδＬＧ／δｈｉμ及Ｃ（Ｇ）μｉｊｄｅｆ－２δＬＧ／δΓｉｊμ的合理性，导出了引力波虽存在但不携带能量、动量及自旋的结论．     

拱坝-地基系统的三维有限元并行计算

拱坝稳定和破坏过程的三维有限元分析,对高性能并行计算提出了很高的要求.采用节点联系矩阵的概念,基于Jacobi预处理共轭梯度法,推导了适用于分布存储并行机的有限元并行element-by-element(EBE)方法,可以避免形成整体刚度矩阵,显著减少内存需求,并可自动实现计算任务的分配.编制了有限元并行计算程序,采用悬臂梁算例对其进行了验证,然后应用于二滩拱坝的有限元数值分析.计算结果表明,对拱坝-地基系统这样复杂的三维结构,有限元EBE方法是一种很有效的并行计算方法.     

近300年来的地磁场总能量在地球内部的分布及长期变化

 采用Bloxham J. &; Jackson A.模型(BJ)和国际地磁参考场模型(IGRF)从理论上计算并分析了1690年以来地磁场能量在地球内部的分布及长期变化.结果表明,BJ模型和IGRF模型在相同时段内的总能量变化趋势是基本吻合的.近300a来,地核以外和地表以外地磁场总能量变化的总趋势是持续衰减的,但是地表以外的能量衰减速度比地核以外要快约2.5倍.地磁场总能量随谐波阶数n的变化关系中,各年代n=1～8阶的能量变化相对稳定.磁能密度在地球内部的分布是不均匀的.     

等离子熔积成形混相瞬态场的Level-Set方法模拟

提出了一种二维等离子熔积成形瞬态模型,该模型描述了液／气界面的自由表面发展,并模拟了熔池内流体流动和传热．采用Level—Set方法处理液／气界面边界条件,考虑了熔体流动的主要驱动力——表面张力梯度、表面曲率、浮力以及工件表面的对流散热等因素．用固液相统一模型来描述固／液界面处的熔融和凝固过程,并开发了相应的软件．对高温合金K163在不同扫描速度下的熔积层表面形貌、温度场以及熔池内流场进行了模拟分析．     

长直椭柱导体表面静电场的数值计算

依据最低能量原理,将椭柱导体表面的电荷离散成有限电荷微元,通过电荷微元的坐标轮动,寻求体系的最低能量位形,得到了体系达到静电平衡时的电荷密度分布,进而依据高斯定理描述了导体表面的电场分布。     

区域流场对含水层采能区地温场的影响

建立三维水热耦合数值模拟模型,对不同地下水天然流动情况下,含水层采能过程中及采能后地温场的演化进行了模拟和分析。结果表明,对于地下水流动较为显著的地区,地温场的变化幅度不仅受地下水天然流速的影响,还与井位布局方向密切相关。区域地下水的天然流速越大,系统停运期抽水井的温度恢复速度越快;对于相同地下水天然流速,地下水流向沿抽水井指向回灌井比垂直于抽灌井对之间连线方向的情况,抽水井温度变化幅度要小。