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1.It shows there is a esti-mation O(h+(Δh)~(1/2)) for energy and L_2 models if Mh is bounded (M—the number of vary net-work,h—the maximun boundary length of the finited element;Δt—sfep length of the time).
它表明,当 Mh 有界时,能量模与 L_2模有估计 O(h+(△t)~(1/2)(M 表示变网格的次数;h 表示有限元的最大边长;△t 表示时间步长).收藏指正
2.The net collocation point method with spline function is proposed to derive the formulation system of stochastic buckling analysis for cylinderic shells under various boundary conditions.
提出了样条函数的网状配点法,推导了不同边界条件下圆柱壳屈曲的随机分析公式系统。收藏指正
3.Designning well tube and drill-hole diameter in order to increase thickness of both annular packing gravel and water-resisting clay, nylon net packing around well tube filters, designing filter layer on the boundary between packing gravel and water-resisting clay and ramming the gravel by working the piston into the well after gravel packing completion and the filling clay for salt-water resisting etc. we succeeded in constructing 3 drinking-water wells in Minqin County, proved the affectivity and feasibility of using it and giving a certain technical demonstration of construction of drinking-water well in the same similar to this area.
通过孔径与管径的调配设计,增大环状粒料层和止水粘土层的厚度;滤水管外包尼龙纱网;粒料与止水粘土接触界面上设计反滤层;填粒后先行拉活塞利用水力夯实粒料层,再投粘土球止掉上部咸水等措施,在民勤县三口人饮水井施工中取得显著效果,证明了该套成井工艺的有效性和可行性,有望为同类地区人饮水井施工提供技术示范作用。收藏指正
4.The introduction of the zonal net volume transport is based on the observed fact that the Brazil Warm Current flows in and the Peru Cold Current flows out through the north boundary ,and there is an eastward water transport of more than 100 Sv (about 134 Sv on an ave-rage) through the Drake Passage.
基于巴西暖流穿过北边界流入和秘鲁寒流穿过北边界流出,以及常年有大于100Sv(平均约134Sv)的水体自西向东穿过Drake海峡的观测事实,引入了净通量条件。收藏指正
5.The results show that a warm high ridge at the middle level and transformed surface cold high over the plain provide a good background condition; a cooling process produced by net surface radiation fluxes is the trigger and strengthening mechanism for the fog event; the subsidence flow at the middle and low tropospheric levels is favorable for the setting-up and maintenance of stable stratification at the boundary layer and weak wind condition at the ground layer over the fog region; the transportation of weak warm advection at lower levels and weak lift motion at the boundary layer play a very important role to the long maintenance of the fog event; the intrusion of north wind accompanied by cold advection is a main dynamic factor of the fog dissipation.
结果表明:在中高层暖性高压脊及地面变性冷高压稳定维持的大尺度背景条件下,地表净辐射引起的近地层冷却是大雾过程的触发和加强机制;中低空下沉气流的存在有助于近地层的弱风条件和稳定层结的建立;低层暖平流的输入和边界层的浅层抬升是大雾长时间持续的原因;伴随冷空气南下的偏北大风是驱使大雾消散的动力因子。收藏指正
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