非开挖施工建模的现状和前景

讨论了非开挖施工主要级别的建模：微隧顶管、HDD和夯管锤，并通过微隧顶管建模的过程说明定位于稳定性与鲁棒性理论、多体动力学理论的必然趋向，以及建模工作将会成为非开挖产业文化的一部分，将推动非开挖产业的发展，并由高端基础研发达到市场份额占有的目的。     

Ｊ酱吹奈侍?:企业融资困难、决策不科学、激励机制不完善以及发展规模受限制。在利益最大化的驱使

1. Introduction Two kinds of convective activities—dry convectioand moist convention—are often mentioned when referring to severe storm forecasting. Usually dry convection only serves as a kind of adjustment or a liftincondition for severe storms. Moi…     

稳健最优不变二次无偏估计

导出了稳健最优不变二次无偏估计、稳健最小范数二次无偏估计、稳健Ｈｅｌｍｅｒｔ估计，并说明了最优不变二次无偏估计、最小范数二次无偏估计以及Ｈｅｌｍｅｒｔ估计等均是稳健最优不变二次无偏估计的特例。     

不变量方法

不变量方法是一种数字技术,该方法对给定长度有限的时间序列,可以构造出一个常微分方程组。该方程组的解在有限时段上的采样值与给定序列重合。观测研究是对无法确定其方程的动力系统进行的研究;不变量方法提出了动力数值试验的可能性。     

The Genesis of Intermediate and Silicic Magmas in Deep Crustal Hot Zones

A model for the generation of intermediate and silicic igneousrocks is presented, based on experimental data and numericalmodelling. The model is directed at subduction-related magmatism,but has general applicability to magmas generated in other platetectonic settings, including continental rift zones. In themodel mantle-derived hydrous basalts emplaced as a successionof sills into the lower crust generate a deep crustal hot zone.Numerical modelling of the hot zone shows that melts are generatedfrom two distinct sources; partial crystallization of basaltsills to produce residual H₂O-rich melts; and partial meltingof pre-existing crustal rocks. Incubation times between theinjection of the first sill and generation of residual meltsfrom basalt crystallization are controlled by the initial geotherm,the magma input rate and the emplacement depth. After this incubationperiod, the melt fraction and composition of residual meltsare controlled by the temperature of the crust into which thebasalt is intruded. Heat and H₂O transfer from the crystallizingbasalt promote partial melting of the surrounding crust, whichcan include meta-sedimentary and meta-igneous basement rocksand earlier basalt intrusions. Mixing of residual and crustalpartial melts leads to diversity in isotope and trace elementchemistry. Hot zone melts are H₂O-rich. Consequently, they havelow viscosity and density, and can readily detach from theirsource and ascend rapidly. In the case of adiabatic ascent themagma attains a super-liquidus state, because of the relativeslopes of the adiabat and the liquidus. This leads to resorptionof any entrained crystals or country rock xenoliths. Crystallizationbegins only when the ascending magma intersects its H₂O-saturatedliquidus at shallow depths. Decompression and degassing arethe driving forces behind crystallization, which takes placeat shallow depth on timescales of decades or less. Degassingand crystallization at shallow depth lead to large increasesin viscosity and stalling of the magma to form volcano-feedingmagma chambers and shallow plutons. It is proposed that chemicaldiversity in arc magmas is largely acquired in the lower crust,whereas textural diversity is related to shallow-level crystallization. KEY WORDS: magma genesis; deep hot zone; residual melt; partial melt; adiabatic ascent     

大气辐射校正方法分析

阐述遥感影像的大气辐射校正的原因及目的,并以徐州地区的CBERS-02星影像数据为基础,应用软件MATLAB7.0,分析大气辐射校正的三种方法,即利用辐射传输方程求解的方法、基于地面场地数据或辅助数据进行辐射校正方法及利用波段特性进行大气辐射校正方法。其中,重点剖析利用波段特性进行大气辐射校正的方法。     

具有跳跃项的Duffing方程的拟周期解

本文研究了一类具有非对称项和有界扰动项的Duffing方程。当扰动项是拟周期函数时,利用典则变换和光滑拟周期扭转映射的不变曲线定理,证明了方程任意解的有界性和拟周期解的存在性。     

DMSP/OLS和VIIRS/DNB夜间灯光影像的校正及拟合

运用不变目标法对DMSP/OLS影像数据进行了相互校正、连续性校正和过饱和校正,以校正后的DMSP/OLS数据为参考对VⅡRS/DNB数据进行了重分类,利用两者影像数据在时间与空间中的重叠区域拟合VⅡRS/DNB数据,并对结果进行了评价,目的是获得长时间序列连续稳定的夜间灯光数据。同时建立了新疆区域校正后影像数据与社会经济指标中年末人口总数、生产总值、平均每天耗电量、建设用地之间的关系,探讨了夜间灯光数据在长时间序列下模拟社会经济参量的能力。结果表明,运用不变目标法校正后的夜间灯光影像更稳定、更连续,缩小了VⅡRS/DNB数据与DMSP/OLS数据像元DN值量级差异,使长时间序列下的灯光数据具有可比性。校正后长时间序列夜间灯光数据与社会经济参量的相关性高,说明校正后的长时间序列灯光影像数据在省级尺度上与社会经济指标契合。     

Rundle模式地震释放的能量及其标度关系

本文扼要介绍了有关Ｒｕｎｄｌｅ模式地震分叉结构及其爆发判据的主要研究结果。在此基础上推导出强地震过程释放的能量及其标度关系。本系列的研究工作,对地震预报研究有参考价值。