Radially accelerated optimal feedback orbits in central gravity field with linear drag

The solution of a feedback optimal control problem arising in orbital mechanics is addressed in this paper. The dynamics is that of a massless body moving in a central gravitational force field subject also to a drag and a radial modulated force. The drag is linearly proportional to the velocity and inversely proportional to the square of the distance from the center of attraction. The problem is tackled by exploiting the properties of a suitably devised linearizing map that transforms the nonlinear dynamics into an inhomogeneous linear system of differential equations supplemented by a quadratic objective function. The generating function method is then applied to this new system, and the solution is back transformed in the old variables. The proposed technique, in contrast to the classical optimal control problem, allows us to derive analytic closed-loop solutions without solving any two-point boundary value problem. Applications are discussed.     

Comparison between neuro-fuzzy and fractal models for permeability prediction

We have used different techniques for permeability prediction using porosity core data from one well at the Maracaibo Lake, Venezuela. One of these techniques is statistical and uses neuro-fuzzy concepts. Another has been developed by Pape et al. (Geophysics 64(5):1447–1460, 1999), based on fractal theory and the Kozeny–Carman equations. We have also calculated permeability values using the empirical model obtained in 1949 by Tixier and a simple linear regression between the logarithms of permeability and porosity. We have used 100% of the permeability–porosity data to obtain the predictor equations in each case. The best fit, in terms of the root mean-square error, was obtained with the statistical approach. The results obtained from the fractal model, the Tixier equation or the linear approach do not improve the neuro-fuzzy results. We have also randomly taken 25% of the porosity data to obtain the predictor equations. The increase of the input data density for the neuro-fuzzy approach improves the results, as is expected for a statistical analysis. On the contrary, for the physical model based on the fractal theory, the decrease in the data density could allow reaching the ideal theoretical Kozeny–Carman model, on which are based the fractal equations, and hence, the permeability prediction using these expressions is improved.     

网络RTK对流层拟合模型分析

为了拟合网络RTK中用户端双差对流层延迟,本文分析了基于距离的线性内插模型(DIM)、线性内插模型(LIM)原理,提出了指数拟合模型:以主参考站为原点,系数项与用户端和辅参考站间夹角成反比,指数底数值为0.35,用户端到主参考站与辅参考站到主参考站间距离比值被1减为指数。通过分析上述模型的误差系数给出了模型优缺点,试验验证了指数模型的有效性和稳定性:卫星拟合精度一般优于2cm,实现了单历元平面定位精度优于2cm,高程精度优于3cm。     

声波方程逆散射反演的近似方法

我们在文献[1]里研究了介质参考波速沿某个方向线性变化时的三维声散射理论,导出了声波方程逆散射反演问题解的解析表达式.考虑到应用时的实际条件,本文根据上述反演方法导出2.5维模型的声波方程逆散射反演的波速扰动计算公式,给出该方法在“高频”近似条件下的波速扰动反演计算公式,从而使我们提出的“参考波速线性变化时的声波方程逆散射反演”理论更接近实际应用条件.本文给出的这些反演公式仍然具有原方法的优点,即不但可以使Born近似的假定在大多数情况下能得以满足,而且可以利用快速Fourier变换来快速实现介质波速扰动的反演成象.     

非量测相机摄影测量的整体平差

论述了整体平差处理非量测相机摄影测量问题的计算模型，并对一些实例进行了解算。通过实例解算结果的分析比较，获得一些有益的结论。     

青海柴达木盆地大地热流测量与统计热流计算

１９９１年６-８月对青海柴达木盆地２１个石油勘探孔进行了钻孔温度测量,其中８个用于热流计算;从油田已有的测温资料中选取了１４个孔用作热流研究．为解决线性温度段与采样段的不匹配,对１７６块岩样的实测热导率与岩样的埋藏深度及地层年代之间的相关性进行了系统分析,求出热流计算段的加权平均热导率,共获得２２个热流值,其变化范围３２-７５ｍＷ／ｍ^２,平均约５３ｍＷ／ｍ^２．为阐明全盆地热流分布趋势,采用网格化方法计算统计热流．实测和统计热流一致表明,柴达木盆地热流值呈西高东低的分布特征．     

三角网格有限元法波动模拟的数值频散及稳定性研究

三角网格有限元法能够准确模拟复杂构造和复杂介质条件下的地震波场,数值频散和稳定性条件是地震波数值模拟中参数选择的主要依据.基于均匀的线性三角网格单元,根据结构刚度矩阵的组装原理以及平面波理论,推导了集中质量矩阵下两种网格结构的声波频散函数以及稳定性条件,并对数值频散特性以及稳定性进行了详细研究:三角网格单元中波动的数值频散除了受到空间采样间隔、单元网格纵横比和波传播方向等常规因素的影响外,还受到网格布局的影响,过锐或过钝的三角单元会对波动数值频散产生不良的影响,不同类型的单元网格、单元纵横比对应着不同的稳定性条件,正三角单元中的波动具有较好的数值频散特性,其数值各向异性(频散随波传播方向的变化)效应最弱,稳定性条件也较为宽松.最后通过数值模拟直观地验证了以上分析结果,为有限元正演三角网格的剖分和参数的设置提供一定的理论依据.     

Automated mapping of impervious surfaces in urban and suburban areas: Linear spectral unmixing of high spatial resolution imagery

Quantifying impervious surfaces in urban and suburban areas is a key step toward a sustainable urban planning and management strategy. With the availability of fine-scale remote sensing imagery, automated mapping of impervious surfaces has attracted growing attention. However, the vast majority of existing studies have selected pixel-based and object-based methods for impervious surface mapping, with few adopting sub-pixel analysis of high spatial resolution imagery. This research makes use of a vegetation-bright impervious-dark impervious linear spectral mixture model to characterize urban and suburban surface components. A WorldView-3 image acquired on May 9th, 2015 is analyzed for its potential in automated unmixing of meaningful surface materials for two urban subsets and one suburban subset in Toronto, ON, Canada. Given the wide distribution of shadows in urban areas, the linear spectral unmixing is implemented in non-shadowed and shadowed areas separately for the two urban subsets. The results indicate that the accuracy of impervious surface mapping in suburban areas reaches up to 86.99%, much higher than the accuracies in urban areas (80.03% and 79.67%). Despite its merits in mapping accuracy and automation, the application of our proposed vegetation-bright impervious-dark impervious model to map impervious surfaces is limited due to the absence of soil component. To further extend the operational transferability of our proposed method, especially for the areas where plenty of bare soils exist during urbanization or reclamation, it is still of great necessity to mask out bare soils by automated classification prior to the implementation of linear spectral unmixing.     

大地电磁资料精细处理和二维反演解释技术研究(五)--利用阻抗张量成像识别大地线性构造

大地线性构造往往与块体或物性的边界、断裂的几何延伸相关联,是地学研究的重要目标构造.在大地电磁法中,传统的方法是通过反演得到的电性结构的差异来解译线性构造,是一种间接分析方法.由于线性构造发育处走向和倾向明显,二维性较其他地方一般会更强,故而在阻抗张量成像分析中,相应的二维有效因子就会比较大,最佳主轴统计分布会更加明显.据此,本文利用大地电磁阻抗张量成像（包括最佳主轴统计成像、构造维性成像）来探测识别大地线性构造.本文首先通过三维理论模型的研究结果来验证这一技术在线性结构探测中的有效性,然后将其应用于郯庐断裂带南段实测剖面的具体分析中,展示了这一技术在线性构造探测中的实用性及其数据处理与分析过程.本文研究表明,大地电磁阻抗张量成像技术可独立于反演为地质解释尤其是线性构造的解释提供诸多参考信息.

     

Effect of vertical overturning circulation scale and moist static energy tendency on MJO phase speed

本文通过对1979-2019年ERA-I再分析资料进行诊断分析,研究了MJO垂直环流(VOC)纬向尺度和湿静力能(MSE)趋势纬向不对称性对MJO传播速度的综合影响.研究结果表明,MJO传播速度与VOC的纬向尺度和MSE趋势纬向梯度之间存在显著的正相关关系.基于上述两个参数,本文建立了线性回归模型,该模型可以较好的估计...