为了改善传统模基参数估计(model-based parameter estimation,MBPE)计算量大、参数难选择以及复杂环境电磁场重构困难的问题,提出将滑动窗口法与模基参数估计法相结合(model-based parameter estimation with the sliding window,SW-MB...为了改善传统模基参数估计(model-based parameter estimation,MBPE)计算量大、参数难选择以及复杂环境电磁场重构困难的问题,提出将滑动窗口法与模基参数估计法相结合(model-based parameter estimation with the sliding window,SW-MBPE)算法,通过少量采样数据即可重构二维空间的电磁场分布。将研究区域划分为不同的滑动窗,再通过模基参数估计(model-based parameter estimation,MBPE)算法在各个窗口内重构电磁场,既可大幅度减小计算量,又能灵活适应剧烈变化的电磁场;通过对相邻窗口重复计算区域的平均化处理,使滑动窗边缘得以平滑,以减轻分块效应。分析SW-MBPE算法的主要参数,得出1组适用于空间电磁场重构的模型参数。仿真结果表明,在均匀采样11%的情况下,SW-MBPE算法重构的FSIM值可达到0.8,可取得较好的重构效果。展开更多
Gravity and electromagnetism are two sides of the same coin, which is the clue of this unification. Gravity and electromagnetism are represented by two mathematical structures, symmetric and antisymmetric respectively...Gravity and electromagnetism are two sides of the same coin, which is the clue of this unification. Gravity and electromagnetism are represented by two mathematical structures, symmetric and antisymmetric respectively. Einstein gravitational field equation is the symmetric mathematical structure. Electrodynamics Lagrangian is three parts, for electromagnetic field, Dirac field and interaction term. The definition of canonical energy momentum tensor was used for each term in Electrodynamics Lagrangian to construct the antisymmetric mathematical structure; symmetric and antisymmetric gravitational field equations are two sides of the same Lagrangian.展开更多
文摘Gravity and electromagnetism are two sides of the same coin, which is the clue of this unification. Gravity and electromagnetism are represented by two mathematical structures, symmetric and antisymmetric respectively. Einstein gravitational field equation is the symmetric mathematical structure. Electrodynamics Lagrangian is three parts, for electromagnetic field, Dirac field and interaction term. The definition of canonical energy momentum tensor was used for each term in Electrodynamics Lagrangian to construct the antisymmetric mathematical structure; symmetric and antisymmetric gravitational field equations are two sides of the same Lagrangian.
