The full magnetic gradient tensor （MGT） refers to the spatial change rate of the three field components of the geomagnetic field vector along three mutually orthogonal axes. The tensor is of use to geological mapping, resources exploration, magnetic navigation, and others. However, it is very difficult to measure the full magnetic tensor gradient using existing engineering technology. We present a method to use triaxial aeromagnetic gradient measurements for deriving the full MGT. The method uses the triaxial gradient data and makes full use of the variation of the magnetic anomaly modulus in three dimensions to obtain a self-consistent magnetic tensor gradient. Numerical simulations show that the full MGT data obtained with the proposed method are of high precision and satisfy the requirements of data processing. We selected triaxial aeromagnetic gradient data from the Hebei Province for calculating the full MGT. Data processing shows that using triaxial tensor gradient data allows to take advantage of the spatial rate of change of the total field in three dimensions and suppresses part of the independent noise in the aeromagnetic gradient. The calculated tensor components have improved resolution, and the transformed full tensor gradient satisfies the requirement of geological mapping and interpretation.
对实时嵌入式操作系统μC/OS-Ⅱ在TI公司的TMS320VC33芯片上的移植和应用做了具体的讨论和研究。在数字信号处理器(Digital Signal Processor,DSP)芯片上移植实时操作系统,更加充分地发挥DSP的强大数字信号处理功能,并进一步降低DSP软件开发难度,提高了软件的可靠性。介绍实时嵌入式操作系统μC/OS-Ⅱ,分析他在TMS320VC33上移植的具体步骤,详细讨论了任务的划分、管理和同步,对DSP的操作系统移植有实际的指导作用和参考价值。
