核子物理主题探索STEM教学辅助工具PPM设计

Waziruddin, I. Irwandi, Y. Away
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引用次数: 0

摘要

具有精确测量的核物理实验是令人兴奋的事情。该实验支持基于真实实验的STEM方法,特别是如果它是低成本的设备。本研究对质子进动磁强计(PPM)的设计进行了初步研究,该设计将作为STEM学习的教具来探索原子核,并作为磁强计来精确测定地球磁场的强度。PPM信号易受外部磁场变化的影响,使建筑物内的电流、铁磁性材料等外部磁干扰产生噪声。所以测量是在大楼外进行的。该传感器使用两个相互极化的线圈来消除来自外部的噪声。此外,还在带通滤波器中设计了模拟滤波,仅使其通过所需的频率范围。由于PPM信号很小,线圈与合适的电容器耦合,通过电感-电容器谐振效应在期望的目标频率上放大质子辐射的信号。信号PPM在时域内的测量结果虽然可以直观地显示出来,但由于沉浸在噪声中,难以识别。然而,当用人耳听到时,在对线圈施加极化电流后,PPM信号的独特声音将清晰约3秒。使用audacity 3.0.2软件可以将时域的波转换为频域。得到的峰值频率为1914 Hz。根据这些频率的值,根据拉莫尔公式,得到地球磁场的值为44.97 uT。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Design PPM Instrument for STEM Teaching Aid in Exploring Nuclear Physics Topic
Experiments on nuclear physics with precise measurements are exciting things to do. The experiment supports the STEM approach based on real experiments and especially if it is low-cost equipment. In this study, a preliminary study was conducted on the proton precession magnetometer (PPM) design, which will be used as a teaching aid for STEM learning to explore the atomic nucleus and as a magnetometer to determine the strength of the earth's magnetic field accurately. The PPM signal is susceptible to changes in the external magnetic field so that external magnetic disturbances such as electric currents and ferromagnetic materials in the building produce noise. So the measurements are carried out outside the building. The sensor uses two coils that are polarized opposite each other to eliminate the noise from the outside. In addition, analog filtering is also designed in a bandpass filter only to pass the desired frequency range. Since the PPM signal is tiny, the coil is coupled with a suitable capacitor to amplify the signal radiated by the protons through an inductor-capacitor resonance effect at the desired target frequency. Signal PPM measurement results in the time domain can be displayed, although visually, it is difficult to recognize because it is immersed in noise. However, when heard with the human ear, the distinctive sound of the PPM signal will be clear for about 3 seconds after applying polarizing current to the coil. Waves in the time domain can be converted into the frequency domain using audacity 3.0.2 software. The peak frequency obtained is 1914 Hz. Based on the values of these frequencies, based on the Larmor formula, the value of the earth's magnetic field obtained is 44.97 uT.
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