在 UPI 校园区域使用简易摆测定地球重力加速度

Khairul Sabri, Nanda Aisyah Kurniati, Dzulfikar Nasriyan Fadhilah, Dearil Ardiansyah, U. Pendidikan, Indonesia
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引用次数: 0

摘要

很多人认为重力加速度的值总是固定不变的。然而,如果我们仔细观察,每个地方的重力加速度值总是在变化的。这项研究旨在比较地球重力加速度在不同地点的差异。通过这项研究,研究人员可以找出重力差异的原因,其中之一就是高度差异。本研究采用的方法是简单的摆锤实验法,用定量的方法收集各地的数据。结果显示,日本国际协力机构大楼 5 层的 g 值为 9.47 m/s²,FIP 大楼 10 层的 g 值为 9.72 m/s²,FPTK 的 g 值为 9.59 m/s²,而国家教育博物馆的 g 值为 9.72 m/s²。除此之外,还可以发现这四个地方的重力加速度平均值为 9.62 m/s²。从这些结果可以得出结论,地球重力加速度的大小在每个地方都是不同的。除了高度之外,这种差异也可能是由于重力测量的不确定性造成的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Penentuan Percepatan Gravitasi Bumi Menggunakan Bandul Sederhana Di Daerah Kampus UPI
Many people assume that the value of gravitational acceleration always has a fixed value. However, if we look closely, the value of gravitational acceleration always changes in each place. This research aims to compare differences in Earth's gravitational acceleration in various locations. Through this research, researchers can identify the causes of differences in gravity, one of which is differences in height. The method used in this research is a simple pendulum experimental method, with a quantitative approach to collecting data from various places. The results obtained for g in the JICA building on the 5th floor were 9,47 m/s², g in the FIP building on the 10th floor was 9,72 m/s², g in the FPTK 9,59 m/s², and g at the National Museum of Education is 9,72 m/s². Apart from that, it can be found the average magnitude of the gravitational acceleration from these four places is 9,62 m/s². From these results it can be concluded that the magnitude of the Earth’s gravitational acceleration is different in each place. Apart from height, this difference can also occur due to uncertainty in measuring gravity.
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