测量超声波波的坡度,以确定地面的渐变成分

Dudi Darmawan, Suprayogi Suprayogi, Nur Indah Muzayyanah
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引用次数: 0

摘要

关于土壤类型和厚度的信息在规划用于各种目的的土地利用(包括农业和基础设施)方面变得非常重要。测量,以确定这一信息已发展使用各种方法,其中之一是超声波法。而对土层厚度的测量是通过知道土层中波的传播速度来实现的。通常,在各种测量中,假设超声波传播速度恒定。然而,在各种情况下,各层混合形成一个级配层,有必要首先表征土壤。本研究的目的是通过测量超声波在一定厚度下的速度来表征分级土层。改变了渐变层的组成,并测量了传播速度。结果表明:级配层土的组成对超声波传播速度的影响是线性的;对lembang土、红土和腐殖质组成的变化进行了试验,其平均决定系数为0.978,呈线性关系;对级配层土壤组成对波传播速度的影响进行了试验,平均误差为1.32%。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Pengukuran Kecepatan Rambat Gelombang Ultrasonik untuk Menentukan Komposisi Tanah pada Lapisan Gradasi
Information on soil type and thickness becomes important in planning land use for various purposes, both agriculture and infrastructure. Measurements to identify this information have been developed using various methods, one of which is the ultrasonic wave method. However, the measurement of the thickness of the soil layer is carried out by knowing the speed of wave propagation in the layer. Generally, in various measurements, the assumption of a constant ultrasonic wave propagation speed is used. However, in various situations where the layers have mixed to form a gradation layer, it is necessary to characterize the soil first. This study aims to characterize the graded soil layer by measuring the speed of ultrasonic waves at conditioned thickness. The composition of the gradation layer was varied and the speed of propagation was measured. The results show that the composition of the soil in the gradation layer affects the ultrasonic wave propagation speed quite linearly. Experiments carried out on variations in the composition of lembang soil, laterite and humus showed a linear relationship with an average coefficient of determination of 0.978 and the results of testing the function of soil composition in the gradation layer to the speed of wave propagation resulted in an average error of 1.32%.
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