Complexity Analysis of Peat Soil Density Distribution

6th Asian Physics Symposium

Sampurno, Joko^1 ; Faryuni, Irfana Diah^1 ; Latief, Fourier Dzar Eljabbar^2 ; Srigutomo, Wahyu^2

Department of Physics, Faculty of Mathematics and Natural Sciences, Tanjungpura University, Indonesia^1

Department of Physics, Faculty of Mathematics and Natural Sciences, Institut Teknologi Bandung, Jalan Ganesa 10, Bandung

40132, Indonesia^2

关键词: Complexity analysis;    Fourier analysis methods;    Fractal analysis;    High resolution image;    Micro-computerized tomography;    Pixel resolution;    Point of intersections;    Regression lines;   

Others  :  https://iopscience.iop.org/article/10.1088/1742-6596/739/1/012071/pdf
DOI  :  10.1088/1742-6596/739/1/012071

来源: IOP

【 摘 要 】

The distributions of peat soil density have been identified using fractal analysis method. The study was conducted on 5 peat soil samples taken from a ground field in Pontianak, West Kalimantan, at the coordinates (0 ° 4 '2:27 "S, 109 ° 18' 48.59" E). In this study, we used micro computerized tomography (pCT Scanner) at 9.41 micro meter per pixel resolution under peat soil samples to provide 2-D high-resolution images L1-L5 (200 200 pixels) that were used to detect the distribution of peat soil density. The method for determining the fractal dimension and intercept was the 2-D Fourier analysis method. The method was used to obtain the log log-plot of magnitude with frequency. Fractal dimension was obtained from the straight regression line that interpolated the points in the interval with the largest coefficient determination. Intercept defined by the point of intersection on the -axis. The conclusion was that the distributions of peat soil density showing the fractal behaviour with the heterogeneity of the samples from the highest to the lowest were L5, L1, L4, L3 and L2. Meanwhile, the range of density values of the samples from the highest to the lowest was L3, L2, L4, L5 and L1. The study also concluded that the behaviour of the distribution of peat soil density was a weakly anisotropic.