METHOD FOR 3D SOIL HORIZONATION USING DIGITAL IMAGES

D. A. Zhulidova, Z. S. Artem’eva, D. M. Homiakov
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Abstract

We created a three-dimensional (3D) model of the spatial arrangement of soil horizons with broken boundaries using digital images. T is technique was tested on a Retisol - an Alf sol with a glossic horizon. Photographs were taken for 11 vertical sections (2.5 cm distance between sections) of the soil prof le for an area of 30 × 45 cm. Colorimetric accuracy of the images was tested against measurements of moist soil samples made with a portable spectrophotometer. T e selected best images were calibrated using an internal color calibration method for color correction. T e images were combined into a common array to build a 3D optical soil horizon map using the CIELAB color space. A protocol for processing the 3D soil images was created that showed 3D soil structure. It was found that the CIELAB color coordinates can be used to distinguish and delineate AE, E, and EB horizons. We then tested the method to assess soil carbon stocks and found that the stocks using the 3D model were 28% higher than when calculated using the 2D model. We conclude that the optical 3D mapping method can accurately represent the 3D structure and can be used to quantify soil horizon variations.
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利用数字图像进行三维土壤层划分的方法
我们利用数字图像创建了一个边界破碎的土壤层空间排列三维(3D)模型。这项技术在 Retisol(一种具有光泽地层的土壤)上进行了测试。在 30 × 45 厘米的区域内,对土壤剖面的 11 个垂直剖面(剖面间距为 2.5 厘米)进行了拍照。根据便携式分光光度计对潮湿土壤样本的测量结果,对图像的色度准确性进行了测试。选定的最佳图像采用内部色彩校准法进行色彩校正。将这些图像组合成一个共同阵列,使用 CIELAB 色彩空间构建三维光学土壤层图。创建的三维土壤图像处理协议可显示三维土壤结构。结果发现,CIELAB 色彩坐标可用于区分和划分 AE、E 和 EB 地层。然后,我们测试了评估土壤碳储量的方法,发现使用三维模型计算的碳储量比使用二维模型计算的碳储量高出 28%。我们的结论是,光学三维绘图法可以准确地表示三维结构,并可用于量化土壤层的变化。
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