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首页> 外文期刊>Ecological engineering: The Journal of Ecotechnology >Using computed tomography (CT) images and multi-fractal theory to quantify the pore distribution of reconstructed soils during ecological restoration in opencast coal-mine
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Using computed tomography (CT) images and multi-fractal theory to quantify the pore distribution of reconstructed soils during ecological restoration in opencast coal-mine

机译:使用计算机断层扫描(CT)图像和多重分形理论对露天煤矿生态恢复过程中重建土壤的孔隙分布进行量化

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摘要

Opencast coal mining is an anthropogenic activity that changes the antecedent soil profile, including its physical, chemical and biological properties. The compaction resulting from large machinery can have a substantial effect on the reconstructed soil pore structure in opencast coal-mine dumps, thus it was important to reconstruct a suitable soil pore structure for vegetation growth during land reclamation endeavours. To better quantify the characterization of reconstructed soils in opencast coal-mine dumps, high-resolution and lossless computed tomography (CT) images were used to study the effect of dumping and land reclamation on the soil pore structure by scanning soils from the Antaibao Opencast Coal-mine in the Pingshuo mining area. The soils were taken from an undisturbed area and the dump platform using a loess parent material covering with different reclamation time. Photoshop and ArcGIS software were used to process the scanned images and conduct statistical analysis, and multi-fractal theory was used to analyse the distribution characteristics of soil pores. The multi-fractal method can quantify the distribution characterization of the reconstructed soils based on CT images, and multi-fractal parameters, e.g., D(0), D(1), D(0)-D(1), Delta alpha and Delta f, can reflect the heterogeneity of different aspects of the soil pore distribution. Mining and dumping activities significantly affected the pore distribution of reconstructed soils; however land reclamation can be used to develop the soil pore distribution of reconstructed soils. (C) 2016 Elsevier B.V. All rights reserved.
机译:露天煤矿开采是一种人为活动,它改变了以前的土壤剖面,包括其物理,化学和生物学特性。大型机械产生的压实作用可能对露天煤矿场的重建土壤孔隙结构产生重大影响,因此,在开垦土地期间重建适合植被生长的土壤孔隙结构非常重要。为了更好地量化露天煤矿场中重建土壤的特征,使用高分辨率无损计算机断层扫描(CT)图像通过扫描安泰堡露天煤矿的土壤来研究倾倒和开垦对土壤孔隙结构的影响。在平朔矿区开采。使用覆盖时间不同的黄土母料从未受干扰的区域和垃圾堆放平台中取土。用Photoshop和ArcGIS软件处理扫描图像并进行统计分析,采用多分形理论分析土壤孔隙的分布特征。多重分形方法可以基于CT图像和多重分形参数(例如D(0),D(1),D(0)-D(1),Delta alpha和D)对量化的土壤分布特征进行量化。 Δf可以反映土壤孔隙分布不同方面的异质性。采矿和倾倒活动显着影响了重建土壤的孔隙分布。然而,开垦土地可用于发展重建土壤的土壤孔隙分布。 (C)2016 Elsevier B.V.保留所有权利。

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