基于亮度值的土壤薄剖面有机质分解程度分类判别函数

IF 2 Q3 SOIL SCIENCE
Tania González-Vargas, M. C. Gutiérrez-Castorena
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引用次数: 2

摘要

有机质的分解是一个基本的成土过程,因为它影响碳循环和向土壤释放养分。然而,针对微尺度原位分析的定量研究很少,尽管它与分解过程相关。因此,本研究的目的是基于与各形态阶段相关的亮度值,生成有机质分解程度的判别函数,并由此生成专题图。选取森林土壤和堆肥土壤的土壤薄片,在平面偏振光(PPL)、交叉偏振光(XPL)、交叉偏振光和插入延迟板(石膏补偿器)(XPLλ) 3种光源下拍摄岩石显微镜图像。随后,将RGB(红、绿、蓝)图像分解为三个波段,得到每个图像的九个波段。每个波段产生2000个采样点,得到每个有机物分解阶段的亮度值。除孔隙度(P)外,根据分解程度将点分为无(A)、轻(B)、中等(C)、强(D) 4类,并进行线性判别分析,得到各分解程度的分类模型。结果表明,通过特定的光源和一组波段可以突出显示有机质的各个分解程度,所有类别的总体精度为>94%,kappa系数为>0.75。此外,所得到的函数在训练图像和高分辨率马赛克中进行验证,以创建最终的主题地图。线性模型的使用在微观层面上自动化了专题地图的制作和质量,这对监测有机物质分解过程很有用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Brightness Values-Based Discriminant Functions for Classification of Degrees of Organic Matter Decomposition in Soil Thin Sections
The decomposition of organic matter represents a fundamental pedogenetic process, since it impacts the carbon cycle and the release of nutrients to the soil. However, quantitative research aimed at micro-scale in situ analysis is scarce, despite its relevance in the decomposition process. Therefore, the objectives of this research were to generate discriminating functions of the degrees of organic matter decomposition, based on the brightness values associated with each morphological stage, and from this step, to generate thematic maps. Soil thin sections of forest and compost soils were selected, and petrographic microscope images with three light sources were taken: plane polarized light (PPL), crossed-polarized light (XPL), and crossed polarizers and a retardation plate (gypsum compensator) inserted (XPLλ). Subsequently, the RGB (red, green, blue) image was broken down into three bands, resulting in nine bands for each image. Two thousand sampling points were generated for each band, obtaining brightness values for each decomposed organic matter stage. The points were classified into four categories based on their degree of decomposition: no (A), light (B), moderate (C), and strong (D), in addition to porosity (P). Linear discriminant analysis was performed to obtain classification models for each level of decomposition. The results show that each degree of organic matter decomposition can be highlighted through specific light sources and a set of bands, with an overall accuracy of >94% and kappa coefficients of >0.75 for all classes. In addition, the resulting functions were validated in training images and high-resolution mosaics to create final thematic maps. The use of linear models automated the production and quality of thematic maps at the microscopic level, which can be useful in monitoring the organic matter decomposition process.
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来源期刊
CiteScore
2.20
自引率
0.00%
发文量
13
期刊介绍: The Spanish Journal of Soil Science (SJSS) is a peer-reviewed journal with open access for the publication of Soil Science research, which is published every four months. This publication welcomes works from all parts of the world and different geographic areas. It aims to publish original, innovative, and high-quality scientific papers related to field and laboratory research on all basic and applied aspects of Soil Science. The journal is also interested in interdisciplinary studies linked to soil research, short communications presenting new findings and applications, and invited state of art reviews. The journal focuses on all the different areas of Soil Science represented by the Spanish Society of Soil Science: soil genesis, morphology and micromorphology, physics, chemistry, biology, mineralogy, biochemistry and its functions, classification, survey, and soil information systems; soil fertility and plant nutrition, hydrology and geomorphology; soil evaluation and land use planning; soil protection and conservation; soil degradation and remediation; soil quality; soil-plant relationships; soils and land use change; sustainability of ecosystems; soils and environmental quality; methods of soil analysis; pedometrics; new techniques and soil education. Other fields with growing interest include: digital soil mapping, soil nanotechnology, the modelling of biological and biochemical processes, mechanisms and processes responsible for the mobilization and immobilization of nutrients, organic matter stabilization, biogeochemical nutrient cycles, the influence of climatic change on soil processes and soil-plant relationships, carbon sequestration, and the role of soils in climatic change and ecological and environmental processes.
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