利用可见光-近红外光谱信息快速确定不同土壤系列的土壤层特征

IF 3.1 2区 农林科学 Q2 SOIL SCIENCE
Mehmet Ali Çullu , Hamdiye Şeker , Gafur Gozukara , Hikmet Günal , Ali Volkan Bilgili
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引用次数: 0

摘要

可见近红外(Vis-NIR)反射技术是一种功能强大的工具,特别是能更快地获取有关土壤质地、有机质和碳酸钙含量的信息。然而,利用不同土壤系列剖面中的可见近红外数据表征土壤层的研究还很有限。本研究调查了图尔基耶哈兰平原具有不同遗传特性的八个土壤剖面中土壤特性与光谱反射率(可见光-近红外)之间的关系,重点关注剖面内部(A、B 和 C 层)以及不同土壤系列之间的变化。从 A、B 和 C 层共采集了 36 份土壤样本,在测量光谱反射率的同时,还测量了碳酸钙、有机质和粒度分布。碳酸钙(11.58%-52.50%)和有机质含量(0.60%-3.71%)的变化很大,反映了受母质和土地管理影响的复杂土壤成分。在剖面内观察到不同的反射模式,反映了土壤成分的变化。有机质含量较高的 Ap 层通常反射率较低(可见光区域)。粘土含量影响近红外反射率,富含粘土的剖面吸收率较高。由于地层的形成和粘土/碳酸盐的积累,Kaynakli 系列(细壤质、混合、中性典型钙质)在 700 纳米波长后显示出 A 和 B 地层之间反射率的差异。Ck 地层中碳酸钙含量的增加导致反射率高于其他地层。证实可见光-近红外反射率可以解释很大一部分土壤特性差异(A:87.7%;B:88.3%;C:90.6%)。PCA 结果支持这样一种观点,即可见近红外反射测量所捕获的光谱特征表明了 A、B 和 C 层之间的固有差异。这项研究为应用可见近红外光谱仪进行土壤评估和监测提供了越来越多的知识。不过,未来的研究应侧重于了解不同土壤和环境条件下的光谱反射率变化。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Rapid characterization of soil horizons for different soil series utilizing Vis-NIR spectral information

The visible-near infrared (Vis-NIR) reflectance technique is a powerful tool, particularly for obtaining faster information about soil texture, organic matter, and calcium carbonate content. However, there is limited research on the characterization of soil horizons using Vis-NIR data in profiles of different soil series. This study investigated the relationship between soil properties and spectral reflectance (Vis-NIR) in eight soil profiles with varying genetic properties from Harran Plain, Türkiye, focusing on variations within profiles (A, B, and C horizons) and across different soil series. A total of 36 soil samples were collected from the A, B, and C horizons, and spectral reflectance was measured along with calcium carbonate, organic matter, and particle size distribution. High variability was observed in calcium carbonate (11.58–52.50%) and organic matter content (0.60–3.71%), reflecting complex soil composition influenced by parent material and land management. Distinct reflectance patterns were observed within profiles, reflecting variations in soil composition. Ap horizons with higher organic matter content often exhibited lower reflectance (visible region). Clay content influenced NIR reflectance, with higher absorption in clay-rich profiles. The Kaynakli series (Fine-loamy, mixed, mesic Typic Calcixerepts) showed differentiation in reflectance between A and B horizons after 700 nm due to horizon formation and clay/carbonate accumulation. Increasing calcium carbonate content in Ck horizons led to higher reflectance compared to other layers. Confirmed that Vis-NIR reflectance could explain a significant portion of the variance in soil properties (A: 87.7%, B: 88.3%, and C: 90.6%). PCA results supported the notion that spectral signatures captured by Vis-NIR reflectance measurements are indicative of inherent differences between A, B, and C horizons. This study contributes to the growing body of knowledge on the application of Vis-NIR spectroscopy for soil assessment and monitoring. However, future research should focus on understanding spectral reflectance variations under diverse soil and environmental conditions.

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来源期刊
Geoderma Regional
Geoderma Regional Agricultural and Biological Sciences-Soil Science
CiteScore
6.10
自引率
7.30%
发文量
122
审稿时长
76 days
期刊介绍: Global issues require studies and solutions on national and regional levels. Geoderma Regional focuses on studies that increase understanding and advance our scientific knowledge of soils in all regions of the world. The journal embraces every aspect of soil science and welcomes reviews of regional progress.
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