Spectroscopic signatures for expeditious monitoring of contamination risks at abandoned coal mine sites

IF 2.6 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
Jelena Milinovic , Patrícia Santos , Jorge Espinha Marques , Deolinda Flores , Aurora Futuro , Carlos M. Pereira , Manuel Azenha
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引用次数: 0

Abstract

Soil acts as a natural ‘filter’, playing a crucial role in the transfer of geogenic and anthropogenic pollutants from abandoned coal mine sites to surrounding water bodies. Key indicators of soil contamination, such as pH, electrical conductivity (EC), and organic matter (OM), expressed as loss-on-ignition (LOI), can signal contamination risks when they deviate from optimal ranges. To enable sustainable risk assessment through monitoring of pH, EC, and LOI, streamlined spectroscopic techniques Fourier transform infrared (FTIR), near-infrared (NIR), Raman, and X-ray fluorescence (XRF) were applied in combination with multivariate analysis (MVA), to soil samples from two abandoned coal mines in NW Portugal. Partial least squares (PLS) regression models demonstrated that XRF spectroscopic data provided the most accurate assessment of soil pH, EC, and LOI at the local scale (R2 = 0.92–0.99). The most significant spectroscopic signatures, identified through weighted regression coefficients (Bw), enabled robust predictions of these key soil parameters. These findings highlight that these geochemical variables outperform molecular spectroscopy techniques for efficient and environmentally relevant risk monitoring of contamination in abandoned coal mine sites.
用于快速监测废弃煤矿污染风险的光谱特征
土壤是天然的 "过滤器",在废弃煤矿场地的地质和人为污染物向周围水体转移的过程中发挥着至关重要的作用。土壤污染的关键指标,如 pH 值、导电率 (EC) 和有机质 (OM)(以点火损失率 (LOI) 表示),一旦偏离最佳范围,就会发出污染风险信号。为了通过监测 pH 值、EC 值和 LOI 值实现可持续的风险评估,对葡萄牙西北部两个废弃煤矿的土壤样本采用了傅立叶变换红外(FTIR)、近红外(NIR)、拉曼(Raman)和 X 射线荧光(XRF)等简化光谱技术,并结合多元分析(MVA)。偏最小二乘法(PLS)回归模型表明,XRF 光谱数据可在局部范围内对土壤 pH 值、EC 值和 LOI 进行最准确的评估(R2 = 0.92-0.99)。通过加权回归系数(Bw)确定的最重要光谱特征能够对这些关键土壤参数进行可靠的预测。这些研究结果表明,这些地球化学变量优于分子光谱技术,可用于对废弃煤矿场地污染进行高效且与环境相关的风险监测。
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来源期刊
Chemie Der Erde-Geochemistry
Chemie Der Erde-Geochemistry 地学-地球化学与地球物理
CiteScore
7.10
自引率
0.00%
发文量
40
审稿时长
3.0 months
期刊介绍: GEOCHEMISTRY was founded as Chemie der Erde 1914 in Jena, and, hence, is one of the oldest journals for geochemistry-related topics. GEOCHEMISTRY (formerly Chemie der Erde / Geochemistry) publishes original research papers, short communications, reviews of selected topics, and high-class invited review articles addressed at broad geosciences audience. Publications dealing with interdisciplinary questions are particularly welcome. Young scientists are especially encouraged to submit their work. Contributions will be published exclusively in English. The journal, through very personalized consultation and its worldwide distribution, offers entry into the world of international scientific communication, and promotes interdisciplinary discussion on chemical problems in a broad spectrum of geosciences. The following topics are covered by the expertise of the members of the editorial board (see below): -cosmochemistry, meteoritics- igneous, metamorphic, and sedimentary petrology- volcanology- low & high temperature geochemistry- experimental - theoretical - field related studies- mineralogy - crystallography- environmental geosciences- archaeometry
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