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Analysis of deep-ocean sediments from the TAG hydrothermal field (MAR, 26° N): application of short-wave infrared reflectance (SWIR) spectra for offshore geochemical exploration

Purpose The cost-efficient methods of analysis, such as rapid short-wave infrared (SWIR) spectral analysis, have been applied for the efficient exploration of critical raw materials (CRM), including mineral components and rare earth elements (REE) from the deep-ocean sediments. Methods Gravity cored...

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Published in:Journal of soils and sediments 2020-09, Vol.20 (9), p.3472-3486
Main Authors: Milinovic, Jelena, Barriga, Fernando J.A.S., Murton, Bramley J.
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description Purpose The cost-efficient methods of analysis, such as rapid short-wave infrared (SWIR) spectral analysis, have been applied for the efficient exploration of critical raw materials (CRM), including mineral components and rare earth elements (REE) from the deep-ocean sediments. Methods Gravity cored sediment samples were collected during an oceanographic mission to the Trans-Atlantic Geotraverse (TAG) hydrothermal field of the Mid-Atlantic Ridge (MAR, 26° N). SWIR reflectance spectra (dependent variable) of samples were mathematically tested against referent geochemical data (independent variable), obtained by conventional analysis (ICP/OES, ICP/MS), after applied full cross-validation multivariate partial least square regression (CVPLSR). Value of parameter-residual predictive deviation (RPD) was used for evaluation of CVPLSR modeling: RPD > 2.5 (satisfactory calibration model for the screening purposes) and RPD > 5.0 (model adequate for the quality control of the studied elements). Results The CVPLSR modeling provided significant results for the determination of several mineral components: major elements (Fe and Si) had the values of RPD equal to 3.65 and 2.84, respectively, which indicated a viable potential for their routine analysis, whereas RPD for Ca was equal to 5.51, thus assuring its quality control by SWIR analysis, in sediment samples of the studied location. Among the REE, Ce (RPD = 2.55) and Er (RPD = 2.59) yielded the most satisfactory results. Conclusions The findings highlight the benefit of rapidly obtained empirical SWIR-reflectance data, which can be used for near-real-time exploration of geochemical deposits hosted in deep-ocean sediments.
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Methods Gravity cored sediment samples were collected during an oceanographic mission to the Trans-Atlantic Geotraverse (TAG) hydrothermal field of the Mid-Atlantic Ridge (MAR, 26° N). SWIR reflectance spectra (dependent variable) of samples were mathematically tested against referent geochemical data (independent variable), obtained by conventional analysis (ICP/OES, ICP/MS), after applied full cross-validation multivariate partial least square regression (CVPLSR). Value of parameter-residual predictive deviation (RPD) was used for evaluation of CVPLSR modeling: RPD &gt; 2.5 (satisfactory calibration model for the screening purposes) and RPD &gt; 5.0 (model adequate for the quality control of the studied elements). Results The CVPLSR modeling provided significant results for the determination of several mineral components: major elements (Fe and Si) had the values of RPD equal to 3.65 and 2.84, respectively, which indicated a viable potential for their routine analysis, whereas RPD for Ca was equal to 5.51, thus assuring its quality control by SWIR analysis, in sediment samples of the studied location. Among the REE, Ce (RPD = 2.55) and Er (RPD = 2.59) yielded the most satisfactory results. Conclusions The findings highlight the benefit of rapidly obtained empirical SWIR-reflectance data, which can be used for near-real-time exploration of geochemical deposits hosted in deep-ocean sediments.</description><identifier>ISSN: 1439-0108</identifier><identifier>EISSN: 1614-7480</identifier><identifier>DOI: 10.1007/s11368-020-02691-3</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Components ; Cost analysis ; Dependent variables ; Earth and Environmental Science ; Empirical analysis ; Environment ; Environmental Physics ; Exploration ; Geochemistry ; Gravity ; Hydrothermal fields ; Independent variables ; Infrared analysis ; Infrared spectra ; Major elements ; Methods ; Mid-ocean ridges ; Mineral exploration ; Modelling ; Offshore ; Quality assurance ; Quality control ; Rare earth elements ; Raw materials ; Reflectance ; Regression analysis ; Sec 1 • Sediment Quality and Impact Assessment • Research Article ; Sediment ; Sediment deposits ; Sediment samplers ; Sediment samples ; Sediments ; Short wave radiation ; Soil Science &amp; Conservation ; Spectra ; Spectral analysis ; Spectrum analysis</subject><ispartof>Journal of soils and sediments, 2020-09, Vol.20 (9), p.3472-3486</ispartof><rights>Springer-Verlag GmbH Germany, part of Springer Nature 2020</rights><rights>Springer-Verlag GmbH Germany, part of Springer Nature 2020.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c319t-8e1c23f407e4ee2692de54c6c6641dbf837f36f2e93aa04a5a49c913955472023</citedby><cites>FETCH-LOGICAL-c319t-8e1c23f407e4ee2692de54c6c6641dbf837f36f2e93aa04a5a49c913955472023</cites><orcidid>0000-0002-7092-7851</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27923,27924</link.rule.ids></links><search><creatorcontrib>Milinovic, Jelena</creatorcontrib><creatorcontrib>Barriga, Fernando J.A.S.</creatorcontrib><creatorcontrib>Murton, Bramley J.</creatorcontrib><title>Analysis of deep-ocean sediments from the TAG hydrothermal field (MAR, 26° N): application of short-wave infrared reflectance (SWIR) spectra for offshore geochemical exploration</title><title>Journal of soils and sediments</title><addtitle>J Soils Sediments</addtitle><description>Purpose The cost-efficient methods of analysis, such as rapid short-wave infrared (SWIR) spectral analysis, have been applied for the efficient exploration of critical raw materials (CRM), including mineral components and rare earth elements (REE) from the deep-ocean sediments. Methods Gravity cored sediment samples were collected during an oceanographic mission to the Trans-Atlantic Geotraverse (TAG) hydrothermal field of the Mid-Atlantic Ridge (MAR, 26° N). SWIR reflectance spectra (dependent variable) of samples were mathematically tested against referent geochemical data (independent variable), obtained by conventional analysis (ICP/OES, ICP/MS), after applied full cross-validation multivariate partial least square regression (CVPLSR). Value of parameter-residual predictive deviation (RPD) was used for evaluation of CVPLSR modeling: RPD &gt; 2.5 (satisfactory calibration model for the screening purposes) and RPD &gt; 5.0 (model adequate for the quality control of the studied elements). Results The CVPLSR modeling provided significant results for the determination of several mineral components: major elements (Fe and Si) had the values of RPD equal to 3.65 and 2.84, respectively, which indicated a viable potential for their routine analysis, whereas RPD for Ca was equal to 5.51, thus assuring its quality control by SWIR analysis, in sediment samples of the studied location. Among the REE, Ce (RPD = 2.55) and Er (RPD = 2.59) yielded the most satisfactory results. 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Methods Gravity cored sediment samples were collected during an oceanographic mission to the Trans-Atlantic Geotraverse (TAG) hydrothermal field of the Mid-Atlantic Ridge (MAR, 26° N). SWIR reflectance spectra (dependent variable) of samples were mathematically tested against referent geochemical data (independent variable), obtained by conventional analysis (ICP/OES, ICP/MS), after applied full cross-validation multivariate partial least square regression (CVPLSR). Value of parameter-residual predictive deviation (RPD) was used for evaluation of CVPLSR modeling: RPD &gt; 2.5 (satisfactory calibration model for the screening purposes) and RPD &gt; 5.0 (model adequate for the quality control of the studied elements). Results The CVPLSR modeling provided significant results for the determination of several mineral components: major elements (Fe and Si) had the values of RPD equal to 3.65 and 2.84, respectively, which indicated a viable potential for their routine analysis, whereas RPD for Ca was equal to 5.51, thus assuring its quality control by SWIR analysis, in sediment samples of the studied location. Among the REE, Ce (RPD = 2.55) and Er (RPD = 2.59) yielded the most satisfactory results. Conclusions The findings highlight the benefit of rapidly obtained empirical SWIR-reflectance data, which can be used for near-real-time exploration of geochemical deposits hosted in deep-ocean sediments.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s11368-020-02691-3</doi><tpages>15</tpages><orcidid>https://orcid.org/0000-0002-7092-7851</orcidid></addata></record>
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subjects Components
Cost analysis
Dependent variables
Earth and Environmental Science
Empirical analysis
Environment
Environmental Physics
Exploration
Geochemistry
Gravity
Hydrothermal fields
Independent variables
Infrared analysis
Infrared spectra
Major elements
Methods
Mid-ocean ridges
Mineral exploration
Modelling
Offshore
Quality assurance
Quality control
Rare earth elements
Raw materials
Reflectance
Regression analysis
Sec 1 • Sediment Quality and Impact Assessment • Research Article
Sediment
Sediment deposits
Sediment samplers
Sediment samples
Sediments
Short wave radiation
Soil Science & Conservation
Spectra
Spectral analysis
Spectrum analysis
title Analysis of deep-ocean sediments from the TAG hydrothermal field (MAR, 26° N): application of short-wave infrared reflectance (SWIR) spectra for offshore geochemical exploration
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