{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1390868361812372736.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.2465/jmps.241028al"}},{"identifier":{"@type":"URI","@value":"https://www.jstage.jst.go.jp/article/jmps/120/1/120_241028aL/_pdf"}}],"dc:title":[{"@language":"en","@value":"Evaluation of the influence of laser irradiation on Raman spectra of low-grade carbonaceous materials"}],"dc:language":"en","description":[{"type":"abstract","notation":[{"@language":"en","@value":"<p>We evaluated the influence of laser irradiation for Raman spectroscopic analysis of low-grade carbonaceous materials (CMs) using three samples with peak metamorphic temperatures of approximately 200-300 °C. In the analysis, spectra were acquired using a 532 nm laser wavelength and a ×50 objective lens, which are common analytical conditions in CM Raman geothermometry. As CM is opaque, it is easily heated and damaged when irradiated with a high-power laser. However, an excessively low laser power results in a poor signal-to-noise ratio (SNR), making accurate parameter evaluation difficult. First, we investigated the minimum laser power conditions required to obtain a desirable SNR. The full width at half maximum (FWHM) of the D1-band, which is used as a parameter for metamorphic temperature estimation in CM Raman geothermometry, exhibited a considerably large standard deviation and small SNR at a surface laser power of <0.5 mW. Next, we focused on the influence of high irradiation power on the CM Raman spectra. The results show that the FWHM of the D1-band is sensitive to ‘damage’, i.e., the irreversible change in the structure of CM by laser irradiation. On the other hand, the peak position of the D1-band is sensitive to ‘heat’, meaning i.e., the increased surface temperature of CM. In particular, the FWHM of the D1-band increased as the laser power increased to >2.0 mW, which significantly affected the metamorphic temperature estimation. Similar results were obtained for measurements using a ×100 objective lens and different types of micro-Raman spectrometers. When the exposure time exceeded 30 s with sufficient laser power (>0.5 mW), the SNR became almost constant. More than three accumulations were efficient at eliminating cosmic-ray interference. Based on these results, we propose that a laser power of 0.5-2 mW and measurements of 10 s × 3 measurements are the optimum laser irradiation conditions for Raman spectroscopic analysis of low-grade CM.</p>"}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1410868361812372738","@type":"Researcher","foaf:name":[{"@language":"en","@value":"OGINO Shunsuke"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Graduate School of Environmental Studies, Nagoya University"}]},{"@id":"https://cir.nii.ac.jp/crid/1410868361812372736","@type":"Researcher","foaf:name":[{"@language":"en","@value":"KOUKETSU Yui"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Graduate School of Environmental Studies, Nagoya University"}]},{"@id":"https://cir.nii.ac.jp/crid/1410868361812372737","@type":"Researcher","foaf:name":[{"@language":"en","@value":"SHIMIZU Ichiko"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Division of Earth and Planetary Sciences, Graduate School of Science, Kyoto University"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"13456296"},{"@type":"LISSN","@value":"13456296"},{"@type":"EISSN","@value":"13493825"}],"prism:publicationName":[{"@language":"en","@value":"Journal of Mineralogical and Petrological Sciences"},{"@language":"en","@value":"Journal of Mineralogical and Petrological Sciences"}],"dc:publisher":[{"@language":"en","@value":"Japan Association of Mineralogical Sciences"},{"@language":"ja","@value":"一般社団法人　日本鉱物科学会"}],"prism:publicationDate":"2025","prism:volume":"120","prism:number":"1","prism:startingPage":"n/a"},"reviewed":"false","url":[{"@id":"https://www.jstage.jst.go.jp/article/jmps/120/1/120_241028aL/_pdf"}],"availableAt":"2025","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=Carbonaceous%20material%20(CM)","dc:title":"Carbonaceous material (CM)"},{"@id":"https://cir.nii.ac.jp/all?q=Raman%20spectroscopy","dc:title":"Raman spectroscopy"},{"@id":"https://cir.nii.ac.jp/all?q=Laser%20power","dc:title":"Laser power"},{"@id":"https://cir.nii.ac.jp/all?q=Signal-to-noise%20ratio%20(SNR)","dc:title":"Signal-to-noise ratio (SNR)"},{"@id":"https://cir.nii.ac.jp/all?q=CM%20Raman%20geothermometer","dc:title":"CM Raman geothermometer"}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360009142847415424","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Thermal structure in subducted units from continental Moho depths in a palaeo subduction zone, the Asemigawa region of the Sanbagawa metamorphic belt, SW Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013172086495488","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Raman spectroscopy"}]},{"@id":"https://cir.nii.ac.jp/crid/1360016870030587520","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An automatic peak deconvolution method for <scp>Raman</scp> spectra of terrestrial carbonaceous material for application to the geothermometers of <scp>Kouketsu</scp> et al. (2014)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283693140988416","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A new approach to develop the <scp>R</scp>aman carbonaceous material geothermometer for low‐grade metamorphism using peak width"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848663334883712","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An experimental kinetic study on the structural evolution of natural carbonaceous material to graphite"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137046206658816","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Raman spectra of carbonaceous material in metasediments: a new geothermometer"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418519492670976","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Irradiation-induced amorphization of graphite"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262943483691392","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Graphitization in a high-pressure, low-temperature metamorphic gradient: a Raman microspectroscopy and HRTEM study"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945463268864","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"On the characterization of disordered and heterogeneous carbonaceous materials by Raman spectroscopy"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544419492878336","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Proper understanding of down-shifted Raman spectra of natural graphite: Direct estimation of laser-induced rise in sample temperature"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825895860348544","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Evolution of the Raman spectrum of carbonaceous material in low-grade metasediments of the Glarus Alps (Switzerland)"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107368752893440","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Raman Spectrum of Graphite"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107370773000960","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Raman Spectroscopy for Chemical Analysis"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951794319018752","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Extending the applicability of the Raman carbonaceous‐material geothermometer using data from contact metamorphic rocks"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206545559168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Testing for robustness on estimation of graphitization degree by Raman spectroscopy"}]},{"@id":"https://cir.nii.ac.jp/crid/1390011540582487296","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Determination of the laser–induced damage threshold for graphite and coal with deep–UV micro–Raman spectroscopy"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681218573312","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Lithostratigraphy of the Mesozoic Tetori Group in the upper reaches of the Kuzuryu River, central Japan"},{"@value":"福井県九頭竜川上流地方の手取層群の層序と岩相変化"},{"@language":"ja-Kana","@value":"フクイケン クズリュウ ガワジョウリュ"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714791998113024","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Drastic effect of shearing on graphite microtexture : attention and application to Earth science"}]}],"dataSourceIdentifier":[{"@type":"JALC","@value":"oai:japanlinkcenter.org:2014552999"},{"@type":"CROSSREF","@value":"10.2465/jmps.241028al"}]}