dc.contributor.authorChiang, Hong-Wei
dc.contributor.authorLu, Yanbin
dc.contributor.authorWang, Xianfeng
dc.contributor.authorLin, Ke
dc.contributor.authorLiu, Xiaokang
dc.date.accessioned2019-04-15T03:54:02Z
dc.date.available2019-04-15T03:54:02Z
dc.date.issued2019
dc.identifier.citationChiang, H.-W., Lu, Y., Wang, X., Lin, K., & Liu, X. (2019). Optimizing MC-ICP-MS with SEM protocols for determination of U and Th isotope ratios and 230Th ages in carbonates. Quaternary Geochronology, 5075-90. doi:10.1016/j.quageo.2018.10en_US
dc.identifier.issn1871-1014en_US
dc.identifier.urihttp://hdl.handle.net/10220/48030
dc.description.abstractWe have optimized techniques to measure uranium and thorium isotopic compositions using secondary electron multiplier (SEM) and peak-jumping protocols on a multi-collector inductively coupled plasma mass spectrometer (MC-ICP-MS, Thermo Scientific Neptune Plus). This instrument is equipped with an advanced interface pump, X- skimmer cone, Jet sample cone, and desolvating nebulizer system (CETAC Aridus II) that enables overall ioni-zation and transmission efficiency up to 3% for both U and Th. Approximately 50 fg234U or 230Th can routinely yield a precision of 1–2‰ (2σ) for abundance and isotopic measurements. Non-linear behavior was not observed in the MasCom SEM with a retarding potential quadrupole in our MC-ICP-MS system when the beam intensity was limited to < ∼1 × 10 6 cps. We performed a series of tests to examine the influence of tuning parameters, peak shift, and operating voltage of the SEM on isotopic measurements. Results for U/Th standards are consistent with published values and demonstrate the reliability of our protocols. Lastly, the precision and accuracy of 230Th ages based on U and Th isotope ratios is presented for a variety of carbonates, including both modern and secular-equilibrium samples. For corals as young as ∼10-yr old, we have significantly reduced the procedural chemistry blanks so that only 40 mg is required to yield an analytical precision of ± 1.4 yr (2σ). All 230Th ages from modern and fossil corals and speleothems are in agreement with band counting ages.en_US
dc.description.sponsorshipNRF (Natl Research Foundation, S’pore)en_US
dc.description.sponsorshipMOE (Min. of Education, S’pore)en_US
dc.format.extent16 p.en_US
dc.language.isoenen_US
dc.relation.ispartofseriesQuaternary Geochronologyen_US
dc.rights© 2018 The Authors. Published by Elsevier B.V. This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/BY-NC-ND/4.0/).en_US
dc.subjectU-Th Datingen_US
dc.subjectMC-ICP-MSen_US
dc.subjectDRNTU::Science::Geologyen_US
dc.titleOptimizing MC-ICP-MS with SEM protocols for determination of U and Th isotope ratios and 230Th ages in carbonatesen_US
dc.typeJournal Article
dc.contributor.researchEarth Observatory of Singaporeen_US
dc.contributor.schoolAsian School of the Environmenten_US
dc.identifier.doihttp://dx.doi.org/10.1016/j.quageo.2018.10.003
dc.description.versionPublished versionen_US


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