_version_ 1867170390540812288
author Dunlea, Ann G
Murray, Richard W
Tada, Ryuji
Alvarez-Zarikian, Carlos A
Anderson, Chloe H
Gilli, Adrian
Giosan, Liviu
Gorgas, Thomas
Hennekam, Rick
Irino, Tomohisa
Murayama, Masafumi
Peterson, Larry C
Reichart, Gert-Jan
Seki, Arisa
Zheng, Hongbo
Ziegler, Martin
author_facet Dunlea, Ann G
Murray, Richard W
Tada, Ryuji
Alvarez-Zarikian, Carlos A
Anderson, Chloe H
Gilli, Adrian
Giosan, Liviu
Gorgas, Thomas
Hennekam, Rick
Irino, Tomohisa
Murayama, Masafumi
Peterson, Larry C
Reichart, Gert-Jan
Seki, Arisa
Zheng, Hongbo
Ziegler, Martin
collection Datos científicos de ciencias marinas y ambientales
contents Four discrete samples were freeze-dried and powdered and pressed into disc-shaped pellets about 2 cm in diameter from nearby Core MD01-2407 on the Oki Ridge (37°04'N, 134°42'E, 932m water depth). The four samples have a similar matrix to the seven sediment sections scanned in this study. The four samples from Core MD01-2407 covered a range of sediment types (calcareous, siliceous, light-, and dark-colored; Kido et al., 2007) that span the dynamic range of at least Fe and Ca element cps scanned for this study. A set of four pellets was sent to four of the seven labs (1 ITRAX and 3 Avaatech) involved in the study to be scanned using the same instrument parameters they used on the sediment sections. Three labs used the same instrument and parameters used for the sediment section, but the fourth lab replaced the X-ray tube in between scanning the pellets and sediment sections. The major and trace element concentrations of the pellets were also analyzed by inductively coupled plasma (ICP)-optical emission spectrometry (OES) and ICP-mass spectrometry (MS) in the Analytical Geochemistry Facilities at Boston University, Boston, MA, USA. The ICP analyses had ~2% precision and a standard reference material analyzed as an unknown alongside the samples was accurate within precision.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_922042
institution PANGAEA
language en
publishDate 2020
publisher PANGAEA
record_format pangaea
spellingShingle Inter-comparison of ICP and XRF-scanning results by four different XRF-labs (dried pellets from IODP core MD01-2407)
Dunlea, Ann G
Murray, Richard W
Tada, Ryuji
Alvarez-Zarikian, Carlos A
Anderson, Chloe H
Gilli, Adrian
Giosan, Liviu
Gorgas, Thomas
Hennekam, Rick
Irino, Tomohisa
Murayama, Masafumi
Peterson, Larry C
Reichart, Gert-Jan
Seki, Arisa
Zheng, Hongbo
Ziegler, Martin
Aluminium; Barium; Bromine; Calcium; Chlorine; Chromium; Copper; Excitation energy; Gallium; Giant piston corer; GPC; ICP-MS; IMAGES VII - WEPAMA; Inductively coupled plasma mass spectrometry; Inter-lab comparison; IODP; IODP Expedition 346; Iron; Lead; Manganese; Marine sediment; Marion Dufresne (1995); MD012407; MD01-2407; MD122; Molybdenum; Nickel; Paleoceanography; Potassium; Rubidium; Sample comment; Sea of Japan; Sediment Geochemistry; Sediment type; Silicon; Strontium; Sulfur; Time in seconds; Titanium; Vanadium; X-ray fluorescence; X-ray fluorescence (XRF); XRF; XRF calibration; XRF scanning; Yttrium; Zinc; Zirconium
Four discrete samples were freeze-dried and powdered and pressed into disc-shaped pellets about 2 cm in diameter from nearby Core MD01-2407 on the Oki Ridge (37°04'N, 134°42'E, 932m water depth). The four samples have a similar matrix to the seven sediment sections scanned in this study. The four samples from Core MD01-2407 covered a range of sediment types (calcareous, siliceous, light-, and dark-colored; Kido et al., 2007) that span the dynamic range of at least Fe and Ca element cps scanned for this study. A set of four pellets was sent to four of the seven labs (1 ITRAX and 3 Avaatech) involved in the study to be scanned using the same instrument parameters they used on the sediment sections. Three labs used the same instrument and parameters used for the sediment section, but the fourth lab replaced the X-ray tube in between scanning the pellets and sediment sections. The major and trace element concentrations of the pellets were also analyzed by inductively coupled plasma (ICP)-optical emission spectrometry (OES) and ICP-mass spectrometry (MS) in the Analytical Geochemistry Facilities at Boston University, Boston, MA, USA. The ICP analyses had ~2% precision and a standard reference material analyzed as an unknown alongside the samples was accurate within precision.
title Inter-comparison of ICP and XRF-scanning results by four different XRF-labs (dried pellets from IODP core MD01-2407)
topic Aluminium; Barium; Bromine; Calcium; Chlorine; Chromium; Copper; Excitation energy; Gallium; Giant piston corer; GPC; ICP-MS; IMAGES VII - WEPAMA; Inductively coupled plasma mass spectrometry; Inter-lab comparison; IODP; IODP Expedition 346; Iron; Lead; Manganese; Marine sediment; Marion Dufresne (1995); MD012407; MD01-2407; MD122; Molybdenum; Nickel; Paleoceanography; Potassium; Rubidium; Sample comment; Sea of Japan; Sediment Geochemistry; Sediment type; Silicon; Strontium; Sulfur; Time in seconds; Titanium; Vanadium; X-ray fluorescence; X-ray fluorescence (XRF); XRF; XRF calibration; XRF scanning; Yttrium; Zinc; Zirconium
url https://doi.org/10.1594/PANGAEA.922042