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Fundamental elemental component (total carbon, hydrogen, nitrogen, and sulfur) fluctuations help define the origin, depositional environment, and diagenetic alteration of source materials. To determine C, H, N, and S, solid samples are reacted with a catalyst, separated by chromatography, and detected by thermal conductivity on a FlashEA 1112 CHNS elemental analyzer. Organic carbon can be directly measured on the elemental analyzer by acidification of the sample to drive off carbonate as carbon dioxide before analyzing. Total organic carbon on this report is measured rather than calculated.
International Ocean Discovery Program, fluid flow, Earth in motion, carbon sequestration, Tuaheni Basin, logging while drilling, IODP, JOIDES Resolution, Expedition 372, slope stability, gas hydrates, Site U1517, Tuaheni Landslide Complex, Hikurangi margin, mass transport deposits, New Zealand
International Ocean Discovery Program, fluid flow, Earth in motion, carbon sequestration, Tuaheni Basin, logging while drilling, IODP, JOIDES Resolution, Expedition 372, slope stability, gas hydrates, Site U1517, Tuaheni Landslide Complex, Hikurangi margin, mass transport deposits, New Zealand
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