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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, Lower Cone, Site U1529, Earth in motion, Expedition 376, IODP, JOIDES Resolution, acidic fluids, hydrogeology, Site U1527, Site U1528, Brothers Arc Flux, dacite lava, deep biosphere, Brothers volcano, Upper Cone, Site U1530, Kermadec arc, hypersaline brine, Site U1531
International Ocean Discovery Program, Lower Cone, Site U1529, Earth in motion, Expedition 376, IODP, JOIDES Resolution, acidic fluids, hydrogeology, Site U1527, Site U1528, Brothers Arc Flux, dacite lava, deep biosphere, Brothers volcano, Upper Cone, Site U1530, Kermadec arc, hypersaline brine, Site U1531
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