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    Excess pCO<sub>2</sub> and carbonate system geochemistry in surface seawater of the exclusive economic zone of Qatar (Arabian Gulf) by Connor Izumi (17337868)

    Published 2022
    “…Salinity-normalized (to S = 40) total alkalinity (NTA) and dissolved inorganic carbon (NDIC) in surface seawater decrease as waters flow north from Hormuz. The slope suggests that removal of C as CaCO<sub>3</sub>, organic matter (CH<sub>2</sub>O) or gas exchange (F<sub>CO2</sub>) is occurring with a ratio of ΔCaCO<sub>3</sub>/(ΔCH<sub>2</sub>O or F<sub>CO2</sub>) = 1:2.86. …”