Estimating submarine groundwater discharge in Jeju volcanic island (Korea) during a typhoon (Kong-rey) using humic-fluorescent dissolved organic matter-Si mass balance.

ABSTRACT: We examined the residence time, seepage rate, and submarine groundwater discharge (SGD)-driven dissolved nutrients and organic matter in Hwasun Bay, Jeju Island, Korea during the occurrence of a typhoon, Kong-rey, using a humic fluorescent dissolved organic matter (FDOM_H)-Si mass balance model. The study period spanned October 4-10, 2018. One day after the typhoon, the residence time and seepage rate were calculated to be 1 day and 0.51 m day^-1, respectively, and the highest SGD-driven fluxes of chemical constituents were estimated (1.7?×?10⁶ mol day^-1 for dissolved inorganic nitrogen, 0.1?×?10⁶ mol day^-1 for dissolved inorganic phosphorus (DIP), 1.1?×?10⁶ mol day^-1 for dissolved silicon, 0.5?×?10⁶ mol day^-1 for dissolved organic carbon, 1.6?×?10⁶ mol day^-1 for dissolved organic nitrogen, 0.4?×?10⁶ mol day^-1 for particulate organic carbon, and 38?×?10⁶ g QS day^-1 for FDOM_H). SGD-driven fluxes of dissolved nutrient and organic matter were over 90% of the total input fluxes in Hwasun Bay. Our results highlight the potential of using the FDOM_H-Si mass balance model to effectively measure SGD within a specific area (i.e., volcanic islands) under specific weather conditions (i.e., typhoon/storm). In oligotrophic oceanic regions, SGD-driven chemical fluxes from highly permeable islands considerably contribute to coastal nutrient budgets and coastal biological production.

SUBMITTER: Cho HM 

PROVIDER: S-EPMC7807084 | biostudies-literature | 2021 Jan

REPOSITORIES: biostudies-literature