How significant is submarine groundwater discharge and its associated dissolved inorganic carbon in a river-dominated shelf system? Academic Article uri icon


  • <p><strong>Abstract.</strong> In order to assess the role of submarine groundwater discharge (SGD) and its impact on the carbonate system on the northern South China Sea (NSCS) shelf, we measured seawater concentrations of four radium isotopes <sup>223,224,226,228</sup>Ra along with carbonate system parameters in June–July, 2008. Complementary groundwater sampling was conducted in coastal areas in December 2008 and October 2010 to constrain the groundwater end-members. The distribution of Ra isotopes in the NSCS was largely controlled by the Pearl River plume and coastal upwelling. Long-lived Ra isotopes (<sup>228</sup>Ra and <sup>226</sup>Ra) were enriched in the river plume but low in the offshore surface water and subsurface water/upwelling zone. In contrast, short-lived Ra isotopes (<sup>224</sup>Ra and <sup>223</sup>Ra) were elevated in the subsurface water/upwelling zone as well as in the river plume but depleted in the offshore surface water. In order to quantify SGD, we adopted two independent mathematical approaches. Using a three end-member mixing model with total alkalinity (TAlk) and Ra isotopes, we derived a SGD flux into the NSCS shelf of 2.3–3.7 × 10<sup>8</sup> m<sup>3</sup> day<sup>?1</sup>. Our second approach involved a simple mass balance of <sup>228</sup>Ra and <sup>226</sup>Ra and resulted in a first order but consistent SGD flux estimate of 2.2–3.7 × 10<sup>8</sup> m<sup>3</sup> day<sup>?1</sup>. These fluxes were equivalent to 12–21 % of the Pearl River discharge, but the source of the SGD was mostly recirculated seawater. Despite the relatively small SGD volume flow compared to the river, the associated material fluxes were substantial given their elevated concentrations of dissolved inorganic solutes. In this case, dissolved inorganic carbon (DIC) flux through SGD was 153–347 × 10<sup>9</sup> mol yr<sup>?1</sup>, or ~23–53 % of the riverine DIC export flux. Our estimates of the groundwater-derived phosphate flux ranged 3–68 × 10<sup>7</sup> mol yr<sup>?1</sup>, which may be responsible for new production on the shelf up to 0.3–6.3 mmol C m<sup>?2</sup> d<sup>?1</sup>. This rate of new production would at most consume 11 % of the DIC contribution delivered by SGD. Hence, SGD may play an important role in the carbon balance over the NSCS shelf.</p>

publication date

  • May 22, 2012