O2 consumption rate and its isotopic fractionation factor in the deep water of the Philippine Sea

Concentration and stable isotopic compositions (delta(18)O) of dissolved O(2) were measured in seawater samples collected from the Philippine Sea in June 2006. The in-situ O(2) consumption rate and the isotopic fractionation factor (alpha(r)) during dissolved O(2) consumption were obtained from field observations by applying a vertical one-dimensional advection diffusion model to the deep water mass of about 1000-4000 m. The average O(2) consumption rate and alpha(r) were, respectively, 0.11 +/- 0.07 mu mol kg(-1) yr(-1) and 0.990 +/- 0.001. These estimated values agree well with values from earlier estimations of Pacific deep water. The in-situ 02 consumption rates are two or more times higher north of 20 degrees N, although the value of alpha(r) was not significantly different between the north and south. Its levels varied rapidly in the water mass of less about 2000 m depth. These results suggest that organic matter from the continent imparts a meaningful contribution to the upper water in the northern part of the area; it might produce the strong O(2) minimum that is evident in the water mass from about 1000-2000 m in the northern part of the Philippine Sea.