Although dissolved inorganic phosphate (DIP) is an important nutrient in the hydrosphere, it is difficult to quantitatively clarify the dynamics of DIP in the hydrosphere using the δ18O value of DIP as a tracer. In this study, we quantified the triple oxygen isotopic compositions (Δ'17O) of DIP relative to VSMOW with the reference line with a slope of 0.528 as an additional tracer to clarify the sources and dynamics of DIP in the hydrosphere. We found significant variation in the Δ'17O values of riverine DIP in urban areas, ranging from -107 × 10-6 to +3 × 10-6, while those of DIP in the effluents from wastewater treatment plants (WWTP) and DIP extracted from the chemical fertilizers showed -56 ± 5 × 10-6 (1SD) and -98 ± 5 × 10-6, respectively. We conclude that both the DIP supplied directly from the artificial loads (the WWTP effluent and chemical fertilizers) showing 17O-depleted Δ'17O values and the DIP turned over via the aquatic biosphere showing 17O-enriched Δ'17O values similar to ambient H2O were the major sources of riverine DIP. High-precision determination of the Δ'17O value of DIP can contribute to quantitative clarification of the dynamics of DIP in the hydrosphere.
Keywords: dissolved inorganic phosphate; dynamics of phosphate in hydrosphere; triple oxygen isotopes; waste water treatment; Δ′17O.