2023 年 57 巻 4 号 p. 279-290
Phosphorus is an essential element for all living organisms and important resource for human society hence, understanding phosphorus cycling is crucial. Although phosphorus possesses only one stable isotope, it exists in the environment as phosphate (PO4), and its oxygen isotope ratio (δ18OPO4) can be used as a tracer. The use of δ18OPO4 has been increasing since the 2000s, contributing toward better understanding of the biogeochemical processes of phosphorus. However, the use of δ18OPO4 has been limited owing to methodological difficulties involved in its sampling and pretreatment. In current studies, δ18OPO4 values are analyzed by converting the PO4 in a sample to silver phosphate (Ag3PO4). The removal of impurities from samples (purification) to produce pure Ag3PO4 is essential for accurate δ18OPO4 measurements. The conventional purification methods can be classified into two main categories, both of which comprise a combination of PO4 precipitation formation and resin treatment. Recently, a solid-phase extraction method has been developed as a new purification method that uses zirconium, which causes specific adsorption with PO4. Zirconium has also been applied to passive sampling. This review presents the basic principles of δ18OPO4 and its applications, focusing on the description of the analytical methods.