“…Any residual APnEOs discharged to an aerobic environment degrade with a half-life of a few days, forming AP 2 EO and APECs, which are subsequently mineralised to CO 2 with a further half-life of a few weeks (Ekelund, Granmo, Magnusson, Berggren, & Bergmann, 1993). However, APs and short-chain APEOs have moderately high log K ow values, slow anaerobic degradation rates and therefore accumulate in sediments (Hale et al, 2000). A removal half-life in excess of 50 years (Shang, Macdonald, & Ikonomou, 1999) means that substantial inventories can be found in sediments near STW outfalls, even decades after their discharge has ceased (Hale et al, 2000).…”