Abstract

Polychlorinated naphthalene (PCN) concentrations and fluxes were measured in a dated core from the profundal sediments of Esthwaite Water, a seasonally anoxic semirural lake in northwest England. The vertical profile shows that the ΣPCN flux remained fairly constant at 0.4−0.6 μg m-2 y-1 from depth until the early 1940s, escalating sharply thereafter to a subsurface maximum of ∼12 μg m-2 y-1 in the late 1950s to mid-1960s followed by a 4-fold decrease to the sediment−water interface. The ΣPCN maximum predates the ΣPCB maximum by ∼20 years, broadly consistent with the time lapse in the production and wide use of both compounds. Furthermore, there was a secondary peak in the profiles of both compound classes corresponding to the period of maximum input of the other compound class. This may be a result of PCNs present as impurities in the manufacture of PCBs and vice versa. The vertical profiles of the individual PCN homologue groups closely followed that of the ΣPCN profile with no overall change in the mas...

Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.