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Molecular Tracers of Saturated and Polycyclic Aromatic Hydrocarbon Inputs into Central Park Lake, New York City
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文摘
Saturated hydrocarbons (SH) and polycyclic aromatichydrocarbons (PAHs) have been quantified in a sedimentcore obtained from Central Park Lake, New York City.Radionuclides 210Pb and 137Cs were used to assign approximatedates to each individual section in the core. The datingprofile based on 210Pb matches very well with the timeconstraints provided by 137Cs. Radionuclide-deriveddepositional dates are consistent with temporal informationfrom the petroleum-indicator ratio U/R [the ratio ofunresolved complex mixture (UCM) to saturated hydrocarbonsin the aliphatic fraction] and the history of fuel use inthe NYC area. Ratios of 1,7-dimethylphenanthrane (DMP)to 1,7-DMP plus 2,6-DMP [1,7/(1,7 + 2,6)-DMP], retene toretene plus chrysene [Ret/(Ret + Chy)], and fluoranthene tofluoranthene plus pyrene [Fl/(Fl + Py)] provide additionalsource discrimination throughout the core. Results show thatthe ratio U/R is sensitive to petroleum inputs andRet/(Ret + Chy) is responsive to contributions fromsoftwood combustion, whereas both Fl/(Fl + Py) and 1,7/(1,7 + 2,6)-DMP can be used to discriminate among wood,coal, and petroleum combustion sources. Combined useof these ratios suggests that in New York City, woodcombustion dominated 100 years ago, with a shift to coalcombustion occurring from the 1900s to the 1950s.Petroleum use began around the 1920s and has dominatedsince the 1940s.

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