Lead isotopes in the Central Yellow Sea Mud: Evidence of atmospheric deposition and its implication for regional energy consumption shift

Anthropogenic activities have increased lead (Pb) emissions and impacted their spatiotemporal distributions in coastal seas. To quantify the increasing variability of Pb and identify the specific origins and their corresponding magnitudes, Pb and Pb isotopes are investigated in a well-placed sediment core covering the period of 1928-2008 in the Central Yellow Sea Mud (CYSM). The concentration of Pb varied from 27.17 mu g/g to 37.30 mu g/g upwardly along the core, with pronounced anthropogenic disturbance since the late 1960s. The Pb input history of the CYSM experienced five stages according to industrialization levels and Pb contamination, with relative pristine stages from 1928 to 1969 and human activity-impacted stages from 1969 to 2008. The Pb-206/Pb-207 ratio demonstrated an overall decreasing profile while the Pb-208/Pb-206 ratio displayed the reverse trend upwardly along the core, possibly due to the atmospheric delivery of anthropogenic Pb emissions from northern China. Furthermore, Pb-208/Pb-206 vs. Pb-206/Pb-207 shows certain linearity between natural sediment sources and anthropogenic emissions of Pb (atmospheric deposition); thus, atmospheric inputs account for 34e43% of the Pb in the sediment since Pb enrichment using the two-endmember mixing model. Moreover, the steep decrease in Pb-206/Pb-207 and rapid increase in Pb-208/Pb-206 since the 1970s suggest the introduction of leaded gasoline and the increasing proportionate consumption of gasoline relative to total energy consumption. The continuously decreasing Pb-206/Pb-207 ratio and increasing Pb-208/Pb-206 ratio since 2000 are the combined results of coal consumption, nonferrous smelting, and residual Pb contamination from leaded gasoline, which is quite distinctive from cases in North America and Europe. The relatively high Pb-206/Pb-207 and low Pb-208/Pb-206 ratios before 1969 represent the natural Pb isotopic signatures. Hence, Pb input is significantly affected by regional energy consumption and restructuring, and the Pb isotopic ratios may be a potential proxy for the shift in energy consumption. (C) 2020 Elsevier Ltd. All rights reserved.

Automated summary

Human activities have increased lead emissions in coastal seas, which have impacted the spatiotemporal distribution of lead. By studying lead and lead isotopes in a sediment core from the Central Yellow Sea Mud, it was found that lead concentrations varied along the core, with a significant anthropogenic disturbance since the late 1960s. The history of lead input experienced different stages, reflecting industrialization levels and lead contamination. The lead isotopic ratios are influenced by regional energy consumption patterns, with distinctive trends observed since 2000.