Pb and Cs measurements in the Circum Bohai Sea coastal region: sedimentation rates and implications

WANG Fu1, WANG Hong2, LI Jianfen2, PEI Yandong2, FAN Changfu2, SHANG Zhiwen2, TIAN Lizhu3, SONG Meiyu4, GENG Yan4

Front. Earth Sci. ›› 0

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Front. Earth Sci. ›› DOI: 10.1007/s11707-008-0046-5

Pb and Cs measurements in the Circum Bohai Sea coastal region: sedimentation rates and implications

  • WANG Fu1, WANG Hong2, LI Jianfen2, PEI Yandong2, FAN Changfu2, SHANG Zhiwen2, TIAN Lizhu3, SONG Meiyu4, GENG Yan4
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Abstract

The representative 210Pb and 137Cs age-depth profiles were selected from more than 100 sites in the Circum Bohai Sea (CBS) coastal region to examine the sedimentation rates and associated environmental changes. There are three unique 210Pbexc distribution patterns: 1) ideal-decaying type, representing relatively constant sediment supply and quieter environmental setting; 2) wiggling type, but with approximately equivalent amplitude, representing coarser sediments and associated stronger flow current environment; and 3) episodic-event-influencing type, each representing typhoon storm- influenced depositional environment. Our results also show that there is a lower sedimentation rate (ca. 0.1 cm/a) in the coastal lowlands, a higher sedimentation rate (ca. 0.5–3 cm/a) in the intertidal flat and an intermediate rate of ca. 0.58 cm/a in the subtidal zone near the Huanghua Harbor. The interbedded silt layer occurring in the core sediment reveals lower 210Pb activities, indicating a discontinuous sedimentation mostly due to typhoon events which dwarfs against 210Pb and 137Cs applicability. Overall, the 210Pb and 137Cs measurements of the present study provide physical insight into the evaluation of the coastal-marine ecological environment and associated management.

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WANG Fu, WANG Hong, LI Jianfen, PEI Yandong, FAN Changfu, SHANG Zhiwen, TIAN Lizhu, SONG Meiyu, GENG Yan. Pb and Cs measurements in the Circum Bohai Sea coastal region: sedimentation rates and implications. Front. Earth Sci., https://doi.org/10.1007/s11707-008-0046-5

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