ORIGINAL RESEARCH
Sedimentation Rates and Heavy Metal
Concentrations in the Tidal Flats
of North Vietnam
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1
Institute of Marine Environment and Resources, Vietnam Academy of Science and Technology, Hai Phong, Vietnam
2
Nuclear Research Institute, Vietnam Atomic Energy Institute, Da Lat, Lam Dong Province, Vietnam
3
Hanoi University of Science, Vietnam National University, Thanh Xuan, Ha Noi, Vietnam
4
Qingdao Institute of Marine Geology, 62 Fuzhounan Road, Qingdao, China
5
State Key Laboratory of Marine Geology, Tongji University, Shanghai, China
Submission date: 2018-04-06
Final revision date: 2018-10-12
Acceptance date: 2018-10-21
Online publication date: 2019-05-29
Publication date: 2019-07-08
Corresponding author
Nhon Dang Hoai
Institute of Marine Environment and Resources (IMER, VAST), 246 Da Nang Street, 180000 Hai Phong City,, Viet Nam
Pol. J. Environ. Stud. 2019;28(5):3721-3733
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ABSTRACT
Tidal flats in the north of Vietnam from Quang Ninh to Ninh Binh provinces are impacted
by land-ocean interaction processes and human activity. The flats are experiencing erosion in some
parts and accretion in others, as well as the accumulation of pollutants. This study examines core
samples extracted from the region to systematically quantify changes in sedimentary processes and
the accumulation of heavy metals. A total of 11 sediment cores were collected from the tidal flats
and analyzed for 210Pb, 226Ra, grain size, and heavy metal content. Sedimentation rates, according to
the constant rate supply model (CRS), ranged from 0.04 to 15.00 cm/year. There was evidence of
spikes in sedimentation rates for brief episodes; however, the average ranged from 0.14 to 3.04 cm/year.
In the north of the study area, the sedimentation rate was low, then increased to the center and
the south. The concentrations of heavy metals (Cu, Zn, Pb, As, and Cd) in the sediments were found
to increase with time. Additionally, an increasing trend was observed from the north to the south
of the study area. The concentrations of heavy metals Cu, Pb, and As in the sediments from the center
to the south exceeded the ISQG levels.