Some Sedimentary Environment Characteristics in the Mong Cai Coastal Area, Quang Ninh Province, Vietnam

B. Loan, Nguyen Huy Hoang, Nguyen Mai Luu, Le Van Nam, Pham Tien Dung, Nguyen Dac Ve, Le Nhu Sieu, Dang Hoai Nhon, Tran Duc Thanh
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Abstract

The sedimentary environment characteristics in Mong Cai coastal area were assessed through pH, Eh, grain sizes, 226Ra, 210Pb, S‰, DO parameters. Mong Cai coastal area is mostly influenced by Ka Long river system that makes changes in the salinity, pH of water, pH and Eh of sediment, grain sizes, and sedimentation rates in the coastal area. There were six sediment types in the coastal area which were coarse sand, medium sand, fine sand, very fine sand, very coarse silt, and coarse silt. Fine sand was common in surface sediments; very fine sand was dominant in sediment core at Ka Long river mount; coarse silt and very coarse silt were common in sediment core at Mui Ngoc. The average sedimentation rate at the Ka Long river mouth (0.72 cm/year) was higher than that at the Mui Ngoc (0.27 cm/year). The sedimentary environment was divided into 3 groups, the first group was marine characteristics higher than the terrigenous characteristic, the second group was terrigenous characteristics higher than marine characteristics, and the third group was marine characteristics. In sediment cores showed 3 stages. In stage 1, distribution fine sand, very fine sand, and very coarse silt, from 52 to 80 cm at the Ka Long river mouth and from 40 to 52 cm at the Mui Ngoc. In stage 2, distribution of very coarse silt, coarse silt, from 38 to 52 cm (1947 - 1877) at Ka Long river mouth with sedimentation rate from 0.08 to 0.31 cm/year, at the Mui Ngoc from 12 to 40 cm (1944 (12 -14 cm)) with sedimentation rate of 0.09 cm/year. In stage 3, distribution very coarse silt, very fine sand, fine sand, from 0 to 38 cm (1919 - 1961) at the Ka Long river mouth with sedimentation rate of 0.34 - 1.62 cm/year, at the Mui Ngoc from 0 to 12 cm (2019 – 1966) with sedimentation rate of 0.07 - 0.51 cm/year.  
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越南广宁省芒彩沿海地区沉积环境特征
通过pH、Eh、粒度、226Ra、210Pb、S‰、DO等参数评价了蒙菜滨海地区沉积环境特征。旺菜海岸带主要受卡龙水系的影响,卡龙水系改变了旺菜海岸带的盐度、水体pH、沉积物pH和Eh、粒度和沉积速率。海岸带沉积物类型主要有粗沙、中沙、细沙、极细沙、极粗粉砂和粗粉砂6种。细砂在表层沉积物中较为常见;卡龙河山沉积物岩心以极细砂为主;梅玉沉积物岩心以粗粉砂和极粗粉砂为主。嘉龙河口的平均沉积速率(0.72 cm/年)高于梅玉溪(0.27 cm/年)。沉积环境分为3组,第一组为海相特征高于陆源特征,第二组为陆源特征高于海相特征,第三组为海相特征。沉积物岩心分为3个阶段。第1阶段分布细砂、极细砂和极粗粉砂,嘉龙河口为52 ~ 80 cm,梅牛为40 ~ 52 cm。在第2阶段,极粗粉砂分布,粗粉砂在嘉龙河口分布38 ~ 52 cm(1947 ~ 1877),沉积速率为0.08 ~ 0.31 cm/年,在梅牛河口分布12 ~ 40 cm (1944 (12 ~ 14 cm)),沉积速率为0.09 cm/年。第三阶段,嘉龙河口分布极粗粉砂、极细砂、细砂,沉积速率为0 ~ 38 cm(1919 ~ 1961),沉积速率为0.34 ~ 1.62 cm/年;梅牛河口分布0 ~ 12 cm(2019 ~ 1966),沉积速率为0.07 ~ 0.51 cm/年。
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