Mineral Compositions and Grain Sizes of Beach Sediments in Northern Vietnam

Abstract: Forty three surface samples from the beaches of northern Vietnam from Quang Ninh to Thua Thien Hue were sampled in July 2024 for grain size and mineralogy analysis. We aim to assess the dynamic conditions and mineral origins of beach sediments. Three types of sediments were distributed on the beach: coarse sand, medium sand, and fine sand. Coarse sand was well sorted and symmetrically skewed. Medium sand was very well to moderately sorted and fine to coarsely skewed. Fine sand was very well to moderately well sorted and fine to coarsely skewed. Mineral contents including quartz, illite, feldspar, kaolinite, goethite, chlorite, calcite, amphibole, and gibbsite were 80.3%, 5.2%, 3.1%, 2.3%, 2.0%, 1.8%, 1.1%, 0.9%, and 0.1%, respectively. The mineral origins were from the mainland, characterized by quartz, feldspar, and amphibole; minerals as illite, chlorite, kaolinite, and goethite were products from chemical weathering of feldspar and amphibole; calcite from biological shells. Beach sediments were divided into three groups, characterized by particle size and quartz (lowest in group 1 and highest in group 3).

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Publication Details

Journal
VNU Journal of Science Earth and Environmental Sciences
Published
2025-05-17
DOI
https://doi.org/10.25073/2588-1094/vnuees.5293
Primary Topic
Geochemistry and Elemental Analysis
Type
article
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article

Mineral Compositions and Grain Sizes of Beach Sediments in Northern Vietnam

Lai Thi Bich Thuy, Bừi Thi Thanh Loan, Nguyen Van Nam, Hoang Thi Chien et al.
VNU Journal of Science Earth and Environmental Sciences
Geochemistry and Elemental Analysis
article

Mineral Compositions and Grain Sizes of Beach Sediments in Northern Vietnam

Lai Thi Bich Thuy, Bừi Thi Thanh Loan, Nguyen Van Nam, Hoang Thi Chien, Đặng Hoài Nhơn, Nguyen Thi Mai Luu, Nguyen Dac Ve
article en

Abstract

Abstract: Forty three surface samples from the beaches of northern Vietnam from Quang Ninh to Thua Thien Hue were sampled in July 2024 for grain size and mineralogy analysis. We aim to assess the dynamic conditions and mineral origins of beach sediments. Three types of sediments were distributed on the beach: coarse sand, medium sand, and fine sand. Coarse sand was well sorted and symmetrically skewed. Medium sand was very well to moderately sorted and fine to coarsely skewed. Fine sand was very well to moderately well sorted and fine to coarsely skewed. Mineral contents including quartz, illite, feldspar, kaolinite, goethite, chlorite, calcite, amphibole, and gibbsite were 80.3%, 5.2%, 3.1%, 2.3%, 2.0%, 1.8%, 1.1%, 0.9%, and 0.1%, respectively. The mineral origins were from the mainland, characterized by quartz, feldspar, and amphibole; minerals as illite, chlorite, kaolinite, and goethite were products from chemical weathering of feldspar and amphibole; calcite from biological shells. Beach sediments were divided into three groups, characterized by particle size and quartz (lowest in group 1 and highest in group 3).

VNU Journal of Science Earth and Environmental Sciences
Nhà hàng bệnh viện Mỹ Đức (VN)
Openalex Percentile: Top 90%
Geochemistry and Elemental Analysis
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