Affiliations 

  • 1 Department of Civil & Structural Engineering, Faculty of Engineering & Built Environment, Universiti Kebangsaan Malaysia, 43600 UKM Bangi, Malaysia. Electronic address: hanna@ukm.edu.my
  • 2 Department of Civil & Structural Engineering, Faculty of Engineering & Built Environment, Universiti Kebangsaan Malaysia, 43600 UKM Bangi, Malaysia
  • 3 Department of Civil & Structural Engineering, Faculty of Engineering & Built Environment, Universiti Kebangsaan Malaysia, 43600 UKM Bangi, Malaysia; Earth Observation Centre, Institute of Climate Change, Universiti Kebangsaan Malaysia, 43600 UKM Bangi, Selangor, Malaysia. Electronic address: knam@ukm.edu.my
  • 4 National Hydraulic Research Institute Malaysia, Jalan Putra Permai, Selangor, 43300 Seri Kembangan, Malaysia. Electronic address: yannie@nahrim.gov.my
  • 5 National Hydraulic Research Institute Malaysia, Jalan Putra Permai, Selangor, 43300 Seri Kembangan, Malaysia. Electronic address: wanhafiz@nahrim.gov.my
Sci Total Environ, 2017 Nov 15;598:525-537.
PMID: 28454026 DOI: 10.1016/j.scitotenv.2017.04.093

Abstract

This study investigates the textural characteristics of sediments collected at eroded and deposited areas of highly severed eroded coastline of Batu Pahat, Malaysia. Samples were taken from systematically selected 23 locations along the 67km stretch of coastline and are extended to the fluvial sediments of the main river of Batu Pahat. Grain size distribution analysis was conducted to identify its textural characteristics and associated sedimentary transport behaviours. Sediments obtained along the coastline were fine-grained material with averaged mean size of 7.25 ϕ, poorly sorted, positively skewed and has wide distributions. Samples from eroded and deposition regions displayed no distinctive characteristics and exhibited similar profiles. The high energy condition transported the sediments as suspension, mostly as pelagic and the sediments were deposited as shallow marine and agitated deposits. The fluvial sediments of up to 3km into the river have particularly similar profile of textural characteristics with the neighbouring marine sediments from the river mouth. Profiles were similar with marine sediments about 3km opposite the main current and can go up to 10km along the current of Malacca Straits.

* Title and MeSH Headings from MEDLINE®/PubMed®, a database of the U.S. National Library of Medicine.