Textural characteristics of sediments and the distribution of heavy minerals in the coastal region between Sipasurabil and Bramhagiri, east coast of Odisha, India

Authors

  • R B Rao Formerly at CSIR - Institute of Minerals & Materials Technology, Bhubaneswar, Odisha – 751 012, India
  • B Mishra Formerly at IREL (India) Limited, Chhatrapur, Odisha – 761 020, India
  • S Rourtray Centurion University of Technology and Management, Bhubaneswar, Odisha – 752 050, India
  • R Swain C V Raman Global University, Bhubaneswar, Odisha – 752 054, India
  • S S Srikant Department of Electronics and Communication Engineering, SRM Institute of Science and Technology, Delhi-NCR Campus, Modinagar, Ghaziabad, Uttar Pradesh – 201 204, India
  • D Singh Formerly at IREL (India) Limited, Chhatrapur, Odisha – 761 020, India

DOI:

https://doi.org/10.56042/ijms.v54i10.18831

Keywords:

Graphical mean size, Kurtosis, Sedimentary, Skewness, Sorting, Texture

Abstract

This study focuses on the textural characteristics of beach sand, specifically examining the lighter mineral group quartz, and the total heavy minerals in the coastal deposits from Sipasurubili to Brahmagiri in Odisha. The research area spans 3 kilometres along the coast and 1 kilometre in width. Samples were collected during three different seasons from the shoreline, backshore, frontal dune, central dune, and back dune. These samples were analysed using several statistical parameters, including graphical mean grain size, standard deviation, skewness, and kurtosis, to assess the sedimentary characteristics. Findings indicate that the graphical analysis of sediment grain sizes from Sipasurubili to the Brahmagiri coast, specifically from shore to back dune sand samples collected during autumn, summer, and winter, suggests that the graphical mean size for beach sand and quartz is nearly equivalent. In contrast, the observations regarding heavy minerals differ. The heavy minerals observed are ilmenite, rutile, sillimanite, garnet, zircon and monazite. Skewness analysis demonstrates that quartz particles exhibit a highly skewed distribution across all seasons of quartz and heavy mineral concentration. Furthermore, the particle distribution of heavy minerals shows similar skewness in both autumn and summer, in contrast to the distribution observed during the winter season across various concentration zones. It has been noted that quartz displays a mesokurtic distribution, while total heavy minerals exhibit both mesokurtic and platykurtic characteristics, particularly during the summer season.

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Published

2026-09-08

Issue

Section

Research Articles

How to Cite

Textural characteristics of sediments and the distribution of heavy minerals in the coastal region between Sipasurabil and Bramhagiri, east coast of Odisha, India. (2026). Indian Journal of Geo-Marine Sciences (IJMS), 54(10), 535-552. https://doi.org/10.56042/ijms.v54i10.18831

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