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Using 7 Be and 137 Cs for Assessing the Land Stability of Alexandria Region, Egypt

Author

Listed:
  • Ibrahim H. Saleh

    (Department of Environmental Studies and Research, Institute of Graduate Studies and Research, Alexandria University, Alexandria 21526, Egypt)

  • Nessma M. Ibrahim

    (Department of Environmental Studies and Research, Institute of Graduate Studies and Research, Alexandria University, Alexandria 21526, Egypt)

  • Mahmoud Adel Hassaan

    (Department of Environmental Studies and Research, Institute of Graduate Studies and Research, Alexandria University, Alexandria 21526, Egypt)

  • Zekry F. Ghatass

    (Department of Environmental Studies and Research, Institute of Graduate Studies and Research, Alexandria University, Alexandria 21526, Egypt)

  • Jack Arayro

    (College of Engineering and Technology, American University of the Middle East, Egaila 54200, Kuwait)

  • Rabih Mezher

    (College of Engineering and Technology, American University of the Middle East, Egaila 54200, Kuwait)

  • Mohmad Ibosayyed

    (Renewable Energy and Environmental Technology Center, University of Tabuk, Tabuk 47913, Saudi Arabia)

  • Mohamed Elsafi

    (Physics Department, Faculty of Science, Alexandria University, Alexandria 21511, Egypt)

Abstract

This paper presents an assessment of land stability using fallout environmental radioisotopes 7 Be and 137 Cs. The measurement of both isotopes was carried out in samples of soil collected from twenty-five sites covering the studied region. At each site, the samples were taken from five consecutive vertical depth levels to show the vertical displacement or compactness of the soil column. The collected samples were carefully transferred for radioactivity measurement at Alexandria University’s Institute of Graduate Studies and Research. A high-resolution gamma-ray spectrometer utilizing high-purity germanium was employed for the measurements. Surface distribution of the radionuclides levels was used to show the studied lands’ stability over the short- and long-term based on the used radionuclides’ nuclear half-life. For short-term (months) stability, 7 Be (half-life: 35.5 days) levels showed that about 73% of the area is very low in stability, while the areas that recorded low, moderate, and high stability are at 18%, 4%, and 5%, respectively. For long-term (years) stability, 137 Cs (half-life: 30 years) levels showed that about 80% of the areas are very low in stability, while the remaining areas, predicted as 12.8%, 5.6%, and 1.6%, are low, moderate, and high stability, respectively. It is clear that the eastern side of Alexandria is suffering from soil erosion and subsidence; on the other hand, the western side is more stable. Consequently, due to the origin of the soil, the nature of soil geological formations, and the environmental prevailing conditions, Alexandria is found to be more vulnerable to the consequences of sea-level rise and climate change. Therefore, adequate strategic management, including mitigation measures and adaptation, should be planned and implemented.

Suggested Citation

  • Ibrahim H. Saleh & Nessma M. Ibrahim & Mahmoud Adel Hassaan & Zekry F. Ghatass & Jack Arayro & Rabih Mezher & Mohmad Ibosayyed & Mohamed Elsafi, 2024. "Using 7 Be and 137 Cs for Assessing the Land Stability of Alexandria Region, Egypt," Sustainability, MDPI, vol. 16(4), pages 1-15, February.
  • Handle: RePEc:gam:jsusta:v:16:y:2024:i:4:p:1692-:d:1341477
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