Estimation of soil characteristics based on the depth distributions of 238U, 232Th, 226Ra, 40K activity concentrations using laboratory HPGe gamma spectrometry

Author:

Loan Truong Thi Hong,Ba Vu Ngoc,Đao Nguyen Quang,Anh Nguyen Ngoc,Man Mai Thanh,Thy Truong Huu Ngan,Hong Huynh Thi Yen,Van Thang Nguyen,Hoang Truong Minh

Publisher

Springer Science and Business Media LLC

Subject

Health, Toxicology and Mutagenesis,Public Health, Environmental and Occupational Health,Spectroscopy,Pollution,Radiology Nuclear Medicine and imaging,Nuclear Energy and Engineering,Analytical Chemistry

Reference27 articles.

1. Constable JL, Hubbard FH (1981) U, Th, and K distribution in a differentiated charnockite—granite intrusion and associated rocks from SW Sweden. Mineral Mag 44:409–415

2. Uddin F (2008) Clays, nanoclays, and montmorillonite minerals. Metall Mater Trans A 39:2804–2814

3. Al-Ani T, Sarapää O (2008) Clay and clay mineralogy. Physical–chemical properties and industrial uses. Geological Survey of Finland, GTK Publisher, pp 3–4

4. Hesselbo SP (1996) Spectral gamma-ray logs in relation to clay mineralogy and sequence stratigraphy, Cenozoic of the Atlantic margin, offshore New Jersey. In: Proceedings of the Ocean Drilling Program, scientific results, vol 150, pp 411–422

5. Rahman AYAA (2013) Clay Lithofacies and depositional environment, as deduced from natural gamma-ray spectroscopy and petrographical data of the Abu Roash “E” member, GPT field, Western Desert, Egypt. Middle East J Sci Res 16(8):1027–1036

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