2016
DOI: 10.1002/xrs.2689
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Importance of photo atomic cross section for studying physical properties of different types of soil

Abstract: The objective of this work is focused on development of a classification tool for identifying soil texture based on photon attenuation interaction atomic cross-section data. The total mass attenuation coefficients (μ/ρ) and the atomic cross sections (σ a ) of soils with different textures have been calculated for total photon interactions in a wide energy range (1 keV to 100 GeV). The values of these parameters have been found to change with soil composition in low energies (1-100 keV), whereas their behavior … Show more

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Cited by 7 publications
(4 citation statements)
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“…This property is closely related to the soil composition and the contribution of its fractions (Hillel, 2004;Lal and Shukla, 2004). The wide distribution of textures and particle densities analyzed highlights the importance of different particle sizes for radiation attenuation (Medhat and Pires, 2016;Ferreira et al, 2018). According to the USDA classification system, the sand fraction contains particles ranging in diameter from 2,000 to 50 μm, the silt fraction from 50 to 2 μm, and the clay fraction consists of <2 μm particles (Hillel, 2004).…”
Section: Resultsmentioning
confidence: 99%
See 1 more Smart Citation
“…This property is closely related to the soil composition and the contribution of its fractions (Hillel, 2004;Lal and Shukla, 2004). The wide distribution of textures and particle densities analyzed highlights the importance of different particle sizes for radiation attenuation (Medhat and Pires, 2016;Ferreira et al, 2018). According to the USDA classification system, the sand fraction contains particles ranging in diameter from 2,000 to 50 μm, the silt fraction from 50 to 2 μm, and the clay fraction consists of <2 μm particles (Hillel, 2004).…”
Section: Resultsmentioning
confidence: 99%
“…Radiation interaction properties such as mass attenuation coefficient (μ), atomic (σ a ) and electronic (σ e ) cross-sections, effective atomic number (Z eff ), and electron density (N el ) can be determined when the composition and density of the materials are known (Han and Demir, 2009;Medhat and Pires, 2016;Ferreira et al, 2018). Many types of analyses can be conducted based on these parameters and XRF measurements, such as variations of the interaction parameters with photon energy or the contribution of processes such as the photoelectric effect, coherent and incoherent scatterings, and pair production to the mass attenuation coefficient (Camargo et al, 2021).…”
Section: Introductionmentioning
confidence: 99%
“…In this energy band, the incoherent scattering is the dominant effect of the radiation attenuation. For the high energy region (>10 MeV), μ/ρ presented a slight increase influenced by the pair production, whose cross-section shows dependency with Z 2 [ 38 , 39 ].…”
Section: Discussionmentioning
confidence: 99%
“…Elements of high atomic number such as Fe 2 O 3 and TiO 2 greatly influenced the attenuation of low photon energies (Camargo et al, 2021). Following the same idea, Medhat and Pires (2016) published another study with a detailed analysis of the photon atomic cross-section (σ a ) of soils of different types. The development of a tool to classify soils with distinct textures based on the photon atomic cross-section (Equation 16) was proposed (Figure 4).…”
Section: Gamma-ray Attenuation Methodsmentioning
confidence: 99%