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Gamma-ray beam attenuation to assess the influence of soil texture on structure deformation

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Języki publikacji
EN
Abstrakty
EN
Gamma-ray beam attenuation is a non-invasive technique that permits analysis of soil porosity without disturbing the region of interest of the core sample. The technique has as additional advantage to allow measurements point by point on a millimetric scale in contrast to other methodologies that are invasive and analyze the soil properties in the bulk sample volume. Soil porosity can be used as an important parameter to quantify soil structural damages, which affect soil aeration, water movement and retention. In this study, porosities of three soils different in texture were measured at various positions in order to analyze the impact of the sampling procedure on the structure of each particular soil texture. The gamma-ray attenuation system consisted of an 241Am radioactive source having an activity of 3.7 GBq, collimated with cylindrical lead collimators of 2 mm diameter. The results obtained show the presence of dense regions near the edges of samples and that different soil textures can suffer distinct deformations at sampling.
Czasopismo
Rocznik
Strony
125--129
Opis fizyczny
Bibliogr. 17 poz., rys.
Twórcy
autor
autor
autor
  • Center for Nuclear Energy in Agriculture, The University of Săo Paulo, C. P. 96, C. E. P. 13.400-970, Piracicaba, SP, Brazil, Tel.: +55 19 3429 4600 ext. 4712, Fax: +55 19 3429 4610,, lfpires@cena.usp.br
Bibliografia
  • 1. Appoloni CR, Rios EA (1994) Mass attenuation coefficients of Brazilian soils in the range 10−1450 KeV.Appl Radiat Isot 45:287−291
  • 2. Coppola M, Reiniger P (1974) Influence of the chemical composition on the gamma-ray attenuation by soils. Soil Sci 117:331−335
  • 3. Ferraz ESB, Mansell RS (1979) Determining water content and bulk density of soil by gamma-ray attenuation methods. IFAS, Florida, pp 1−51
  • 4. Flint AL, Flint LE (2002) The solid phase: Particle density. In: Dane JH, Topp GC (eds) Methods of soil analysis. Part 4: Physical methods. Soil Sci Soc Am Book Series, vol. 5. Madison, pp 229−240
  • 5. Grohmann F (1960) Distribuição do tamanho de poros em tręs tipos de solos do Estado de São Paulo. Bragantia 19:319−328
  • 6.Helsel DR, Hirsch RM (eds) (1992) Statistical methods in water resources. Elsevier, New York
  • 7.7. Hillel D (ed) (1982) Introduction to soil physics.Academic Press, San Diego
  • 8. Jenkins R, Gould RW, Gedcke D (eds) (1981)Quantitative X-ray spectrometry. Marcel Dekker Inc.,New York
  • 9. Kutílek M, Nielsen DR (eds) (1994) Soil hydrology.Catena Verlag, Reiskirchen
  • 10. Oliveira JCM, Appoloni CR, Coimbra MM et al. (1998)Soil structure evaluated by gamma-ray attenuation. Soil Till Res 48:127−133
  • 11. Pagliai M, Rousseva S, Vignozzi N et al. (1999) Tillage impact on soil quality. I. Soil porosity and related physical properties. Ital J Agron 2:11−20
  • 12. Phogat VK, Aylmore LAG (1989) Evaluation of soil structure by using computer-assisted tomography. Aust J Soil Res 27:313−323
  • 13. Pires LF, Bacchi OOS, Reichardt K (2004) Damage to soil physical properties caused by soil sampler devices as assessed by gamma-ray computed tomography. Aust J Soil Res 42:857−863
  • 14. Pires LF, Bacchi OOS, Reichardt K (2005) Gamma-ray computed tomography to evaluate wetting/drying soil structure changes. Nucl Instrum Meth B 229:443−456
  • 15. Pottker WE, Appoloni CR (2001) Measurement of amorphous materials porosity by gamma-ray transmission methodology. Radiat Phys Chem 61:535−536
  • 16. Vanden Bygaart AJ, Protz R (1999) The representative elementary area (REA) in studies of quantitative soil micromorphology. Geoderma 89:333−346
  • 17. Vomocil JA (1954) In situ measurement of bulk density of soil by gamma absorption technique. Soil Sci 77:341−342
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BUJ6-0004-0018
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