Variability of 40K isotopic composition in forest soils under different environmental conditions

Fujiyoshi, Ryoko; Takekoshi, Naoki; Okamoto, Kazumasa

doi:10.1007/s10967-013-2797-z

Cited by 5 publications

(3 citation statements)

References 19 publications

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“…Determined soil 40 K/K t ratios were between 0.009 and 0.013% in the study of Fujiyoshi et al. (). For the relation pH‐ 40 K/K t ‐ratio, correlation coefficients of r = 0.9 were determined.…”

Section: Fundamentalsmentioning

confidence: 98%

“…Equisetum hyemale L. plants in Sapporo showed significantly reduced 40 K/K t ratios of 0.0042 ( 0.0001)%, its litter even showed ratios of 0.0059 ( 0.0002)%, leading to the assumption of 40 K discrimination by certain plants. Determined soil 40 K/K t ratios were between 0.009 and 0.013% in the study of Fujiyoshi et al (2014). For the relation pH-40 K/K t -ratio, correlation coefficients of r = 0.9 were determined.…”

Section: Change Of Natural Isotope Ratiosmentioning

confidence: 99%

“…This has, however, to be tested in future studies. Fujiyoshi et al (2014) screened the 40 K/K t ratio in forest soils in Japan and Slovenia comparing gamma-ray spectrometry and x-ray fluorescence data. Potassium-40/K t values varied with depth in both carbonaceous and siliceous soils.…”

Section: Change Of Natural Isotope Ratiosmentioning

confidence: 99%

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Gamma‐ray spectrometry as versatile tool in soil science: A critical review

Reinhardt

Herrmann

2018

J. Plant Nutr. Soil Sci.

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Gamma‐ray spectrometry is an established method in geo‐sciences. This article gives an overview on fundamentals of gamma‐ray spectrometry that are relevant to soil science including basic technical aspects, and discusses influencing factors, inconsistencies, limitations, and open questions related to the method. Gamma‐ray spectrometry relies on counting gamma quanta during radionuclide decay of 40K, 238U, and 232Th, but secular equilibrium for the decay series of U and Th must be given as decays of their respective daughter radionuclides are used for determination. Secular equilibrium for U and Th decay series, however, is not always given leading to, e.g., anomalies in U concentration measurements. For soil science, gamma‐ray spectrometry is of specific value since it does not only detect a signal from the landscape surface, but integrates information over a certain volume. Besides, different spatial scales can be covered using either ground‐based or airborne sensing techniques. Together with other remote sensing methods, gamma signatures can provide completive information for understanding land forming processes and soil properties distributions. At first, signals depend on bedrock composition. The signals are in second order altered by weathering processes leading to more interpretation opportunities and challenges. Due to their physico‐chemical properties, radionuclides behave differently in soils and their properties can be distinguished via the resulting signatures. Hence, gamma signatures of soils are specific for local environments. Processes like soil erosion can superimpose gamma signals from in situ weathering. Soil mappings, available K and texture determination, or peat and soil erosion mapping are possible applications being discussed in this review.

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Section: Fundamentalsmentioning

confidence: 98%

Section: Change Of Natural Isotope Ratiosmentioning

confidence: 99%