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- W2187494688 abstract "Negative muons can activate nuclei of almost all elements after thermalization, capture and reaction by weak interaction. While muons can penetrate some 100 m of solid rock or soil (low-energy ones a few m limited by decay), γ radiation from the secondary nuclides (T1/2 between 10 s and some days) has a range of about 50 cm. Hence a muon beam passed parallel to some soil surface (horizontally or next to a borehole or well) will produce a linear trace of secondarily formed radionuclides which reveal their presence by γ radiation escaping to the nearby surface while the long range of the muon beam permits to analyze surface regions of an area of some 200 m diameter from a single, fixed point of muon production and injection. Reactions among µ -" @default.
- W2187494688 created "2016-06-24" @default.
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- W2187494688 date "2013-01-01" @default.
- W2187494688 modified "2023-09-27" @default.
- W2187494688 title "Muon beams for environmental analysis: determining both element contents and subsoil redox conditions over soccer-playground-size areas" @default.
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