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Radioactivity is a spontaneous disintegration of an unstable nuclide and is a random process, as all the nuclei in the sample do not decay simultaneously. The number of disintegrations per unit time is called the activity (A), which is directly proportional to the number of nuclei in the sample. The decay constant (λ) is an average probability of decay per nucleus in unit time.
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The average temperature of Earth is the subject of much current discussion. Earth is in radiative contact with both the Sun and dark space; it receives almost all its energy from the radiation of the Sun and reflects some of it into outer space. Dark space is very cold, about 3 K, so Earth radiates energy into it. For instance, heat transfer occurs from soil and grasses, the rate of which can be so rapid that frost can occur on clear summer evenings, even in warm latitudes.
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Editorial remarks on radioecology topics in RPD.

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Summary
This summary is machine-generated.

This guide helps authors and reviewers improve radioecology research publication quality for Radiation Protection Dosimetry. It offers practical tips for clear topic presentation and manuscript review in this specialized scientific field.

Area of Science:

  • Radioecology
  • Radiation Protection Dosimetry

Background:

  • Authors need guidance on presenting radioecology topics for publication.
  • Reviewers require support for manuscript evaluation in this field.

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