Bathed in Radiation
http://edu-observatory.org/olli/Rad/index.html



   RADIATION
  


   BACKGROUND RADIATION
  
                    0.34 µSv/hr equals 2.98 mSv/yr

   RADIATION SOURCES
  

    Potassium-40 (K-40) is a naturally occurring radioactive
    isotope of potassium with a half-life of approximately 1.25
    billion years. It undergoes decay via beta emission and
    electron capture, producing argon-40 and calcium-40. As one
    of the primary sources of natural radioactivity, K-40
    contributes to background radiation and is present in trace
    amounts in all potassium-containing materials.
    
    Potassium-40 is found in nature as a small fraction of
    natural potassium, present in soils, rocks, and oceans. It
    is also found in food sources rich in potassium, such as
    bananas, potatoes, and certain nuts, making it an integral
    part of the human diet and environment. Despite its
    radioactivity, the levels of K-40 in natural settings are
    low and pose no significant health risk.
    

   RADIATION SOURCES IN THE CONTEXT OF A WARMING PLANET
  
  

    Radon-222 (Rn-222) occurs naturally - part of the uranium-238 
    decay chain. It is found in soil, rocks, and groundwater in
    areas with high uranium or radium content. It can
    accumulate in enclosed spaces like basements and buildings,
    where it is a significant contributor to natural background
    radiation. High levels of radon in homes and workplaces are
    considered a health hazard due to its radioactive decay
    products, which can attach to dust particles and be
    inhaled. Monitoring and mitigation measures are often
    implemented in regions with elevated radon levels to
    minimize health risks.


   IONIZING RADIATION
  

   MRI vs CT RADIATION
  









  


   SOLAR RADIATION
  


  



   SOLAR WIND
  

   Solar Flare
  

   GEOMAGNETIC STORMS
  

   GEOMAGNETIC STORMS
  
  











   RADIACODE 103G GAMMA SCINTILLATOR  REVIEW    
  
   Gadolinium Aluminum Gallium Garnet (GAGG:Ce)

   RADIACODE LIBRARY  REVIEW 
  

   RADIACODE 103G DOSE RATE CALIBRATION  MORE ABOUT DOSE 
  

   DOSE RATE CALIBRATION SUMMARY  MORE ABOUT DOSE 
  






   DIURNAL RADIATION PATTERNS FROM RADON
  
  






   GAMMA RADIATION FROM LIGHTNING
  






   AMERICIUM-241 (USED IN MOST SMOKE DETECTORS)
  
  
     
    Americium-241 is an alpha particle emitter, often used
    in smoke detectors. The alpha particles do not escape their
    containers. Note, however, that any nucleus undergoing
    radioactive decay also emits weak gamma and x-ray photons
    and is often detectable with gamma ray scintillators.

    So should we be concerned about this radiation source? Not
    really. The weak gamma and x-ray emissions fall off as the
    square of the distance so they are literally undetectable
    several feet away. At just one centimeter from the source
    the Radiacode 103G measured a dose rate of 0.44 µSv/h which 
    is slightly higher than the US average background level of
    0.34 µSv/hr. No concern.


  
 





     
     
     
    
 
    sam.wormley@icloud.com