The $S.I.$ unit of radioactivity is
Roentgen
Rutherford
Curie
Becqueral
(d) The $SI$ unit of radioactivity is becquerel $(Bq).$
$1 \mathrm{Bq}=1 \mathrm{dps}=1 \mu r d$
$1 c=3.7 \times 10^{10} B q$
The rate of disintegration of a fixed quantity of a radioactive element can be increased by
$3.8$ days is the half-life period of a sample. After how many days, the sample will become $\frac{{1}}{{8}} \, th$ of the original substance
The normal activity of living carbon-containing matter is found to be about $15$ decays per minute for every gram of carbon. This activity arises from the small proportion of radioactive $_{6}^{14} C$ present with the stable carbon isotope $_{6}^{12} C$. When the organism is dead, its interaction with the atmosphere (which maintains the above equilibrium activity) ceases and its activity begins to drop. From the known half-life ($5730$ years) of $_{6}^{14} C ,$ and the measured activity, the age of the specimen can be approximately estimated. This is the principle of $_{6}^{14} C$ dating used in archaeology. Suppose a specimen from Mohenjodaro gives an activity of $9$ decays per minute per gram of carbon. Estimate the approximate age (in $years$) of the Indus-Valley civilisation
$37$ Rutherford equals
A element used for radioactive carbon dating for more than $5600$ years is
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