<span>A small proportion of helium in the crust is helium that was trapped in the Earth when the Earth formed and has not yet escaped. Most helium on Earth, however, forms as a result of alpha decay of uranium and thorium. The emitted alpha particles, once they grab a couple of stray electrons, become helium atoms and can accumulate in gas reservoirs along with things such as methane.</span>
<u>Answer:</u> The chemical equation is written below.
<u>Explanation:</u>
Transmutation is defined as the process in which one chemical isotope gets converted to another chemical isotope. The number of protons or neutrons in the isotope gets changed.
The chemical equation for the reaction of curium-242 nucleus with alpha particle (helium nucleus) follows:
![_{96}^{242}\textrm{Cm}+_4^2\textrm{He}\rightarrow _{98}^{245}\textrm{Cf}+_0^1\textrm{n}](https://tex.z-dn.net/?f=_%7B96%7D%5E%7B242%7D%5Ctextrm%7BCm%7D%2B_4%5E2%5Ctextrm%7BHe%7D%5Crightarrow%20_%7B98%7D%5E%7B245%7D%5Ctextrm%7BCf%7D%2B_0%5E1%5Ctextrm%7Bn%7D)
The product formed in the nuclear reaction are californium-245 nucleus and a neutron particle.
It's lone a little distinction (103 degrees versus 104 degrees in water), and I trust the standard rationalization is that since F is more electronegative than H, the electrons in the O-F bond invest more energy far from the O (and near the F) than the electrons in the O-H bond. That moves the powerful focal point of the unpleasant constrain between the bonding sets far from the O, and thus far from each other. So the shock between the bonding sets is marginally less, while the repugnance between the solitary matches on the O is the same - the outcome is the edge between the bonds is somewhat less.
Spontaneous at low temperatures.
Answer:
True
Explanation:
if there was nothing to avoid of objects pulling towards one another many results may happen