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Radda [10]
3 years ago
7

Explain what happens when a cold air mass overtakes a warm air mass?

Chemistry
1 answer:
SVEN [57.7K]3 years ago
6 0
Is this a multiple answer?
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An isotope undergoes radioactive decay. The new isotope that forms has an atomic number that is 2 less than the original isotope
jeka57 [31]
It is an alpha decay because when this phenomena occurs an atomic nucleus emits an alpha particle (helium nucleus) and consequentially decays into another atom with a mass number that is reduced by four an atomic number that is reduced by 2 two. The helium atom consists of two protons and two neutrons.

Therefore, the answer is <span>alpha decay because alpha particles have two protons and two neutrons</span>
3 0
3 years ago
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what is the substances would be produced during the chemical reaction between potassium hydroxide and hydrochloric acid
tino4ka555 [31]
Potassium chloride and water
3 0
4 years ago
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Please help me with number 4 and 5 on my study guide
Shtirlitz [24]

Answer:

help with problem 4

Explanation:

4. protons are equal to atomic numbers. neutrons are atomic mass minus atomic number. electrons are equal to protons.

5. I don't know, sorry.

5 0
2 years ago
A metal from group 1 and a nonmetal from group 17 are
MrMuchimi
3.) likely to form an ionic bond

Metals and non-metals combine to form ionic bonds.
8 0
3 years ago
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What is the limiting factor in determining the accumulation of siliceous ooze/calcareous ooze, respectively?
zhannawk [14.2K]

Answer:

productivity and water depth

Explanation:

The productivity and the depth of water are both equally important as it directly affects the accumulation of biogenic sediments such as the siliceous ooze and calcareous ooze. In the equator and the coastal upwelling areas, and at the site of divergence of oceans, there occurs a high rate and amount of productivity, and these are considered to be the primary productivity.  

The siliceous oozes are a good indicator of extensively high productivity in comparison to the carbonate oozes. The main reason behind this is that the silica can be easily dissolved in the surface water. On the other hand, the carbonates dissolve at a relatively lower ocean water depth, so there requires a high amount of surface productivity in order to allow these siliceous oozes to reach the ocean bottom.

Thus, the water depth and productivity, both are considered as the limiting factor in determining the accumulation of biogenic oozes.

8 0
3 years ago
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