Answer:
<h2>The answer is 66 g</h2>
Explanation:
The mass of a substance when given the density and volume can be found by using the formula
<h3>mass = Density × volume</h3>
From the question
volume of hexane = 100 m L
density = 0.66 g/mL
The mass is
mass = 0.66 × 100
We have the final answer as
<h3>66 g</h3>
Hope this helps you
The answer is 1.5*10^-12 square meters. For a detailed calculation, please refer to the attachment.
the total number of particles is provided in table one as 133 this is the sum of all the isotopes of Mnmium. you will use this value to do table 2 by dividing each isotope by the total number of particles (133).
silicone has an average atomic mass of 28.085 according to the periodic table, this tells us that the Si28 should be the most abundant isotope of the three
to calculate the average atomic mass of silver, we are given the abundance of each isotope and the formula to calculate the average atomic mass is (mass of isotope 1 x abundance percentage) plus (mass of isotope 2 x abundance percentage)...... so the average atomic mass of silver would be ( 107 x 52%) + (109x48%) = 107.96 this value is closer to the atomic mass of silver 107 because it is the most abundant
from the pie chart it is clear to see that Chlorine-35 is the most abundant at 76%
we will determine the average atomic mass of chlorine using the same formula as with silver for the previous question. Chlorine-35 is 76% and Chlorine-37 is 24% therefore (35x 76%)+(37x24%) = 35
Answer:
True
Explanation:
It is true that every element in the periodic table follows the Aufbau's principle.
The principle states that "the sublevels with lower energies are filled up before those with higher energies".
- Sublevels do not fill up in numerical order.
- This is true when writing the electronic configuration of all atoms on the periodic table.
ANDESITE is a fine grained rock that formed when magma irrupt it onto the surface and crystallized quickly ANDESITE & DIORITE have a composition that is intermediate between basalt.This is because their parent magmas formed from the PARTIAL melting of a BASALTIC oceanic plate.
