Let's assume that CH₄ has ideal gas behavior.
Then we can use ideal gas formula,
PV = nRT
Where, P is the pressure of the gas (Pa), V is the volume of the gas (m³), n is the number of moles of gas (mol), R is the universal gas constant ( 8.314 J mol⁻¹ K⁻¹) and T is temperature in Kelvin.
P = 1 atm = 101325 Pa
V = 1.50 L = 1.50 x 10⁻³ m³
n = ?
R = 8.314 J mol⁻¹ K⁻¹
T = 0 °C = 273 K
By substitution,
101325 Pa x 1.50 x 10⁻³ m³ = n x 8.314 J mol⁻¹ K⁻¹ x 273 K
n = 0.0669 mol
Hence, moles of CH₄ = 0.0669 mol
Moles = mass / molar mass
Molar mass of CH₄ = 16 g mol⁻¹
Mass of CH₄ = moles x molar mass
= 0.0669 mol x 16 g mol⁻¹
= 1.0704 g
Hence, mass of CH₄ in 1.50 L at STP is 1.0704 g
Explanation:
The added greenhouse gases absorb the heat. They then radiate this heat. Some of the heat will head away from the Earth, some of it will be absorbed by another greenhouse gas molecule, and some of it will wind up back at the planet's surface again. With more greenhouse gases, heat will stick around, warming the planet.
Answer:
Explanation:
Firstly balance the chemical reaction,
→ 
Molecular weight of 
=103g/mole;
Molecular weight of 
=164g/mole;
Moles are:
Number of mole of =0.275
From the balanced equation,
3 mole of gives 1 mole of 
1 mole of gives 1/3 mole of
Hence;
0.275 mole of will produce 
mole of
Hence,
The amount of time it takes for 1/2 of it to decay or dissapear
this is liike compound interest because it takes the same amount of time to decay 1/2 of it, regardless of the amount
example
lets say half life of element x is 1 year
if yo has 32 grams, after 1 year, it decays to 16g
2 years decays to 8
3 years decays to 4
4 years decays to 2
5 years decays to 1
etc
hope this helps (I'm not the best at chem)
