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Musya8 [376]
4 years ago
11

Evolution of the earths atmosphere

Chemistry
1 answer:
Alex4 years ago
7 0

Answer:

The early atmosphere

Its early atmosphere was probably formed from the gases given out by volcanoes. It is believed that there was intense volcanic activity for the first billion years of the Earth's existence. The early atmosphere was probably mostly carbon dioxide, with little or no oxygen.

Explanation:

Hope this helps! Brainly if so!

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NEED HELP ASAP; PLEASE SHOW YOUR WORK.
Sindrei [870]

Answer:

n = 0.3 mol

Explanation:

Given data:

Volume of gas = 8.0 L

Temperature of gas = 45 °C (45+273 = 318 K)

Pressure of gas = 0.966 atm

Moles of gas present = ?

Ideal gas constant = R = 0.021 atm.L/mol.K

Solution:

Formula:

PV = nRT

P = Pressure

V = volume

n = number of moles

R = ideal gas constant

T = temperature

Now we will put the values:

0.966 atm × 8 L = n × 0.0821 atm.L/mol.K × 318 K

7.728 atm.L = n × 26.12  atm.L/mol

7.728 atm.L / 26.12  atm.L/mol = n

n = 0.3 mol

5 0
4 years ago
Which .1 M solution has a pH greater than 7
ElenaW [278]

Answer:

KOH for which PH= 13

Explanation:

5 0
4 years ago
Which of these steps would most likely be part of a lab procedure?
Svetlanka [38]
What is the option just give that thing also
4 0
3 years ago
Light energy is captured by the green pigment ___________________________.
Anna71 [15]

Answer:

Chlorophyll

Explanation:

chlo·ro·phyll

noun

a green pigment, present in all green plants and in cyanobacteria, responsible for the absorption of light to provide energy for photosynthesis. Its molecule contains a magnesium atom held in a porphyrin ring.

7 0
3 years ago
From the values of ΔH and ΔS, predict which of the following reactions would be spontaneous at 28°C: reaction A: ΔH = 10.5 kJ/mo
Ainat [17]

Answer: A:

ΔH = 10.5 kJ/mol, ΔS = 30.0 J/K·mol is non-spontaneous.

ΔH = 1.8 kJ/mol, ΔS = −113 J/K · mol is non-spontaneous.

Reaction A can become spontaneous

Reaction A is spontaneous at 76.85 °C

Explanation:

It's helpful to memorize that if:

-ΔS is greater than 0 and ΔH is less than 0; its spontaneous at all temperatures.

-ΔS is less than 0 and ΔH is greater than 0; its non-spontaneous at all temperature.

-ΔS is greater than 0 and ΔH is greater than 0; its spontaneous at high temperatures and non-spontaneous at low temperatures.

-ΔS is less than 0 and ΔH is less than 0; its spontaneous at low temperatures and non-spontaneous at high temperatures.

This comes from the equation ΔG=ΔH-TΔS

where ΔG is Gibbs free energy, ΔH is enthalpy, T is temperature (in Kelvin), and ΔS is entropy.

Without getting too in depth as to what each of those mean (you could take an entire class on entropy alone), the temperature at which the spontaneity changes is equal to ΔG (Gibbs free energy) at 0.

So take the above equation and set ΔG = 0, and rearrange the equation to solve for T.

ΔG=ΔH-TΔS

0=ΔH-TΔS

add TΔS to the other side

TΔS=ΔH

divide the right side by ΔS to find T (temperature)

T=ΔH/ΔS

Now we can find the temperature that the first reaction would occur at spontaneously.

We need to make sure that we have the same units for ΔH and ΔS, so divide 30 by 1000 to convert J/Kmol into kJ/kmol so that we have kJ for ΔH and ΔS.

30/1000 = 0.03 kJ

Plug in the values for the modified equation T=ΔH/ΔS

10.5 kJ/0.03 kJ = 350 K

The temperature is in Kelvin, so subtract 273.15 to convert it into Celsius

350-273.15 = 76.85 °C

7 0
4 years ago
Read 2 more answers
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