Answer:
final temperature is 469.71 K = 196.71 °C
Explanation:
Given data
volume V = 1010 cm3 = 0.00101 m³
temperature = 20.7°C = 20.7 + 273 = 293.7 K
pressure P1 = 1.04 x 10^5 Pa
volume = 1570 cm3
pressure P2 = 1.07 x 10^5 Pa
to find out
number of moles of oxygen and final temperature
solution
we know that for ideal gas
PV = nRT
put here all value to get n
R gas constant = 8.314472 J/mol−K and T = 293.7 K and V = 0.00101 m³
and P = 1.04 x 10^5
so n = ( 1.04 x 10^5 × 0.00101 ) / ( 8.314472 × 293.7 )
n = 0.043015 moles
and
now we use equation
P1V1 /T1 = P2V2 / T2
1.04 x 10^5 × 1010 / 293.7 = 1.07 x 10^5 × 1570 / T2
T2 = 49338663 / 105040 = 469.71 K
so final temperature is 469.71 K = 196.71 °C
<span>Thermocline is a layer between
warm water from the ocean’s surface and cool water from below the ocean. In here,
the temperature decreases rapidly from the warmer layer to the colder layer. A thermocline forms due to the heat of the sun
heating the ocean’s surface. Because of the difference in density between warm
and cooler ocean water, cooler ocean water sinks and warmer ocean water floats.
This is caused due to the heat and mass transfer between particles of the
ocean. The answer is letter C. The sun’s radiation does not extend below a
certain depth; therefore, deeper ocean water is colder than surface water.</span>
Answer:
In the picture.
Explanation:
I hope that it's a clear explanation.