Answer:


Explanation:
<u>Data</u>
<u>mass m= 100g</u>
<u>Length L= 5cm</u>
<u>we can use:</u>
<u>gm-kL= 0</u>
<u>divide both side by m</u>
<u>g - </u>
<u>=0</u>
<u>where</u>
= 
^{2}
so now
= 


square both side


We can apply:
u(t)=Acoswt +Bsinwt
u(t)=Acos14t +Bsin14t
u(0)=0 where A=0
therefore
u(0) = Bsin14t
(0) = 10 ⇒ 10=14B ⇒ B=
B=
so now u(t)=
sin14t
so t will be:
t=
t=
t=0.22 seconds
An additional 10ppm of methane will change the upward IR heat flux (in tropical
atmosphere) from 289.29 W/m2
to 286.211 W/m2
, which is a reduction of 3.08
W/m2
.
An additional 10ppm of CO2 will change the upward IR heat flux from 289.29 W/m2
to 289.29 W/m2
, which is a change of 0.13 W/m2
.
Therefore, an additional 10 ppm of methane would have a much larger impact on
the outgoing infrared flux than an additional 10 ppm of CO2 at current
concentrations
<span>21343 km / 150 km/hr = 142.29 hrs</span>
Calorimeter is an instrument which is used for measurement of heat liberation or absorption from a system during the flow of energy.
Answer: Option A
<u>Explanation:</u>
When the heat is liberated from the system, during the flow of energy it undergoes a exothermic reaction. Similarly, when the heat is absorbed by the system during the flow of energy, the system undergoes an endothermic reaction.
The calorimeter as the name suggest is the meter to calibrate calorie. Calorie here refers to the heat energy, which is being calibrated or measured during the flow of energy, either liberated from the system or being absorbed by the system.