Question
Question: Depth of the sea is maximum at the Mariana Trench in the West Pacific Ocean. Trench has a maximum de...
Depth of the sea is maximum at the Mariana Trench in the West Pacific Ocean. Trench has a maximum depth of about 11km. At the bottom of the trench water column above it exerts 1000atmpressure. Percentage change in density of seawater at such depth will be around
(Given , B=2×109Nm−2 and patm=1×105Nm−2)
Solution
Hint Given the depth and bulk modulus of the sea water. Assume the volume at the surface as V1and volume at the depth as V2 and the density as ρ1and ρ2. Using Bulk modulus formula, calculate change in volume and use that to calculate density change and hence percentage.
Complete Step By Step Solution
First we calculate the change in volume from the top surface to the bottom surface of the mariana trench using the given bulk modulus formula. Bulk modulus of any substance is defined as its measure of it’s resistance to compression.
Mathematically, Bulk modulus is given as
B=VΔVΔP, where ΔPis change in pressure from top surface to the bottom surface
And ΔVis the change in volume of water from top surface to the bottom.
⇒B=VΔV(1000×105Nm−2)
We know B value , taking VΔVto the other side we get,
⇒VΔV=B(1000×105Nm−2)
⇒VΔV=(2×109Nm−2)(1000×105Nm−2)
Now, Vis initial volume V1
⇒V1V1−V2=201
⇒V1(1−201)=V2
Now, density at 11km depth is given as
ρ2=Volume2mass
Mass of water is constant throughout ,Hence
⇒ρ2=V2ρ1×V1
Substituting for V2, we get
⇒ρ2=V1(1−201)ρ1×V1
Cancelling out V1we get,
⇒ρ2=0.95ρ1
Now ,we need to calculate change in density percentage given by the formula
⇒ρ1ρ2−ρ1×100
⇒ρ10.95ρ1−ρ1×100
⇒ρ1ρ1(0.0526)×100
∴5%
Hence, the percentage change in density sums unto 5%.
Note We can also calculate the percentage change in density by considering the hydrostatic pressure exerted by the water on the bottom surface and by the atmosphere on top. Hydrostatic pressure is the pressure exerted by a fluid which is at a specified equilibrium at any given point on the fluid due to gravitational force. It is mathematically represented as the product of depth, density of the surface and gravitational force g.