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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 11km11km. At the bottom of the trench water column above it exerts 1000atm1000atmpressure. Percentage change in density of seawater at such depth will be around
(Given , B=2×109Nm2B = 2 \times {10^9}N{m^{ - 2}} and patm=1×105Nm2{p_{atm}} = 1 \times {10^5}N{m^{ - 2}})

Explanation

Solution

Hint Given the depth and bulk modulus of the sea water. Assume the volume at the surface as V1{V_1}and volume at the depth as V2{V_2} and the density as ρ1{\rho _1}and ρ2{\rho _2}. 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=ΔPΔVVB = \dfrac{{\Delta P}}{{\dfrac{{\Delta V}}{V}}}, where ΔP\Delta Pis change in pressure from top surface to the bottom surface
And ΔV\Delta Vis the change in volume of water from top surface to the bottom.
B=(1000×105Nm2)ΔVV\Rightarrow B = \dfrac{{(1000 \times {{10}^5}N{m^{ - 2}})}}{{\dfrac{{\Delta V}}{V}}}
We know B value , taking ΔVV\dfrac{{\Delta V}}{V}to the other side we get,
ΔVV=(1000×105Nm2)B\Rightarrow \dfrac{{\Delta V}}{V} = \dfrac{{(1000 \times {{10}^5}N{m^{ - 2}})}}{B}
ΔVV=(1000×105Nm2)(2×109Nm2)\Rightarrow \dfrac{{\Delta V}}{V} = \dfrac{{(1000 \times {{10}^5}N{m^{ - 2}})}}{{(2 \times {{10}^9}N{m^{ - 2}})}}
Now, VVis initial volume V1{V_1}
V1V2V1=120\Rightarrow \dfrac{{{V_1} - {V_2}}}{{{V_1}}} = \dfrac{1}{{20}}
V1(1120)=V2\Rightarrow {V_1}(1 - \dfrac{1}{{20}}) = {V_2}
Now, density at 11km depth is given as
ρ2=massVolume2{\rho _2} = \dfrac{{mass}}{{Volum{e_2}}}
Mass of water is constant throughout ,Hence
ρ2=ρ1×V1V2\Rightarrow {\rho _2} = \dfrac{{{\rho _1} \times {V_1}}}{{{V_2}}}
Substituting for V2{V_2}, we get
ρ2=ρ1×V1V1(1120)\Rightarrow {\rho _2} = \dfrac{{{\rho _1} \times {V_1}}}{{{V_1}(1 - \dfrac{1}{{20}})}}
Cancelling out V1{V_1}we get,
ρ2=ρ10.95\Rightarrow {\rho _2} = \dfrac{{{\rho _1}}}{{0.95}}
Now ,we need to calculate change in density percentage given by the formula
ρ2ρ1ρ1×100\Rightarrow \dfrac{{{\rho _2} - {\rho _1}}}{{{\rho _1}}} \times 100
ρ10.95ρ1ρ1×100\Rightarrow \dfrac{{\dfrac{{{\rho _1}}}{{0.95}} - {\rho _1}}}{{{\rho _1}}} \times 100
ρ1(0.0526)ρ1×100\Rightarrow \dfrac{{{\rho _1}(0.0526)}}{{{\rho _1}}} \times 100
5%\therefore 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.