Water Evaporation and Change in Depth

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SUMMARY

The discussion focuses on the mathematical modeling of water evaporation in an open bowl, demonstrating that the depth of water decreases at a constant rate, irrespective of the bowl's shape. Participants, including chisigma, magneto, MarkFL, and Pranav, confirmed this conclusion through a rigorous analysis involving the relationship between the volume of water and its surface area. The key equation derived is $\frac{dh}{dt}=-k$, indicating a constant rate of depth decrease, where $k$ is a positive constant related to the evaporation rate.

PREREQUISITES
  • Understanding of calculus, specifically integration and differentiation.
  • Familiarity with the concept of proportionality in mathematical modeling.
  • Knowledge of basic physics principles related to evaporation.
  • Ability to interpret mathematical equations and their implications.
NEXT STEPS
  • Explore the implications of surface area on evaporation rates in different container shapes.
  • Investigate the effects of temperature and humidity on the evaporation constant $k$.
  • Learn about differential equations and their applications in modeling physical phenomena.
  • Examine real-world applications of evaporation modeling in environmental science.
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Mathematicians, physics students, environmental scientists, and anyone interested in the principles of fluid dynamics and evaporation processes.

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Thanks again to those who participated in last week's POTW! Here's this week's problem!

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Problem: Water in an open bowl evaporates at a rate proportional to the area of the surface of the water (this means that the rate of decrease of the volume is proportional to the area of the surface). Show that the depth of the water decreases at a constant rate, regardless of the shape of the bowl.

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Remember to read the http://www.mathhelpboards.com/showthread.php?772-Problem-of-the-Week-%28POTW%29-Procedure-and-Guidelines to find out how to http://www.mathhelpboards.com/forms.php?do=form&fid=2!
 
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This week's problem was correctly answered by chisigma, magneto, MarkFL, and Pranav. You can find Pranav's solution below.

[sp]Let at any time $t$, the area of water open to the atmosphere be $A(h)$ where $h$ is the height of water level from the bottom of container.

Clearly, volume of the remaining water is given by $\displaystyle V(h)=\int_0^h A(y)\,dy\,\,\, (*)$. As per the question:

$$\frac{dV}{dt}=-kA(h)$$

where $k$ is some positive constant.

But from (*), we have:
$$\frac{dV}{dt}=A(h)\frac{dh}{dt}$$
Hence,
$$A(h)\frac{dh}{dt}=-kA(h)$$
$$\Rightarrow \frac{dh}{dt}=-k$$
which shows that the rate of change of height is independent of shape of bowl and decreases at constant rate.[/sp]
 

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