Question

Draw the temperature profile that is assumed in the derivation of the d2 -law for evaporation inside and outside of a droplet as a function of the radius.

Short answer

Question: Describe the temperature profile inside and outside of a droplet as a function of radius, according to the d2-law for evaporation. Answer: According to the d2-law for evaporation, the temperature profile inside the droplet is assumed to be constant (T_i) and independent of the radial distance (r) from the center. In contrast, the temperature profile outside the droplet is assumed to be a linear function of distance from the droplet surface, given by T(r) = T_i + K(r-R) for r > R, where K is a constant determining the temperature gradient and R is the droplet radius.

Step-by-step solution

Understanding the d2-law and its assumptions

The d2-law is a simplified model for the evaporation rate of a droplet. It assumes that the temperature profile inside the droplet remains uniform, and the temperature outside the droplet is a linear function of the distance from the droplet surface. Additionally, the d2-law considers that the mass transfer is governed by diffusion.

Temperature inside the droplet

As per the d2-law, the temperature profile inside the droplet is assumed to be constant. This means that the temperature is the same at any point within the droplet, regardless of distance from the center. We can represent this as: T(r) = T_i, for 0 ≤ r ≤ R, where T(r) is the temperature at a radius 'r', T_i is the constant temperature inside the droplet, and R is the droplet radius.

Temperature outside the droplet

The d2-law assumes the temperature profile outside the droplet to be a linear function of the distance from the droplet surface. We can represent this linear relationship as: T(r) = T_i + K(r-R), for r > R, where K is a constant determining the temperature gradient, and r is the distance from the center of the droplet.

Plotting the temperature profile

To plot the temperature profile, follow these steps: 1. On the horizontal axis, represent the radial distance (r) from the center of the droplet, ranging from 0 to the desired maximum distance. 2. On the vertical axis, represent the temperature (T). 3. Draw a horizontal line at T_i for the region 0 ≤ r ≤ R, representing the constant temperature inside the droplet. 4. Draw a straight line with a slope K, starting from the point (R, T_i) and extending further for r > R, representing the linear temperature gradient outside the droplet. The resulting plot represents the assumed temperature profile in the d2-law evaporation model, inside and outside of the droplet as a function of the radius r.

Key concepts

Temperature Profile

A temperature profile describes how temperature changes from one point to another within a given system, such as a droplet in the case of the d2-law. It provides insights into how temperature distributes inside and around the droplet. In the d2-law evaporation model, we assume that the temperature within the droplet remains uniform. This means that all parts of the droplet share the same temperature, which simplifies calculations.
However, outside the droplet, the temperature changes linearly with distance. This linearity assumption is crucial for computational convenience and understanding external temperature variations.

In a plotted temperature profile:

• Inside the droplet: Temperature is constant at a value called T_i, regardless of the radial position.
• Outside the droplet: Temperature increases linearly with distance from the droplet's surface.

The simplicity of these assumptions facilitates the theoretical analysis of droplet evaporation.

Droplet Evaporation

Droplet evaporation is the process where liquid molecules turn into vapor, shrinking the droplet over time. This phenomenon is particularly important in areas like meteorology, combustion, and pharmaceuticals. The d2-law suggests that evaporation in droplets happens uniformly over time, considering a constant temperature inside the droplet and a temperature gradient outside.
The droplet's size decrease follows the squared radius relationship; hence, the term "d2-law." This means as the droplet evaporates, it gets gradually smaller in a predictable pattern. Understanding how evaporation works helps engineers and scientists develop better technologies and predict natural processes more effectively.
Several factors influence evaporation:

• Temperature: Higher temperatures generally increase evaporation rates.
• Droplet size: Smaller droplets tend to evaporate faster than larger ones.
• Surrounding air flow: Movement can expedite vapor removal and enhance evaporation.

By mastering these concepts, one can enhance control over evaporation in practical applications, from optimizing fuel combustion to controlling humidity in the environment.

Diffusion Mass Transfer

Diffusion mass transfer is a process where substances spread from regions of higher concentration to lower concentration. In the context of droplet evaporation, it means that the vapor molecules move away from the droplet surface, driven by the concentration difference between the droplet surface and the surrounding air. This movement is crucial because it explains how and why the droplet shrinks over time.

• Diffusion is a natural process occurring in all states of matter.
• The rate of diffusion affects how fast a droplet will evaporate.
• The d2-law assumes that mass transfer happens solely through diffusion at the droplet surface.

Understanding diffusion provides an essential framework for predicting evaporation rates under different conditions. It allows for better modeling in various applications, such as designing efficient heating systems or understanding weather patterns.

Temperature Gradient

A temperature gradient refers to the rate of temperature change over a specific distance. It is essential to describe how heat is distributed and transferred in media, such as around a droplet during evaporation. In our model, this gradient is linear outside the droplet, which simplifies calculations by assuming steady heat distribution away from the droplet.
This gradient is fundamental because:

• It determines the direction of heat flow.
• Higher gradients mean more rapid temperature change with distance, affecting evaporation speed.
• Understanding gradients can help adjust conditions for desired evaporation rates in technology and industrial processes.

Knowing how to quantify and manipulate temperature gradients is valuable in fields such as material science, environmental engineering, and thermal management.