Abstract

The atmosphere contains 3400 trillion gallons of water vapor, which would be enough to cover the entire Earth with a one-inch layer of water. As air humidity is available everywhere, it acts as an abundant renewable water reservoir, known as atmospheric water. The efficiency of an atmospheric water harvesting system depends on the sorption capacities of water-based absorption materials. Using anhydrous salts is an efficient process in capturing and delivering water from ambient air, especially under a condition of low relative humidity, as low as 15%. Many water-scarce countries, like Saudi Arabia, receive high annual solar radiation and have relatively high humidity levels. This study is focused on the simulation and modeling of the water absorption capacities of three anhydrous salts under different relative humidity environments: copper chloride (CuCl2), copper sulfate (CuSO4), and magnesium sulfate (MgSO4), to produce atmospheric drinking water in water-scarce regions. By using a mathematical model to simulate water absorption, this study attempts to compare and model the results of the current computed model with the laboratory experimental results under static and dynamic relative humidities. This paper also proposes a prototype of a system to produce atmospheric water using these anhydrous salts. A sensitivity analysis was also undertaken on these three selected salts to determine how the uniformity of their stratified structures, thicknesses, and porosities as applied in the mathematical model influence the results.

Highlights

  • About 4 billion people, or two-thirds of the world’s population, suffer from water scarcity [1]

  • Atmospheric water usually exists in three basic types [4]: clouds floating in the sky, fogs that are close to the land, and water vapor in the air

  • This paper reports on a project that simulated and modeled an atmospheric watergeneration unit using anhydrous salts: copper chloride, copper sulfate, and magnesium sulfate, to produce atmospheric water from thin air

Read more

Summary

Introduction

About 4 billion people, or two-thirds of the world’s population, suffer from water scarcity [1]. About 13 sextillion (1021 ) liters of water exist in the atmosphere at any given time [2]. This atmospheric water, which is considered a substantial renewable source or reservoir of water, enough to satisfy everyone’s needs in the world, has been overlooked [3]. Atmospheric water usually exists in three basic types [4]: clouds floating in the sky, fogs that are close to the land, and water vapor in the air. Clouds and fogs are all made up of tiny drops of water, typically with a diameters of 1 to 40 mm, compared with the sizes of rain droplets, which vary from 0.5 to 5 mm. The concentrations of water droplets in fogs are usually larger

Results
Discussion
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call