Capturing carbon from our atmosphere grows to be of extreme importance as “Earth’s temperature has risen by an average of 0.11 degrees Fahrenheit (0.06 degrees Celsius) per decade since 1850, or about 2 degrees Fahrenheit in total” (Lindsey and Dahlman 2024). Carbon and other elements help create a greenhouse effect, which keeps our Earth at a suitable temperature to support life. Currently, more carbon dioxide is in our atmosphere than is considered optimal for maintaining a stable climate. So what can we do about that?