Welcome to the second Expedition weekly deep dive at Survivaltech.club!
This week has been thrilling. I’ve learnt so much about methane (and quantum mechanics)! Now I’m beyond excited to share the findings with you!
Methane - what a molecule!
Methane (CH4) is a beautiful formation of atoms (=molecule) in its simplicity. It has one carbon atom and four hydrogen atoms. The carbon atom gets positioned in the center and is surrounded by four hydrogen atoms.
Chemists call methane an alkane, a hydrocarbon with single bonds. Bonds get formed between carbon and hydrogen atoms. These bonds are called covalent bonds, as the atoms share electrons.
Why do these bonds form? The simplified answer is that the bonding allows the atoms to hang out with minimized energy in this universe. You wouldn’t want to use any extra energy to heat or cool your house because it costs money, right.
Methane (CH4) is one of the greenhouse gases that are warming our planet. It exists naturally in the Earth’s atmosphere and helps keep the Earth warm enough.
But as with other greenhouse gases, our humanity is emitting methane into the air. This excess amount of methane in the atmosphere is causing our planet to heat up.
There is very little methane in the atmosphere. Only 0.00018% of air is methane. As a general note, greenhouse gases constitute only a tiny part of the air (approximately 0.04%), yet they are responsible for climate change.
Still, methane accounts effectively for 17% of the total annual greenhouse gases. Note that the chart below is in CO2e, which takes into account the differing global warming potential of greenhouse gases.
Methane’s warming potential is huge.
Methane is a potent greenhouse gas. As I pointed out last week, methane is approximately 30 times more potent greenhouse gas than carbon dioxide over a 100 years.
Since the next 10-30 years are probably our most essential decades to mitigate climate change, wouldn’t it make sense to focus on reducing methane emissions?
Primary sources of methane emissions
570 million tons (Mt) of methane is released into the atmosphere every year. 60% of this methane is human-made (anthropogenic), and 40% comes from natural sources.
Sources of human-made methane:
Agriculture: Burping cows, rice fields
Oil and natural gas production: leaks and ventilation
Waste: decomposing landfills and wastewater
(Releases from permafrost. Permafrost has trapped in colossal amounts of methane. Now that permafrost is melting due to global warming, they are releasing methane.)
Natural sources of methane include primarily wetlands.
Across these categories, methane ends up in the atmosphere via two pathways:
Decomposition of organic matter in an oxygen-free environment
Leaks (indeliberate and deliberate)
1. Decomposition of organic matter
Organic matter like you and I, other animals, and plants will eventually die and be decomposed. Since Mother Nature wants to recycle the building blocks and build new things, different microbes step in as organisms die and decompose the matter.
If this decomposition takes place in an oxygen-free environment, particular microbes called methanogens take the lead in breaking down the organisms. As a result, methane gets formed.
This process of breaking down organic matter in oxygen-free environments is called methanogenesis.
The production of methane via methanogenesis occurs in several places:
in the gut of ruminants, like cows and cattle, when they digest food.
on rice fields, when they are flooded with water and deprived of oxygen. This occurs naturally in wetlands.
on landfills and wastewater, when organic matter decomposes in oxygen-free environments.
2. Leaks (indeliberate and deliberate)
Methane gets leaked to the atmosphere from:
production of oil and natural gas
Natural gas, which we use as an energy source, consists of 95% methane. When natural gas is produced, processed, and distributed, not all pipes and tanks are gas-tight, and the natural gas leaks into freedom.
Furthermore, oil production emits methane. Natural gas is often found in conjunction with oil deposits. When oil is drilled, methane escapes.
Biogas also contains mainly methane. Biogas production takes advantage of methanogenesis we talked about earlier. Biogas producers take organic waste and manure and then decompose them in an oxygen-free environment. This process results in methane.
Biogas is a renewable energy source. However, when we burn it, we still release carbon dioxide into the air. Could we turn this renewable methane into something valuable and use solar and wind (and fusion!) to generate energy?
Cool solutions for reducing methane emissions
We have solutions to reduce methane emissions. Here are some of the cool ones that I found.
Microbial carbon capture fuel cells
Microbial carbon capture fuel cells make clean electricity from waste. Wow.
A microbial fuel cell is a device that converts organic waste into electricity with the help of microbes. When a chemical reaction takes place in this apparatus, a flow of electrons and so electricity gets produced. However, carbon dioxide gets produced as an end-product in this reaction.
On a molecular level, why is methane better at trapping heat than carbon dioxide?
What valuable things could we make out of methane? Burning methane as fuel is an option, but a rather stupid one in my opinion. When methane burns (or oxidizes how a chemist would describe this), methane turns into carbon dioxide and water. So we still end up with carbon dioxide in the air.
NOAA. Critical Thinking Activity: The Methane Cycle. Link
Pandit, S., Nayak, B. K. & Das, D. (2012). Microbial carbon capture cell using cyanobacteria for simultaneous power generation, carbon dioxide sequestration and wastewater management. Bioresource Technology, 107, 97-102.
Pratt, C. & Tate, K. (2018). Mitigating Methane: Emerging Technologies To Combat Climate Change’s Second Leading Contributor. Environmental Science & Technology, 52, 6084-6097.
Ritchie, H. & Roser, M. (2020). By gas: how much does each contribute to total greenhouse gas emissions. Link
Schiermeier, Q. (2020). Global methane levels soar to record high. Nature, 14th July. Link
Struzik, E. (2020). How Thawing Permafrost Is Beginning To Transform the Arctic. Yale Environment 360. Link
Su, J., Hu, C., Yan, X. et al. (2015). Expression of barley SUSIBA2 transcription factor yields high-starch low-methane rice. Nature, 523, 602–606.