How is methane formed?
When biological material (composed of carbon) is broken down by microorganisms in lakes, rivers and ponds, it releases CO2 and methane. The microorganisms are crucial because, without them, dead plants and animals would accumulate over time. This process primarily occurs in the shallow bottoms of lakes and rivers, within the sediment. When a significant amount of biological material is broken down there, it often exceeds what other microorganisms can consume and the excess methane is released into the air.
Bubbles
As mentioned earlier, methane contributes to global warming. To mitigate this, it's essential to reduce the amount of methane entering the atmosphere. Therefore, understanding the conditions under which more (or less) methane is released from surface waters is crucial. Methane bubbles, which can sometimes be seen rising up in the water column, and sometimes get stuck in the ice where you may have seen them, significantly contribute to methane levels in the atmosphere. Sarian Kosten and her colleagues have investigated and discovered several aspects of these methane bubbles in the Netherlands and Brazil:
- Methane emissions from water are challenging to measure accurately because the emissions vary a lot spatially: you could measure almost nothing at one location while some meters away a lot of bubbles are emitted.
- Methane can be 'released' from the sediment by disturbances such as boats, fish, or low-pressure areas above the water.
- Higher temperatures cause more methane bubbles to be released from the sediment.
- Increased nutrients in the water, such as fertilizers, lead to higher methane emissions.
- Emissions from polluted waters such as eutrophic ponds used for fish farming tend to be particularly high.
Did you know that the researchers had a special device built at the TechnoCentre of Radboud University to better measure methane bubbles?