Plants make sugar. Yes, really.
Through photosynthesis, plants create sugars and send some of that energy into the soil, feeding microbial life below ground. In return, those microbes help cycle nutrients, release CO2, and support the carbon cycle in ways most people never see.
But here’s the real question: what happens when soil can’t breathe?
When soil becomes compacted, oxygen drops. And when oxygen drops, you start losing the aerobic microbes that do much of the heavy lifting in healthy soil.
Aerobic microbes are the workhorses. They thrive where oxygen is present, especially around plant roots, and they play a major role in nutrient cycling and plant support. In a healthy system, they should dominate.
That said, anaerobic microbes also have a role.
You generally want a much smaller anaerobic population, roughly 20%, with the remaining 80% being aerobic. Anaerobic microbes are usually found in and just below the compaction layer, where oxygen is limited. Their role is to begin breaking down that compacted zone and opening the soil back up.
In other words, they help turn six inches of breathing soil into six and a half.
That matters.
Because without that function, the soil does not start to reopen. The aerobic microbes cannot do that job alone. So both groups matter, but they matter in different places and for different reasons.
The plant, however, prefers some distance from the anaerobic crowd.
Anaerobic microbes are not generally meant to be close to the root zone. They do not work with plants in the same productive way. Their role is more structural and transitional, helping make the soil more hospitable over time.
The aerobic microbes are the ones closely tied to the roots.
They need oxygen.
They need a food source.
And that food source comes from the plant.
That’s the beauty of the system.
Plants are not just growing in soil. They are actively managing relationships underground, feeding the biology that feeds them back.
Healthy soil is not just dirt.
It is a living economy built on air, carbon, biology, and exchange.
How often are we treating compaction as a mechanical problem when it is also a biological one?
Are we paying enough attention to whether our soils can actually breathe?
And if plants are feeding the biology that feeds them back, what does that say about how we should be managing the ground beneath our feet?