A drought usually gets blamed on the sky. However, part of how hard a dry year bites is decided on the ground, by whether the rain that does fall can soak in and stay there.
I think this is the half of a dry year we can actually do something about, because the sky is out of our hands, and the paddock under it is not.
Two plain definitions help here. Infiltration is how fast rain soaks into the ground instead of running off it. Soil carbon is what is left of roots, microbes and plants in the soil, and it is what makes good soil dark and crumbly.
In this clip, former CSIRO soil microbiologist Walter Jehne pushes a spade into a paddock at Langhorne Creek in South Australia, in the middle of a February summer, and shows what soil that can drink looks like:
• The spade goes in easily, which he says means an open, loose structure.
• Roots run right through it, and the soil is dark, high in carbon and full of aggregates, meaning crumbs that hold together when wet.
• That "soil carbon sponge", in his words, is critical whatever the rainfall is, for getting the water in and storing it.
• His task for "all over Australia" is rebuilding how well our soils take in and hold the rain.
The research backs the first half of that more firmly than the second. A 2019 review of field trials found that ground kept under living roots and cover let rain in faster than bare, worked ground. More carbon does help soil hold water that plants can use, but by less than the figures shared online suggest, and it depends a great deal on the type of soil; one large review of the evidence called the effect limited.
So the bigger difference is often whether the rain gets in at all. A crusted, bare paddock can shed a storm that a covered, crumbly one would drink. None of this means soil can end a drought, but how dry a year gets on the ground depends partly on whether the soil can drink.