Farmers face a ‘geographic lottery’ in terms of soil carbon sequestration, if plans to reward them financially for increasing soil carbon stocks are to be introduced, two leading soil scientists have confirmed. Rothamsted Research Prof. Andrew Neal and Prof. David Powlson are confirming that geological history alone determines the type of soil found on a farm.

And this is the key factor that may make capturing more carbon in the soil nigh on impossible for some farmers.

Prof. Neal explained: “Farmers on sandy soils will struggle to increase the carbon content of their soil. They might be doing all the right things to increase the carbon flowing through their soils, but it won’t show up when they come to test the soil.”

Improving soil carbon sequestration

Common ways to improve soil carbon include the addition of manures or crop residues, growing cover crops in the winter and the rearing of grazing livestock and crops together. The problem, according to Prof. Neal, is that the potential for carbon sequestration is strongly influenced by soil type - particularly texture - and the starting carbon content, which will be a legacy of past farming practices. Prof. Neal continued: “Changes in soil carbon in response to alterations in management practice occur slowly.
It’s also difficult to measure the likely small changes in soil carbon within a short time period.
“Indicators such as soil microbial biomass are useful in showing whether organic carbon is increasing or decreasing in response to a change of management. “But these measurements provide neither an estimate of soil carbon stocks, nor a prediction of absolute changes in carbon," he added

Measuring carbon

Prof. Neal and Prof. Powlson are proposing an alternative system that measures the flow of carbon through soil, rather than the actual amount in soil at a given time.

They refer to it as a dynamic rather than static view of soil.

“If a system of policy requirements or financial incentives for increasing soil carbon is to be instituted, we propose an alternative approach using carbon models to predict probable changes in soil carbon taking account of the farmer’s soil type, local climate, cropping practices and starting soil carbon content,” said Powlson.
This could be combined with closer monitoring at a network of benchmark sites.
“There is much interest in sequestering carbon in soil as a means of mitigating climate change by making payments to farmers in return for the amount of carbon sequestered," he continued.
There are several ‘early warning’ methods that may be successful in detecting whether or not a soil is increasing its carbon content, and this is helpful. But they will probably not provide direct evidence of the absolute change in total carbon that has occurred.”
Soil organic matter contains about 50% carbon and influences virtually all soil properties. Recent research using Rothamsted soils by Prof. Neal and colleagues has shown how the structure of the soil is affected by the processing of organic matter inputs by soil microbes as metabolites form associations with mineral particles.

The resulting structure in turn impacts oxygen diffusion through the soil and the microbial processing of carbon and other nutrients important for crop and livestock nutrition.

Prof. Neal said: “Imaging of pore networks clearly shows how a clay-rich soil adapts to differences in organic inputs, but a sandy soil shows little adaptation.
Thus, the physical structure and resulting changes in biological activity, are less influenced by organic inputs in sandy soils.
“This is consistent with the observation that sandy soils have much less capacity to sequester carbon than soils of finer texture.”