Aarhus Universitets segl

Specific surface area to soil organic carbon ratio as a new novel soil health indicator?

Main subject area: Soil health; clay: OC ratio; specific surface area; clay mineralogy

Short project description

Around 60-70% of EU soils are unhealthy mainly because of unsustainable management practices. The ratio of clay to soil organic carbon (clay:OC)  may be used as an indicator of soil health. A threshold (ratio of clay to organic carbon of 10 kg kg−1) has been found to be a promising constraint for a soil’s ability to maintain or regenerate functional structure

Soil has a large specific surface area, which leads to much interaction of ions and water molecules with the soil particles. Specific surface area (SA) (m2/g) determines many physical and chemical properties of soils, and many phenomena relate to SA. The measurement of soil specific SA may be a more meaningful index for characterizing a soil than the percentages of sand, silt, and clay. The magnitude of the specific surface area of a soil depends largely on the amount of clay and the type of clay minerals in the soil. Hence specific surface area has the potential to be a better comparable measure across soils in Europe, and with this project we aim to test the use of specific surface area to OC ratio.

The measurement of SA is done in the laboratory and can also be determined by NIR or water vapor sorption.

Project start

September 2024

Physical location of project and students work

Department of Agroecology, AU Foulum, 8830 Tjele

Extent and type of project

30 ECTS: Theoretical thesis based on literature studies and/or analysis of issued and edited data sets.

45 ECTS: Experimental theses in which the student is responsible for collection and analysis of his/her own original data.

60 ECTS: Experimental theses in which the student is responsible for planning, trial design and collection and analysis of his/her own original data.

Additional information

References:

Dexter, A. R., Richard, G., Arrouays, D., Czyz, E. A., Jolivet, C., and Duval, O. 2008. Complexed organic matter controls soil physical properties, Geoderma, 144, 620–627