Keller T., Colombi T., Ruiz S., Schymanski S., Weisskopf P., Köstel J. K., Sommer M., Stadelmann V., Breitenstein D., Kirchgessner N., Walter A., Or D.
Soil structure recovery following compaction – short-term evolution of soil physical properties in a loamy soil.
Soil Science Society of America Journal, 85, (4), 2021, 1002-1020.
Soil compaction by farm machinery may persist for decades, hampering soil productivity
and functioning. Assessing compaction costs and guiding recovery strategies
are hindered by paucity of data on soil structure recovery rates. A long-term Soil
Structure Observatory was established on a loamy soil in Switzerland to monitor
soil structure recovery after prescribed compaction, and to better assess the roles of
natural processes (vegetation, macrofauna, and shrink–swell cycles) on recovery patterns.
The aim of this study was to quantify short-term soil structure recovery under
natural conditions in the presence and absence of plant cover (ley and bare soil).
We measured soil porosity and gas and water transport capabilities at 0.1 and 0.3 m
depth. Two years after the compaction event, soil physical properties have not recovered
to precompaction levels, even within the topsoil. Surprisingly, no differences
were observed in the recovery patterns of ley and bare soil treatments. Measurements
show that recovery rates differ among soil properties with the most severely
affected properties by compaction (permeability) exhibiting highest recovery rates.
Total soil porosity shows no recovery trend, suggesting lack of soil decompaction.
Improved soil functions and decompaction are distinct aspects of soil structure recovery,
with the latter requiring net upward transport of soil mass. We suggest that soil
structure recovery proceeds at two fronts: from the soil surface downward, and
expanding around local biologically-active pockets (marked by biopores) into the
compacted soil volumes. This concept could be tested with additional data of longer
time series at our site as well as in other soils and climates.