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Soil compaction negatively influences many important soil functions, including crop growth. Compaction occurs when the applied stress, , overcomes the soil strength. Soil strength in relation to compaction is typically expressed by the soil precompression stress, pc. Deformation is assumed to be elastic and reversible as long as pc. This work examined soil stress-strain behavior as measured in situduring wheeling experiments and related it to the stress-strain behavior and pcmeasured on soil cores in uniaxial compression tests in the laboratory. The data analyzed were from a large number of wheeling experiments carried out in Sweden and Denmark on soils with a wide range of texture. Contradicting the concept of precompression stress, we observed residual strain, [Latin Small Letter Open E]res, at pc. These observations were supported by stress-strain data measured in uniaxial compression tests, which likewise showed [Latin Small Letter Open E]res> 0 at pc. Residual strain was observed in the field when exceeded approximately 40 kPa, and when the ratio pcexceeded roughly 0.1, although [Latin Small Letter Open E]reswas very small at pc< 0.5. These values were similar to those obtained on confined uniaxial compression curves. On the basis of our findings, we question the use of pcas a measure of soil strength and call for a reevaluation of the precompression stress concept.

The article presents a study on soil stress-strain behavior relative to precompression stress in Sweden and Denmark. It analyzes the said behavior as measured in situ in wheeling experiments and its association scaled on soil cores in uniaxial compression tests. It also notes the negative impact of soil compaction on crop growth.