Javascript must be enabled to continue!
Field-scale Assessments of Subsoil Compaction and Soil Structural Functions in Lower Saxony, Germany
View through CrossRef
Subsoil compaction a one of the major threats for crop production and soil ecological functioning in Europe. To quantify its field-scale extent, field investigations were conducted on 26 agricultural fields across Lower Saxony state in northern Germany, covering four dominant soil textures (clay loam, sandy loam, silt, and silty loam) and two field management zones (machinery turning area and main field area). In-situ measurements of penetration resistance and shear strength were conducted on field at 10 cm (topsoil) and 40 cm (subsoil), and bulk density (ρb), saturated hydraulic conductivity (Ks), air permeability (Ka) were measured on undisturbed soil samples at the same depth. The results showed that most machinery turning zones showed clear signs of subsoil compaction. About 80% fields showed 5~60% higher penetration resistance and shear resistance in machinery turning area. For sandy loam soil in the east and north part of Lower Saxony, penetration resistance frequently exceeded 3 MPa, reaching >5 MPa at 40 cm, which is above root limiting thresholds. Compared to main field zone, bulk density in machinery turning area increased by 2-5%, with silty loam field exhibiting the largest increase of bulk density. Additionally, soil pore functions of Ka and Ks in machinery turning area exhibited obvious decline compared to field area especially in the subsoil of silty loam and sandy loam fields. For both machinery turning area and field area, a significant correlation was found between hydraulic conductivity and soil bulk density (R2=0.21, p=0.023) in topsoil with ρb from 1.25~1.60 g cm-3, while in subsoil with ρb from 1.45~1.65 g cm-3 no such correlation was found, indicating the pore functions in subsoil mainly depends on connective pores during the structure formation process. These results demonstrate that traffic-induced subsoil compaction is widely altering soil physical structure and pore functions in Lower Saxony, and the texture-dependent responses highlight the need for specific compaction mitigation strategies during the future field managements.
Title: Field-scale Assessments of Subsoil Compaction and Soil Structural Functions in Lower Saxony, Germany
Description:
Subsoil compaction a one of the major threats for crop production and soil ecological functioning in Europe.
To quantify its field-scale extent, field investigations were conducted on 26 agricultural fields across Lower Saxony state in northern Germany, covering four dominant soil textures (clay loam, sandy loam, silt, and silty loam) and two field management zones (machinery turning area and main field area).
In-situ measurements of penetration resistance and shear strength were conducted on field at 10 cm (topsoil) and 40 cm (subsoil), and bulk density (ρb), saturated hydraulic conductivity (Ks), air permeability (Ka) were measured on undisturbed soil samples at the same depth.
The results showed that most machinery turning zones showed clear signs of subsoil compaction.
About 80% fields showed 5~60% higher penetration resistance and shear resistance in machinery turning area.
For sandy loam soil in the east and north part of Lower Saxony, penetration resistance frequently exceeded 3 MPa, reaching >5 MPa at 40 cm, which is above root limiting thresholds.
Compared to main field zone, bulk density in machinery turning area increased by 2-5%, with silty loam field exhibiting the largest increase of bulk density.
Additionally, soil pore functions of Ka and Ks in machinery turning area exhibited obvious decline compared to field area especially in the subsoil of silty loam and sandy loam fields.
For both machinery turning area and field area, a significant correlation was found between hydraulic conductivity and soil bulk density (R2=0.
21, p=0.
023) in topsoil with ρb from 1.
25~1.
60 g cm-3, while in subsoil with ρb from 1.
45~1.
65 g cm-3 no such correlation was found, indicating the pore functions in subsoil mainly depends on connective pores during the structure formation process.
These results demonstrate that traffic-induced subsoil compaction is widely altering soil physical structure and pore functions in Lower Saxony, and the texture-dependent responses highlight the need for specific compaction mitigation strategies during the future field managements.
Related Results
Protecting the subsoil from compaction through conservation management.
Protecting the subsoil from compaction through conservation management.
The intensification of agriculture has increased production but has also had negative effects on the soil. One negative effect of intensified management is soil compaction caused b...
Estimating subsoil diffusivity and respiration by inverse modelling: results from first case studies
Estimating subsoil diffusivity and respiration by inverse modelling: results from first case studies
Soils are important terrestrial biological reactors and play a central role in the global carbon (C) and nitrogen (N ) cycle. Soils can store large amounts of C and N, but they als...
Soybean Growth and Yield as Affected by Surface and Suboil Compaction
Soybean Growth and Yield as Affected by Surface and Suboil Compaction
AbstractAxle loads from wheel traffic on farmland ranges from less than 4.5 Mg axle−1 to over 20 Mg axle−1. Loads of <4.5 Mg axle−1 generally cause compaction only in the upper ...
Ecological soil physics as section of ecological soil science
Ecological soil physics as section of ecological soil science
Nowadays, there is a general penetration of ecology in other related sciences. Soil science is not an exception. To the evidence of this, the works of soil scientists may serve, th...
Directional Compaction
Directional Compaction
New true-triaxial experiments of sandstone compaction under
non-hydrostatic load 19 demonstrate directional (non-isotropic)
compaction. 20 We introduce a directional compaction...
Corn Growth and Yield as Affected by Surface and Subsoil Compaction
Corn Growth and Yield as Affected by Surface and Subsoil Compaction
AbstractWheel traffic of harvesting operations on agricultural fields often carries compactive loads in excess of 8 Mg. Consequently, soil physical properties may be affected to de...
Soil compaction and soil management – a review
Soil compaction and soil management – a review
Abstract
Soil compaction is an important component of the land degradation syndrome which is an issue for soil management throughout the world. It is a long stand...
Soil and alfalfa response after amelioration of subsoil acidity in a fine sandy loam Podzol in Prince Edward Island
Soil and alfalfa response after amelioration of subsoil acidity in a fine sandy loam Podzol in Prince Edward Island
Subsoils in Prince Edward Island have poor chemical and often physical quality for root growth that may present a barrier to development of alfalfa (Medicago sativa L.). This study...

