ArticleGeoderma2020
Soil degradation and recovery - Changes in organic matter fractions and structural stability.
Article in Geoderma, 2020. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 9 papers.
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Who cites it
9 citing papers in PubMed.
- Impact of solid waste disposal on heavy metals concentration and distribution in a naturally remediated landfill site.Environmental monitoring and assessment · 2026Article
- Urbanization accelerates soil degradation in peri-urban compared to rural farms.Scientific reports · 2025Article
- Utilization of post-fermentation sludge as a soil structure and strength conditioner.Scientific reports · 2025Article
- Climate change and geo-environmental factors influencing desertification: a critical review.Environmental science and pollution research international · 2024Article
- Co-inoculation of fungi and desert cyanobacteria facilitates biological soil crust formation and soil fertility.Frontiers in microbiology · 2024Article
- Data management challenges for artificial intelligence in plant and agricultural research.F1000Research · 2021Article
- Environmental changes in Yellow River Delta with terrace construction and agricultural cropping.PeerJ · 2021Article
- Short-term changes in soil pore size distribution: Impact of land use.Soil & tillage research · 2020Article
- Soil organic matter widens the range of water contents for tillage.Soil & tillage research · 2018Article
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Authors and funding
6 authors.
Funding
No grant is acknowledged in the PubMed record.
Abstract
The combination of concurrent soil degradation and restoration scenarios in a long-term experiment with contrasting treatments under steady-state conditions, similar soil texture and climate make the Highfield land-use change experiment at Rothamsted Research unique. We used soil from this experiment to quantify rates of change in organic matter (OM) fractions and soil structural stability (SSS) six years after the management changed. Soil degradation included the conversion of grassland to arable and bare fallow management, while soil restoration comprised introduction of grassland in arable and bare fallow soil. Soils were tested for clay dispersibility measured on two macro-aggregate sizes (DispClay 1-2 mm and DispClay 8-16 mm) and clay-SOM disintegration (DI, the ratio between clay particles retrieved without and with SOM removal). The SSS tests were related to soil organic carbon (SOC), permanganate oxidizable C (POXC) and hot water-extractable C (HWC). The decrease in SOC after termination of grassland was greater than the increase in SOC when introducing grassland. In contrast, it was faster to restore degraded soil than to degrade grassland soil with respect to SSS at macro-aggregate scale. The effect of management changes was more pronounced for 8-16 mm than 1-2 mm aggregates indicating a larger sensitivity towards tillage-induced breakdown of binding agents in larger aggregates. At microscale, SSS depended on SOC content regardless of management. Soil management affected macroscale structural stability beyond what is revealed from measuring changes in OM fractions, underlining the need to include both bonding and binding mechanisms in the interpretation of changes in SSS induced by management.
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