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Soil carbon (C) losses and soil translocation from tillage operations have been identified as causes of soil degradation and soil erosion.
Application of over-winter green cover (e.g. cover crops) as a measure for reducing nitrate losses from tillage land has been frequently investigated, especially in the unsaturated zone.
Stubble cultivation stimulated N mineralisation but the increase in SMN from tillage in September to November was only 3 kg ha−1 after stubble cultivation, compared with 8 kg ha−1 after mouldboard ploughing.
Combined results from batch experiments, XANES spectroscopy and X-ray diffraction suggested chemical transformations of the topsoil as a result from accumulation of organic matter and airing from tillage followed by enhanced weathering of apatite, amphiboles, clay minerals, and iron oxides.
We analyzed water storage potential under assumed full-scale adoption of NT and CT cropping practices in the Palouse region of eastern Washington State by applying the Distributed Hydrology Soil Vegetation Model (DHSVM) with modifications to represent the physical changes to infiltration, evaporation, and runoff that result from tillage management.
The SOC contents and soil erosion phases can be affected by losses or gains of organic C-rich sediments from tillage translocation and erosion, by management input level differences, oxidation, or as a result of land use and landscape position variations.
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We investigated the changes in WSA and soil C at a site in Akame, Mie, Japan, operating a no-tillage with weed mulch management (NWM) system over a chronosequence from 0 to 17 years after conversion from conventional tillage practices (NWM for 0, 5, 10, 15, and 17 years).
In addition, by using more efficient tractors that decreased diesel inputs, emissions from conventional tillage can be reduced by 33% and emissions from no tillage can be reduced by 24%.
Three replicates of composite samples (each a mixture from 5 cores taken randomly) of top soil were collected from plowing tillage and minimum tillage plots at two soil depths (0 8-cm-upper soil and 12–25-cm-deeper soil) in integrated and organic-farming systems in April 20 8-cm-upper
The potential of carbon sequestration by shifting from conventional tillage to no-tillage in agricultural soils is dependent on several factors [41].
Data from conservation tillage demonstration sites operating for 10 years in northern China were used to conduct a comparative study of subsoiling interval under conservation tillage.
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