Offered Papers Theme B: Grassland and the Environment
Archived
This content is available here strictly for research, reference, and/or recordkeeping and as such it may not be fully accessible. If you work or study at University of Kentucky and would like to request an accessible version, please use the SensusAccess Document Converter.
Publication Date
2005
Location
Dublin Ireland
Description
Humic substances (HS) provide the major sinks for carbon (C) in soils. Although HS have a degree of resistance to microbial degradation, they are degraded in time. Humin, the HS component in association with the soil mineral colloids, has greatest resistance to degradation. To understand the extent to which soil can be a sink for C it is important to know the soil mineralogy, and to be aware of aspects of the structures of the humic components. Enhanced biological oxidation occurs in soils in long term cultivation. Its effects can be observed by comparing the amounts and compositions of the humic components in cultivated soils with those in the same soil types in long term grassland. Three such paired soils were included in the study as well as three grassland soils that are in new lysimeter studies at the Environmental Research Centre, Johnstown Castle. In a study of the humification process, maize (Zea mays L., a C4 plant, with a ��13C value of the order of 12) was incubated in calcareous organic C-free sand, and the products were studied in the same way as those from the soils.
Citation
Byrne, C. M.; Fay, D.; Ferreira, J. A.; and Hayes, M. H. B., "The Nature of Sequestered Carbon in Different Irish Mineral Soils" (2005). IGC Proceedings (1985-2023). 45.
(URL: https://uknowledge.uky.edu/igc/20/themeB/45)
Included in
Agricultural Science Commons, Agronomy and Crop Sciences Commons, Plant Biology Commons, Plant Pathology Commons, Soil Science Commons, Weed Science Commons
The Nature of Sequestered Carbon in Different Irish Mineral Soils
Dublin Ireland
Humic substances (HS) provide the major sinks for carbon (C) in soils. Although HS have a degree of resistance to microbial degradation, they are degraded in time. Humin, the HS component in association with the soil mineral colloids, has greatest resistance to degradation. To understand the extent to which soil can be a sink for C it is important to know the soil mineralogy, and to be aware of aspects of the structures of the humic components. Enhanced biological oxidation occurs in soils in long term cultivation. Its effects can be observed by comparing the amounts and compositions of the humic components in cultivated soils with those in the same soil types in long term grassland. Three such paired soils were included in the study as well as three grassland soils that are in new lysimeter studies at the Environmental Research Centre, Johnstown Castle. In a study of the humification process, maize (Zea mays L., a C4 plant, with a ��13C value of the order of 12) was incubated in calcareous organic C-free sand, and the products were studied in the same way as those from the soils.
