Abstract
In-source pyrolysis-field ionization mass spectrometry (Py-FIMS), in combination with complementary elemental, wet-chemical, biochemical, and microbiological data, has been used to characterize humus composition and dynamics in soil samples from several field plots that have been cultivated in long-term experiments under different management conditions.
Thermograms and Py-FI mass spectra of whole-soil samples from field plots that under very different management show significant differences in humus composition, which may be due to varying stages of decomposition of plant residues and humus genesis. The intensity of soil management significantly affects high-molecular-weight subunits such as dimeric lignin0, arylalkyl-, and aliphatic constituents, even though humus quantity is similar for plots under more practically oriented management, such as crop rotation. The differences in molecular humus subunits of soil samples from different plots, in combination with complementary data, demonstrated that less parent (i.e. primary) material is incorporated in the humus matrix under intense soil management conditions. Samples from different field plots can thus be objectively differentiated on the basis of humus properties using multivariate statistical techniques such as principal component and cluster analyses. This statistical discrimination, using Py-FI mass spectra of the samples, corresponds well with microbial biomasses but is somewhat inconsistent with elemental data and results of chemical degradation procedures. The microflora populations in soils under intense management are limited by low availability and/or quality of carbon substrates. The resulting restricted internal nitrogen cycle causes those soils to have a reduced capacity to immobilize N, leading to relative enrichment of heterocyclic nitrogen compounds that are resistant to mineralization.
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Schulten, HR., Hempfling, R. Influence of agricultural soil management on humus composition and dynamics: Classical and modern analytical techniques. Plant Soil 142, 259–271 (1992). https://doi.org/10.1007/BF00010971
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DOI: https://doi.org/10.1007/BF00010971