Carbon turnover (δ13C) and nitrogen mineralization potential of particulate light soil organic matter after rainforest clearing
- 31 December 1996
- journal article
- Published by Elsevier BV in Soil Biology and Biochemistry
- Vol. 28 (12), 1555-1567
- https://doi.org/10.1016/s0038-0717(96)00264-7
Abstract
No abstract availableKeywords
This publication has 30 references indexed in Scilit:
- Estimating the contribution of legumes to soil organic matter build up in mixed communities ofSoil Biology and Biochemistry, 1996
- Structural and dynamic properties of soil organic-matter as reflected by 13C natural-abundance, pyrolysis mass-spectrometry and solid-state 13C NMR-spectroscopy in density fractions of an oxisol under forest and pastureSoil Research, 1995
- Particulate Soil Organic‐Matter Changes across a Grassland Cultivation SequenceSoil Science Society of America Journal, 1992
- Effect of tillage on soil organic carbon mineralization estimated from 13C abundance in maize fieldsEuropean Journal of Soil Science, 1990
- Assay for microbial biomass based on ninhydrin-reactive nitrogen in extracts of fumigated soilsSoil Biology and Biochemistry, 1988
- Soil Organic Matter Turnover in Long‐term Field Experiments as Revealed by Carbon‐13 Natural AbundanceSoil Science Society of America Journal, 1988
- Natural 13C abundance as a tracer for studies of soil organic matter dynamicsSoil Biology and Biochemistry, 1987
- Depletion of 13C in lignin and its implications for stable carbon isotope studiesNature, 1987
- Long term trends in fertility of soils under continuous cultivation and cereal cropping in southern Queensland. IV. Loss of organic carbon from different density functionsSoil Research, 1986
- Chloroform fumigation and the release of soil nitrogen: The effects of fumigation time and temperatureSoil Biology and Biochemistry, 1985