Near‐edge X‐ray absorption fine structure (NEXAFS) spectroscopy for mapping nano‐scale distribution of organic carbon forms in soil: Application to black carbon particles
By Johannes Lehmann, Biqing Liang, D. Solomon, M. Lerotic, F. Luizão, J. Kinyangi, T. Schäfer, Sue Wirick, Chris Jacobsen. 2005
325 citations recorded by the source corpus.
Subfields: Ecology, Plant Science, Pollution
View Paper: https://www.semanticscholar.org/paper/2d8d2974498f8d166a411066a2f1a751a642f3dd
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Ecology
- J. Thies
- David E. Crowley
- D. Myrold
- M. Kleber
- Johannes Lehmann
- L. Zeglin
- Matthias C. Rillig
- Piero Morseletto
In Plant Science
- J. Pett‐Ridge
- J. Thies
- David E. Crowley
- D. Myrold
- Johannes Lehmann
- Matthias C. Rillig
- F. Borie
- P. Antunes
In Pollution
Citations in the corpus
- Ultrastructural and chemical study of modern and fossil sporoderms by Scanning Transmission X-ray Microscopy (STXM) (2009, unknown): “, 1996) or to phenols (Lehmann et al., 2005).”
- Biochar physicochemical properties: pyrolysis temperature and feedstock kind effects (2020, background): “…groups or other functional groups with a negative charge in the pH range of soils can be the result of two principally different processes: (1) surface oxidation of the biochar particles themselves and (2) adsorption of highly oxidized organic matter onto biochar surfaces (Lehmann et al. 2005).”
- Nano-scale investigation of the association of microbial nitrogen residues with iron (hydr)oxides in a forest soil O-horizon (2012, background): “First, synchrotron-based scanning transmission X-ray microscopy (STXM) in combination with near-edge X-ray absorption fine structure (NEXAFS) spectroscopy, which has been employed to interrogate structurally intact soil micro-aggregates (Wan et al., 2007; Lehmann et al., 2005; Kinyangi et al., 2006)”
- Biochar effects on soil biota – A review (2011, methodology): “…organic matter in soil (Schmidt and Noack, 2000), and are known to change over time due to weathering processes, interactions with soil mineral and organic matter and oxidation by microorganisms in soil (Lehmann et al., 2005; Cheng et al., 2008; Cheng and Lehmann, 2009; Nguyen et al., 2010).”