Organo-mineral associations in temperate soils: Integrating biology, mineralogy, and organic matter chemistry

By I. Kögel‐Knabner, G. Guggenberger, M. Kleber, E. Kandeler, K. Kalbitz, S. Scheu, K. Eusterhues, P. Leinweber. 2008

1,213 citations recorded by the source corpus.

Subfields: Environmental Chemistry, Pollution, Soil Science

View Paper: https://www.semanticscholar.org/paper/9ce09564b4745f9196609163a7c94ba4b7079a12

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Environmental Chemistry

1. S. Bender
2. Johan Six
3. Noah Fierer
4. Ji‐Zheng He
5. M. Wallenstein

In Pollution

1. Noah Fierer
2. A. S. Grandy
3. Ji‐Zheng He
4. M. Wallenstein

In Soil Science

1. M. Wallenstein
2. A. S. Grandy
3. Johan Six
4. Eldor A. Paul
5. S. Bender
6. Noah Fierer
7. Ji‐Zheng He
8. J. Mayer

Citations in the corpus

• Searching for unifying principles in soil ecology (2009, background): “texture and mineralogy) that regulate the turnover rates of soil carbon pools (Sollins et al., 1996; Six et al., 2002; Mikutta et al., 2006; Kögel-Knabner et al., 2008).”
• Conceptualizing soil organic matter into particulate and mineral‐associated forms to address global change in the 21st century (2019, background): “Occlusion in large aggregates slows decomposition, but to a lesser degree than mineral association (Kögel‐Knabner et al., 2008; Poeplau et al., 2018; Puget, Chenu, & Balesdent, 2000; Schrumpf et al., 2013).”
• The Microbial Efficiency‐Matrix Stabilization (MEMS) framework integrates plant litter decomposition with soil organic matter stabilization: do labile plant inputs form stable soil organic matter? (2013, background): “Chemical recalcitrance and spatial inaccessibility operate over the short-to-medium term (e.g., decades), whereas matrix stabilization controls SOM persistence over the longterm (e.g., centuries) (Kogel-Knabner et al., 2008).”
• Soil-carbon preservation through habitat constraints and biological limitations on decomposer activity (2008, neutral): “Empirical work of the research program " Soils as source and sink of CO 2 " (Kögel-Knabner et al., 2008a, this issue, pp. 5–13) has consistently revealed that decomposer organisms are specialized towards particular microhabitats and C pools.”
• Linking 3D Soil Structure and Plant-Microbe-Soil Carbon Transfer in the Rhizosphere (2018, background): “The binding of organic matter to mineral surfaces, including oxides, has been reviewed in the literature (Kögel-Knabner et al., 2008) and more recently directly observed at the microscale (Xiao et al.”
• Review on iron availability in soil: interaction of Fe minerals, plants, and microbes (2014, background): “HS increase Fe bioavailability through their Fechelating properties and have redox-reactive properties (Kögel-Knabner et al. 2008).”