Increased availability of phosphorus after drying and rewetting of a grassland soil: processes and plant use
Author:
Publisher
Springer Science and Business Media LLC
Subject
Plant Science,Soil Science
Link
http://link.springer.com/content/pdf/10.1007/s11104-013-1651-y.pdf
Reference51 articles.
1. Achat DL, Augusto L, Gallet-Budynek A, Bakker MR (2012) Drying-induced changes in phosphorus status of soils with contrasting soil organic matter contents – Implications for laboratory approaches. Geoderma 187–188:41–48. doi: 10.1016/j.geoderma.2012.04.014
2. Adu JK, Oades JM (1978) Physical factors influencing decomposition of organic materials in soil aggregates. Soil Biol Biochem 10(2):109–115
3. Alef K (1995) Soil respiration. In: Alef K, Nannipieri P (eds) Methods in applied soil microbiology and biochemistry. Academic, London, pp 214–219
4. Aponte C, Maranon T, Garcia LV (2010) Microbial C, N and P in soils of Mediterranean oak forests: influence of season, canopy cover and soil depth. Biogeochemistry 101(1–3):77–92. doi: 10.1007/s10533-010-9418-5
5. Appel T (1998) Non-biomass soil organic N - the substrate for N mineralization flushes following soil drying-rewetting and for organic N rendered CaCl2-extractable upon soil drying. Soil Biol Biochem 30(10–11):1445–1456
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