The Non-Limiting and Least Limiting Water Ranges for Soil Nitrogen Mineralization
Author:
Affiliation:
1. Greenhouse & Processing Crops Research Centre; Agriculture & Agri-Food Canada; Harrow ON Canada N0R 1G0
2. Dep. of Land Resource Science; Univ. of Guelph; Guelph ON Canada N1G 2W1
Funder
Ontario Research Enhancement Program
Publisher
Wiley
Subject
Soil Science
Link
http://onlinelibrary.wiley.com/wol1/doi/10.2136/sssaj2003.1388/fullpdf
Reference34 articles.
1. Nitrogen mineralization and microbial biomass as affected by soil compaction;Breland;Soil Biol. Biochem.,1996
2. The sensitivity of shoot growth of corn to the least limiting water range of soils;Da Silva;Plant Soil,1996
3. Factors contributing to temporal stability in spatial patterns of water content in the tillage zone;Da Silva;Soil Tillage Res.,2001
4. Influence of soil compaction on carbon and nitrogen mineralization of soil organic matter and crop residues;De Neve;Biol. Fertil. Soils,2000
5. Nitric oxide and nitrous oxide production from soil: Water and oxygen effects;Drury;Soil Sci. Soc. Am. J.,1992
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