Freeze–Thaw Effects on Sorption Desorption of Ammonium in Wetland Soils

Chapter
Part of the Springer Theses book series (Springer Theses)

Abstract

Ammonium ions (NH4 +) are a primary form of mineralized nitrogen (N) in most flooded wetland soils. NH4 + ions can be adsorbed by plants or be electrostatically held on negatively charged surfaces of soil particles. They can be prevented from further oxidation and are stable in wetland soils because of their anaerobic nature.

Keywords

Sorption Capacity Cation Exchange Capacity Natural Wetland Wetland Soil Sanjiang Plain 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

References

  1. Avnimelech Y, Laher M. Ammonium volatilization from soils: Equilibrium considerations [J]. Soil Sci Soc Am J. 1977;41:1080–4.CrossRefGoogle Scholar
  2. Bedard-Haughn A, Matson AL, Pennock DJ. Land use effects on gross nitrogen mineralization, nitrification, and N2O emissions in ephemeral wetlands. Soil Biol Biochem. 2006; 38:3398–3406.Google Scholar
  3. Fenn LB, Datcha JE, Wo E. Substitution of ammonium and potassium for added calcium in reduction of ammonia loss from surfaced-applied urea. Soil Sci Soc Am J. 1982;46:771–6.CrossRefGoogle Scholar
  4. Fitzhugh RD, Driscoll CT, Groffman PM, Tierney GL, Fahey TJ, Hardy JP. Effects of soil freezing, disturbance on soil solution nitrogen, phosphorus, and carbon chemistry in a northern hardwood ecosystem. Biogeochemistry. 2001;56:215–38.CrossRefGoogle Scholar
  5. Harter RD, Baker DE. Applications and misapplications of Langmuir equation to soil sorption phenomena. Soil Sci Soc Am J. 1977;41:1077–80.CrossRefGoogle Scholar
  6. Henry HAL. Soil freeze–thaw cycle experiments: trends, methodological weaknesses and suggested improvements. Soil Biol Biochem. 2007;39:977–86.CrossRefGoogle Scholar
  7. Lipson DA, Schmidt SK. Seasonal changes in an alpine soil bacterial community in the Colorado rocky mountains. Appl Environ Microbiol. 2004;70:2867–79.CrossRefGoogle Scholar
  8. Lumbanraja J, Evangelou VP. Adsorption–desorption of potassium and ammonium at low cation concentrations in three Kentucky subsoils. Soil Sci. 1994;157:269–78.CrossRefGoogle Scholar
  9. Maehlum T, Jenssen PD, Warne WS. Cold-climate constructed wetlands. Water Sci Technol. 1995;32:95–101.Google Scholar
  10. Matschonat G, Matzner E. Soil chemical properties affecting NH4 + sorption in forest soils. J Plant Nutr Soil Sci. 1996;159:505–11.CrossRefGoogle Scholar
  11. Patrick WH, Reddy KR. Nitrification–denitrification reactions in flooded soils and water bottoms: dependence on oxygen supply and ammonium diffusion. J Environ Qual. 1976;5:469–72.CrossRefGoogle Scholar
  12. Phillips IR. Nitrogen availability and sorption under alternating waterlogged and drying conditions. Commun Soil Sci Plant Anal. 1999;30:1–20.CrossRefGoogle Scholar
  13. Phillips IR, Greenway M. Changes in water-soluble and exchangeable ions, cation exchange capacity, and phosphorus (max) in soils under alternating waterlogged and drying conditions. Commun Soil Sci Plant Anal. 1998;29:51–66.CrossRefGoogle Scholar
  14. Schadt CW, Martin AP, Lipson DA, et al. Seasonal dynamics of previously unknown fungal lineages in tundra soils. Science. 2003;301:1359–61.CrossRefGoogle Scholar
  15. Six J, Bossuyt H, Degryse S, et al. A history of research on the link between (micro) aggregates, soil biota, and soil organic matter dynamics. Soil Tillage Res. 2004;79:7–31.CrossRefGoogle Scholar
  16. Sjursen H, Michelsen A, Holmstrup M. Effects of freeze–thaw cycles on microarthropods and nutrient availability in a sub-Arctic soil. Appl Soil Ecol. 2005;28:79–93.CrossRefGoogle Scholar
  17. Tang Y, Feng K, Yin SX. Preferential fixation of ammonium to potassium by soils. Pedosphere. 1996;6:35–8.Google Scholar
  18. Thompson TL, Blackmer AM. Quantity–Intensity relationships of soil ammonia in long-term rotation plots. Soil Sci Soc Am J. 1992;56:494–8.CrossRefGoogle Scholar
  19. Unger PW. Overwinter changes in physical-properties of no-tillage soil. Soil Sci Soc Am J. 1991;55:778–82.CrossRefGoogle Scholar
  20. Vandenbruwane J, De Neve S, Qualls RG, Sleutel S, Hofman G. Comparison of different isotherm models for dissolved organic carbon (DOC) and nitrogen (DON) sorption to mineral soil. Geoderma. 2007;139:144–53.CrossRefGoogle Scholar
  21. Wang FL, Alva AK. Ammonium adsorption and desorption in sandy soils. Soil Sci Soc Am J. 2000;64:1669–74.CrossRefGoogle Scholar
  22. Wang G, Liu J, Zhao H, Wang J, Yu J. Phosphorus sorption by freeze-thaw treated wetland soils derived from a winter-cold zone. Geoderma. 2007;138:153–61.CrossRefGoogle Scholar
  23. Yu XF, ZhangY X, Zou YC, et al. Sorption and desorption of ammonium in wetland soils subject to freeze-thaw. Pedosphere. 2011;21(2):251–8.CrossRefGoogle Scholar

Copyright information

© Springer-Verlag Berlin Heidelberg 2013

Authors and Affiliations

  1. 1.Northeast Institute of Geography and AgroecologyChinese Academy of SciencesChangchunPeople’s Republic of China

Personalised recommendations