Immobilization (soil science)

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Immobilization in soil science is the conversion of inorganic compounds to organic compounds by micro-organisms or plants, by which it is prevented from being accessible to plants.[1] Immobilization is the opposite of mineralization where the inorganic nutrients are taken up by soil microbes making them unavailable for plant uptake.[2] Immobilization process is a biological process controlled by bacteria[3] that consume an inorganic nitrogen and for, amino acids and biological macromolecuels (inorganic forms).[4] Immobilization and mineralization happen continuously and concurrently whereby nitrogen of the decomposing system is transformed steadily from inorganic to organic state by immobilization and back from organic to inorganic state by decay and mineralization.[5]

C:N Ratio[edit]

Whether nitrogen is mineralized or immobilized depends on the C/N ratio of the plant residues.[6] For example, incorporating materials high in carbon to nitrogen ratio such as saw dust and straw will stimulate soil microbial activity,increase demand for nitrogen, leading to immobilization.[7] This is known as priming effect.[8] In general plant residues entering the soil have too little nitrogen for the soil microbial population to convert all of the carbon into their cells. If the C:N ratio of the decomposing plant material is above about 30:1 the soil microbial population may take nitrogen in mineral form (e.g. nitrate). This mineral nitrogen is said to be immobilized. Microorganisms out-compete plants for NH4+ and NO3- during immobilization, and therefore plants can easily become nitrogen deficient.

As carbon dioxide is released via decomposition the C:N ratio of the organic matter decreases, and the microbial demand for mineral nitrogen is decreased. When the C:N ratio falls below about 25:1 further decomposition results in simultaneous mineralization of nitrogen which is in excess to that required by the microbial population.

When decomposition is virtually complete soil mineral nitrogen will be higher than it was initially due to mineralization of the plant residue nitrogen.

Mechanisms of Nitrogen Immobilization

There are two mechanisms of nitrogen immobilization: Nitrogen accumulation in microbial biomass and accumulation of nitrogen in by-products of microbial activity.[9] Nitrogen Accumulation in by-products of microbial activity nitrogen accumulation in decaying plant debris follows a two-phase mechanism Following the initial leaching of soluble materials from fresh detritus, exoenzymes depolymerize the detritus substrate producing reactive carbohydrates, phenolics, small peptides, and amino acids, this is a period whereby microbial growth is rapid. with microbes converting substrate nitrogen and exogenous nitrogen into microbial biomass and exuded products of microbial activity.[10]

References[edit]

  1. ^ Principles and Practices of Soil Science, the soil as a natural resource (4th edition), R.E. White
  2. ^ "Immobilization". lawr.ucdavis.edu. Retrieved 2019-11-20.
  3. ^ Schimel, D. S. (1988-10-01). "Calculation of microbial growth efficiency from15N immobilization". Biogeochemistry. 6 (3): 239–243. doi:10.1007/BF02182998. ISSN 1573-515X.
  4. ^ Batlle-Aguilar, J.; Brovelli, A.; Porporato, A.; Barry, D. A. (2011-04-01). "Modelling soil carbon and nitrogen cycles during land use change. A review". Agronomy for Sustainable Development. 31 (2): 251–274. doi:10.1051/agro/2010007. ISSN 1773-0155.
  5. ^ Kai, Hideaki; Ahmad, Ziauddin; Harada, Togoro (September 1969). "Factors affecting immobilization and release of nitrogen in soil and chemical characteristics of the nitrogen newly immobilized: I. Effect of Temperature on Immobilization and Release of Nitrogen in Soil". Soil Science and Plant Nutrition. 15 (5): 207–213. doi:10.1080/00380768.1969.10432803. ISSN 0038-0768.
  6. ^ R.G. McLaren & K. Cameron Soil Science: Sustainable production and environmental protection (2nd edition), Oxford University Press, (1996) ISBN 0-19-558345-0
  7. ^ Szili-Kovács, Tibor; Török, Katalin; Tilston, Emma L.; Hopkins, David W. (2007-08-01). "Promoting microbial immobilization of soil nitrogen during restoration of abandoned agricultural fields by organic additions". Biology and Fertility of Soils. 43 (6): 823–828. doi:10.1007/s00374-007-0182-1. ISSN 1432-0789.
  8. ^ Bastida, Felipe; García, Carlos; Fierer, Noah; Eldridge, David J.; Bowker, Matthew A.; Abades, Sebastián; Alfaro, Fernando D.; Asefaw Berhe, Asmeret; Cutler, Nick A.; Gallardo, Antonio; García-Velázquez, Laura (2019-08-02). "Global ecological predictors of the soil priming effect". Nature Communications. 10 (1): 3481. doi:10.1038/s41467-019-11472-7. ISSN 2041-1723. PMC 6677791. PMID 31375717.
  9. ^ "Nitrogen Immobilization - an overview | ScienceDirect Topics". www.sciencedirect.com. Retrieved 2019-11-21.
  10. ^ "Nitrogen Immobilization - an overview | ScienceDirect Topics". www.sciencedirect.com. Retrieved 2019-11-21.

See also[edit]