Available C and N Affect the Utilization of Organic N by Soil Microorganisms

Release Time:2016-10-25 Big Small

Nitrogen is an essential element for growth and development of plants and microorganisms. Eighty five percent of Nitrogen in soil exists in organic form. By traditional view point, the organic N in soil must be mineralized into in-organic form before it is used by microorganisms. However, recent research showed that small-molecule organic N such as those in amino acids, may be taken up directly as intact molecules or de-aminated extra-cellularly followed by the uptake of ammonium (NH4) absorbed by plants and microorganisms and termed as Direct Rout. The ratio of direct use of organic small molecule N by Soil affects the quantitative characterization of N use efficiency and is one of the new hot spot in the research on N cycling in farmland ecosystem.

Associate Prof ZHANG Lili in research group of Plant Nutrition and Fertilizer has been working on this subject since 2011. Recently, she tested the effect of available C (glucose) and N (ammonium sulfate) on absorption of amino acid by soil microorganism using a laboratory experiment with glycine, NH4 and different levels of glucose. The results show that the when Nitrogen source (NH4) added alone, amino acid is used mainly by the direct route. When high level carbon source-glucose was also added, initially, the major route of N absorption was direct amino acid absorption because high amount of glucose strongly promoted the growth of the microbial biomass, resulting in increased C and N requirements. With consume of Carbon source, the route gradually shifted from direct uptake to N uptake after extracellular deamination followed by uptake of NH4 or intracellular deamination and excretion of NH4.

The results indicate that amino acids can not only supply N but also C for proliferation of soil microorganisms. In the future, more work should focus on the assimilation competition of organic N between plants roots and soil microorganisms.

The results were published entitled as Available C and N Affect the Utilization of Glycine by Soil Microorganisms in Geoderma (2016, 283:28-32, DOIorg/10.1016/j.geoderma.2016.07.022).

The work was supported by the state key R & D project 2016YFD0300904and NNSFC (41571290; 41301253; 41401291).

 

Full text URL: http://www.sciencedirect.com/science/article/pii/S0016706116303160

Abstract: Soil microorganisms utilize a wide range of mineral and organic nitrogen (N) sources. Organic molecules, such as amino acids, may be taken up directly as intact molecules or deaminated extracellularly followed by the uptake of ammonium (NH4+). We determined the effect of available C (glucose) and N (ammonium sulfate) on the uptake of amino acid by microorganisms using a laboratory incubation experiment with glycine, NH4+ and different levels of glucose. A 15N-labelling mirror image approach was used to determine the mineralization rate of glycine-N and gross N mineralization over a 60 day-period in treatments with C and N additions. The pre-incubation experiment showed that added glycine was consumed within 24 h in all treatments. With addition of NH4+, only 11% to 44% of glycine N was mineralized, showing that the direct uptake dominated when available C was limited. In soil amended with NH4+ and a high level of glucose (C/N ratio = 30), mineralization of glycine N remained low (5%) initially but increased to 65% by day 60, indicating a shift either from direct uptake of intact amino acids to extracellular deamination followed by uptake of NH4+, or increased intracellular deamination and excretion of NH4+. The results indicate that microorganisms can potentially satisfy both C and N requirements through direct assimilation of amino acids depending on the availability of soil C and N.

Publication Name: Yang Lijie, Zhang Lili, Daniel Geisseler, Wu Zhijie, Gong Ping, Xue Yan, Yu Chunxiao, Juan Yinghua,William R.Horwath. 

Email: llzhang@iae.ac.cn