Microbial uptake of low‐molecular‐weight organic substances out‐competes sorption in soil

Low‐molecular‐weight organic substances (LMWOS) such as amino acids, sugars and carboxylates, are rapidly turned over in soil. Despite their importance, it remains unknown how the competition between microbial uptake and sorption to the soil matrix affects the LMWOS turnover in soil solution. This study describes the dynamics of LMWOS fluxes (10 µm) in various pools (dissolved, sorbed, decomposed to CO2 and incorporated into microbial biomass) and also assesses the LMWOS distribution in these pools over a very wide concentration range (0.01–1000 µm). Representatives of each LMWOS group (glucose for sugars, alanine for amino acids, acetate for carboxylates), uniformly 14C‐labelled, were added to sterilized or non‐sterilized soil and analysed in different pools between 1 minute and 5.6 hours after addition. LMWOS were almost completely taken up by microorganisms within the first 30 minutes. Surprisingly, microbial uptake was much faster than the physicochemical sorption (estimated in sterilized soil), which needed 60 minutes to reach quasi‐equilibrium for alanine and about 400 minutes for glucose. Only acetate sorption was instantaneous. At a concentration of 100 µm, microbial decomposition after 4.5 hours was greater for alanine (76.7 ± 1.1%) than for acetate (55.2 ± 0.9%) or glucose (28.5 ± 1.5%). In contrast, incorporation into microbial biomass was greater for glucose (59.8 ± 1.2%) than for acetate (23.4 ± 5.9%) or alanine (5.2 ± 2.8%). Between 10 and 500 µm, the pathways of the three LMWOS changed: at 500 µm, alanine and acetate were less mineralized and more was incorporated into microbial biomass than at 10 µm, while glucose incorporation decreased. Despite the fact that the LMWOS concentrations in soil solution were important for competition between sorption and microbial uptake, their fate in soil is mainly determined by microbial uptake and further microbial transformations. For these substances, which represent the three main groups of LMWOS in soil, the microbial uptake out‐competes sorption.

[1]  G. Neumann,et al.  Rhizodeposition of maize: Short-term carbon budget and composition , 2010 .

[2]  Y. Kuzyakov,et al.  Sorption, microbial uptake and decomposition of acetate in soil: transformations revealed by position-specific 14C labeling. , 2010 .

[3]  Y. Kuzyakov,et al.  Root uptake of N-containing and N-free low molecular weight organic substances by maize: a 14C/15N tracer study , 2008 .

[4]  Y. Kuzyakov,et al.  Microbial utilization and mineralization of [14C]glucose added in six orders of concentration to soil , 2008 .

[5]  David L. Jones,et al.  Decoupling of microbial glucose uptake and mineralization in soil , 2008 .

[6]  Y. Kuzyakov,et al.  Carbohydrate and amino acid composition of dissolved organic matter leached from soil , 2007 .

[7]  Y. Kuzyakov,et al.  Three-source partitioning of CO2 efflux from soil planted with maize by 13C natural abundance fails due to inactive microbial biomass , 2006 .

[8]  Davey L. Jones,et al.  Glucose uptake by maize roots and its transformation in the rhizosphere , 2006 .

[9]  M. C. Hermosín,et al.  Sorption and leaching behaviour of polar aromatic acids in agricultural soils by batch and column leaching tests , 2005 .

[10]  V. H. Alvarez,et al.  Diffusive flux of cationic micronutrients in two Oxisols as affected by low‐molecular‐weight organic acids and cover‐crop residue , 2005 .

[11]  N. Menzies,et al.  Competitive sorption reactions between phosphorus and organic matter in soil: a review , 2005 .

[12]  P. Nannipieri,et al.  Microbial diversity and soil functions , 2003 .

[13]  Davey L. Jones,et al.  Low molecular weight organic acid adsorption in forest soils: effects on soil solution concentrations and biodegradation rates , 2003 .

[14]  David L. Jones,et al.  Biodegradation of low molecular weight organic acids in coniferous forest podzolic soils , 2002 .

[15]  Ji‐Zheng He,et al.  Adsorption of phosphate and tartrate on hydroxy-aluminum-oxalate precipitates , 2000 .

[16]  David L. Jones,et al.  Mineralization of Amino Acids Applied to Soils Impact of Soil Sieving, Storage, and Inorganic Nitrogen Additions , 1999 .

[17]  A. Hodge,et al.  Biodegradation kinetics and sorption reactions of three differently charged amino acids in soil and their effects on plant organic nitrogen availability , 1999 .

[18]  Davey L. Jones Amino acid biodegradation and its potential effects on organic nitrogen capture by plants , 1999 .

[19]  David L. Jones Organic acids in the rhizosphere – a critical review , 1998, Plant and Soil.

[20]  Davey L. Jones,et al.  Influence of sorption on the biological utilization of two simple carbon substrates , 1998 .

[21]  D. Jones,et al.  Sorption of organic acids in acid soils and its implications in the rhizosphere , 1998 .

[22]  Y. Kuzyakov,et al.  CO2 efflux by rapid decomposition of low molecular organic substances in soils , 1998 .

[23]  Y. Kuzyakov The role of amino acids and nucleic bases in turnover of nitrogen and carbon in soil humic fractions , 1997 .

[24]  W. Jury,et al.  Description of Simazine Transport with Rate‐Limited, Two‐Stage, Linear and Nonlinear Sorption , 1995 .

[25]  P. Kuikman,et al.  Microbial utilization of 14C[U]glucose in soil is affected by the amount and timing of glucose additions , 1994 .

[26]  Deutsche Ausgabe World Reference Base for Soil Resources 2006 , 2007 .

[27]  R. Buresh,et al.  Soil solution sampling for-organic acids in rice paddy soils , 2006 .

[28]  D. Jones,et al.  Organic acid behavior in soils – misconceptions and knowledge gaps , 2004, Plant and Soil.

[29]  Davey L. Jones,et al.  Organic acid behaviour in a calcareous soil: Sorption reactions and biodegradation rates. , 2001 .

[30]  A. Guckert,et al.  Short-term utilisation of 14C-[U]glucose by soil microorganisms in relation to carbon availability , 2001 .

[31]  J. Deckers,et al.  World Reference Base for Soil Resources , 1998 .

[32]  Y. Kuzyakov,et al.  Incorporation of 14C and 15N amino acids and nucleic bases into humus and the turnover of atomic-molecular composition , 1993 .

[33]  K. Loague,et al.  Statistical and graphical methods for evaluating solute transport models: Overview and application , 1991 .

[34]  Ingrid Kraffczyk,et al.  Soluble root exudates of maize: Influence of potassium supply and rhizosphere microorganisms. , 1984 .