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Mineralisation and sorption of dissolved organic nitrogen compounds in litter and soil from sugarcane fields. / Mariano, Eduardo; Jones, Davey L.; Hill, Paul W. et al.
In: Soil Biology and Biochemistry, Vol. 103, 01.12.2016, p. 522-532.

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Mariano E, Jones DL, Hill PW, Trivelin PCO. Mineralisation and sorption of dissolved organic nitrogen compounds in litter and soil from sugarcane fields. Soil Biology and Biochemistry. 2016 Dec 1;103:522-532. Epub 2016 Oct 14. doi: 10.1016/j.soilbio.2016.10.004

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Mariano, Eduardo ; Jones, Davey L. ; Hill, Paul W. et al. / Mineralisation and sorption of dissolved organic nitrogen compounds in litter and soil from sugarcane fields. In: Soil Biology and Biochemistry. 2016 ; Vol. 103. pp. 522-532.

RIS

TY - JOUR

T1 - Mineralisation and sorption of dissolved organic nitrogen compounds in litter and soil from sugarcane fields

AU - Mariano, Eduardo

AU - Jones, Davey L.

AU - Hill, Paul W.

AU - Trivelin, Paulo C. O.

PY - 2016/12/1

Y1 - 2016/12/1

N2 - Dissolved organic nitrogen (DON) represents an important soluble nutrient pool in soil, however, little is known about the dynamics of DON in the litter and topsoil of Brazilian sugarcane (Saccharum spp.) fields, particularly those that are harvested mechanically, without burning. Therefore, the aim of this study was to determine the microbial mineralisation and sorption affinity of DON compounds in litter and soil from the litter-soil transition zone of two sugarcane plantations located in southeastern Brazil. We directly measured the C mineralisation of 14C-labelled amino acids (mix of 17 amino acids), peptides (l-dialanine and l-trialanine), urea, and protein (isolated from tobacco leaves) by capturing 14CO2 evolved from the litter and soil over 168 h. A sorption assay was performed using the same treatments. We found differences in the organic and mineral N pools of the litter and soil, as well as in microbial community composition. Except for protein in the soil, the DON compounds were taken up rapidly by microbes. However, the C use efficiency was higher for the amino acid mix than for the peptides and urea, indicating more rapid post-uptake catabolism (with subsequent mineralisation as 14CO2) of both compounds. In addition, protein had the highest sorption affinity, especially in soil, and the weak sorption affinity of the amino acids, peptides, and urea indicates moderate bioavailability of these fractions to microbes and plants. We conclude that strong sorption of protein to the solid phase limits its bioavailability and represents a rate limiting step in DON turnover.

AB - Dissolved organic nitrogen (DON) represents an important soluble nutrient pool in soil, however, little is known about the dynamics of DON in the litter and topsoil of Brazilian sugarcane (Saccharum spp.) fields, particularly those that are harvested mechanically, without burning. Therefore, the aim of this study was to determine the microbial mineralisation and sorption affinity of DON compounds in litter and soil from the litter-soil transition zone of two sugarcane plantations located in southeastern Brazil. We directly measured the C mineralisation of 14C-labelled amino acids (mix of 17 amino acids), peptides (l-dialanine and l-trialanine), urea, and protein (isolated from tobacco leaves) by capturing 14CO2 evolved from the litter and soil over 168 h. A sorption assay was performed using the same treatments. We found differences in the organic and mineral N pools of the litter and soil, as well as in microbial community composition. Except for protein in the soil, the DON compounds were taken up rapidly by microbes. However, the C use efficiency was higher for the amino acid mix than for the peptides and urea, indicating more rapid post-uptake catabolism (with subsequent mineralisation as 14CO2) of both compounds. In addition, protein had the highest sorption affinity, especially in soil, and the weak sorption affinity of the amino acids, peptides, and urea indicates moderate bioavailability of these fractions to microbes and plants. We conclude that strong sorption of protein to the solid phase limits its bioavailability and represents a rate limiting step in DON turnover.

KW - Carbon cycling

KW - Nitrogen cycling

KW - Amino acid

KW - Peptide

KW - Urea

KW - Protein

U2 - 10.1016/j.soilbio.2016.10.004

DO - 10.1016/j.soilbio.2016.10.004

M3 - Article

VL - 103

SP - 522

EP - 532

JO - Soil Biology and Biochemistry

JF - Soil Biology and Biochemistry

SN - 0038-0717

ER -