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The soil microbial community and plant biomass differentially contribute to the retention and recycling of urinary-N in grasslands

Abstract:
Highlights•15N-labelled urine was traced into plant, microbial and leaching pools in a grassland mesocosm.•Leaching losses were reduced, and plant uptake increased during periods of low rainfall.•Microbial uptake of urinary-N occurred via mineralisation-immobilisation and intact pathways.•Microbial assimilation was dominated by bacteria over fungi.AbstractUrine patches in grazed systems are hotspots for nitrogen (N) cycling and losses to the wider environment. Retention and subsequent recycling of urinary-N is key to minimise losses and increase ecosystem nitrogen use efficiency. Biosynthesis into the microbial organic N pool is an important N pathway but this has not been directly quantified in a urine patch. Herein, we present the results of a time course experiment using soil mesocosms sown with perennial ryegrass (Lolium perenne L.) and treated with 15N-labelled sheep urine to determine partitioning of the applied N between plant, soil biomass pools and leaching losses following simulated rainfall events. 15N-tracing used bulk and compound-specific 15N-stable isotope probing (SIP) to determine the fate of urinary N. Initial high leaching losses (233 kg N ha−1) were comprised of native soil N, ammonium and nitrate derived from urine by urea hydrolysis and nitrification, respectively. Leaching subsequently decreased whilst uptake into plant biomass and microbial biosynthesis increased during periods of low rainfall. Uptake into above and belowground plant biomass was the largest fate of urinary-15N after 94 d (42%), although assimilation into microbial biomass dominated for ca. 1 month after urine deposition (34%). Compound-specific 15N–SIP of amino acids and amino sugars revealed immobilisation of urinary-N following mineralisation was the dominant pathway for biosynthesis, with incorporation into bacterial organic N pools more rapid than into the fungal biomass. There was also intact utilisation of glycine derived from urine. This study provides clear evidence that direct assimilation of urine-derived N into microbial organic N pools is an important process for retaining N in a urine patch, which will subsequently support plant N supply during microbial turnover
Publication status:
Published
Peer review status:
Peer reviewed

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Publisher copy:
10.1016/j.soilbio.2023.109011
Publication website:
https://research.bangor.ac.uk/portal/files/56690154/1_s2.0_S0038071723000731_main.pdf

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Author
ORCID:
0000-0001-6335-1690
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Author
ORCID:
0000-0002-0605-3918
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ORCID:
0000-0002-7703-8475
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Author
ORCID:
0000-0002-8479-8157


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Funder identifier:
10.13039/501100000270


Publisher:
Elsevier
Journal:
Soil Biology and Biochemistry More from this journal
Volume:
180
Pages:
109011-109011
Article number:
109011
Publication date:
2023-03-16
DOI:
EISSN:
1879-3428
ISSN:
0038-0717


Language:
English
Keywords:
Pubs id:
1598402
Local pid:
pubs:1598402
Source identifiers:
W4327596375
Deposit date:
2026-06-05
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