Search

Incorporation of nitrogen (N) into soil microbial protein is central to the soil N cycle to mitigate N losses and support plant N supply. However, the effect of factors, such as water filled pore space (WFPS), which influence inorganic N transformations and losses, and thus microbial incorporation, are only poorly understood. This work aimed to bridge this gap, using compound-specific 15N-stable isotope probing to quantify microbial assimilation into the largest defined soil organic N pool, protein-N. This approach applied differentially 15N-labelled ammonium nitrate (NH 4 NO 3) to an unfertilised UK grassland in a soil mesocosm study over 10 days. The soil microbial community showed a strong preference for NH 4 + over NO 3 −, which varied with WFPS (85% > 55% > 70%). This preference decreased for amino acids further in biosynthetic proximity to the transamination step in amino acid biosynthesis. Combined incorporation of NH 4 + and NO 3 − increased total hydrolysable amino acid-N concentration linked to WFPS (55% ∼ 85% > 70%). Incorporation rates of applied 15N showed the same trend as NH 4 + preference with WFPS (85% > 55% > 70%), which is related to microbial activity and nutrient mobility. Despite differences in incorporation, when normalised to soil available N, incorporation was comparable in the short-term. Mechanistic control of WFPS via assimilation into the largest soil organic N pool is important to mitigate potential positive feedbacks to N losses and support N supply to plants. • Total hydrolysable amino acid concentration increased at 55% and 85% WFPS. • Incorporation into the soil microbial protein pool showed a preference for NH 4 + over NO 3 −. • Preference of amino acids depended on biosynthetic proximity to transamination. • 15N incorporation into soil microbial protein was influenced by WFPS (85% > 55%>70%). [ABSTRACT FROM AUTHOR]

Urine 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. [Display omitted] • 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. [ABSTRACT FROM AUTHOR]

Efficient fertiliser nitrogen (N) management is critical to global food production and ecosystem health. Considering sheep grazing systems as whole ecosystems, and quantifying key ecosystem services provided by the soil microbial community, including plant N supply and N pollution mitigation, is essential in assessments of N use efficiency (NUE). Using a systems approach, we disassembled a low-intensity sheep (>5 ewe ha−1) grazed grassland, dominated by Lolium perenne , into a series of interlinked 15N-tracer experiments in North Wales during a summer growing season to assess fertiliser-N partitioning. 15N was traced into soil microbial protein-N via compound-specific amino acid 15N-stable isotope probing, with subsequent integration to provide a whole-system perspective. Retention of feed-N into sheep was low (11 %), despite high grass 15N-fertiliser uptake (58 %). The majority of grazed-N re-entered the soil N-cycle as excreta (47 % of total 15N) during the peak growing season. Quantifying 15N-assimilation into soil microbial protein (0–15 cm) demonstrated the central role soil microbes occupy in capturing excess fertiliser (16 %) and urinary-N (8 %) of the total 15N-fertiliser applied, thereby reducing N losses and subsequently supporting plant N supply. This approach emphasises how future management of moderate intensity grazing systems should target sheep NUE, alongside the role of the soil microbial community to retain, and later recycle N, for plant supply, optimising essential ecosystem service provisioning. • Interlinked whole ecosystem 15N tracing study for holistic approach • Mass balance of N cycle through grazing system revealed importance of soil retention to reduce losses. • Microbial assimilation of fertiliser and urine is a major fate of applied 15N. [ABSTRACT FROM AUTHOR]