Skip to main page content
U.S. flag

An official website of the United States government

Dot gov

The .gov means it’s official.
Federal government websites often end in .gov or .mil. Before sharing sensitive information, make sure you’re on a federal government site.

Https

The site is secure.
The https:// ensures that you are connecting to the official website and that any information you provide is encrypted and transmitted securely.

Access keys NCBI Homepage MyNCBI Homepage Main Content Main Navigation
. 2019 Oct 31;10(1):4981.
doi: 10.1038/s41467-019-12948-2.

Soil net nitrogen mineralisation across global grasslands

Affiliations

Soil net nitrogen mineralisation across global grasslands

A C Risch et al. Nat Commun. .

Abstract

Soil nitrogen mineralisation (Nmin), the conversion of organic into inorganic N, is important for productivity and nutrient cycling. The balance between mineralisation and immobilisation (net Nmin) varies with soil properties and climate. However, because most global-scale assessments of net Nmin are laboratory-based, its regulation under field-conditions and implications for real-world soil functioning remain uncertain. Here, we explore the drivers of realised (field) and potential (laboratory) soil net Nmin across 30 grasslands worldwide. We find that realised Nmin is largely explained by temperature of the wettest quarter, microbial biomass, clay content and bulk density. Potential Nmin only weakly correlates with realised Nmin, but contributes to explain realised net Nmin when combined with soil and climatic variables. We provide novel insights of global realised soil net Nmin and show that potential soil net Nmin data available in the literature could be parameterised with soil and climate data to better predict realised Nmin.

PubMed Disclaimer

Conflict of interest statement

The authors declare no competing interests.

Figures

Fig. 1
Fig. 1
Realised soil net N mineralisation. a Photo of a cylinder used during field measurements. A mesh-bag filled with ion-exchange resin is visible at the top of the cylinder. b Schematic N mineralisation processes as found within our cylinders. An exchange resin bag on top captured atmospheric N deposition/N in run-off, another resin bag at the bottom of the cylinder captured N leaching from the soil column. Details on calculation of soil net N mineralisation based on the variables measured are given in the “Methods” section
Fig. 2
Fig. 2
Geographic and climatic distribution of experimental sites. a Location of the 30 NutNet sites where the field experiment was conducted and soil samples were collected for laboratory analyses. b The 30 study sites represent a wide range of mean annual temperature (MAT) and mean annual precipitation (MAP). Our sites also cover a wide range of soil edaphic conditions as described in the main text and shown in Supplementary Table 2. Source data are provided in the source data file
Fig. 3
Fig. 3
Conceptual model on the expected causal relationships between environmental variables, soil properties and potential soil net Nmin to estimate realised soil net Nmin. The conceptual model is based on hypotheses derived from the literature and our linear mixed effects model results (see Table 1 for hypotheses and references). Tvar = temperature variability, T.q.wet = temperature of the wettest quarter
Fig. 4
Fig. 4
Global patterns in realised and potential soil net N mineralisation (soil net Nmin). a Realised soil net Nmin at 30 NutNet sites ordered according to increasing realised soil net Nmin. b Potential soil net Nmin at the 30 NutNet sites. Order of sites according to a. The box represents the median (50th percentile), 25th and 75th percentile of the data for each site. The whiskers represent 1.5 times the inter-quartile range. Source data are provided in the source data file
Fig. 5
Fig. 5
Global drivers of realised soil net N mineralisation (soil net Nmin). a Structural equation modelling diagram representing connections between climatic conditions, soil physical, chemical and biological properties found to influence realised and potential soil net N mineralisation. The width of the connections represents estimates of the standardised path coefficients, with solid lines representing a positive relationship and dashed lines a negative relationship. Significant connections and R2 are shown in black, non-significant ones in light-grey. b Standardised total, direct and indirect effects of variables associated with realised soil net N min. p < 0.1, *p < 0.05, **p < 0.01, ***p < 0.001. Clay content = soil clay content, Microbial biomass = soil microbial biomass, Tvar = temperature seasonality, T.q.wet = temperature of the wettest quarter. The total number of observations = 85, the total number of sites = 30

Similar articles

Cited by

References

    1. Elser JJ, et al. Global analysis of nitrogen and phosphorus limitation of primary producers in freshwater, marine and terrestrial ecosystems. Ecol. Lett. 2007;10:1135–1142. doi: 10.1111/j.1461-0248.2007.01113.x. - DOI - PubMed
    1. Harpole WS, et al. Nutrient co-limitation of primary producer communities. Ecol. Lett. 2011;14:852–862. doi: 10.1111/j.1461-0248.2011.01651.x. - DOI - PubMed
    1. Fay PA, et al. Grassland productivity limited by multiple nutrients. Nat. Plants. 2015;1:1–5. doi: 10.1038/nplants.2015.80. - DOI - PubMed
    1. Neff JC, et al. Variable effects of nitrogen additions on the stability and turnover of soil carbon. Nature. 2002;419:915–917. doi: 10.1038/nature01136. - DOI - PubMed
    1. Schimel JP, Bennett J. Nitrogen mineralization: challenges of a changing paradigm. Ecology. 2004;85:591–602. doi: 10.1890/03-8002. - DOI

Publication types