4.7 Article

Resolving the spatial variability of soil N using fractions of soil organic matter

Journal

AGRICULTURE ECOSYSTEMS & ENVIRONMENT
Volume 147, Issue -, Pages 66-72

Publisher

ELSEVIER SCIENCE BV
DOI: 10.1016/j.agee.2011.06.016

Keywords

MinN; Nested sampling; Physical fractionation; Variogram; Site specific N management; N losses

Funding

  1. National Commission for Scientific and Technological Research (Conicyt - Chile)
  2. University of Concepcion (Chile)
  3. Natural Environment Research Council [bgs05008] Funding Source: researchfish
  4. NERC [bgs05008] Funding Source: UKRI

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The spatial variability of soil nitrogen (N) mineralisation has not been extensively studied, which limits our capacity to make N fertiliser recommendations. Even less attention has been paid to the scale-dependence of the variation. The objective of this research was to investigate the scale-dependence of variation of mineral N (MinN, N-NO3- plus N-NH4+) at within-field scales. The study was based on the spatial dependence of the labile fractions of SOM, the key fractions for N mineralisation. Soils were sampled in an unbalanced nested design in a 4-ha arable field to examine the distribution of the variation of SOM at 30, 10, 1, and 0.12 m. Organic matter in free and intra-aggregate light fractions (FLF and IALF) was extracted by physical fractionation. The variation occurred entirely within 0.12 m for FLF and at 10 m for IALF. A subsequent sampling on a 5-m grid was undertaken to link the status of the SOM fractions to MinN, which showed uncorrelated spatial dependence. A uniform application of N fertiliser would be suitable in this case. The failure of SOM fractions to identify any spatial dependence of MinN suggests that other soil variables, or crop indicators, should be tested to see if they can identify different N supply areas within the field for a more efficient and environmentally friendly N management. (C) 2011 Elsevier BM. All rights reserved.

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