Soil-plant nitrogen isotope composition and nitrogen cycling after biochar applications

Environ Sci Pollut Res Int. 2021 Feb;28(6):6684-6690. doi: 10.1007/s11356-020-11016-3. Epub 2020 Oct 2.

Abstract

Biochar has strong potential to improve nitrogen (N) use efficiency in both agricultural and horticultural systems. Biochar is usually co-applied with full rates of fertiliser. However, the extent to which N cycling can be affected after biochar application to meet plant N requirement remains uncertain. This study aimed to explore N cycling up to 2 years after biochar application. We applied pine woodchip biochar at 0, 10 and 30 t ha-1 (B0, B10, B30, respectively) in a macadamia orchard and evaluated the N isotope composition (δ15N) of soil, microbial biomass and macadamia leaves. Soil total N (TN) and inorganic N pools were also measured up to 2 years after biochar application. Biochar did not alter soil TN but soil NO3--N increased at months 12 and 24 after biochar application. Soil NO3--N concentrations were always over ideal levels of 15 μg g-1 in B30 throughout the study. Stepwise regression indicated that foliar δ15N decreases after biochar application were explained by increased NO3--N concentrations in B30. Foliar TN and photosynthesis were not affected by biochar application. The soil in the high rate biochar plots had excess NO3--N concentrations (over 30 μg g-1) from month 20 onwards. Therefore, N fertiliser applications could be adjusted to prevent excessive N inputs and increase farm profitability.

Keywords: Macadamia integrifolia; Nitrogen isotope composition; Nitrogen retention; Photosynthesis; Wood-based biochar.

MeSH terms

  • Charcoal*
  • Nitrogen / analysis
  • Nitrogen Isotopes
  • Soil*

Substances

  • Nitrogen Isotopes
  • Soil
  • biochar
  • Charcoal
  • Nitrogen