Modelling the Interactions of Soils, Climate, and Management for Grass Production in England and Wales

Michail L. Giannitsopoulos*, Paul Burgess, Goetz M Richter, Matt J Bell, CFE Topp, Julie Ingram, Taro Takahashi

*Corresponding author for this work

    Research output: Contribution to journalArticlepeer-review

    3 Citations (Scopus)
    16 Downloads (Pure)

    Abstract

    This study examines the effectiveness of a model called LINGRA-N-Plus to simulate the interaction of climate, soil and management on the green leaf and total dry matter yields of ryegrass in England and Wales. The LINGRA-N-Plus model includes modifications of the LINGRA-N model such as temperature- and moisture-dependent soil nitrogen mineralization and differential partitioning to leaves and stems with thermal time from the last harvest. The resulting model was calibrated against the green leaf and total grass yields from a harvest interval x nitrogen application experiment described by Wilman et al. (1976). When the LINGRA-N-Plus model was validated against total grass yields from nitrogen experiments at ten sites described by Morrison et al. (1980), its modelling efficiency improved greatly compared to the original LINGRA-N. High predicted yields, at zero nitrogen application, were related to soils with a high initial nitrogen content. The lowest predicted yields occurred at sites with low rainfall and shallow rooting depth; mitigating the effect of drought at such sites increased yields by up to 4 t ha−1. The results highlight the usefulness of grass
    models, such as LINGRA-N-Plus, to explore the combined effects of climate, soil, and management, like nitrogen application, and harvest intervals on grass productivity.
    Original languageEnglish
    Article number677
    Number of pages21
    JournalAgronomy
    Volume11
    Issue number4
    Early online date2 Apr 2021
    DOIs
    Publication statusFirst published - 2 Apr 2021

    Keywords

    • LINGRA
    • Nitrogen
    • Soil moisture deficit
    • Soil organic matter
    • Water stress

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