5 research outputs found

    Re-estimating NH<sub>3</sub> Emissions from Chinese Cropland by a New Nonlinear Model

    No full text
    Ammonia (NH<sub>3</sub>) released to the atmosphere leads to a cascade of impacts on the environment, yet estimation of NH<sub>3</sub> volatilization from cropland soils (<i>V</i><sub>NH<sub>3</sub></sub>) in a broad spatial scale is still quite uncertain in China. This mainly stems from nonlinear relationships between <i>V</i><sub>NH<sub>3</sub></sub> and relevant factors. On the basis of 495 site-years of measurements at 78 sites across Chinese croplands, we developed a nonlinear Bayesian tree regression model to determine how environmental factors modulate the local derivative of <i>V</i><sub>NH<sub>3</sub></sub> to nitrogen application rates (<i>N</i><sub>rate</sub>) (VR, %). The <i>V</i><sub>NH<sub>3</sub></sub>–<i>N</i><sub>rate</sub> relationship was nonlinear. The VR of upland soils and paddy soils depended primarily on local water input and <i>N</i><sub>rate</sub>, respectively. Our model demonstrated good reproductions of <i>V</i><sub>NH<sub>3</sub></sub> compared to previous models, i.e., more than 91% of the observed VR variance at sites in China and 79% of those at validation sites outside China. The observed spatial pattern of <i>V</i><sub>NH<sub>3</sub></sub> in China agreed well with satellite-based estimates of NH<sub>3</sub> column concentrations. The average VRs in China derived from our model were 14.8 ± 2.9% and 11.8 ± 2.0% for upland soils and paddy soils, respectively. The estimated annual NH<sub>3</sub> emission in China (3.96 ± 0.76 TgNH<sub>3</sub>·yr<sup>–1</sup>) was 40% greater than that based on the IPCC Tier 1 guideline

    Re-estimating NH<sub>3</sub> Emissions from Chinese Cropland by a New Nonlinear Model

    No full text
    Ammonia (NH<sub>3</sub>) released to the atmosphere leads to a cascade of impacts on the environment, yet estimation of NH<sub>3</sub> volatilization from cropland soils (<i>V</i><sub>NH<sub>3</sub></sub>) in a broad spatial scale is still quite uncertain in China. This mainly stems from nonlinear relationships between <i>V</i><sub>NH<sub>3</sub></sub> and relevant factors. On the basis of 495 site-years of measurements at 78 sites across Chinese croplands, we developed a nonlinear Bayesian tree regression model to determine how environmental factors modulate the local derivative of <i>V</i><sub>NH<sub>3</sub></sub> to nitrogen application rates (<i>N</i><sub>rate</sub>) (VR, %). The <i>V</i><sub>NH<sub>3</sub></sub>–<i>N</i><sub>rate</sub> relationship was nonlinear. The VR of upland soils and paddy soils depended primarily on local water input and <i>N</i><sub>rate</sub>, respectively. Our model demonstrated good reproductions of <i>V</i><sub>NH<sub>3</sub></sub> compared to previous models, i.e., more than 91% of the observed VR variance at sites in China and 79% of those at validation sites outside China. The observed spatial pattern of <i>V</i><sub>NH<sub>3</sub></sub> in China agreed well with satellite-based estimates of NH<sub>3</sub> column concentrations. The average VRs in China derived from our model were 14.8 ± 2.9% and 11.8 ± 2.0% for upland soils and paddy soils, respectively. The estimated annual NH<sub>3</sub> emission in China (3.96 ± 0.76 TgNH<sub>3</sub>·yr<sup>–1</sup>) was 40% greater than that based on the IPCC Tier 1 guideline
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