反硝化建模:我们能报告我们不知道的事情吗?

IF 8.3 Q1 GEOSCIENCES, MULTIDISCIPLINARY AGU Advances Pub Date : 2023-10-29 DOI:10.1029/2023AV000990
B. Grosz, A. Matson, K. Butterbach-Bahl, T. Clough, E. A. Davidson, R. Dechow, S. DelGrosso, E. Diamantopoulos, P. Dörsch, E. Haas, H. He, C. V. Henri, D. Hui, K. Kleineidam, D. Kraus, M. Kuhnert, J. Léonard, C. Müller, S. O. Petersen, D. Sihi, I. Vogeler, R. Well, J. Yeluripati, J. Zhang, C. Scheer
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引用次数: 0

摘要

生物地球化学模型模拟土壤氮(N)周转,通常用于评估脱氮造成的氮损失。尽管模型模拟了完整的N预算,通常只有N池/通量的子集(即N2O、NO3−${\text{NO}_{3}}^{-}$、NH3、NOx)被公布,因为无法公布全部预算通过测量数据进行验证。实地研究很少包括全氮平衡,尤其是难以量化的N2通量。基于可用的现场数据限制建模结果的发布意味着错过了提高对建模过程理解的机会。我们建议建模者社区支持在未来的研究中公布所有模拟的N池和过程。
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Modeling Denitrification: Can We Report What We Don't Know?

Biogeochemical models simulate soil nitrogen (N) turnover and are often used to assess N losses through denitrification. Though models simulate a complete N budget, often only a subset of N pools/fluxes (i.e., N2O, NO 3 ${{\text{NO}}_{3}}^{-}$ , NH3, NOx) are published since the full budget cannot be validated with measured data. Field studies rarely include full N balances, especially N2 fluxes, which are difficult to quantify. Limiting publication of modeling results based on available field data represents a missed opportunity to improve the understanding of modeled processes. We propose that the modeler community support publication of all simulated N pools and processes in future studies.

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