Reevaluating multi-pool first-order kinetic models for fitting soil incubation data

IF 6.6 1区 农林科学 Q1 SOIL SCIENCE Geoderma Pub Date : 2025-02-18 DOI:10.1016/j.geoderma.2025.117218
Shuhao Zhou , Daifeng Xiang , Gangsheng Wang , Liping Zhang , Zehao Lv , Shanshan Qi , Wanyu Li
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Abstract

Soil incubation experiments are frequently conducted to investigate soil carbon (C) cycling and its response to environmental changes. Multi-pool first-order models, which apply constant kinetic rate parameters for each pool, are widely used for fitting these datasets due to their simplicity. However, their ability to accurately represent instantaneous C effluxes is often overlooked, as cumulative effluxes are typically prioritized. Here, we calibrated a three-pool first-order model using a 384-day incubation dataset with fluctuating CO2 and CH4 effluxes. Despite constantly good performance for cumulative C effluxes (R2 = 0.99–1.00), the R2 values vary greatly with experimental conditions for instantaneous effluxes (R2 = 0.36–0.93), depending on the frequency of aerobic-anaerobic shifts. The results are regardless of the objective function used for model fitting (i.e., maximizing R2 for instantaneous or cumulative C effluxes). Compared to cumulative effluxes, we propose emphasizing instantaneous effluxes and calibrating additional variables in soil C modeling. This strategy can offer more insights for improving predictions and enhancing understanding of soil C-climate feedbacks under dynamic environmental conditions.
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重新评估拟合土壤培养数据的多池一阶动力学模型
土壤培养实验是研究土壤碳循环及其对环境变化响应的常用方法。多池一阶模型对每个池采用恒定的动力学速率参数,由于其简单,被广泛用于拟合这些数据集。然而,它们准确表示瞬时碳流出的能力往往被忽视,因为累积流出通常被优先考虑。在这里,我们使用具有波动的CO2和CH4外排的384天孵育数据集校准了一个三池一阶模型。尽管累积C外排的性能一直很好(R2 = 0.99-1.00),但瞬时外排的实验条件不同,R2值差异很大(R2 = 0.36-0.93),取决于好氧-厌氧转换的频率。结果与模型拟合使用的目标函数无关(即,最大化瞬时或累积碳流出的R2)。与累积外排相比,我们建议在土壤C模型中强调瞬时外排和校准附加变量。该策略可为改进动态环境条件下土壤c -气候反馈的预测和理解提供更多见解。
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来源期刊
Geoderma
Geoderma 农林科学-土壤科学
CiteScore
11.80
自引率
6.60%
发文量
597
审稿时长
58 days
期刊介绍: Geoderma - the global journal of soil science - welcomes authors, readers and soil research from all parts of the world, encourages worldwide soil studies, and embraces all aspects of soil science and its associated pedagogy. The journal particularly welcomes interdisciplinary work focusing on dynamic soil processes and functions across space and time.
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