土壤性质对氮矿化影响的重要性和不一致性:系统综述

Gabriela Mendoza-Carreón, J. P. Flores-Márgez, Pedro Osuna-Ávila, S. Sanogo
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引用次数: 0

摘要

气候和土壤性质对氮矿化(Nmin)有着深刻的影响。因此,迫切需要确定涉及有机物分解的物理-化学-生物因素如何影响全球报告的预测模型。本文反映了在构建Nmin模型过程中被认为相关和使用的因素的研究重点。将1990年以来发表的影响土壤Nmin或N有效性因素的文献数据下载到Access数据库中。利用不同的双变量和多变量统计技术,我们对90篇研究论文的785个统计分析结果进行了汇总,这些统计分析将Nmin与环境因素、管理策略和土壤生物和物理化学属性联系起来。为了组织目的,我们决定根据矿化相关性质的相似性将结果分为环境因素(18.6%)、生态系统/植被(14.52%)、管理(7.64%)、土壤理化性质(34.65%)、有机质(16.05%)和微生物群(6.37%)。土壤中氮含量(铵态氮、硝酸盐氮、有机氮和全氮)测量的响应变量为16.2%,其中83.88%代表矿化过程中的氮,包括潜在矿化氮。由于Nmin是因变量,结果包含109个自变量,其中47.7%的结果看似不一致,说明Nmin的影响不同。研究发现,结果的差异主要与生态系统或变量相互作用的差异有关。我们认为,获取Nmin的一般预测模型或根据当地条件构建特定的方程对优化作物生产的氮素管理有一定的限制。一个更有用的策略是为Nmin生成一个预测模型,包括一个区域和生态系统内的重要土壤和天气条件;因此,这些信息可以支持土壤和作物管理决策。
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Importance and inconsistencies of the influence of soil properties on nitrogen mineralization: a systematic review
Climate and soil properties profoundly impact N mineralization (Nmin). Hence, there is a critical need to identify how physical-chemical-biological factors involved in organic matter decomposition influence globally reported predictive models. This paper reflects research focused on those factors considered relevant and used during the construction of Nmin models. The literature data found on factors affecting Nmin or N availability in soils published since 1990 was downloaded to a database in Access. Using different bivariate and multivariate statistical techniques, we compiled results of 785 statistical analyses presented by authors of 90 research articles that related Nmin and environmental factors, management strategies, and soil biological and physicochemical attributes. For organization purposes, we decided to group results according to the similarity of properties related to mineralization into environmental factors (18.6%), ecosystem/vegetation (14.52%), management (7.64%), soil physicochemical properties (34.65%), organic matter (16.05%), and microbiota (6.37%). The measurements of the response variables were 16.2% using N content in soil (as ammonium, nitrates, Organic N and Total N), and 83.88% represent N in the process of mineralization, including potentially mineralized N. As Nmin is the dependent variable, the results included 109 independent variables, of which 47.7% presented seemingly inconsistent results, which means different effects in Nmin. The difference in results was found to be related mostly to a difference in ecosystems or variable interactions. We conclude that acquiring a general prediction model for Nmin or constructing a specific equation for local conditions poses a limitation to optimizing N management for crop production. A more useful strategy is to generate a prediction model for Nmin, including significative soil and weather conditions, within a region and ecosystem; thus, the information can support soil and crop management decisions.
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