土壤背景N2O排放对土地利用、土壤性质与气候参数的响应——基于全球的荟萃分析

Responses of soil background N2O emissions to land use, soil properties, and climate parameters based on a global Meta analysis

  • 摘要: 土壤背景N2O排放是指未施用氮肥或未进行土壤管理措施的土壤所排放的N2O。随着人为活动的增加, 土壤背景N2O排放逐年增加, 对环境和气候的影响日益显著。然而, 目前关于土壤背景N2O排放的主要控制因素和潜在机制尚不清楚。本文根据全球282项研究的土壤背景N2O排放的实地观测数据以及气候因子和土壤因子数据, 绘制了纳入本研究中的地点分布图。本研究涉及的站点广泛分布于全球六大洲, 涵盖了三种主要的土地利用类型, 包括耕地、林地和草地。研究发现, 全球土壤背景N2O排放范围为0.01~56.40 kg(N)∙hm−2∙a−1, 其平均值为1.68 kg(N)∙hm−2∙a−1。其中, 草地土壤背景N2O排放分布范围最广, 为0.03~56.40 kg(N)∙hm−2∙a−1, 耕地和林地土壤背景N2O排放分别为0.01~7.10和0.12~4.70 kg(N)∙hm−2∙a−1。进一步通过荟萃分析和多元线性逐步回归分析, 系统评估并深入研究了影响土壤背景N2O排放的多种因子, 包括土壤pH值、土壤容重、土壤总氮、年平均温度、平均年降水量之间的相关性。进一步探究了不同土地利用类型的土壤性质和气候参数与土壤背景N2O排放之间的相关性。主要得到以下结果: 1)与气候因子相比,土壤属性对土壤背景N2O排放的影响程度更大; 2)在全球范围内不同土地利用方式下的土壤背景N2O排放存在差异; 3)土壤pH值对耕地、林地和草地的背景N2O排放均有显著影响。本研究为可持续农业的发展和管理战略提供了一定的启示和研究意义。同时为减少温室气体排放、保护臭氧层和缓解气候变化提供了重要支持。

     

    Abstract: Soil background N2O emission is the N2O released from soil without nitrogen fertilizer application or soil management during the planting cycle. With the increase of human activities, the amount of background N2O emission from soil gradually increases, and its impact on environment and climate is increasingly significant. However, the key controlling factors and underlying mechanisms related to background N2O emission from soil are remain unclear. To address this knowledge gap, the distribution of the 282 studes included in this research was mapped based on field observations data of soil background N2O emissions, as well as climate and soil factor data, from around the world The study sites are globally distributed across six continents and cover three predominant land-use types: cropland, forestland, and grassland. The results showed that the global background N2O emission ranged from 0.01 kg to 56.40 kg(N)∙hm−2∙a−1, with an average of 1.68 kg(N)∙hm−2∙a−1. Among them, the range of soil background N2O emission in grassland ecosystem was the widest, from 0.03−56.40 kg(N)∙hm−2∙a−1. The soil background N2O emissions in cropland and forestland ecosystems ecosystems were in the range of 0.01 to 7.10 and 0.12 to 4.70 kg(N)∙hm−2∙a−1, respectively. Further, a systematic evaluation and in-depth investigation of the various factors affecting soil background N2O emissions including soil pH, soil bulk density, soil total nitrogen, annual mean temperature, annual mean precipitation.Additionally, we explored the relationships between soil properties and meteorological parameters and soil background N2O emissions across different land use types. The main results were as follows: 1) compared with climate factors, soil properties had a greater impact on soil background N2O emissions; 2) soil background N2O emissions under different land use patterns were different on a global scale; 3) soil pH had significant effects on soil background N2O emissions in cropland, forestland and grassland ecosystems. This study provides valuable insights into the development and management strategy of sustainable agriculture and offers a scientific basis for mitigating N2O emissions from soil. It also provides critical support for reducing greenhouse gas emissions, protecting the ozone layer, and mitigating the impacts of climate change on ecosystems.

     

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