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Peat Soil Burning in the Mezzano Lowland (Po Plain Italy): Triggering Mechanisms and Environmental Consequences

机译:泥炭土壤燃烧在Mezzano Lowland(Po平原意大利):触发机制和环境后果

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摘要

The effects of peat burning on organic‐rich agricultural soils of the Mezzano Lowland (NE Italy) were evaluated on soil profiles variously affected by smoldering. Profiles were investigated for pH, electrical conductivity, bulk density, elemental and isotopic composition of distinct carbon (and nitrogen) fractions. The results suggest that the horizons affected by carbon loss lie at depths 10–70 cm, where the highest temperatures are developed. We suggest that the exothermal oxidation of methane (mediated by biological activity) plays a significant role in the triggering mechanism. In the interested soils we estimated a potential loss of Soil Organic Carbon of approximately 110 kg m−2 within the first meter, corresponding to 580 kg CO2 m−3. The released greenhouse gas is coupled with a loss of soil structure and nutrients. Moreover, the process plausibly triggers mobility of metals bound in organometallic complexes. All these consequences negatively affect the environment, the agricultural activities and possibly also health of the local people.
机译:泥炭燃烧对梅萨低地(NE意大利)有机肥大农业土壤的影响在各种闷烧的土壤剖面上进行了评价。研究了不同碳(和氮气)级分的pH,电导率,堆积密度,元素和同位素组成的pH,导电性,散装密度,元素和同位素组成。结果表明,受碳损失影响的地平线位于10-70厘米的深度,其中开发了最高温度。我们表明甲烷的放热氧化(通过生物活性介导)在触发机制中起着重要作用。在感兴趣的土壤中,我们估计潜在的土壤有机碳损失约110千克-2在第一米内,对应580 kg co2 m-3。释放的温室气体与土壤结构和营养素的损失相结合。此外,该方法可赋予有机金属配合物中金属的迁移率。所有这些后果对环境影响,农业活动和当地人民的健康产生了负面影响。

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