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首页> 外文期刊>European Journal of Soil Science >Negative priming of native soil organic carbon mineralization by oilseed biochars of contrasting quality
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Negative priming of native soil organic carbon mineralization by oilseed biochars of contrasting quality

机译:品质不同的油料生物炭对原生土壤有机碳矿化的负向激发作用

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Oilseed-derived biochar, a by-product of pyrolysis for biodiesel production, is richer in aliphatic compounds than the commonly studied wood-derived biochar, affecting both its mineralization in soil and its interaction with native soil organic carbon (nSOC). Here, we investigated the soil C sequestration potential of three different oilseed biochars derived from C-3 plant material: soyabean, castor bean and jatropha cake. The chemical composition of these biochars was determined by elemental analysis (CHN) and C-13 NMR spectroscopy. The cumulative CO2 efflux from 30-day laboratory incubations of biochar mixed with a sandy soil containing nSOC from C-4 plants was measured as a proxy for mineralization rate. The relative contribution of each source to CO2 production was calculated based on the C-13-signatures of total CO2 efflux and the source materials (soil and biochars). Our results showed that: (i) castor bean biochar contained relatively large amounts of aliphatic compounds, resulting in a greater mineralization rate than soyabean and jatropha biochars; (ii) CO2 efflux from the soil-biochar mixtures originated mostly from the biochars, suggesting that these biochars contain rapidly decomposable compounds; and (iii) all three oilseed biochars decelerated nSOC mineralization. This negative priming effect appeared to be caused by different factors. We conclude that oilseed biochars have the potential to increase soil C stocks directly and increase soil C sequestration indirectly in the short term through negative priming of nSOC mineralization.
机译:来自油籽的生物炭,是生物柴油生产热解的副产品,比通常研究的源自木材的生物炭富含脂肪族化合物,不仅影响其在土壤中的矿化作用,还影响其与天然土壤有机碳(nSOC)的相互作用。在这里,我们研究了从C-3植物材料中提取的三种不同油料生物炭的土壤C螯合潜力:大豆,蓖麻子和麻风树饼。这些生物炭的化学组成通过元素分析(CHN)和C-13 NMR光谱确定。测量了生物炭与C-4植物中含nSOC的沙土混合的30天实验室培养物的累积CO2外流,作为矿化速率的指标。根据总CO2排放量的C-13特征和原料(土壤和生物炭)计算每种来源对CO2产生的相对贡献。我们的结果表明:(i)蓖麻子生物炭含有相对大量的脂肪族化合物,比大豆和麻风树生物炭产生更高的矿化率; (ii)土壤-生物炭混合物中的CO 2外排主要来自生物炭,这表明这些生物炭中含有可快速分解的化合物; (iii)所有三种油料生物炭均使nSOC矿化速度降低。这种负启动效应似乎是由不同因素引起的。我们得出结论,油籽生物炭有可能通过nSOC矿化作用的负向激发在短期内直接增加土壤C储量并间接增加土壤C的固存。

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