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Biochar Decelerates Soil Organic Nitrogen Cycling but Stimulates Soil Nitrification in a Temperate Arable Field Trial

机译:生物炭在温和的耕地试验中可降低土壤有机氮循环但能刺激土壤硝化作用

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摘要

Biochar production and subsequent soil incorporation could provide carbon farming solutions to global climate change and escalating food demand. There is evidence that biochar amendment causes fundamental changes in soil nutrient cycles, often resulting in marked increases in crop production, particularly in acidic and in infertile soils with low soil organic matter contents, although comparable outcomes in temperate soils are variable. We offer insight into the mechanisms underlying these findings by focusing attention on the soil nitrogen (N) cycle, specifically on hitherto unmeasured processes of organic N cycling in arable soils. We here investigated the impacts of biochar addition on soil organic and inorganic N pools and on gross transformation rates of both pools in a biochar field trial on arable land (Chernozem) in Traismauer, Lower Austria. We found that biochar increased total soil organic carbon but decreased the extractable organic C pool and soil nitrate. While gross rates of organic N transformation processes were reduced by 50–80%, gross N mineralization of organic N was not affected. In contrast, biochar promoted soil ammonia-oxidizer populations (bacterial and archaeal nitrifiers) and accelerated gross nitrification rates more than two-fold. Our findings indicate a de-coupling of the soil organic and inorganic N cycles, with a build-up of organic N, and deceleration of inorganic N release from this pool. The results therefore suggest that addition of inorganic fertilizer-N in combination with biochar could compensate for the reduction in organic N mineralization, with plants and microbes drawing on fertilizer-N for growth, in turn fuelling the belowground build-up of organic N. We conclude that combined addition of biochar with fertilizer-N may increase soil organic N in turn enhancing soil carbon sequestration and thereby could play a fundamental role in future soil management strategies.
机译:生物炭的生产和随后的土壤掺入可以为全球气候变化和不断增长的粮食需求提供碳农业解决方案。有证据表明,生物炭的改良会引起土壤养分循环的根本变化,通常会导致作物产量显着增加,特别是在土壤有机质含量较低的酸性土壤和不育土壤中,尽管在温带土壤中的可比结果是可变的。通过关注土壤氮(N)循环,特别是迄今无法测量的耕地土壤中有机氮循环的过程,我们提供了洞悉这些发现的机制。我们在下奥地利州Traismauer的可耕地(Chernozem)生物炭田间试验中,研究了生物炭添加对土壤有机氮和无机氮库以及两种氮库总转化率的影响。我们发现生物炭增加了土壤总有机碳,但减少了可提取的有机碳库和土壤硝酸盐。虽然有机氮转化过程的总速率降低了50–80%,但有机氮的总氮矿化量并未受到影响。相比之下,生物炭促进了土壤氨氧化剂的数量(细菌和古细菌硝化剂),并加速了总硝化速率的两倍以上。我们的发现表明,土壤有机氮和无机氮循环之间的脱钩以及有机氮的积累,以及无机氮从该池中的释放减少。因此,结果表明,将无机肥料-N与生物炭结合使用可以补偿有机氮矿化的减少,而植物和微生物则利用肥料-N进行生长,从而为地下有机氮的积累提供了动力。结论认为,生物炭与氮肥的组合添加可增加土壤有机氮,反过来增强土壤碳固存,从而可能在未来的土壤管理策略中发挥重要作用。

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