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首页> 外文期刊>Global change biology >Excessive use of nitrogen in Chinese agriculture results in high N2O/(N2O+N2) product ratio of denitrification, primarily due to acidification of the soils.
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Excessive use of nitrogen in Chinese agriculture results in high N2O/(N2O+N2) product ratio of denitrification, primarily due to acidification of the soils.

机译:中国农业中过量使用氮导致反硝化的N 2 O /(N 2 O + N 2 )产品比率高,这主要是由于酸化土壤。

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China is the world's largest producer and consumer of fertilizer N, and decades of overuse has caused nitrate leaching and possibly soil acidification. We hypothesized that this would enhance the soils' propensity to emit N2O from denitrification by reducing the expression of the enzyme N2O reductase. We investigated this by standardized oxic/anoxic incubations of soils from five long-term fertilization experiments in different regions of China. After adjusting the nitrate concentration to 2 mM, we measured oxic respiration (R), potential denitrification (D), substrate-induced denitrification, and the denitrification product stoichiometry (NO, N2O, N2). Soils with a history of high fertilizer N levels had high N2O/(N2O+N2) ratios, but only in those field experiments where soil pH had been lowered by N fertilization. By comparing all soils, we found a strong negative correlation between pH and the N2O/(N2O+N2) product ratio (r2=0.759, P<0.001). In contrast, the potential denitrification (D) was found to be a linear function of oxic respiration (R), and the ratio D/R was largely unaffected by soil pH. The immediate effect of liming acidified soils was lowered N2O/(N2O+N2) ratios. The results provide evidence that soil pH has a marginal direct effect on potential denitrification, but that it is the master variable controlling the percentage of denitrified N emitted as N2O. It has been known for long that low pH may result in high N2O/(N2O+N2) product ratios of denitrification, but our documentation of a pervasive pH-control of this ratio across soil types and management practices is new. The results are in good agreement with new understanding of how pH may interfere with the expression of N2O reductase. We argue that the management of soil pH should be high on the agenda for mitigating N2O emissions in the future, particularly for countries where ongoing intensification of plant production is likely to acidify the soils.
机译:中国是世界上最大的氮肥生产国和消费国,几十年来的过度使用已导致硝酸盐的淋溶和土壤酸化。我们假设这将通过减少N 2 O还原酶的表达来增强土壤反硝化过程中释放N 2 O的倾向。我们通过在中国不同地区进行的五次长期施肥实验对土壤进行了标准的有氧/缺氧培养,对此进行了调查。将硝酸盐浓度调节至2 mM后,我们测量了氧呼吸(R),潜在的反硝化(D),底物诱导的反硝化和反硝化产物化学计量(NO,N 2 O,N 2 )。肥料氮含量较高的土壤中N 2 O /(N 2 O + N 2 )的比率较高,但仅在这些比率中氮肥使土壤pH降低的田间试验。通过比较所有土壤,我们发现pH与N 2 O /(N 2 O + N 2 )乘积比之间存在很强的负相关性(r 2 = 0.759,P <0.001)。相反,发现潜在的反硝化作用(D)是氧呼吸(R)的线性函数,并且比率D / R在很大程度上不受土壤pH的影响。石灰酸化土壤的立竿见影的效果是降低了N 2 O /(N 2 O + N 2 )的比率。结果提供了证据,表明土壤pH值对潜在的反硝化作用有边际直接影响,但它是控制以N 2 O排放的反硝化氮百分比的主要变量。长期以来已知低pH值可能导致反硝化的N 2 O /(N 2 O + N 2 )产品比率高,但是我们关于在整个土壤类型和管理实践中普遍控制此比例的pH值的文档是新的。该结果与关于pH如何干扰N 2 O还原酶表达的新认识非常吻合。我们认为,对土壤pH的管理应在未来减轻N 2 O排放的议程中置于高度优先位置,特别是对于那些持续进行植物生产可能使土壤酸化的国家。

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