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氧气直接调节农业土壤中的一氧化二氮生成。

Oxygen Regulates Nitrous Oxide Production Directly in Agricultural Soils.

机构信息

College of Resources and Environmental Sciences , China Agricultural University , Beijing 100193 , China.

SRUC , West Mains Road , Edinburgh EH9 3JG , Scotland , U.K.

出版信息

Environ Sci Technol. 2019 Nov 5;53(21):12539-12547. doi: 10.1021/acs.est.9b03089. Epub 2019 Oct 22.

Abstract

Oxygen (O) plays a critical and yet poorly understood role in regulating nitrous oxide (NO) production in well-structured agricultural soils. We investigated the effects of O dynamics on NO production in a typical intensively managed Chinese cropping system under a range of environmental conditions (temperature, moisture, ammonium, nitrate, dissolved organic carbon, and so forth). Climate and management (fertilization, irrigation, precipitation, and temperature), and their interactions significantly affected soil O and NO concentrations ( < 0.05). Soil O concentration was the most significant factor correlating with soil NO concentration ( = -0.71) when compared with temperature, water-filled pore space, and ammonium concentration ( = 0.30, 0.25, and 0.26, respectively). Soil NO concentration increased exponentially with decreasing soil O concentrations. The exponential model of N treatments and fertilization with irrigation/precipitation events predicted 74-90% and 58% of the variance in soil NO concentrations, respectively. Our results highlight that the soil O status is the proximal, direct, and the most decisive environmental trigger for NO production, outweighing the effects of other factors and could be a key variable integrating the aggregated effects of various complex interacting variables. This study offers new opportunities for developing more sensitive approaches to predicting and through appropriate management interventions mitigating NO emissions from agricultural soils.

摘要

氧气(O)在调节农业土壤中一氧化二氮(NO)的产生方面起着至关重要但尚未被充分理解的作用。我们研究了在一系列环境条件(温度、水分、铵、硝酸盐、溶解有机碳等)下,氧气动态对典型集约化管理的中国种植系统中一氧化二氮产生的影响。气候和管理(施肥、灌溉、降水和温度)及其相互作用显著影响土壤氧气和一氧化二氮浓度(<0.05)。与温度、水饱和孔隙空间和铵浓度(=0.30、0.25 和 0.26)相比,土壤氧气浓度与土壤一氧化二氮浓度相关性最强(=−0.71)。土壤一氧化二氮浓度随土壤氧气浓度的降低而呈指数增加。氮处理和施肥与灌溉/降水事件的指数模型分别预测了土壤一氧化二氮浓度方差的 74-90%和 58%。我们的研究结果强调,土壤氧气状况是直接决定一氧化二氮产生的近端、直接和最决定性的环境触发因素,超过了其他因素的影响,并且可能是整合各种复杂相互作用变量的综合效应的关键变量。这项研究为开发更敏感的方法来预测和通过适当的管理干预来减轻农业土壤中的一氧化二氮排放提供了新的机会。

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