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Nitric oxide emissions from fertilized and biosolids-amended soil

机译:施肥和生物固体改良土壤排放的一氧化氮

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摘要

Nitric oxide (NO) emissions from soil amended with municipal wastewater biosolids or mineral fertilizer can adversely impact ozone levels in the lower troposphere and are studied here. A comprehensive laboratory protocol was developed and conducted to consider the influence of biosolids-amended (BSA) soil and mineral-fertilizer-amended (MFA) soil, as compared with unamended soil, on NO emissions with varying temperature, moisture content, and pH. NO plays an important role in the formation of tropospheric ozone. Minimization of NO flux from soil is advantageous, protecting air quality as well as conserving valued nitrogen fertilizers. BSA and MFA soils were found to produce NO emissions over five times greater than unamended soils. Distinctions between NO flux from MFA and BSA soil cannot be made. NO flux from soils at pH 6.25 and 6.75 were not found to be statistically different. Soils with higher water-filled pore space (WFPS) and temperature are generally shown to produce greater quantities of NO within the range of temperature (15 degrees -28 degreesC) and WFPS (3-40%) studied. [References: 28]
机译:土壤中一氧化氮(NO)的排放量经过市政废水生物固体或矿物肥料的改良,可能会对对流层下部的臭氧水平产生不利影响,在此进行研究。制定并进行了一项全面的实验室规程,以考虑与未修正的土壤相比,生物固体修正(BSA)土壤和矿物肥料修正(MFA)土壤对随温度,湿度和pH值变化的NO排放的影响。 NO在对流层臭氧的形成中起着重要作用。最大限度地减少土壤中的NO排放是有利的,它可以保护空气质量并节省有价值的氮肥。发现BSA和MFA土壤的NO排放量是未改良土壤的五倍以上。无法区分来自MFA和BSA土壤的NO通量。从pH值为6.25和6.75的土壤中获得的NO通量没有统计学差异。通常,在所研究的温度范围(15度-28摄氏度)和WFPS范围(3-40%)内,充满水的孔隙空间(WFPS)和温度较高的土壤通常会产生大量的NO。 [参考:28]

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