Groffman Peter M, Williams Candiss O, Pouyat Richard V, Band Lawrence E, Yesilonis Ian D
Cary Institute of Ecosystem Studies, Box AB, Millbrook, NY 12545, USA.
J Environ Qual. 2009 Jul 23;38(5):1848-60. doi: 10.2134/jeq2008.0521. Print 2009 Sep-Oct.
Urban landscapes contain a mix of land-use types with different patterns of nitrogen (N) cycling and export. We measured nitrate (NO(3)(-)) leaching and soil:atmosphere nitrous oxide (N(2)O) flux in four urban grassland and eight forested long-term study plots in the Baltimore, Maryland metropolitan area. We evaluated ancillary controls on these fluxes by measuring soil temperature, moisture, and soil:atmosphere fluxes of carbon dioxide on these plots and by sampling a larger group of forest, grass, and agricultural sites once to evaluate soil organic matter, microbial biomass, and potential net N mineralization and nitrification. Annual NO(3)(-) leaching ranged from 0.05 to 4.1 g N m(-2) yr(-1) and was higher in grass than forest plots, except in a very dry year and when a disturbed forest plot was included in the analysis. Nitrous oxide fluxes ranged from 0.05 to >0.3 g N m(-2) yr(-1), with few differences between grass and forest plots and markedly higher fluxes in wet years. Differences in NO(3)(-) leaching and N(2)O flux between forests and grasslands were not as high as expected given the higher frequency of disturbance and fertilization in the grasslands. Carbon dioxide flux, organic matter, and microbial biomass were as high or higher in urban grasslands than in forests, suggesting that active carbon cycling creates sinks for N in vegetation and soil in these ecosystems. Although urban grasslands export more N to the environment than native forests, they have considerable capacity for N retention that should be considered in evaluations of land-use change.
城市景观包含多种土地利用类型,其氮(N)循环和输出模式各不相同。我们在马里兰州巴尔的摩市大都市区的四个城市草地和八个森林长期研究样地中测量了硝酸盐(NO₃⁻)淋溶以及土壤 - 大气间的一氧化二氮(N₂O)通量。我们通过测量这些样地的土壤温度、湿度以及土壤 - 大气间的二氧化碳通量,并对一组更大的森林、草地和农业用地进行一次采样以评估土壤有机质、微生物生物量以及潜在的净氮矿化和硝化作用,来评估对这些通量的辅助控制因素。年NO₃⁻淋溶量在0.05至4.1 g N m⁻² yr⁻¹之间,除了在非常干旱的年份以及将一个受干扰的森林样地纳入分析时,草地的NO₃⁻淋溶量高于森林样地。一氧化二氮通量在0.05至>0.3 g N m⁻² yr⁻¹之间,草地和森林样地之间差异不大,在湿润年份通量明显更高。考虑到草地中干扰和施肥的频率更高,森林和草地之间NO₃⁻淋溶和N₂O通量的差异并没有预期的那么大。城市草地中的二氧化碳通量、有机质和微生物生物量与森林中的一样高或更高,这表明活跃的碳循环在这些生态系统的植被和土壤中形成了氮汇。尽管城市草地向环境中输出的氮比原生森林更多,但它们具有相当大的氮保留能力,在评估土地利用变化时应予以考虑。