García-Méndez Georgina, Maass J Manuel, Matson Pamela A, Vitousek Peter M
Centro de Ecología, Universidad Nacional Autónoma de México, Apartado Postal 70-275, 04510, México, D.F., México.
Earth Systems Science Division, NASA-Ames Research Center, 94305, Moffett Field, CA, USA.
Oecologia. 1991 Nov;88(3):362-366. doi: 10.1007/BF00317579.
Emissions of nitrous oxide and soil nitrogen pools and transformations were measured over an annual cycle in two forests and one pasture in tropical deciduous forest near Chamela, México. Nitrous oxide flux was moderately high (0.5-2.5 ng cm h) during the wet season and low (<0.3 ng cm h) during the dry season. Annual emissions of nitrogen as nitrous oxide were calculated to be 0.5-0.7 kg ha y, with no substantial difference between the forests and pasture. Wetting of dry soil caused a large but short-lived pulse of NO flux that accounted for <2% of annual flux. Variation in soil water through the season was the primary controlling factor for pool sizes of ammonium and nitrate, nitrogen transformations, and NO flux.
在墨西哥查梅拉附近的热带落叶林的两片森林和一片牧场中,对一氧化二氮排放以及土壤氮库和转化进行了为期一年的测量。湿季一氧化二氮通量适中偏高(0.5 - 2.5纳克/平方厘米·小时),旱季则较低(<0.3纳克/平方厘米·小时)。计算得出以一氧化二氮形式排放的氮的年排放量为0.5 - 0.7千克/公顷·年,森林和牧场之间没有显著差异。干燥土壤的湿润引发了一氧化氮通量的一个大但短暂的脉冲,其占年通量的比例小于2%。整个季节土壤水分的变化是铵和硝酸盐库大小、氮转化以及一氧化氮通量的主要控制因素。