首页> 外文会议>International Nitrogen Conference; 20041012-16; Nanjing(CN) >EFFECT OF NITROGEN DEPOSITION ON STREAM WATER NITRATE AND NITROUS GAS EMISSION IN LARCH FOREST IN THE NORTHERN JAPAN
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EFFECT OF NITROGEN DEPOSITION ON STREAM WATER NITRATE AND NITROUS GAS EMISSION IN LARCH FOREST IN THE NORTHERN JAPAN

机译:氮素沉积对日本北部落叶松林地流水硝酸盐和硝态氮排放的影响

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In this report, we show that the spatial variation in nitrogen deposition enables to detect the effect of anthropogenic N deposition on biogeochemical processes in forest ecosystems. We measured nitrogen deposition (throughfall fluxes), stream water chemistry and trace gases emission from forest floors over five adjacent small catchments in which soil types (Hapludants) and vegetation composition (fifty to sixty years old larch plantation) were fairly identical. Thirty-two throughfall collectors were set up in the five catchments (six to eight collectors in each catchment) and throughfall samples were collected after a rain event, while stream water samples were collected once or twice a month. The monitoring was carried out during a period of six months (2002 June to 2002 November). In July 2002 fluxes of trace gases (N_2O, NO, CH_4) were measured beside throughfall collectors. Throughfall DIN (dissolved inorganic nitrogen) fluxes were highly variable: the highest N input, 1.32 kg-N·ha~(-1) 6 months~(-1), was 66 times higher than the lowest input, 0.02 kg·N·ha~(-1) 6 months~(-1). The DIN inputs showed a sgnificant correlation (p < 0.05) with the stream nitrate concentrations (r = 0.88) and with N_2O emission from forest floors (r = 0.40), suggesting that the N deposition less than 10 kg-N·ha~(-1)·yr~(-1) is enough to affect NO_3 export and N_2O emission from forest ecosystems.
机译:在本报告中,我们表明氮沉降的空间变化能够检测人为氮沉降对森林生态系统生物地球化学过程的影响。我们测量了五个相邻小流域的森林地板上的氮沉降(穿透通量),溪流水化学和微量气体排放,这些小流域的土壤类型(Hapludant)和植被组成(五十至六十年的落叶松人工林)相当相同。在五个流域设置了32个通流收集器(每个流域中有六个至八个收集器),降雨后收集了通流样品,而每月采集一次或两次溪流水样品。监测进行了六个月(2002年6月至2002年11月)。在2002年7月,在贯通收集器旁边测量了痕量气体(N_2O,NO,CH_4)的通量。贯穿的DIN(溶解无机氮)通量变化很大:最高氮输入为1.32 kg-N·ha〜(-1)6个月〜(-1),是最低氮输入的0.02 kg·N·的66倍。 ha〜(-1)6个月〜(-1)。 DIN输入与硝酸盐流浓度(r = 0.88)和林地N_2O排放量(r = 0.40)呈显着的相关性(p <0.05),这表明氮的沉积量小于10 kg-N·ha〜( -1)·yr〜(-1)足以影响森林生态系统的NO_3出口和N_2O排放。

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