Kyushu University Forest, Kyushu University, 394 Tsubakuro, Sasaguri, Fukuoka, 811-2415, Japan.
Environ Pollut. 2021 Oct 15;287:117634. doi: 10.1016/j.envpol.2021.117634. Epub 2021 Jun 23.
Japan receives nitrogenous air pollutants via long-range transport from China. However, emissions of nitrogenous air pollutants in China have stabilized or decreased in recent years. This study examined both the long-term trends in atmospheric nitrogen (N) deposition from the 1990s to the 2010s and the response of stream water nitrate (NO) leaching from forested areas in western Japan. A long-term (1992-2018) temporal analysis of atmospheric N deposition in Fukuoka (western Japan) was conducted. Atmospheric bulk N deposition was collected at forested sites in a suburban forest (S) and a rural forest (R) in western Japan during 2009-2018. Stream water samples were also collected from four locations at sites S and R during the same period. Results showed that atmospheric N deposition in Fukuoka started to decrease from the mid-2000s at an annual rate of -2.5% yr. The decrease in atmospheric N deposition was attributable mainly to decreased atmospheric ammonium (NH) deposition, which caused greater contribution of NO deposition to atmospheric N deposition. Concentrations of NO in the stream water samples from three of the four locations decreased significantly at an annual rate of -3.7 to -0.7% yr. However, stream water NO concentrations increased in one watershed where understory vegetation has been deteriorating owing to the increased deer population. This might weaken the recovery of N leaching from forested areas.
日本通过长距离传输接收来自中国的含氮空气污染物。然而,近年来中国的含氮空气污染物排放量已经稳定或减少。本研究考察了从 20 世纪 90 年代到 21 世纪 10 年代大气氮(N)沉积的长期趋势,以及日本西部森林地区溪流水中硝酸盐(NO)淋溶的响应。对日本西部福冈(日本西部)的大气 N 沉积进行了长期(1992-2018 年)时间分析。在 2009-2018 年期间,在日本西部的一个郊区森林(S)和一个农村森林(R)的森林地点收集了大气 N 总沉积。同时,还从 S 和 R 的四个地点收集了溪流水样。结果表明,福冈的大气 N 沉积从 2000 年代中期开始以每年-2.5%的速度减少。大气 N 沉积的减少主要归因于大气氨(NH)沉积的减少,这导致 NO 沉积对大气 N 沉积的贡献更大。来自四个地点中三个地点的溪流水样中 NO 的浓度以每年-3.7 至-0.7%的速度显著下降。然而,在一个流域中,由于鹿群的增加,林下植被恶化,溪流水 NO 浓度增加。这可能会削弱森林地区 N 淋溶的恢复。