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首页> 外文期刊>Journal of forest research >Nitrate leaching from Japanese temperate forest ecosystems in response to elevated atmospheric N deposition
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Nitrate leaching from Japanese temperate forest ecosystems in response to elevated atmospheric N deposition

机译:硝酸盐从日本温带森林生态系统辐射响应升高的大气压沉积

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摘要

The effects of elevated atmospheric nitrogen (N) deposition on N cycling in Japanese forest ecosystems are reviewed here to assess the sensitivity of nitrate (NO3-) leaching from forests to streams in response to this deposition. Long-term monitoring of atmospheric N deposition throughout Japan suggests that long-range transport of air pollutants from East Asia accounts for recent increases in atmospheric N deposition in Japan. A new conceptual model of N saturation proposes that kinetic N saturation can be related to unavoidable hydrological nitrate (NO3-) loss from Japanese forests having an Asian monsoon climate with warm and wet summers. Soil microbes, including fungi and ammonia-oxidizing archaea, are important players in these forest ecosystems, affecting nutrient cycling in response to increased atmospheric N deposition. Similarly, a new framework based on a mycorrhizal-associated nutrient economy provides an understanding of NO3- leaching in soils from temperate forests, suggesting that arbuscular mycorrhizal (AM)-dominated forests leach more NO3- in response to N deposition than ectomycorrhizal fungi-dominated forests. Because Japanese cedar and cypress are AM-associated trees, they are likely susceptible to NO3- leaching. Maturation and poor management of such plantations may accelerate NO3- leaching. Grazing by increasing deer populations also enhances NO3- leaching from the soil system. We argue that several factors, including long-range transport of air pollutants, an Asian monsoon climate setting, as well as maturation and poor management of AM-associated plantations, will make Japanese temperate forests more sensitive to increased atmospheric N deposition in East Asia over the next decades.
机译:这里审查了升高的大气氮(n)沉积对N循环循环的影响,此处审查了评估硝酸盐(NO3-)从森林中浸出的敏感性,以响应该沉积。在日本沉积大气压沉积的长期监测表明,来自东亚的空气污染物的远程运输占日本大气中的大气沉积的增加。 N饱和度的新概念模型提出了动力学N饱和度与日本森林的不可避免的水文硝酸盐(NO 3)损失有关,其中欧洲季风气候与温暖和潮湿的夏季。土壤微生物,包括真菌和氨氧化archaea,是这些森林生态系统中的重要参与者,影响营养循环,以响应大气压增加的沉积。同样,基于菌根相关的营养经济的新框架在温带森林中的土壤中提供了No3-浸出的理解,这表明丛枝菌根(AM) - 胚芽林浸出更多NO 3-响应于N沉积而不是Eccocrohizal真菌占主导地位森林。因为日本雪松和赛普拉斯是am相关的树木,所以它们可能易于NO3-浸出。这种种植园的成熟和差的管理可能会加速NO3-浸出。通过增加鹿种群进行放牧也增强了土壤系统的NO3-浸出。我们认为,包括远程空气污染物,亚洲季风气候设施以及成熟和对am相关的种植园的成熟和糟糕的管理,包括日本温带森林对东亚的大气沉积更加敏感的若干因素未来几十年。

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