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首页> 外文期刊>Water, Air, & Soil Pollution >Input–Output Budgets for Inorganic Nitrogen Under Acid Rain in a Subtropical Evergreen Mixed Forest in Central-South China
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Input–Output Budgets for Inorganic Nitrogen Under Acid Rain in a Subtropical Evergreen Mixed Forest in Central-South China

机译:中国中南部亚热带常绿混交林中酸雨下无机氮的投入产出预算

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Inorganic nitrogen deposition and leaching in stream water were monitored from January, 2001 to December, 2004 in a subtropical evergreen mixed forest in central-south China. The seasonal concentration and flux of inorganic nitrogen in bulk precipitation and stream water, seasonal mean net retention of nitrogen and net flux of H+ transformed by nitrogen were estimated and quantified in Shaoshan forest. The research results show that the correlation coefficient of fluxes between bulk precipitation and stream water is significant, with a coefficient 0.916 at the 0.01 level. Mean fluxes of inorganic nitrogen input are 2.62 g m−2 a−1 and 0.516 g m−2 a−1 in form of bulk precipitation and dry deposition respectively, and output in stream water is around 0.22 g m−2 a−1, which indicates that most of nitrogen input is reserved in the forest. Net retention of nitrogen reaches 2.916 g m−2 a−1, just higher than other study plots over the world. Along with the translating of nitrogen ( textNH4+ - textN{text{NH}}_4^ + - {text{N}} and textNO3- - textN{text{NO}}_3^ - - {text{N}}), H+ is imported to the forest ecosystem at the same time. At our study plots, net flux of H+ transformed by nitrogen is about 73.57 mmol m−2 a−1. The positive value suggests that Shaoshan forest is still a finer buffering system to nitrogen deposition and it is far from nitrogen saturation in spite of the high nitrogen deposition.
机译:2001年1月至2004年12月,在中国中南部的亚热带常绿混交林中监测了溪流水中的无机氮沉积和浸出。估算并量化了韶山森林大量降水和溪流水中无机氮的季节浓度和通量,氮的季节平均净保留量和氮转化的H + 净通量。研究结果表明,散装降水与溪流水通量的相关系数很显着,在0.01水平上的相关系数为0.916。无机氮输入的平均通量为2.62 gm -2 a -1 和0.516 gm -2 a -1 分别以大量沉淀和干沉降的形式存在,流水中的产量约为0.22 gm -2 a -1 ,这表明氮的大部分输入保留在土壤中。森林。氮的净保留量达到2.916 g m −2 a −1 ,仅高于全球其他研究区。随着氮的翻译(textNH 4 + -textN {text {NH}} _ 4 ^ +-{text {N}}和textNO 3 --textN {text {NO}} _ 3 ^--{text {N}}),同时将H + 导入森林生态系统。在我们的研究区,氮转化的H + 的净通量约为73.57 mmol m −2 a -1 。正值表明,韶山森林仍然是氮沉降的更好缓冲系统,尽管氮沉降很高,但距离氮饱和还很远。

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