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首页> 外文期刊>Botanical Bulletin of Academia Sinica >NITROGEN NUTRITIONAL STATUS AND FATE OF APPLIED N IN MANGROVE SOILS
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NITROGEN NUTRITIONAL STATUS AND FATE OF APPLIED N IN MANGROVE SOILS

机译:红壤性土壤中氮素的养分状况和氮素分配状况

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摘要

Fluctuation of inorganic N content in mangrove soils of the Tamshui estuary, northwestern Taiwan, showed that ammonium concentrations ranged from 0.15 to 17.10 mg N kg(-1) soil, while nitrate ranged from trace amounts to 2.54 mg N kg(-1) soil. Geographic and edaphic factors caused the difference of inorganic N between the sites. These levels were much higher than values reported elsewhere. Pot experiments showed the added N-15 labeled ammonium (6 mg N per pot) disappeared rapidly. The N-15 residues remaining in the soil were mostly in the organic form. N uptake by Kandelia candel was 13.1% after one month and 19.6% after three months. Recoveries of applied N after three months were 40.3% in planted treatment and 32.6% in unplanted treatment. Most of the N loss, occurring in the first month, can be attributed to denitrification. The large N loss suggests a high potential for mangrove soils to remove high input of N from the river through denitrification.
机译:台湾西北部淡水河口红树林土壤中无机氮含量的波动表明,铵盐浓度范围为0.15至17.10 mg N kg(-1),而硝酸盐含量范围为痕量至2.54 mg N kg(-1)。 。地理和地理因素造成了站点之间无机氮的差异。这些水平远高于其他地方报告的值。锅实验表明,添加的N-15标记的铵盐(每锅6毫克氮)迅速消失。残留在土壤中的N-15残留物大部分为有机形式。一个月后,Kandelia candel吸收的氮为13.1%,三个月后为19.6%。三个月后,种植处理的氮恢复率为40.3%,未种植处理的氮恢复率为32.6%。氮的大部分损失发生在第一个月,可以归因于反硝化作用。大量的氮流失表明红树林土壤具有很高的潜力,可以通过反硝化作用从河流中去除大量的氮。

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