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Nitrification and denitrification potentials of soil in Liaohe estuary wetland

机译:辽河河口湿地土壤硝化与脱氮潜力

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Nitrification and denitrification plays an important role in the nitrogen cycle in wetlands. The nitrification and denitrification potentials of soil from different depths (0-40 cm) in Liaohe estuary wetland were studied with laboratorial batch incubation for three weeks. The results showed that the percent of nitrification and denitrification in soil at different depth were about 25-40% and 31-63% of soil total added nitrogen over three weeks, respectively. Both the denitrification and nitrification of soil at different depth showed an exponential decay trend over the incubation period. The corresponding rates were 0.013-0.021 mg·kg~(-1)·d~(-1) and 0.017-0.057 mg·kg~(-1)·d~(-1). The value of surface soil (0-5cm) was significant higher than that of the subsoil (5-40 cm) (p < 0.05) and there was no significant difference between values of the subsoil (p > 0.05).
机译:硝化和反硝化在湿地的氮循环中起重要作用。研究了辽河河口湿地不同深度(0-40厘米)的土壤硝化和脱氮电位,实验室批量孵育三周。结果表明,不同深度的土壤中硝化和脱氮的百分比分别为约25-40%和31-63%的土壤总增加氮。不同深度的土壤的脱氮和硝化均显示出培养期的指数衰减趋势。相应的速率为0.013-0.021 mg·kg〜(-1)·d〜(-1)和0.017-0.057 mg·kg〜(-1)·d〜(-1)。表面土壤(0-5cm)的值显着高于底土(5-40cm)(P <0.05),底层的值没有显着差异(p> 0.05)。

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