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底泥中氮的主要迁移转化过程及其转化模型的研究

TRANSPORTATION AND TRANSLOCATION OF NITROGEN IN SEDIMENT

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【作者】 戴树桂; 张明顺; 庄源益;

【Author】 Dai Shugui,Zhang Mingshun,Zhuang Yuanyi (Department of Environmental Science,Nankai University,Tianjin)

【机构】 南开大学环境科学系; 南开大学环境科学系 天津; 天津 中国环境管理干部学院; 天津;

【摘要】 研究了NO3--N,NH4+-N在底泥中的扩散、吸附以及NO3--N的反硝化等过程.结果表明,在泥-水界面间,NH4+-N主要向上浮水中扩散,NO3--N主要向间隙水中扩散.扩散到间隙水中的NO3--N45%被吸附,30%因反硝化作用而失掉,其反硝化速率常数在7—11cm层最大.氮的吸附速率常数在表层最大.建立了间隙水中NO3--N和NH4+-N的转化模型,并计算了氮在泥-水界面间的扩散量,计算结果与实测结果基本相符.

【Abstract】 The diffusion and the adsorption of NO8-N and NH4-N and the denr-trification of NO8-N in sediment were studied. NH4-N diffused cross the interface of water-sediment into the water column while NO8-N transferred in another direction.In interstitial water,45 percent of NO8-N from overlying water was adsorbed and 30 percent was lost during denitrifica-tion. The denitrification rate constant of NO8-N reached its maximum between 7-11 cm of the sediment and the maximum adsorption occurred in the top few centimeters of the sediment. Transport models of NO8-N and NH4-N in interstitial water were suggested and applied to calculate the amounts of nitrogen transferred cross the interface.

【关键词】 氮; 循环; 模型; 富营养化;
【Key words】 nitrogen; sediment; mass transfer.;
  • 【文献出处】 环境科学学报 ,Acta Scientiae Circumstantiae , 编辑部邮箱 ,1990年01期
  • 【被引频次】40
  • 【下载频次】486
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