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出 处:《价值工程》2017年第12期195-197,共3页Value Engineering
摘 要:为研究铁离子对氮素迁移转化规律的影响,开展室内土柱模拟实验。结果表明:Fe^(2+)通入前,硝态氮和亚硝态氮穿透时间基本一致,趋于平衡,而NH_4^+因含水层介质的吸附作用,其穿透时间较长。FeSO_4溶液通入后,硝酸盐和亚硝酸盐出现明显的下降,Fe^(2+)的存在导致硝态氮的浓度降低而氨氮的浓度升高,Fe^(2+)还原硝酸盐间生成NH_4^+;随着Fe^(2+)持续通入后,生成的Fe^(3+)转化Fe(OH)_3沉淀物,吸附NH_4^+,导致氨氮的浓度降低。因此,铁离子的存在对地下水环境中三氮的转化具有极大的影响,故在地下水高浓度铁的地下水环境下,不可忽视铁离子的存在对三氮的影响。In order to study the effect of iron ions on nitrogen transport and transformation,the indoor soil column simulation experiment was carried out.The results showed that before Fe^2+ was introduced,the permeation time of nitrate nitrogen and nitrite nitrogen was basically the same,and the permeation time of NH4+was higher due to the adsorption of aquifer media.After the FeSO4 solution was introduced,the nitrate and nitrite were decreased obviously.The presence of Fe^2+ resulted in the decrease of the concentration of nitrate nitrogen and the increase of ammonia nitrogen.NH4^+was generated during Fe^2+ reducing the nitrates.After continuous introduction of Fe^2+ ,the Fe^3+ converted to Fe(OH)3 precipitate,and adsorbed NH4+,resulting in a decrease in ammonia concentration.Therefore,the presence of iron ions has a great influence on the transformation of tri-nitrogen in the groundwater environment.Therefore,the influence of iron ions on the tri-nitrogen concentration can not be neglected in the groundwater environment with high concentration of iron.
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