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Effect of salinity and inorganic nitrogen concentrations on nitrification and denitrification rates in intertidal sediments and rocky biofilms of the Douro River estuary, Portugal

机译:盐度和无机氮浓度对葡萄牙杜罗河河口潮间带沉积物和岩石生物膜硝化和反硝化速率的影响

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The regulatory effects of salinity and inorganic nitrogen compounds on nitrification and denitrification were studied in intertidal sandy sediments and rocky biofilms in the Douro River estuary, Portugal, over a 12-month period. Nitrification and denitrification rates were measured in slurries of field samples and enrichment experiments using the difluoromethane and the acetylene inhibition techniques, respectively. Salinity did not regulate denitrification in either environment, suggesting that halotolerant bacteria dominated the denitrifier communities. However, nitrification rates were stimulated when salinity increased from 0 to 15 practical salinity units. NO_3~- addition experiments revealed that NO_3~- availability stimulates denitrification rates in sandy sediments, but not in rocky biofilms; however, in rocky biofilms a positive and linear relationship was observed between denitrification rates and water column NO_3~-concentrations (r = 0.92) during the monthly surveys. The N_2O:N_2 ratios increased rapidly when NO_3~- increased from 63 to 363 μM; however, results from monthly surveys showed that environmental parameters other than NO_3~-availability may be important in controlling the variation in N_2O production via denitrification. Ammonium additions to sandy sediments stimulated nitrification rates by 35% for the 20 μM NH_4~+ addition, but NH_4~+ appeared to inhibit nitrification at high concentration addition (200 μM NH_4~+). In contrast, rocky biofilm nitrification was stimulated by 65% when 200 μM NH_4~+ was added.
机译:在12个月的时间内,研究了葡萄牙杜罗河河口潮间带沙质沉积物和岩石生物膜中盐分和无机氮化合物对硝化和反硝化的调节作用。分别使用二氟甲烷和乙炔抑制技术在田间样品的浆液和富集实验中测量了硝化率和反硝化率。在这两种环境中,盐度均不能调节反硝化作用,这表明,耐盐细菌占主导地位。但是,当盐度从0到15实际盐度单位增加时,硝化速率受到刺激。 NO_3〜-的添加实验表明,NO_3〜-的有效性可刺激沙质沉积物中的反硝化速率,但不会刺激岩石生物膜。然而,在岩石生物膜中,每月的调查中反硝化率与水柱NO_3〜浓度(r = 0.92)之间呈正线性关系。当NO_3〜-从63μM增加到363μM时,N_2O:N_2比值迅速增加。然而,每月调查的结果表明,除NO_3〜有效性以外的环境参数可能对通过反硝化控制N_2O产量的变化很重要。添加20μMNH_4〜+时,向沙质沉积物中添加铵可使硝化率提高35%,但在高浓度添加(200μMNH_4〜+)时,NH_4〜+似乎会抑制硝化作用。相反,当添加200μMNH_4〜+时,岩石生物膜的硝化作用被激发了65%。

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