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Denitrification Potential And Its Relation To Organic Carbon Quality In Three Coastal Wetland Soils

机译:三种滨海湿地土壤的反硝化潜力及其与有机碳质量的关系

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Capacity of a wetland to remove nitrate through denitrification is controlled by its physico-chemical and biological characteristics.Understanding these characteristics will help better to guide beneficial use of wetlands in processing nitrate.This study was conducted to determine the relationship between soil organic carbon (SOC) quality and denitrification rate in Louisiana coastal wetlands.Composite soil samples of different depths were collected from three different wetlands along a salinity gradient,namely,bottomland forest swamp (FS),freshwater marsh (FM),and saline marsh (SM) located in the Barataria Basin estuary.Potential denitrification rate (PDR) was measured by acetylene inhibition method and distribution of carbon (C) moieties in organic C was determined by ~(13)C solid-state NMR.Of the three wetlands,the FM soil profile exhibited the highest PDR on both unit weight and unit volume basis as compared to FS and SM.The FM also tended to yield higher amount of N_2O as compared to the FS and SM especially at earlier stages of denitrification,suggesting incomplete reduction of NO_3~-at FM and potential for emission of N_2O.Saline marsh soil profile had the lowest PDR on the unit volume basis.Increasing incubation concentration from 2 to 10 mg NO_3~--N L~(-2) increased PDR by 2 to 6 fold with the highest increase in the top horizons of FS and SM soils.Regression analysis showed that across these three wetland systems,organic C has significant effect in regulating PDR.Of the compositional C moieties,polysaccharides positively influenced denitrification rate whereas phenolics (likely phenolic adehydes and ketonics) negatively affected denitrification rate in these wetland soils.These results could have significant implication in integrated assessment and management of wetlands for treating nutrient-rich biosolids and wastewaters,non-point source agricultural runoff,and nitrate found in the diverted Mississippi River water used for coastal restoration.
机译:湿地通过反硝化去除硝酸盐的能力受其理化和生物学特性的控制,了解这些特性将有助于更好地指导湿地在硝酸盐处理中的有益用途。本研究旨在确定土壤有机碳(SOC)之间的关系。州沿海湿地的质量和反硝化率。沿着盐度梯度从三个不同的湿地收集了不同深度的复合土壤样品,即盐碱化沼泽(FS),淡水沼泽(FM)和盐沼(SM)。通过乙炔抑制法测量潜在的反硝化速率(PDR),并通过〜(13)C固态NMR确定有机C中碳(C)部分的分布。在这三个湿地中,FM土壤剖面与FS和SM相比,单位重量和单位体积的PDR最高。与FM和FM相比,FM倾向于产生更高的N_2O量。 FS和SM尤其是在反硝化的早期阶段,这表明FM中NO_3〜-的还原不完全和N_2O的排放潜力。盐沼土壤剖面的PDR以单位体积为基础最低,孵化浓度从2增加到10 mg NO_3〜--NL〜(-2)使PDR增加2到6倍,其中FS和SM土壤的最高层增加最多。回归分析表明,在这三个湿地系统中,有机碳对PDR的调节作用显着。在组成碳的C部分中,多糖对反硝化率有积极影响,而酚类(可能是酚醛和酮类)对这些湿地土壤的反硝化率有负面影响。这些结果可能对湿地综合评估和管理,以处理营养丰富的生物固体和废水具有重要意义。 ,非点源农业径流和用于沿海恢复的密西西比河分流水中发现的硝酸盐。

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