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Nitrogen dynamics in diesel biodegradation: Effects of water potential, soil C:N ratios, and nitrogen cycling on biodegradation efficacy.

机译:柴油生物降解中的氮动力学:水势,土壤碳氮比和氮循环对生物降解功效的影响。

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Respirometric experiments were performed to evaluate the role of nitrogen in aerobic diesel biodegradation. Specific objectives included (1) evaluating the effects of water potential induced by various nitrogen amendments on diesel biodegradation rates in arid region soils, (2) comparing concurrent effects of C:N ratios and soil water potential on diesel degradation rates, and (3) measuring gross rates of nitrogen cycling processes in diesel-contaminated soil to determine duration of fertilizer bioavailability. In all studies, increasing nitrogen fertilization resulted in a decrease in total water potential and correlated with an increase in lag phase and overall reduction in microbial respiration. Highest respiration and estimated diesel degradation was observed in the 250 mg N/kg soil treatments regardless of diesel concentration, nitrogen source, or soil used, suggesting an inhibitory osmotic effect from higher rates of nitrogen application. The depression of water potential resulting in a 50% reduction in respiration was much greater than that observed in humid region soil, suggesting higher salt tolerance by microbial populations of arid region soils.; Due to the dependence on contaminant concentrations, use of C:N ratios was problematic in optimizing nitrogen augmentation, leading to over-fertilization in highly contaminated soils. Optimal C:N levels among those tested were 17:1, 34:1, and 68:1 for 5,000, 10,000 and 20,000 mg/kg diesel treatments respectively. Determining nitrogen augmentation on the basis of soil pore water nitrogen (mg N/kg soil H2O) is independent of hydrocarbon concentration but takes into account soil moisture content. In the soil studied, optimal nitrogen fertilization was observed at an average soil pore water nitrogen level of 1950 mg N/kg H2O at all levels of diesel contamination.; Based on the nitrogen transformation rates estimated, the duration of fertilizer contribution to the inorganic nitrogen pool at 5,000 mg/kg diesel was estimated at 0.9, 1.9, and 3.2 years in the 250, 500, and 1000 mg/kg nitrogen treatments respectively. The estimation was conservative as ammonium fixation, gross nitrogen immobilization, and nitrification were assumed as losses of fertilizer with only gross mineralization of native organic nitrogen contributing to the most active portion of the nitrogen pool.
机译:进行了呼吸测定实验以评估氮在好氧柴油生物降解中的作用。具体目标包括(1)评估各种氮改良剂引起的水势对干旱地区土壤中柴油生物降解率的影响;(2)比较C:N比和土壤水势对柴油降解率的同时影响;以及(3)测量柴油污染土壤中氮循环过程的总速率,以确定肥料生物利用度的持续时间。在所有研究中,增加的氮肥导致总水势降低,并且与滞后期的增加和微生物呼吸的总体减少有关。在250 mg N / kg的土壤处理中观察到最高的呼吸作用和估计的柴油降解,而与柴油浓度,氮源或所用土壤无关,这表明较高的氮肥施用量具有抑制渗透作用。导致呼吸减少50%的水势下降幅度远远大于在潮湿地区的土壤,这表明干旱地区土壤的微生物种群具有更高的耐盐性。由于对污染物浓度的依赖性,使用C:N比在优化氮肥增加方面存在问题,从而导致高度污染的土壤过度施肥。对于5,000、10,000和20,000 mg / kg柴油处理,测试的最佳C:N水平分别为17:1、34:1和68:1。根据土壤孔隙水中的氮(mg N / kg土壤H2O)确定氮的增加与碳氢化合物的浓度无关,但要考虑土壤的水分含量。在所研究的土壤中,在所有柴油污染水平下,在平均土壤孔隙水氮水平为1950 mg N / kg H2O时均观察到最佳氮肥施肥。根据估算的氮转化率,在250、500和1000 mg / kg的氮肥处理中,5,000 mg / kg柴油时肥料对无机氮库的贡献持续时间分别为0.9、1.9和3.2年。该估计是保守的,因为铵固定,总固氮和硝化作用被认为是肥料的损失,只有自然有机氮的总矿化才是氮库中最活跃的部分。

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