华北平原几种主要类型土壤的硝化及反硝化活性

取用华北平原5种主要土壤进行实验室培养试验,研究不同类型土壤间硝化反硝化活性的差异。结果表明,培养28h后砂姜黑土、潮土、褐土、盐渍土和风沙土的硝化率分别为7.9%、20.8%、46.4%、22.5%和20.3%;148h后砂姜黑土的硝化率为18.7%,其它4种土壤达98.4%—100%,基本硝化完全;培养268h释放的N2O总量分别为0.04、0.27、0.24、0.41和0.45μgN·g-1土。培养650h的反硝化损失量分别为0.6、0.3、0.08、0.02和0.05μgN·g-1土。可见,不同的土壤中砂姜黑土的硝化作用活性较弱,而反硝化活性较强;潮土、褐土、盐渍土和风沙土的硝化作用活性较强,而反硝化活性相对较弱。土壤的硝化及反硝化作用与土壤质地和pH有关,与硝化和反硝化菌数量无明显相关性。     

以CuO为主要活性组分同时脱硫脱硝催化剂的研究

根据同时脱硫脱硝的要求，对以ＣｕＯ为主要活性组分催化剂的制备过程和反应动力学进行了研究，通过实验获得浸清液浓度、浸渍时间，活化温度和活化时间等最佳制备条件，以及ＳＯ２和ＮＯｘ脱除率达９０％以上的反应温度、空间速度、ＣｕＳＯ４／ＣｕＯ摩尔比和Ｃｕ／Ｓ比等工艺参数。     

SBR法处理高浓度生活污水研究

对SBR法处理高浓度生活污水的可行性进行了研究。结果表明,该工艺在悬浮性固体(MLSS)含量为3 g／L,COD容积负荷为1．0 kg／(kg·d),好氧4 h,溶解氧(DO)3～5 mg／L;厌氧2 h,DO<0．2 mg／L;好氧1 h,DO3 mg／L;缺氧1 h,DO<0．5 mg／L以及试验温度22～28℃,周期为9 h的运行条件下,对COD、NH(?)-N、TP去除率分别为97．5％,94．9％,97．1％;该工艺有利于反硝化除磷过程的同步实现,其适宜的污泥龄为20 d。     

以棉花为碳源去除地下水硝酸盐的研究

采用室内试验装置,研究了以棉花为碳源和反应介质的生物反应器去除地下水中的硝酸盐。结果表明,以棉花为碳源的反应器启动快。在室温25℃±1℃,进水硝酸盐氮浓度为22.6mgN·L-1,水力停留时间不小于9.8h时,反应器对硝酸盐氮可以100%去除,出水未检出亚硝酸盐。反硝化反应受温度变化及水力停留时间影响大:14℃的反硝化速率不到25℃的1/2;当水力停留时间为7.2h,N去除效率只有45%。反硝化反应受pH值和DO的影响小,当pH值在6～9,进水DO在2～6mg·L-1范围变化时,反应器去除效率没有变化。在反应进行过程中,棉花也被消耗掉。     

The Effects of Different Fertilizing Methods on Nitrification and Denitrification in Black Soil in Songnen Plain

The paper compared the effects of application of farm manure with chemical fertilizers on nitrification and denitrification in black soil, the result showed that the numbers of nitrobacterias and denitrobacterias in farm manure treatment were both higher than that of other treatments. The intensity of denitrification in chemical treatment was higher than that of manure treatment. The content of organic matter in soil was correlated with the intensity of nitrification and denitrification, and the coefficients were resnectively 0.9981 and 0.8693.     

阿氏节杆菌菌株DA-1的厌氧反硝化研究

阿氏节杆菌(Arthrobacter arilaitensis)菌株DA-1是一株氨氮降解细菌,且在有氧及厌氧条件下均具有反硝化作用.通过对该菌的厌氧反硝化条件进行优化,考察了碳源、C/N、温度和初始pH对其反硝化作用的影响.结果表明,乙酸钠为最佳的反硝化碳源,当C/N为10∶1、温度为30℃、初始pH为7.0时,A.arilaitensis DA-1能获得最高的反硝化效率,在该条件下,向硝酸盐模拟污水(NO3--N浓度为25mg/L)中接入2％(V/V)的A.arilaitensis DA-1菌剂,经过48 h的静置培养,N03--N的去除量达到了20.13 mg/L,而此时NO2--N积累浓度仅为0.56 mg/L.     

The influencing factors of N2O emission and denitrification in the soil of water-level-fluctuation zone in the Three Gorges Reservoir area

In order to study the influences of water filled pore space (WFPS), temperature, the addition of nitrate (NO -3) and carbon source on N2O emission and denitrification in the soil of water-level-fluctuation zone in the Three Gorges Reservoir area, C2H2 in hibition incubation experiments are applied. Results from experiments in laboratory and in situ field are analyzed. Results show that the WFPS is a main factor determining N2O emission and denitrification. Denitrification rate increases while the WFPS increases, and the maximum denitrification rate and the maximum N2O emission rate appear when the WFPS is 100% and 60%, respectively. In addition, while the temperature is between 10 ℃ and 40 ℃, the increase of temperature contributes to the increase of the N2O emission and denitrification rates. Furthermore, it is found that the N2O emission and denitrification rates are significantly and positively correlated with temperature. The addition of carbon source could increase denitrification performance in soil. However, the addition of nitrate has a negative impact on the denitrification performance, because nitrogen source is not the main factor determining denitrification performance and excessive nitrate could inhibit the denitrification in these experiments. The addition of glucose, which is a carbon source easily be utilized by denitrifying bacteria, could significantly increase the denitrification rate in soil, and the maximum denitrification rate takes place while the carbon content in per kilogram soil is 240 mg.     

Nitrogen Removal Improvement by Adding Peat in Deep Soil of Su bsu rface Wastewater Infiltration System

In order to enhance the nitrogen removal, a subsurface wastewater infiltration system （SWIS） was improved by adding peat in deep soil as carbon source for denitrification process. The effects of addition of carbon source in the underpart of the SWIS on nitrogen removal at different influents （with the total nitrogen （TN） concentration 40 and 80 mg L^-1, respectively） were investigated by soil column simulating experiments. When the relatively light pollution influent with 40 mg L^-1 TN was used, the average concentrations of NO3-N and TN in effluents were （4.69±0.235）, （6.18±0.079） mg L^-1, respectively, decreased by 32 and 30.8% than the control; the NO3--N concentration of all effluents was below the maximum contaminant level of 10 mg L^-1; as high as 92.67% of the TN removal efficiency was achieved. When relatively heavy pollution influent with 80 mg LITN was used, the average concentrations of NO3--N and TN in effluents were （10.2±0.265）, （12.5±0.148） mg L^-1 respectively, decreased by 20 and 21.2% than the control; the NO3--N concentration of all effluents met the grade Ⅲ of the national quality standard for ground water of China （GB/T 14848-1993） with the values less than 20 mg L^-1; the TN removal efficiency of 94.1% was achieved. In summary, adding peat in the underpart of the SWIS significantly decreased TN and NO3- -N concentration in effluents and the nitrogen removal efficiency improved significantly.     

不同氮硫浓度及氮硫比对硫酸盐还原厌氧氨氧化脱氮效果的影响

在硫酸盐还原厌氧氨氧化（Sulfate-Reducing Anaerobic Ammonium Oxidation,SRAO）脱氮工艺的基础上,探究了SO42-浓度在100 mg/L的条件下,控制NH4+的投加量在不同N/S（NH4+-N/SO42-）浓度比下ASBR（Anaerobic Sequencing Batch Reactor）反应器的运行效果及其脱氮性能。N/S从1.0增大到3.0时,ASBR中氨氮的平均去除率从78.5%增加到94.4%,但体系内SAD（Sulfur Autotrophic Denitrification）菌的丰度及活性未受到明显抑制,SRAO作用和ANAMMOX（Anaerobic Ammonia Oxidation）作用始终是ASBR脱氮的主要途径。当N/S的浓度比由3增至4时,ASBR中氨氮的平均去除率由94.4%下降为69.2%。这表明随着N/S的增大,体系内ANAMMOX菌和SRAO菌活性的降低,抑制了体系脱氮性能。这时SAD菌的丰度及活性略有增加。硫的去除率随N/S比的变化趋势和总氮的去除规律类似,在N/S=3时达到最大74.2%。结合高通量测序结果,说明不同N/S下的脱氮微生物优势菌群会不断变化,改变体系脱氮除硫性能。     

Denitrification characteristics of pond sediments in a Chinese agricultural watershed

Ponds are widely distributed in rice-based agricultural watersheds, particularly in southern China, and may play an important role in nitrate (     ) removal. However, the denitrification rate of pond sediment, measured using the acetylene (C₂H₂) inhibition technique, indicated that the amount of nitrogen removed by denitrification accounted for <1% of the total nitrogen applied. The present study was undertaken to determine the effects of sediment depth and temperature on denitrification of pond sediment using the C₂H₂ inhibition technique. The highest denitrification potential was found in the upper 5 cm of sediment, but this only accounted for approximately 34% of the total denitrification of the upper 0–30 cm of sediment, suggesting that sediment denitrification potential would be underestimated if only the upper 5 cm of sediment was measured. The denitrification potential was low and showed a weak response over a temperature range of 6–18°C, whereas denitrification increased significantly from 18 to 30°C, indicating that denitrification may play an important role in the removal of     in warm seasons. A comparison of the     disappearance and C₂H₂ inhibition methods showed that they were significantly ( P  < 0.01) and positively correlated. However, the C₂H₂ inhibition method gave only approximately 25% of the values determined by the     disappearance method.