养殖密度对硝化型生物絮团系统中凡纳滨对虾生长和水质的影响

利用硝化型生物絮团系统进行凡纳滨对虾的养殖,并通过设置不同的养殖密度探究不同养殖密度下硝化型生物絮团系统对凡纳滨对虾生长性能和水质情况的影响。实验选择同一批标粗到一定规格的健康凡纳滨对虾[体长(4.80±0.25) cm,体质量(0.98±0.16)g],分成5个密度梯度组放养到养殖池中,进行为期45 d的养殖。结果表明:80～610尾/m~3范围内,硝化型生物絮团系统对非离子氨和亚硝酸盐氮可以控制在警戒浓度(0.2 mg/L)附近波动,为凡纳滨对虾健康生长提供了良好的环境,保证养殖存活率,另外该系统下适当的排污可以避免高密度养殖下硝酸盐氮积累太快;80～610尾/m~3时存活率随密度升高而下降,但产量随密度升高而增加。     

循环水养殖系统生物滤池细菌群落的PCR-DGGE分析

通过模拟实验对循环水养殖系统中不同初始NH ₄N浓度的生物滤池中生物膜上和水中的细菌数量及群落种类组成进行了研究。对成熟生物膜及水体样品中的异养菌、氨氧化菌、亚硝酸盐氧化菌的培养计数结果表明,随着生物滤池初始氨氮浓度增大,除异养细菌数量逐渐下降外,生物膜上的氨氧化菌和亚硝酸盐氧化菌数量呈逐渐增加趋势,且均高出水样3~4个数量级;同时对上述样品的16S rRNA基因片段的PCR扩增产物进行变性梯度凝胶电泳(DGGE)分析及其序列同源性分析的结果表明,生物膜和水中都有较高的细菌多样性,同一初始氨氮浓度的滤池中生物膜上的细菌多样性高于水中的。生物滤池中的细菌主要由拟杆菌门的黄杆菌纲和变形菌门的α-、β-、γ-变形菌纲的15种细菌组成。生物膜上的优势菌包括奥雷氏菌属、湖饲养者菌属、泥滩杆菌属、沉积杆菌属、雷辛格氏菌属、冷蛇形菌属和亚硝化单胞菌属等;水体中的优势菌则有明显差异,主要有蛋黄色杆菌属、Nautella,玫瑰杆菌属和一种硫氧化菌等。初始氨氮越高的滤池中,亚硝化单胞菌属的细菌在生物膜上所占比例越高,逐渐成为优势菌之一。实验证实,挂膜初期,提高水体中初始氨氮浓度,有利于硝化细菌的富集和固着,提高生物滤池的除氮效率。     

硝化细菌浓度及滤料对养殖水中氨氮处理效果的影响

分别研究了不同硝化细菌浓度(0、20、60、120 mL/100 L)和不同微生物滤料(珊瑚石、锅炉煤渣、牡蛎壳)对养殖水中氨氮处理效果的影响。结果显示,添加硝化细菌后,水体中的氨氮浓度呈现下降趋势,在8～12 h出现极低值后,开始上升,但上升速度较慢;随着水体中硝化细菌添加量的增加,水体中的氨氮浓度下降速度加快;水体中亚硝酸氮浓度呈现先上升后下降的趋势,并在4～6 h出现极高值,然后迅速下降,且硝化细菌添加量越高,下降速度越快。硝化细菌对以珊瑚石和锅炉煤渣为滤料的养殖水体中氨氮和亚硝酸氮的处理效果显著优于牡蛎壳,但珊瑚石和锅炉煤渣之间无显著差异。综合试验结果,应急水质处理时,硝化细菌菌剂的添加量以一次60 mL/100 L(或以活菌计数为1.2×109个/100 L)、间隔24 h添加1次为宜;经过脱硫筛选之后的锅炉煤渣可以作为循环水养殖用滤料。     

The effects of nitrogen sludge load and DO on high concentration nitrous nitrifying system

The purpose of this paper is to investigate the impact of nitrogen sludge load and dissolved oxygen(DO) on nitrite nitrification system. The following conclusions have been drawn based on the experimental data and analysis results: 1) The ammonium degradation rate and the nitrous accumulation rate of high concentration nitrous nitrifying system decline with the increase of NH+4-N sludge load. When HRT is less than two days, the ammonium degradation rate rapidly declines to 25%~29% with the increase of NH+4-N sludge load. When HRT is beyond two days, the ammonium rate of the system slowly falls to 50%~60% with the NH+4-N sludge load increased. When HRT is 2.5 days or 3 days, the declined trend of the system nitrous accumulation rate is not obvious with the NH+4-N sludge load increased. When HRT is 5 days, the decrease of nitrous accumulation rate is caused by the adaptation of sludge. So the NH+4-N sludge load of high concentration nitrous accumulation system should not be too high; 2)With the increase of DO, the ammonium degradation of high concentration nitrous nitrifying system is gradually increased. When the DO is less than 0.7 mg/L, it is not conductive to the ammonium degradation. When the DO is higher than 2 mg/L, the oxide of NH+4-N is changed into the increased of NO3-N and the nitrous accumulation rate declined. If the concentration of DO is controlled within 0.7to 1.3 mg/L, the high concentration nitrous nitrifying system can have a good NH+4-N degradation rate and nitrous accumulation rate.     

丙酮酸钠对硝化细菌制剂活性的影响

分别研究丙酮酸钠对淡水型和海水型硝化细菌制剂中氨氧化细菌(AOB)和亚硝酸盐氧化细菌(NOB)活性的影响。结果表明,丙酮酸钠能明显提高AOB活性,缩短其对环境的适应时间。在丙酮酸钠浓度为7mmol/L时,12h海水型硝化细菌和淡水型硝化细菌对氨氮去除率分别为54.7%和63.4%,是对照组的8.82倍和2.98倍。丙酮酸钠对NOB活性影响与AOB存在不同,其中,丙酮酸钠对海水型硝化细菌NOB有抑制作用,并随其浓度升高而增大,但对淡水型硝化细菌NOB活性影响较小。     

氨氮质量浓度及附着基筛选对硝化细菌氨氮净化影响

将带有试验硝化细菌——食油假单胞菌X14-1-1的等面积陶粒、聚氯乙烯、纤维、火山岩、无纺布和流化床6种材料的附着基分别放入1 L的充气瓶内,在36℃、130 r/m in的摇床上混合培养48 h后,洗脱计数测定菌种附着数量.模拟氨氮去除率试验中氨氮初始质量浓度为0(不加硫酸铵)、10、20、30、40、50、60 m...     

控释掺混肥对大蒜根际土壤微生物的影响

通过大田试验系统研究了控释掺混肥对大蒜根际土壤微生物数量的变化。结果显示：（1）大蒜根际土壤中细菌、放线菌数量和微生物总量随控释掺混肥施入量的增加而增多,而真菌数量减少。控释掺混肥与习惯施肥（CCF）相比,等量（CRF1）和减量20％（CRF2）时大蒜根际土壤中细菌、放线菌数量和微生物总量极显著地高于CCF,真菌数量极显著地低于CCF。（2）CRF1和CRF2处理土壤生理功能微生物（自生固氮菌、氨化细菌、硝化细菌和纤维素分解菌）的数量不仅显著高于不施肥处理,而且还显著高于CCF,60%控释掺混肥用量处理（CRF3）略低于CCF,但差异不显著。研究表明控释掺混肥可通过促进细菌、放线菌和生理功能微生物的繁殖来提高土壤速效养分含量,进而提高大蒜鳞茎产量。     

短程硝化反应器过程动力学特性研究

    采用脉冲刺激响应技术对内循环颗粒污泥床短程硝化反应器进行了示踪试验,结果表明反应器循环区的串联级数N为1.02,流态接近全混流反应器(CSTR),反应器沉淀区的分散数D/uL为0.00148,流态接近平推流反应器(PFR),整个反应器的流动模型可以表示为全混流反应器和平推流反应器的串联组合.对内循环颗粒污泥床短程硝化反应器曝气过程中的氨逃逸进行了分析,建立了氨逃逸的动力学模型,测得稳态运行时氨逃逸系数KNH3为0.692 L·h-1.通过物料平衡,建立了内循环颗粒污泥床短程硝化反应器的过程动力学模型,测得稳态运行时的模型参数:氨氮最大比去除速率vmax=8.13mg NH4+-N.(g MLSS)-1·h-1、饱和常数Ks=1.73 mg NH4+-N·L-1,动力学模型的计算值与试验值吻合良好,两者的平均相对误差为12.8%.     

Improvement of preservation method for ammonia-oxidizing bacteria by freeze-drying

Long-term preservation of ammonia-oxidizing bacteria had been achieved until now by using the silica gel-freezing method. Recently, the freeze-drying method for the preservation of microorganisms has been widely used, and has been applied to the preservation of ammonia-oxidizing bacteria. The 10% skim milk-l% pyruvate or glutamate ratio was optimum as a dispersion-medium, and the preservation temperature of the freeze-dried cells was effective at -80°C. This method of preservation was found to be considerably more effective than the silica gel-freezing method.     

Length of Incubation for the Estimation of the Most Probable Number of Nitrifying Bacteria in Soil

Abstract

The Zn content in 8 soil chemical fractions was determined for 21 greenhouse soils and for 8 reference (open field) soils from Kochi Prefecture, Japan to investigate the forms of spontaneously accumulated Zn in the greenhouse soils associated with heavy application of fertilizers and manures. Sequential extraction method was applied to every soil and each Zn fraction was designated as exchangeable (Ex-Zn), Pb-displaceable (Pb-Zn), acid soluble (Aci-Zn), Mn oxide-occluded (MnO-Zn), organically bound (OM-Zn), amorphous Fe oxide-occluded (AFeO-Zn), crystalline Fe oxide-occluded (CFeO-Zn), and residual (Res-Zn) fractions. The Zn content of the greenhouse soils was significantly higher than that of the reference soils in every fraction, except for the CFeO-Zn, and Res-Zn fractions. The Pb-Zn, Aci-Zn, and MnO-Zn fractions showed a difference of more than 60% in the total Zn content between the two soil groups. The amounts of Zn extracted in the Pb-Zn, Aci-Zn, MnO-Zn, AFeO-Zn, and CFeO-Zn fractions of the greenhouse soils increased con-comitantly with the accumulation of applied macro-nutrients. These results indicated that the accumulation of Zn in greenhouse soils caused by intensive fertilization had proceeded through specific adsorption onto or occlusion by the oxides and hydroxides of Fe and Mn in soils.