White J P, Schwert D P, Ondrako J P, Morgan L L
Appl Environ Microbiol. 1977 Apr;33(4):918-25. doi: 10.1128/aem.33.4.918-925.1977.
Nitrification, previously shown to occur in the stream under study, ensued only when the stream received heated (28 degree C or above) discharges and was negligible when water temperatures were 17 degree C or lower. The most probable number os ammonium oxidizer in stream bed sediments exceeded intrite oxidizers by ratios of 43:1 to 1,113:1, and the average rate of ammonium oxidation in this stream, 0.50 mg of NH4-N/liter per h exceeded the rate of nitrite oxidation, 0.29 mg of NO2-N/liter per h, resulting in an accumulation of nitrite. Nitrification rates were influenced by the dissolved oxygen concentration, increasing during daylight hours and exhibiting maximum rates during the summer months.
硝化作用此前已被证明在该研究溪流中会发生,只有当溪流接受加热(28摄氏度或以上)排放时才会出现,而当水温为17摄氏度或更低时则可忽略不计。河床沉积物中最可能的铵氧化菌数量超过亚硝酸盐氧化菌的比例为43:1至1113:1,该溪流中铵氧化的平均速率为每小时0.50毫克NH₄-N/升,超过了亚硝酸盐氧化速率(每小时0.29毫克NO₂-N/升),导致亚硝酸盐积累。硝化速率受溶解氧浓度影响,在白天增加,并在夏季月份呈现最高速率。