Nitrification Rates and Controls: The Deep Oligotropic Nitrogen Cycle

硝化速率与控制：深寡向氮循环水。塔式硝化(nh3 .…N0.2和N0..2 . .N0>0.3)是重要的生物地球化学PON/DON汇和N0.3的来源。直接测量这些速率需要(1)测量底物水平，(2)检测孵育过程中的微小变化，以及(3)原位>孵育技术。地下矿化区第一次实际硝化速率将采用新的1.5 n ~ 1.80.2倍。labellingisotope技术。N0.2氧化的自然速率将通过示踪剂的转化来确定。水平 . 1.5 n.1.80 . .2 to.1.5N . . 1.80.3;同位素稀释0.1…5N.1.8.0.2和ıN0.2！池大小的变化会使nh3的氧化速率变为nh2。时间。>原位孵育将使用改良的泰勒/多尔蒂潜水孵育装置（SID）…

Nitrification Rates and Controls: The Deep Oligotropic NitrogenCycle Water.column nitrification (NH.3 .. N0.2 and N0..2 .. N0>0.3) is thecrucial biogeochemical PON/DON sink and source of N0.3 for newprimary production. Measuring these rates directly will requireadvances in (1) measuring substrate levels, (2) detecting smallchanges in incubations, and (3) >in situ> incubation technology. The first real nitrification rates in the subsurface Nremineralization region will use new .1.5N..1.80.2 double.labellingisotope techniques. Natural rates of N0.2 oxidation will bedetermined from transformation of tracer.level .1.5N.1.80..2 to.1.5N..1.80.3; isotope dilution of .1..5N.1.8.0.2 and ıN0.2! pool size changeswill give rates of oxidation of NH.3 to NO.2. Time.course >in situ>incubations will utilize a modified Taylor/Doherty SubmersibleIncubation Device (SID)...