摘要
Nitrite dynamics could be highly associated with forest N cycles. However, they have often been overlooked mainly because of the experimental difficulties that occur owing to chemical reactive nature of NO2鈭?/sup>. We investigated NO2鈭?/sup> dynamics in an N-saturated forest soil with a recently developed method using 15N. Soils were aerobically incubated for 145聽h after 15NO2鈭?/sup> addition, and changes in 14N and 15N concentrations of NO2鈭?/sup>, NO3鈭?/sup>, NH4+, and dissolved organic N (DON) were monitored. Simultaneous production and consumption of NO2鈭?/sup> were observed. The turnover rate of NO2鈭?/sup> was even faster than that of NH4+ and NO3鈭?/sup> calculated in other studies. Of the added 15NO2鈭?/sup>, 28.5%was oxidized to NO3鈭?/sup> and 17.8%was incorporated into the DON pool within 4聽h. The remainder might be emitted as gas or fixed by insoluble soil organic matter. Our results suggested that rapid NO2鈭?/sup> turnover could be a major driving force for N transformations in forest soil.