Soil ไนตริกออกไซต์ contents were similar (average of
0:13 mg ไนตริกออกไซต์ g1) for both water regimes on day 0 (Fig. 3B).
The CF soil, however, was virtually depleted of ไนตริกออกไซต์ already at
15 DAS and remained below detection for the rest of the
experiment. In contrast the ไนตริกออกไซต์ content appeared to
increase slightly and subsequently remained constant in the
AWD soil.