The influence of atmospheric NH3 on the apoplastic pH of green leaves: a non-invasive approach with pH-sensitive microelectrodes

The apoplastic pH of intact green leaves of Bromus erectus was measured non -invasively by inserting blunt microelectrodes through stomatal openings. A fter making electrical contact, the recorded signal was stable for hours, y ielding a pH of 4.67 +/- 0.10. The leaves responded to 'light-off' with an initial transient acidification and subsequent sustained alkalinization of 0.2-0.3 pH; 'light-on' caused the opposite response. Flushing the leaves wi th 280 nmol NH3 mol(-1) air within 18 +/- 6 s alkalinized the apoplast by 0 .22 +/- 0.07 pH, followed by a slower pH increase to reach a steady-state a lkalinization of 0.53 +/- 0.14 after 19 +/- 7 min. This pH shift was persis tent as long as the NH3 was flushed, and readily returned to its initial va lue after replacing the NH3 with clean air. The resultant [NH4+] increase w ithin the apoplast was measured with a NH4+-selective microelectrode. In th e presence of 280 nmol NH3 mol(-1) air, apoplastic NH4+ initially increased within 15 +/- 10 s to 1.53 +/- 0.41 mM, to reach a steady state of 1.62 +/ - 0.16 mM after 27 +/- 7 min. An apoplastic buffer capacity of 6 mM pH(-1) unit was calculated from the initial changes of pH and [NH4+], whereas the steady-state values yielded 2.7 mM pH(-1). Infiltrated leaves responded to NH4+ with concentration-dependent depolarizations, the maxima of which yiel ded saturation kinetics indicating carrier-mediated NH4+ uptake into adjace nt cells, as well as a linear component indicating nonspecific transport. W e infer that the initial alkalinization is due to rapid conversion of NH3 t o NH4+, whereas the slower pH increase would be caused by regulatory proces ses involving both membrane transport, and (mainly) NH4+ assimilation. Poss ible consequences of the NH3-induced pH shift for the development of plants growing in polluted areas are discussed.