Rainbow trout that were held under control conditions, at pH8·0, in moderately hard Hamilton tap water, had Cl − and Na + influx rates ( J CL in and J Na , respectively) of 270 and 300 μmol kg −1 h −1 , respectively. Exposure to pH 9·5 water led to an immediate 67% decline in J CL in and a 45% reduction in J Na in at 0–1 h. Influx rates declined further and by 4–5 h the net decreases in both J CL in and J Na in approximated 80%. By 24 h J CL in had recovered to rates not significantly different from those at pH 8·0; while J Na in only partially recovered and remained about 50% lower than control measurements through 72 h. The complete recovery of J CL in and partial recovery of J Na in may have been related to a fourfold greater branchial chloride cell (CC) fractional surface area observed in rainbow trout exposed to pH 9·5 for 72 h. Ammonia excretion ( J Amm ) was about 170 μmol N kg −1 h −1 at pH 8·0 but was initially reduced by 90% over the first hour of high pH exposure. J Amm rapidly recovered and by 24 h it had returned to pre‐exposure levels. This recovery tended to parallel the partial recovery of J Na in . However, subsequent addition of amiloride (10 −4 M) to the water at 75 h led to no change in J Amm , despite a 50% reduction in J Na in . Thus, it does not appear that there is a linkage between Na + influx and the recovery of ammonia excretion under highly alkaline conditions.
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Wilkie et al. (1994) studied this question.
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