"Is it possible that this lead to an increase of "permanent cavitation"?"
Yes, of course, if the NPSHa at installation altitude is lower than the pump's published NPSHr (defined at 3% head loss with cool water at <presumedly> sea level atmospheric pressure).
At some new altitude, the only thing that appears to change would be the atmospheric pressure. We have to ask, what effects if any that would have on the pump head curve and the NPSHr curve. It wouldn't appear to have any effect on the pump curve. Now, would NPSHr be affected? At any flowrate, would the onset of cavitation be any different when at altitude than when at sea level? If you had a closed system at sea level and at altitude, no. Any supposed difference would have to be attributed to a change in atmospheric pressure. If you use absolute pressure units, it seems apparent to me that the only difference would be accounted for when solving for NPSHa, so nothing else to consider. NPSHa is less, margin is less, so using the NPSHa solution method covers us quite well.
Yes you could redefine the NPSHr curve onset of cavitation for some arbitrary difference in %head loss, 3%, 5%, 10%... , but why do that when the normal NPSHa method already considers this and tells us everything we really need to know. We would wind up with an infinite number of pump curves for just one pump for all altitudes(??) We could just as easily say we should define pump curves for all possible combinations of fluids, each with different vapor pressures, or alternatively, for one fluid at all its possible vapor pressures. Much easier to just do one for cool water at sea level and remember to operate it within the limits of NSPHa > NPSHr.
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"Pumping accounts for 20% of the world’s energy used by electric motors and 25-50% of the total electrical energy usage in certain industrial facilities."-DOE statistic (Note: Make that
99% for pipeline companies)