by BronF » 2011-10-07, 05:59
Hi Chris
It's been a while since my last post and I have continued to investigate the analysis of mine waters using ICP-MS. It's true that every mine water is different in terms of metal/metalloid concentrations, however, I believe their one common feature is that the salt content is generally much higher than 'natural' riverine waters from which high metal/metalloid certified reference waters are generally sourced.
The presence of salts in the matrix is a very significant issue in terms of polyatomic interferences and salting of the cone. This is usually dealt with by increasing the dilution factor of the samples. However, this comes at a cost of losing counts for certain elements of interest. The effect of salts on measured sample concentrations can be insidious as your CRWs (which are typically low in salts) generally come back with good recovery. You only know that you have a problem when you run the same sample at two different dilution factors and get vastly different results.
There are corrections that can be applied for these interferences but inital detection of the problem can be difficult without a good CRW. The other issue and perhaps the reason for why there is yet to be a 'mine water' CRW, is that I assume a water high in salt and metal content would be hard to keep stable. Hence, getting the same measured concentration values across multiple labs would be difficult, if impossible, owing to the chemical nature of the water.
No easy answers. Just some thoughts to add to the forum.
Bron.