Filtering involves forcing water through a membrane filled with tiny holes, about 25 microns across (¼ of a
human hair). The filter removes suspended solids from the water, and in fact, the weight of the solids
caught in the filter is one common analysis parameter: total suspended solids (TSS). Such solids can be
virtually invisible to the naked eye, but not dissolved, so they'll eventually settle out if the sample is
left undisturbed. Polluted coalmine water can have tiny bits of iron hydroxide (a.k.a. yellow boy) suspended
in it. In a water sample fixed with acid but not filtered in the field, this iron hydroxide will dissolve
into the water before it arrives at the laboratory, which will give incorrect test results for metals.
Alternatively, in a sample that is not acidified, dissolved oxygen can cause dissolved ferrous iron to
oxygenate into ferric iron en route to the lab. Unless the insoluble ferric iron is filtered out at sampling
time, the lab can't determine how much ferrous vs. ferric iron the water actually contained when it was
sampled. Ferrous iron oxygenation also consumes acid, so certain laboratory acidity or pH measurements will
be wrong.
Although filtering water samples eliminates these errors to some extent, it requires special equipment and
training. Many volunteer groups leave filtering to the analysis laboratory, accepting any inaccuracies that
creep in beforehand. Ultimately, the decision to filter relies on a group’s capacity and requirements, and
it should be discussed with the laboratory that receives the water samples.