Rick
Well-Known Member
This interests me:drool: How can I in a relatively precice way determine pH of the "root-water"? With very diluted fertilizers (TDS 100ppm) and very open mixes, how do we measure it? I have tried pH meters and indicators, but frankly, this is not straight forward.
Another thing is an obesrevation I have made with fertilizer solutions containing urea. Let me explain;
Ok immediately after mixing, the pH is, say 5.1 at a conductivity of 160 microsiemens/cm (uncertain about the units, correct me if I am wrong) with quite a bit of urea this should be close to a TDS of 100ppm. If the same water is poured into a cup and kept for a day or two, the pH can be measured to 7.0 and conductivity to 190 microsiemens/cm. Here its imaginable that the urea splits to ammonia causing this change. So far so good?
Here comes the question: if the water changes during storage(hours!) how is the situation down at the root level? Would not ammonia (NH3) consume H+ and increase the pH of the mix? Ok, if it is absorbed by the plant, locally H+ is released and this can lower the pH locally. However, if you water every day or so (like I do), at every watering, the root system get flushed with fresh fertilizer and I would claim that there is no chance of a quantitative conversion of the urea to make the mix become acid. Chances are that the opposite happens, that the urea causes the substrate pH to increase instead.
Then my final question: for very open mixes with fairly low CEC; how do I measure the pH? Has anyone actually conducted this exercise?
:confus:
Most of us aren't watering every day. So I would agree if you water that freqently and have a low water retentive and low CEC mix, then pH in is probably close to pH out. But it sounds like many only water once or twice a week, and use water absorbant mixes. So in that case plug the pot and fill with RO water. Give it an hour or so and then test. Or pour through a pot several times until you get an equilibrium value.