Cdsdave said:
He said it was best to adjust the KH and not try to adjust the PH directly. What's your opinion.
Short answer....
Correct, it is best to adjust KH when you are trying to adjust the pH to be
lower since the KH is what controls the low end of the pH range and prevent the pH from changing lower.
Here is my attempt at explaining on
how to stabilise a pH at 7.0 for a freshwater outdoor pond.
Grr, I can't find the thread I wanted to, but to quickly tell ya... Oyster shells (calcium carbonate) works better when the pH is below 8.3~8.5 since it functions more as a KH stabilizer rather than a calcium stabilizer eventhough it does release some calcium.
Long answer....
A layman version of the
Henderson-Hasselbalch equation for the pH formula is...
pH = pKa + log([HCO3-]/[H2CO3])... H2CO3 is carbonic acid, that is created when carbon dioxide (CO2) dissolves into water (H2O). Carbonic acid is considered to be the weak acid. HCO3- is the inorganic carbon, bicarbonate, that is found in baking soda, which is sodium bicarbonate (NaHCO3). Bicarbonate is considered to be a form of salt that reacts with carbonic acid. The relationship between a weak acid and its salt is what creates the buffer, which then determines the pH. There are two salts that react with carbonic acid. One salt is bicarbonate (HCO3-) and the other salt is carbonate (CO32-). This particular buffer system is called a carbonate buffer whenever these two salts and carbonic acid are predominant in the pond water. pKa is the coefficient of the hydrogen cation (H+) present in the salt. Since there is only one hydrogen cation present between the two salts, then this indicates there is only buffer range for the bicarbonate/carbonate buffer range, which is around 8.3~11.2. As nature creates hydroxides (OH-), then carbonates (CO32-) are created and this increased carbonate concentration raised the pH above 8.3. When the water is more closely to complete bicarbonate concentration, then the water's pH is around 8.3~8.5. When the water is more closely to complete carbonate concentration, then the water's pH is around 10.8 ~ 11.2.
Do not confuse sodium (Na++) by calling this a salt. In stoichemistry, sodium acts as a type of electrolyte, in regards to these buffer systems. Sodium is often used since its electochemical bond is very easy to break in water to release constiuent component, such as bicarbonate in baking soda (that is sodium bicarbonate).
There is also an equilibrium dance that occurs with carbonic acid (H2CO3), bicarbonate (HC03-), carbonate (CO32-), and carbon dioxide (CO2-). To better understand this pattern, then google "freshwater carbonate speciation diaphragm", which is a
Bjerrum plot. Many environmental variables change this diaphragm so the ones you google will not necessarily apply to your pond water, but it is close enough to give you an idea of the equilibrium dance that is occuring.
So, after that nasty technical explanation and leaving out some other details, this partially explains how KH and pH are related. When KH changes, the equilibrium dance allows the pH to change. KH is simply a better control variable that applies to the low end of the pH range when wanting to lower the pH rather than using the pH test kits. When you are changing the pH, you want to look at the most accurate proactive control variables that are available.
pH tests tell you how the water is reacting to the stabilizer products. Stabilizer products such as calcium chloride, baking soda, calcium carbonate, etc. This is why you are being
reactive when testing pH and
proactive when testing for the KH or GH (calcium).
Although GH test kits also test for a presence of calcium, keep in mind GH tests are testing for many other divalent minerals, which are any mineral with two positive charges, that have zero impact on stabilizing pH and this same definition can only be loosely applied to KH. Divalent minerals are sodium (Na++), calcium (Ca++), iron (Fe++), magnesium (Mg++), manganese (Mn++), and many other minerals. GH test kits is not a direct calcium test kit. You can get a calcium test kit, which are used by coral reef keepers, but they are significantly more expensive.
You can document the GH test kit number to indicate whenever your calcium concentrations start to drop, but, if you are using Koi Clay or plant medium or other products in the water that add to the minerals, then the GH test kit is not a reliable way to indirectly test for calcium.
So, a cheaper route and more accurate route is to indirectly test for calcium by monitoring reactive control variables, that is the pH. When pH reaches 9.0 or higher, then this means your calcium concentrations is starting to become too low to stabilize the high end pH range. The calcium concentrations required is dependent on the pond's water chemistry and other contaminants present in the pond.
Alkalinity is simply any buffer element, including borate, phosphate, bicarbonate, and many other buffer combinations, that helps water resist a decrease in pH change contributed by an acid that releases free hydrogen cations (H+). KH tests this type of pH change tolerance, when decreased, in the water's alkalinity. KH test kit is
not a direct test for bicarbonates, such as baking soda, but there is zero practical test a hobbyist can do to test for the true bicarbonate concentration. KH is an acid titration plus indicator solution test. The reagant in the KH test kit is actually a weak acid, custom made by the manufacturer, with a set pH in the low 5s, around 5.0~5.4 pH. A solution is acidic due to the extra hydrogen cations (H+). Whenever an acid reacts with water, the extra hydrogen cations react with the alkalinity buffers, essentially "burning" away the alkalinity, that are present until the water's pH reaches the pH of the reagant solution. Bicarbonate is known to be present in the pH range of 5.0~8.5 and 8.3~8.5 is its baseline pH. So, when the KH test kit vial solution changes colors, then this indicates the pH of the vial solution is around lowish 5.0s, which means there is very little measureable bicarbonate present. This is why we are assuming the KH test kit is a test for bicarbonate (HCO3-). This is how the
API KH test kit functions. So, if it took 4 drops of reagent to merely just noticeably change colors in the vial, then this means all of the alkalinity has been "burnt" off and then we multiply 17.848 by 4 drops to get 71ppm or 71mg/L of alkalinity. There is a more precise definition for the term KH so to use KH in reference to alkalinity is not entirely correct, but it is just the common marketing nomenclature used nowadays since it is faster/shorter to type.
As far as I am aware, the only way to indirectly test for carbonate (CO32-) is to use a
HACH alkalinity reagant titration test kit using a phenolphthalein acid regeant, which has a pH of 8.3, and I am told this type of test is more prominent in coral reef aquariums, although not for sure why except maybe to test for the calcium hardness. When the vial's water solution reaches a 8.3 pH, then this means there is very little measureable carbonate present.
Carbonate (CO32-) has a strong electrochemical affinity to connect to Calcium (Ca++). So, when free soluble calcium is present, then carbonate and calcium precipitates by forming an insoluble product called calcium carbonate (CaCO3). As the water becomes more acidic, then the free hydrogen cations (H+) breaks this electrochemical bond of calcium carbonate (CaCO3) causing it to dissolve so to created bicarbonate (HCO3-) and free soluble calcium (Ca++), at different concentrations depending on the molar mass of the acid.
Not all compounds are instantly consumed. There will always be a presence of calcium, bicarbonate, carbonate, carbon dioxide, and carbonic acid present in the water. So, even though you might have 20 mg/L of free soluble Calcium in the water, this does not necessarily mean this is the amount that is needed to neutralize the present carbonate. This is only one reason why some ponds might require more calcium than other ponds.
There are many other equilibrias involved as well such as ammonia and phosphates, but this is the general jest of it.
It is all just basic pond water chemistry. It's not rocket science.
:cheerful: :claphands:
So, you kind of see how everything comes in full circle... that is if I did not mangle the explanation too much. I am relatively young to this as well, but I find the technical details relaxing and enjoyable. Give a yell if ya need any clarification or question.