Like most of you probably, when I first got into this hobby, the chemistry all seemed a bit daunting. And for awhile I had some trouble keeping everything straight. I also had a lot of questions no one at the LFS felt like answering (apparently). Now that I'm oh so much older and wiser, I wanted to share my "cheat sheet" with you all... and include some answers to those questions I couldn't get at my LFS.
Broken down to basics, we're just talking about charged particles (ions) in water. The ones we care a lot about are H+(hydrogen), Na+(sodium), Ca2+(calcium), OH-(hydroxide ion), Cl-(chloride), CO3^2- (carbonate), HCO3^-1 (bicarbonate). The positively charged particles match up with negatively charged particles to make different chemicals. It might sound a little complicated, but don't over think it. It's kinda like putting magnetics together...
This chart shows how the different combinations of positive and negative ions give us our basic inorganic additives:
So where do these ions come from? Well, check it out...
1. What's the difference between pH and alkalinity?
pH is short for "power of Hydrogen." It's the concentration of H+ in a solution (aka acidity).
Alkalinity is a more complicated beast. In function, it's a buffer. Buffers inhibits sudden changes in pH over a certain range. The ability of the buffer to prevent sudden changes in pH is called a "buffer capacity." As we usually use the term in the hobby, alkalinity is the "buffer capacity" of our water. Bicarbonate and carbonate are the major contributors to alkalinity. They're not the only contributors, but in our tanks, they're by far the most important. (The contribution of borate is an interesting topic, but I don't want to give you all a headache. If you're curious, here's RHF great article on that: Boron in a Reef Tank (and its effect on pH buffering))
2. Is aragonite a good Ca/alkalinity suppliment?
No. The answer as to why is a bit complicated. But basically, there's already so much Ca and CO3 in the water already, that additional CaCO3 isn't going to dissolve unless you put it in more acidic conditions. This *can* happen in an aragonite sand bed. But if and when it does, it's not a good sign.
3. Why does calcium go down when alkalinity goes up and vice versa?
It's a complicated thing I could never hope to explain better than Mr. Farley has here: Calcium and Alkalinity Balance Issues
4. What do the alkalinity tests actually test for?
Most don't test for any one compound. Most of them are titration kits that give you an idea of buffer capacity by finding out how much acid it takes to break the buffer (the point at which the buffer can no longer inhibit the change in pH). For more info on all that: What is Alkalinity
5. Where do dissolved silicates come from?
Lots of places (like tap water)... but not from silica sand.
I hope this can be of some help to anyone starting out.
Broken down to basics, we're just talking about charged particles (ions) in water. The ones we care a lot about are H+(hydrogen), Na+(sodium), Ca2+(calcium), OH-(hydroxide ion), Cl-(chloride), CO3^2- (carbonate), HCO3^-1 (bicarbonate). The positively charged particles match up with negatively charged particles to make different chemicals. It might sound a little complicated, but don't over think it. It's kinda like putting magnetics together...
This chart shows how the different combinations of positive and negative ions give us our basic inorganic additives:
So where do these ions come from? Well, check it out...
1. What's the difference between pH and alkalinity?
pH is short for "power of Hydrogen." It's the concentration of H+ in a solution (aka acidity).
Alkalinity is a more complicated beast. In function, it's a buffer. Buffers inhibits sudden changes in pH over a certain range. The ability of the buffer to prevent sudden changes in pH is called a "buffer capacity." As we usually use the term in the hobby, alkalinity is the "buffer capacity" of our water. Bicarbonate and carbonate are the major contributors to alkalinity. They're not the only contributors, but in our tanks, they're by far the most important. (The contribution of borate is an interesting topic, but I don't want to give you all a headache. If you're curious, here's RHF great article on that: Boron in a Reef Tank (and its effect on pH buffering))
2. Is aragonite a good Ca/alkalinity suppliment?
No. The answer as to why is a bit complicated. But basically, there's already so much Ca and CO3 in the water already, that additional CaCO3 isn't going to dissolve unless you put it in more acidic conditions. This *can* happen in an aragonite sand bed. But if and when it does, it's not a good sign.
3. Why does calcium go down when alkalinity goes up and vice versa?
It's a complicated thing I could never hope to explain better than Mr. Farley has here: Calcium and Alkalinity Balance Issues
4. What do the alkalinity tests actually test for?
Most don't test for any one compound. Most of them are titration kits that give you an idea of buffer capacity by finding out how much acid it takes to break the buffer (the point at which the buffer can no longer inhibit the change in pH). For more info on all that: What is Alkalinity
5. Where do dissolved silicates come from?
Lots of places (like tap water)... but not from silica sand.
I hope this can be of some help to anyone starting out.
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