A no-nonsense summary for aquarists
Article by Anthony Calfo
One of the most frustrating aspects of reef keeping for aquarists is undoubtedly water chemistry. Aquarists without a formal education in the sciences may find the challenge to understand the relationship between calcium and alkalinity in reef aquariums formidable. Adequate and consistent levels of calcium and alkalinity not only insure continued growth of invertebrates, but also are required for their very survival and sustenance in the shadow of system stability at large. Saltwater chemistry is indeed a complex matter and there are admittedly numerous factors that can influence the tide and turn of various equations in balance. Nevertheless, none are so significant or challenging that fundamentally good husbandry with regular partial water changes and basic supplementation won't allow you to run a simple and successful aquarium without resorting to rocket science, an abacus and a crystal ball! If you will indulge some generalizations about the dynamics of invertebrate growth (calcification and skeletogenesis), I can proffer a very simple explanation of the application of calcium and alkalinity that will spare you the need to earn a degree in chemistry just to keep a health reef aquarium.
The first thing that we need to recognize is that calcareous animals need adequate supplies of both calcium and alkalinity to grow. Corals, coralline algae, and shelled animals alike are comprised of more than just calcium...they are made of calcium carbonate. It is possible to also form skeletons with strontium and silica components, but most aquarists need only focus on the fact that skeletogenesis (skeletal growth) is essentially founded on the composition of both calcium and carbonate elements from the environment (water and/or food) by the process we call calcification.
Calcium is easily learned and applied by most aquarists (simple dosing and test kits), but alkalinity is rather less clear. Some folks mistake "Alkalinity as an expression of the pH scale" (in contrast to acidity). Alkalinity and pH, however, are distinctly different from each other, although their definitions and functions can be easily confused.
For those of you as uninformed about water chemistry as I was when I first entered the hobby, know that Alkalinity is a measure of water's ability to neutralize acids and resist change with a reserve of "hard" minerals (pool of dissolved buffers). One the contrary, pH is a measurement of the concentration of hydrogen ions in water in terms of acidity or alkalinity. So, the alkalinity of water in terms of pH merely refers to the basic end of a pH scale (alkaline) in contrast to the acidic end of the scale. It is a separate matter, however, from Alkalinity as a measure of water hardness.
There are several minerals that commonly contribute to the overall hardness of water, but calcium and magnesium are the primary elements. A higher measure of water hardness (Alkalinity) translates to a higher buffering ability, and subsequently a lower chance of a pH change in the system. Alkalinity can be measured as GH (total or General hardness) or KH (Carbonate hardness). I would recommend a carbonate hardness test kit as your primary measure of alkalinity.
It is easy to believe that water with "alkaline" or basic pH is likely to be high in alkalinity (buffering capacity). However, this is not always true. Water with a high pH but a low alkalinity, albeit uncommon, is possible and regarded as unstable. Aerated RO water (purified by reverse osmosis) or DI water (demineralized by de-ionization) is commonly in this category. Such unbuffered water will quickly decline in pH with the natural accumulation of organic acids in the aquarium. Reef aquarists that are surprised to see a falling or depressed pH in their systems despite high calcium levels may have neglected to measure and maintain alkalinity.
-The Guidelines
For most marine aquariums, calcium is recommended within a range of 350-450 ppm. Alkalinity is recommended with a range of 8 to 12. Reef aquarists with very large populations of stony corals or with fast growth as a priority, however, may entertain levels somewhat higher. These are special circumstances that indeed have benefits, limitations and inherent dangers and require specific address beyond the scope of this article as a primer. Casual aquarists instead can rest comfortably within the outlined ranges and enjoy healthy corals and good growth of calcifying organisms in display.
Ironically, within the recommended ranges of 350-450ppm Ca(calcium) and 8-12 dKH Alk(alkalinity it is not neccessary to maintain both parameters at the higher end concurrently. In fact it is not practical or easily attained in most systems. In gross terms, high calcium and high alkalinity are mutually exclusive. Alas, too many aquarists get caught up in the roller coaster applications of excessive amounts of supplements (randomly applied or not) and skew the balance of Ca and Alk in the system. Maintaining stable and consistent levels should not be difficult at all. To illuminate this paradox I offer you a simple analogy with marbles.
-The Marble Analogy
Fact; it is only possible to dissolve so many solids into a given volume of water (calcium, carbonates, and everything else). At the risk of oversimplifying the dynamic, imagine a bowl that holds one hundred marbles representing the total dissolved solids in seawater in a given system. If red marbles represented calcium, and blue marbles represented carbonates(alkalinity), the bowl can still only hold one hundred marbles no matter what mix of color they are. Now, if seventy marbles were the equivalent of 400-ppm calcium and the remaining marbles were blue, the only way to increase calcium would be to displace alkalinity (to remove blue marbles). In troubled systems, the misapplication of calcium supplements (dosing suddenly or to excess) is known to cause a sudden precipitation of carbonates (the alkalinity falls/crashes) that is commonly referred to as a "snowstorm". it is instigated by the influx of a large or rapid amount of calcium entering the system that spikes the pH immediately surrounding carbonate molecules and causes a crystalline precipitation (fallout). In keeping with our analogy, a "snowstorm" would be like taking another bowl of one hundred red marbles (calcium) and trying to pour it into the original bowl of mixed, colored marbles (balanced calcium and alkalinity). The result is the displacement of all blue marbles 9carbonate/alkalinity) and the overflow of excess red marbles beyond the one hundred marble limit. The ramifications of this is an aquarium is a crash in water chemistry and water quality that cannot be corrected while the chemical reaction occurs. Dosing more supplements to try to correct the imbalance (or even doing a concurrent water change with hopes of dilution) will only serve to feed the chain reaction. Tragically, the "snowstorm" must be allowed to finish and an aquarium system is traumatized in the process.
To safely avoid dangerous inbalances in the Ca-Alk dynamic, aquarists simply need to avoid pushing either component to an extreme end or both simultaneously high. Instead think of the relationship as a Hi-Lo situation within the safe ranges. Within the accepted ranges (350-450ppm Ca and 8-12 dKH Alk), one parameter can be pushed to a high end while the other is allowed to stay toward the middle or lower end. Any reasonably mix of the two will still provide more than enough of both elements for successful calcification. More importantly, consistent levels of both are far more supportive of growth in calcareous organisms than the inconsistent but high average of either component otherwise. Many aquarists enjoy phenomenal growth in their reef creatures with rather modest Ca and Alk levels. indeed, consistency with all aspects of aquatic husbandry is more conductive to success than random high points.
(CONT).
Article by Anthony Calfo
One of the most frustrating aspects of reef keeping for aquarists is undoubtedly water chemistry. Aquarists without a formal education in the sciences may find the challenge to understand the relationship between calcium and alkalinity in reef aquariums formidable. Adequate and consistent levels of calcium and alkalinity not only insure continued growth of invertebrates, but also are required for their very survival and sustenance in the shadow of system stability at large. Saltwater chemistry is indeed a complex matter and there are admittedly numerous factors that can influence the tide and turn of various equations in balance. Nevertheless, none are so significant or challenging that fundamentally good husbandry with regular partial water changes and basic supplementation won't allow you to run a simple and successful aquarium without resorting to rocket science, an abacus and a crystal ball! If you will indulge some generalizations about the dynamics of invertebrate growth (calcification and skeletogenesis), I can proffer a very simple explanation of the application of calcium and alkalinity that will spare you the need to earn a degree in chemistry just to keep a health reef aquarium.
The first thing that we need to recognize is that calcareous animals need adequate supplies of both calcium and alkalinity to grow. Corals, coralline algae, and shelled animals alike are comprised of more than just calcium...they are made of calcium carbonate. It is possible to also form skeletons with strontium and silica components, but most aquarists need only focus on the fact that skeletogenesis (skeletal growth) is essentially founded on the composition of both calcium and carbonate elements from the environment (water and/or food) by the process we call calcification.
Calcium is easily learned and applied by most aquarists (simple dosing and test kits), but alkalinity is rather less clear. Some folks mistake "Alkalinity as an expression of the pH scale" (in contrast to acidity). Alkalinity and pH, however, are distinctly different from each other, although their definitions and functions can be easily confused.
For those of you as uninformed about water chemistry as I was when I first entered the hobby, know that Alkalinity is a measure of water's ability to neutralize acids and resist change with a reserve of "hard" minerals (pool of dissolved buffers). One the contrary, pH is a measurement of the concentration of hydrogen ions in water in terms of acidity or alkalinity. So, the alkalinity of water in terms of pH merely refers to the basic end of a pH scale (alkaline) in contrast to the acidic end of the scale. It is a separate matter, however, from Alkalinity as a measure of water hardness.
There are several minerals that commonly contribute to the overall hardness of water, but calcium and magnesium are the primary elements. A higher measure of water hardness (Alkalinity) translates to a higher buffering ability, and subsequently a lower chance of a pH change in the system. Alkalinity can be measured as GH (total or General hardness) or KH (Carbonate hardness). I would recommend a carbonate hardness test kit as your primary measure of alkalinity.
It is easy to believe that water with "alkaline" or basic pH is likely to be high in alkalinity (buffering capacity). However, this is not always true. Water with a high pH but a low alkalinity, albeit uncommon, is possible and regarded as unstable. Aerated RO water (purified by reverse osmosis) or DI water (demineralized by de-ionization) is commonly in this category. Such unbuffered water will quickly decline in pH with the natural accumulation of organic acids in the aquarium. Reef aquarists that are surprised to see a falling or depressed pH in their systems despite high calcium levels may have neglected to measure and maintain alkalinity.
-The Guidelines
For most marine aquariums, calcium is recommended within a range of 350-450 ppm. Alkalinity is recommended with a range of 8 to 12. Reef aquarists with very large populations of stony corals or with fast growth as a priority, however, may entertain levels somewhat higher. These are special circumstances that indeed have benefits, limitations and inherent dangers and require specific address beyond the scope of this article as a primer. Casual aquarists instead can rest comfortably within the outlined ranges and enjoy healthy corals and good growth of calcifying organisms in display.
Ironically, within the recommended ranges of 350-450ppm Ca(calcium) and 8-12 dKH Alk(alkalinity it is not neccessary to maintain both parameters at the higher end concurrently. In fact it is not practical or easily attained in most systems. In gross terms, high calcium and high alkalinity are mutually exclusive. Alas, too many aquarists get caught up in the roller coaster applications of excessive amounts of supplements (randomly applied or not) and skew the balance of Ca and Alk in the system. Maintaining stable and consistent levels should not be difficult at all. To illuminate this paradox I offer you a simple analogy with marbles.
-The Marble Analogy
Fact; it is only possible to dissolve so many solids into a given volume of water (calcium, carbonates, and everything else). At the risk of oversimplifying the dynamic, imagine a bowl that holds one hundred marbles representing the total dissolved solids in seawater in a given system. If red marbles represented calcium, and blue marbles represented carbonates(alkalinity), the bowl can still only hold one hundred marbles no matter what mix of color they are. Now, if seventy marbles were the equivalent of 400-ppm calcium and the remaining marbles were blue, the only way to increase calcium would be to displace alkalinity (to remove blue marbles). In troubled systems, the misapplication of calcium supplements (dosing suddenly or to excess) is known to cause a sudden precipitation of carbonates (the alkalinity falls/crashes) that is commonly referred to as a "snowstorm". it is instigated by the influx of a large or rapid amount of calcium entering the system that spikes the pH immediately surrounding carbonate molecules and causes a crystalline precipitation (fallout). In keeping with our analogy, a "snowstorm" would be like taking another bowl of one hundred red marbles (calcium) and trying to pour it into the original bowl of mixed, colored marbles (balanced calcium and alkalinity). The result is the displacement of all blue marbles 9carbonate/alkalinity) and the overflow of excess red marbles beyond the one hundred marble limit. The ramifications of this is an aquarium is a crash in water chemistry and water quality that cannot be corrected while the chemical reaction occurs. Dosing more supplements to try to correct the imbalance (or even doing a concurrent water change with hopes of dilution) will only serve to feed the chain reaction. Tragically, the "snowstorm" must be allowed to finish and an aquarium system is traumatized in the process.
To safely avoid dangerous inbalances in the Ca-Alk dynamic, aquarists simply need to avoid pushing either component to an extreme end or both simultaneously high. Instead think of the relationship as a Hi-Lo situation within the safe ranges. Within the accepted ranges (350-450ppm Ca and 8-12 dKH Alk), one parameter can be pushed to a high end while the other is allowed to stay toward the middle or lower end. Any reasonably mix of the two will still provide more than enough of both elements for successful calcification. More importantly, consistent levels of both are far more supportive of growth in calcareous organisms than the inconsistent but high average of either component otherwise. Many aquarists enjoy phenomenal growth in their reef creatures with rather modest Ca and Alk levels. indeed, consistency with all aspects of aquatic husbandry is more conductive to success than random high points.
(CONT).