| |
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 chemistry just to
keep a healthy 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 a measure of the buffering
ability of seawater” (expressed in degrees of hardness) with
“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). On 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.
For most marine aquariums, calcium is recommended
within a range of 350-450ppm. Alkalinity is recommended with a range
of 8 to 12 dKH. 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
and 450 ppm Ca (calcium) and 8-12 dKH Alk (alkalinity) it is not
necessary 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 application
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.
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 (carbonates/alkalinity)
and the overflow of excess red marbles beyond the one hundred marble
limit. The ramifications of this in 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 imbalances 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 (350-450 ppm Ca and 8-12 dKH Alk), one parameter
can be pushed to a high end while the other is allowed to stray
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
conducive to success than random high points.
My ultimate advice for aquarists regarding supplementation
here is to use kalkwasser (calcium hydroxide) in combination with
a deep sand bed (fine aragonite) and/or a calcium reactor. These
combinations are time-tested (20 years) and reliable with the most
benefits and least trouble when properly applied.
There are many calcium and alkalinity boosting
products on the market but most are easily abused with little explanation
or support from the labeling, instruction or even popular literature
in the hobby. The following is a brief summary of the merits and
demerits of each categorically:
(Calcium
hydroxide: AKA “Kalkwasser”): In summation, one of the
absolute best supplements to dose calcium in aquaria with a long
list of benefits and few disadvantages. Easy to use, but easy to
abuse. Follow dosing protocol strictly.
| Advantage: |
A potent and direct method of providing calcium |
| |
Caustic nature increases pH and indirectly supports Alkalinity
by tempering acids that would otherwise burden the buffer pool |
| |
Is self-purifying by virtue of its highly caustic nature.
Most impurities commonly found in the raw reagent precipitate
out. Aids the neutralizing precipitation of nuisance phosphate
in aquaria. This is a tremendous advantage over all other methods
of dosing. |
| |
Improves skimmer performance (saponification). |
| |
Dosing at night tempers pH swings from inevitable drop from
respiration by photosynthetic dynamics. |
| |
No negative, residual by-product of its use (like accumulating
Chloride ions with “Liquid calcium” products) |
| |
A long-term calcium supplement |
| Disadvantage: |
High pH limits supplementation to dosing at night or in increments
that will not raise pH suddenly by more than .2 |
| |
Dosing by the commonly recommended supersaturated solutions
is tedious and messy (instead, see “Slurry method”
in the Book of Coral Propagation, Volume 1 for a tidy and succinct
dosing method). |
| |
Can be dangerous or stressful to system if misapplied. |
(Calcium Chloride):
Perhaps the most commonly used and abused methods for dosing calcium.
Not recommended for long-term use.
| Advantage: |
A potent and fast method for dosing Calcium without any impact
on pH. |
| |
Clean, easy and brief application. |
| |
Very safe and not easily overdosed in the short-term. |
| Disadvantage: |
Potentially dangerous accumulation of by-product Chloride
ions can skew water chemistry and plague Ca/Alk balance with
long-term use (1-2 years). |
| |
Requires aquarist to conduct more frequent and larger water
changes on the system to dilute and delay Chloride ion accumulation. |
| |
No ancillary benefits like Calcium hydroxide (support of pH,
Alk, skimmer, etc.) |
| |
A temporary calcium supplement only to be used for “quick
fixes” of strayed Ca. |
(Aragonite sand): Be
sure to purchase media comprised of aragonite (oolitic) material
and not calcite. Both calcite and aragonite are forms of calcium
carbonate, but only aragonite will dissolve easily at the necessarily
high pH of a healthy marine system. Grain size should be sugar fine
at 10 cm or more depth. Courser grains require even greater sand
bed depth and stronger water flow to succeed.
| Advantage: |
A very natural, significant and passive way of supporting
both Calcium and Alkalinity through the dissolution of aragonite
in balanced quantity. |
| |
Long list of natural and organic benefits to elaborate for
the scope of this summary. Distinguished by natural nitrate
reduction with deep enough media (over 10cm), natural plankton
encouraged and cultured in situ, reflects light back up to corals
and plants thereby reducing or preventing bleaching undersides
in captivity, etc. |
| |
Very safe and not easily corrupted without gross negligence
or misapplication of standard aquatic husbandry. |
| |
In some systems it can singly support Ca and Alk without any
other supplements. |
| Disadvantage: |
Somewhat uncontrolled/unpredictable. Requires monitoring and
supplementation. |
| |
Falls prey easily to misapplication by ill-advised or misinformed
aquarists. Lack of adequate water flow in the display or installation
at an improper depth (less than 7 cm) can contribute to nutrient
accumulation (AKA: “Nutrient sink”) and algae. |
After a long time,
calcium rectors are finally gaining due recognition for their great
worth and validity as a pivotal component in an optimal marine aquarium
system.
| Advantage: |
A very potent method for dosing and maintaining Calcium and
Alkalinity with superb consistency and reliability. The “ultimate”
strategy for many aquarists. |
| |
Low-maintenance in service, inexpensive operating cost, ideal
once properly tuned. |
| |
In some systems it can singly support Ca and Alk without any
other supplements. |
| Disadvantage: |
Expensive and initially complicated hardware to install and
tune. |
| |
Performance is influenced by the quality and dissolution of
reactor media. |
| |
Impure media is not self-purifying (like Calcium hydroxide)
by the process/application and can impart contaminants into
the system. |
| |
Gross misapplication can be dangerous or stressful to the
system. |
a popular
compromise for aquarists that find Calcium hydroxide (“kalkwasser”)
too tedious, but cannot afford a calcium reactor. A reasonably good
supplement with regular water changes and water quality.
| Advantage: |
Very clean, easy and reliable to dose if application is followed
strictly. Provides elements of calcium and alkalinity in balance.
|
| Disadvantage: |
Very strict application protocol. Must be shaken/mixed vigorously
before every application as the components of the clear supplement
stratify and separate (the product does not stay uniformly mixed
in bottle)! Neglect otherwise can severely corrupt Ca/Alk balance
and make a problem system even worse. |
| |
Requires that a system be in balance BEFORE supplementation
begins. Large water changes are necessary on problem systems
(to restore balance) before two-part supplements can carry on
the job of metering Ca and Alk. |
| |
Categorically it is the most expensive long-term supplement
of Ca and Alk |
The
common culinary ingredient, sodium bicarbonate, is an often used
and abused method of increasing the pH/alkalinity of an aquarium
system. Unsupported, however, it is only temporarily effective and
it is easily misapplied (spiking and stressing the system). Although
it is the single largest component in commercial “seabuffers”,
it is not recommended for casual aquarists as a sole supplement
when the safer and more effective options outlined above are available.
(“Seabuffers”):
Although not a reliable source of calcium, commercial “seabuffers”
are traditional vehicles for dosing and supporting adequate pH and
alkalinity in the aquarium. Different brands have variations in
their recipes, but most are fundamentally comprised of bicarbonate,
carbonate and a little borate. Some embellished supplements may
include calcium oxide, magnesium sulfate and other desirable ingredients.
Categorically, they not unreasonably expensive to dose long term
and they are fairly reliable. Aquarists using such supplements,
however, will need to measure water quality as much or more than
any strategy of supplementation. Calcium hydroxide (“kalkwasser”)
employed with a deep sand bed or a calcium reactor can often eliminate
the need for the use of seabuffers. They are an effective, but tedious
and time-consuming way to supplement pH/Alk.
(Calcium
gluconate): This calcium supplement is an exception to the above
warnings about the dangers of “Liquid calcium” products.
Sugar-based calcium is an essentially safe source of calcium, but
has not clearly demonstrated its efficacy for coral growth. It has,
however, been shown to greatly accelerate the growth of desirable
coralline algae species. As such, it is recommended as a supplement
to a primary method for dosing calcium.
In summary, and for the benefit of distracted speed-readers,
maintain Calcium at levels between 350 and 450 ppm Ca, and alkalinity
between 8-12 dKH without ever resting both concurrently at the highest
end of their range. Calcium hydroxide (“kalkwasser”)
dosed properly in concert with a deep sand bed (10cm + sugar fine
aragonite) or a calcium reactor will yield the most benefits when
supplementing Calcium and Alkalinity. Leading you to the next open
door for advanced reef chemistry, I also recommend keeping magnesium
levels at approximately 3 times the Calcium level (~1200 ppm Mg).
For those not inclined to complicate their hobby with advanced studies
of the dynamics of seawater, rest assured that regular partial water
changes will serve your system well to dilute and refresh water
quality.
In shared admiration of the sea… Anthony
Calfo.
About the author:
Anthony Calfo is a life-time aquarist and hobby author, having published
books and numerous articles on aquatic science and aquariology. He has
presented lectures and workshops to organizations and events for more
than a decade and can be reached daily for comment and questions on message
boards around the world. For books or more information, you can find him
at http://www.marinedepot.com/FORUMS/
|
|