Beginner FAQ: Practical Water Chemistry
Water in nature is rarely pure in the ``distilled water'' sense; it
contains dissolved salts, buffers, nutrients, etc., with exact
concentrations dependent on local conditions. Fish (and plants) have
evolved over millions of years to the specific water conditions in
their native habitats and may be unable to survive in significantly
different environments.
Beginners (especially the lazy) should take the easy approach
of selecting fish whose needs match the qualities of their normal tap
water. Alternatively, an advanced (and energetic!) aquarist can
change the water characteristics to match the fish's needs, though
doing so is almost always more difficult than first appears. In
either case, you need to know enough about water chemistry to ensure
that the water in your tank has the right properties for the fish you
are keeping.
Water has four measurable properties that are commonly used
to characterize its chemistry. They are pH, buffering capacity, general
hardness and salinity. In addition, there are several
nutrients and trace elements.
pH refers to water being either an acid, base, or neither
(neutral). A pH of 7 is said to be neutral, a pH below 7 is ``acidic''
and a pH above 7 is ``basic'' or ``alkaline''. Like the Richter scale
used to measure earthquakes, the pH scale is logarithmic. A pH of 5.5
is 10 times more acidic than water at a pH of 6.5. Thus, changing the
pH by a small amount (suddenly) is more of a chemical change (and more
stressful to fish!) than might first appear.
To a fishkeeper, two aspects of pH are important. First, rapid changes
in pH are stressful to fish and should be avoided. Changing the pH by
more than .3 units per day is known to stress fish. Thus, you want
the pH of your tank to remain constant and stable over the long haul.
Second, fish have adapted to thrive in a (sometimes narrow) pH range.
You want to be sure that your tank's pH matches the specific
requirements of the fish you are keeping.
Most fish can adjust to a pH somewhat outside of their optimal
range. If your water's pH is naturally within the range of 6.5 to
7.5, you will be able to keep most species of fish without any
problems. If your pH lies within this range, there is probably no
need to adjust it upward or downward.
Buffering capacity refers to water's ability to keep the pH
stable as acids or bases are added. pH and buffering capacity are
intertwined with one another; although one might think that adding
equal volumes of an acid and neutral water would result in a pH
halfway in between, this rarely happens in practice. If the water has
sufficient buffering capacity, the buffering capacity can absorb and
neutralize the added acid without significantly changing the pH.
Conceptually, a buffer acts somewhat like a large sponge. As more
acid is added, the ``sponge'' absorbs the acid without changing the pH
much. The ``sponge's'' capacity is limited however; once the buffering
capacity is used up, the pH changes more rapidly as acids are added.
Buffering has both positive and negative consequences. On the plus
side, the nitrogen cycle produces nitric acid (nitrate). Without
buffering, your tank's pH would drop over time (a bad thing). With
sufficient buffering, the pH stays stable (a good thing). On the
negative side, hard tap water often almost always has a large
buffering capacity. If the pH of the water is too high for your fish,
the buffering capacity makes it difficult to lower the pH to a more
appropriate value. Naive attempts to change the pH of water usually
fail because buffering effects are ignored.
In freshwater aquariums, most of water's buffering capacity is due
to carbonates and bicarbonates. Thus, the terms ``carbonate hardness''
(KH), ``alkalinity'' and ``buffering capacity'' are used interchangeably.
Although technically not the same things, they are equivalent in
practice in the context of fishkeeping. Note: the term ``alkalinity''
should not be confused with the term ``alkaline''. Alkalinity refers to
buffering, while alkaline refers to a solution that is a base (i.e., pH
> 7).
How much buffering does your tank need? Most aquarium buffering
capacity test kits actually measure KH. The larger the KH, the more
resistant to pH changes your water will be. A tank's KH should be high
enough to prevent large pH swings in your tank over time. If your KH
is below roughly 4.5 dH, you should pay special attention to your
tank's pH (e.g, test weekly, until you get a feel for how stable the
pH is). This is ESPECIALLY important if you neglect to do frequent
partial water changes. In particular, the nitrogen cycle creates
a tendency for an established tank's pH to decrease over time. The
exact amount of pH change depends on the quantity and rate of nitrates
produced, as well as the KH. If your pH drops more than roughly two
tenths of a point over a month, you should consider increasing the KH
or performing partial water changes more frequently. KH doesn't
affect fish directly, so there is no need to match fish species to a
particular KH.
Note: it is not a good idea to use distilled water in your tank. By
definition, distilled water has essentially no KH. That means that
adding even a little bit of acid will change the pH significantly
(stressing fish). Because of its instability, distilled (or any
essentially pure water) is never used directly. Tap water or other
salts must first be added to it in order to increase its GH and KH.
General hardness (GH) refers to the dissolved concentration of
magnesium and calcium ions. When fish are said to prefer ``soft'' or
``hard'' water, it is GH (not KH) that is being referred to.
Note: GH, KH and pH form the Bermuda's Triangle of water
chemistry. Although the three properties are distinct, they all
interact with each other to varying degrees, making it difficult to
adjust one without impacting the other. That is one reason why
beginning aquarists are advised NOT to tamper with these parameters
unless absolutely necessary. As an example, ``hard'' water frequently
often comes from limestone aquifers. Limestone contains calcium
carbonate, which when dissolved in water increases both the GH (from
calcium) and KH (from carbonate) components. Increasing the KH
component also usually increases pH as well. Conceptually, the KH acts
as a ``sponge'' absorbing the acid present in the water, raising the
water's pH.
Water hardness follows the following guidelines. The unit dH means
``degree hardness'', while ppm means ``parts per million'', which is
roughly equivalent to mg/L in water. 1 unit dH equals 17.8 ppm CaCO3.
Most test kits give the hardness in units of CaCO3; this means the
hardness is equivalent to that much CaCO3 in water but does not mean
it actually came from CaCO3.
General Hardness
0 - 4 dH, 0 - 70 ppm : very soft
4 - 8 dH, 70 - 140 ppm : soft
8 - 12 dH, 140 - 210 ppm : medium hard
12 - 18 dH, 210 - 320 ppm : fairly hard
18 - 30 dH, 320 - 530 ppm : hard
higher : liquid rock (Lake Malawi and Los Angeles, CA)
Salinity refers to the total amount of dissolved substances.
Salinity measurements count both GH and KH components as well as such
other substances as sodium. Knowing water's salinity becomes important
in salt water aquariums. In freshwater tanks, knowing pH, GH and KH
suffices.
Salinity is usually expressed in terms of its specific gravity, the
ratio of a solution's weight to weight of an equal volume of distilled
water. Because water expands when heated (changing its density), a
common reference temperature of 59F degrees is used. Salinity is
measured with a hydrometer, which is calibrated for use at a specific
temperature (e.g., 75F degrees is common).
One component of salinity that neither GH or KH includes is sodium.
Some freshwater fish tolerate (or even prefer) a small amount of salt
(it stimulates slime coat growth). Moreover, parasites (e.g., ick) do
not tolerate salt at all. Thus, salt in concentrations of (up to) 1
tablespoon per 5 gallons can actually help prevent and cure ick and
other parasitic infections.
On the other hand, some species of fish do not tolerate ANY salt
well. Scaleless fish (in general) and some Corydoras catfish are far
more sensitive to salt than most freshwater fish. Add salt only if
you are certain that all of your tank's inhabitants prefer it or can
at least tolerate it.
In addition to GH, KH, pH and salinity, there are a few other
substances you may want to know about. Most tap water contains an
assortment of nutrients and
trace elements in very low concentrations. The presence
(or absence) of trace elements can be important in some situations,
specifically:
- nitrates, which are discussed in great length in this FAQ in conjunction
with the NITROGEN CYCLE;
- phosphates, the second most prominent nutrient.
Phosphates have been linked to algae growth. If you have persistent
algae problems, high phosphates may be a contributing factor. In a
plant tank, ideal phosphate levels are .2 mg/L or lower. To control
algae, frequent partial water changes are often recommended to reduce
nutrient levels. If your tap water contains excess phosphate, water
changes may be aggravating the situation. Your local water company
can tell you what the exact phosphate levels are.
- iron, manganese and other trace elements.
Plants need iron in trace quantities to grow. Tap water in many
areas contains no iron at all. Consult the
PLANT FAQ for more details.
The following measurements are approximate; use a test kit to verify
you've achieved the intended results. Note that if your water is
extremely soft to begin with (1 degree KH or less), you may get a
drastic change in pH as the buffer is added.
To raise both GH and KH simultaneously, add calcium carbonate
(CaCO3). 1/2 teaspoon per 100 liters of water will increase both the
KH and GH by about 1-2 dH. Alternatively, add some sea shells, coral,
limestone, marble chips, etc. to your filter.
To raise the KH without raising the GH, add sodium bicarbonate
(NaHCO3), commonly known as baking soda. 1/2 teaspoon per 100 Liters
raises the KH by about 1 dH. Sodium bicarbonate drives the pH towards
an equilibrium value of 8.2.
One can raise or lower pH by adding chemicals. Because of
buffering, however, the process is difficult to get right. Increasing
or decreasing the pH (in a stable way) actually involves changing the
KH. The most common approach is to add a buffer (in the previous
section) whose equilibrium
holds the pH at the desired value.
Muriatic (hydrochloric) acid can be used to reduce pH. Note that
the exact quantity needed depends on the water's buffering capacity.
In effect, you add enough acid to use up all the buffering capacity.
Once this has been done, decreasing the pH is easy. However, it should
be noted that the resultant lower-pH water has much less KH buffering
than it did before, making it more susceptible to pH swings when
(for instance)
nitrate levels rise. Warning: It goes without saying that acids are
VERY dangerous! Do not use this approach unless you know what
you are doing, and you should treat the water BEFORE adding it
to the aquarium.
Products such as ``pH-Down'' are often based on a phosphoric acid buffer.
Phosphoric acid tends to keep the pH at roughly 6.5, depending on
how much you use.
Unfortunately, use of phosphoric acid has the BIG side
effect of raising the phosphate level in your tank, stimulating algae
growth. It is difficult to control algae growth in a tank with
elevated phosphate levels.
The only advantage over hydrochloric acid is that pH will be somewhat
better buffered at its lower value.
One safe way to lower pH WITHOUT adjusting KH is to bubble
CO2 (carbon dioxide) through the tank. The CO2 dissolves in water, and
some of it forms carbonic acid. The formation of acid lowers the pH.
Of course, in order for this approach to be practical, a steady source
of CO2 bubbles (e.g. a CO2 tank) is needed to hold the pH in
place. As soon as the CO2 is gone, the pH bounces back to its previous
value. The high cost of a CO2 injection system precludes its use as a
pH lowering technique in most aquariums (though see the
PLANT FAQ for inexpensive do-it-yourself
alternatives). CO2 injection systems
are highly popular in heavily-planted tanks, because the additional CO2
stimulates plant growth.
Some fish (e.g., discus, cardinal tetras, etc.) prefer soft water.
Although they can survive in harder water, they are unlikely to
breed in it. Thus, you may feel compelled to soften your water despite the
hassle involved in doing so.
Typical home water softeners soften water using a technique known
as ``ion exchange''. That is, they remove calcium and magnesium ions by
replacing them with sodium ions. Although this does technically make
water softer, most fish won't notice the difference. That is, fish
that prefer soft water don't like sodium either, and for them such
water softeners don't help at all. Thus, home water softeners are not
an appropriate way to soften water for aquarium use.
Fish stores also market ``water softening pillows''. They use the
same ion-exchange principle. One ``recharges'' the pillow by soaking it
in a salt water solution, then places it in the tank where the sodium
ions are released into the water and replaced by calcium and magnesium
ions. After a few hours or days, the pillow (along with the calcium
and magnesium) are removed, and the pillow recharged. The pillows
sold in stores are too small to work well in practice, and shouldn't
be used for the same reason cited above.
Peat moss softens water and reduces its hardness (GH). The most
effective way to soften water via peat is to aerate water for 1-2
weeks in a bucket containing peat moss. For example, get a (plastic)
bucket of the appropriate size. Then, get a large quantity of peat
(a gallon or more), boil it (so that it sinks), stuff it in a pillow
case, and place it in the water bucket. Use an air pump to aerate
it. In 1-2 weeks, the water will be softer and more acidic. Use this
aged water when making partial water changes on your tank.
Peat can be bought at pet shops, but it is expensive. It is much
more cost-effective to buy it in bulk at a local gardening shop. Read
labels carefully! You don't want to use peat containing fertilizers or
other additives.
Although some folks place peat in the filters of their tanks, the
technique has a number of drawbacks. First, peat clogs easily, so
adding peat isn't always effective. Second, peat can be messy and may
cloud the water in your tank. Third, the exact quantity of peat
needed to effectively soften your water is difficult to estimate.
Using the wrong amount results in the wrong water chemistry. Finally,
when doing water changes, your tank's chemistry changes when new water
is added (it has the wrong properties). Over the next few days, the
chemistry changes as the peat takes effect. Using aged water helps
ensure that the chemistry of your tank doesn't fluctuate while doing
water changes.
Hard water can also be softened by diluting it with distilled water
or R/O water. R/O (reverse-osmosis) water is purified water made by a
R/O unit. Unfortunately, R/O units are too expensive ($100-$500) for
most hobbyists. R/O water can also be purchased at some fish stores,
but for most folks the expense and hassle are not worth it. The same
applies to distilled water purchased at grocery stores.
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