Water Chemistry
pH
pH defines how acidic or
alkaline the water is. pH come s from the
French word hydrogène, and means "hydrogen power". It equates to
the amount of hydrogen (H+) and hydroxide (OH-) ions are dissolved
in a solution. The more hydrogen ions there are, the more acidic
the water is and the lower the pH is. A solution that
has equal concentrations of hydroxide and hydrogen is termed neutral
with a pH value of 7. A higher concentration of hydroxide ions
would return a value above 7 or alkaline. A lower concentration
of hydrogen ions would return a value below 7 or acidic.
The pH scale is logarithmic, in other words, each step up or
down is 10 times that of the previous one. A pH of 6 is ten
times more acidic than a pH of 7. A pH of 5 is a 100 times
more acidic than 7 and so on.
Most freshwater fish live within a pH range of 5.5 to 7.5
(African cichlids 7.5 to 8.4).
Most Saltwater species are happy around 8.4 For saltwater
specimens there is less margin for error than in freshwater aquaria.
Keep Your marine aquarium buffered!
In ALL cases, it is the rapid fluctuation that is the most
dangerous!
In general. most aquaria will "slide" as ph is reduced by organic
decay. (water changes and vacuuming gravel are vital and
the simplest means to correct for this decrease.) Excess waste
product produces carbonic acid, which acidifies the water and lowers
the pH.
Since the scale is logarithmic, this range represents a variation
of over a 1000 times. Even an apparently small change in
pH can affect fish, causing stress or death.
There are also indirect consequences that can affect
fish. Changes in pH will affect the toxicity of many
dissolved compounds. For example, ammonia becomes more toxic as
pH increases. Also consider that medications are affected which
increases the possibility of overdosing in Lowered ph
conditions.
Nitrifying bacteria, essential in the conversion of ammonia
to nitrate also have a pH range preference, which is between 7.5
and 8.6.
Methods of altering the pH in your freshwater
aquarium:
lower pH (freshwater) · Use a commercial acid buffer ·
Filtering water over peat · Add bogwood to the tank · Inject
carbon dioxide CO2 · Water changes with softened water or RO
(Reverse Osmosis) water
to raise the pH · Aerate the water, driving off the carbon
dioxide (CO2) · Filter over coral or limestone · Add rocks
containing limestone to the tank or use a coral sand substrate ·
Use a commercial alkaline buffer
In Saltwater
· Water changes . Buffers
Remember: Any changes to pH should be
done gradually if possible!!!
Water that is poorly buffered (low kH or temporary hardness)
will be subject to higher pH fluctuations than well-buffered
water. As a general rule, hard water is usually alkaline
(above 7) and well buffered, whereas soft water (below 7)
is usually slightly acidic and poorly buffered. Permanent
hardness also has an affect on the pH therefore in order to
completely understand pH, we must also understand water
hardness.
Water hardness
Water accumulates many dissolved substances before it reaches our
taps. Hardness is a measurement of the concentration of
metal ions such as calcium, magnesium, iron, and zinc.
Most of these concentrations are acquired as rain water
passes over rocks. In most water it consist mainly of
calcium and magnesium salts, with trace amounts of other
metals.
There are two types of hardness that we need
to consider.
Permanent hardness and alkalinity
(kH).(often referred to as carbonate or temporary
hardness) The sum of both types of hardness is
called general hardness (gH)
Alkalinity or temporary (carbonate) hardness (kH) refers to the
hardness derived mainly from carbonate and bicarbonate ions and
directly reflects the buffering capacity of the water. It
can be precipitated and removed by boiling the water. This is
why lime-scale forms in kettles and shower heads.
Permanent hardness measures ions such
as nitrates, sulphates, and chlorides etc, and cannot be removed by
boiling. While there is a connection between water hardness and
buffering, hardness is a product of mainly calcium
and magnesium ions and buffering is produced by bicarbonate
and carbonate ions. As mentioned earlier, hard water is
usually well buffered and soft water is usually less buffered.
It is possible though, based on different water
compositions, to have hard water that is poorly buffered or
soft water that is well buffered. The way to establish the
makeup of your local water is by using a test kit and test
for both gH (general hardness) and kH (temporary
hardness).kH
Carbonate hardness or temporary
hardness. Measures the buffering capacity or the
ability to absorb and neutralize added acid without major changes to
pH. Think of buffering capacity as a big sponge, the
higher the buffering, the bigger the sponge. How much
buffering does your tank need? The higher the kH (the bigger
the sponge), the more resistant to pH changes your water
will be. A tank's kH should be high enough to prevent
large pH swings over time. If your kH is below roughly 4.5
OdH, you should pay special attention to your tank's
pH (e.g., testing periodically) until you get a feel for
how stable the pH is.
Buffering is both good and bad. On the good side,
the nitrogen cycle in our tanks produces nitric acid (nitrate).
If we don’t have buffering (kH), the pH will drop over
time. Sufficient buffering will keep the Ph
stable. On the bad side, hard water almost always has a
large buffering capacity and if the pH is to high for your
fish, this large buffering capacity will make it more
difficult to lower the pH.
Buffering is sometimes referred to as "alkalinity" but should not
be confused with "alkaline". Alkalinity refers to buffering
and alkaline refers to a solution that is base rather than acid
(pH).
Aquariums with a low kH will require more attention to water
changes to control the nitrate level reducing the tendency for
the pH to drop.
As with pH, there are ways to increase and decrease the buffering
capacity of your water.
Ways to increase kH:
· Adding commercially available products to increase buffering
capacity · Adding sodium bicarbonate (baking soda). One
teaspoon of baking soda added to 50 liters of water can raise the kH
of the water by approx 4 OdH without a major affect on
pH. · Adding an air stone to increase surface turbulence driving
off carbon dioxide (CO2)
Ways to lower kH
· Adding commercially available products to decrease the
buffering capacity. · Injecting carbon dioxide (CO2) · Use
reverse osmosis (RO) water. You can mix tap water with reverse
osmosis water to achieve the desired kH.
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 in order to increase its gH and kH.
gH
General hardness (GH) refers to the dissolved concentration
primarily of magnesium and calcium ions. Other ions can
contribute to water hardness but are usually insignificant and
difficult to measure. When fish are said to prefer
``soft'' or ``hard'' water, it is gH, not kH that is being referred
to. gH will not directly affect pH although "hard" water
is generally alkaline due to some interaction of gH and kH.
Incorrect gH will affect the transfer of nutrients and waste
products through cell membranes and can affect egg
fertility, proper functioning of internal organs such as kidneys and
growth. Within
reason, most fish and plants can successfully adapt to local gH
conditions, although breeding may be impaired.
Some test kits measure gH or general hardness in German
degrees hardness or OdH, which is equal to 17.9 mg/L. Since
mg/L is equal to ppm (parts per million) simply multiply the
degrees OdH times 17.9 if you prefer to work with ppm.
The following table will give an idea of how hard your
water may be after reading the test results.
General Hardness Table
0 to 4 dH 0 to 70
ppm
Very Soft 4 to 8 dH 70 to 140
ppm
Soft 8 to 12 dH 140 to 210
ppm Medium
Hard 12 to 18 dH 210 to 320
ppm Fairly Hard
18 to 30 dH 320 to 530 ppm
Hard
Higher
Very Hard
Ways to increase gH
Adding limestone to the aquarium (this will also increase kH
which in turn will increase pH) Adding calcium carbonate will
raise gH and kH
Ways to reduce gH
Adding peat moss to your filter Use commercially available
water softening pillows or a water softener Mixing tap water
with reverse osmosis (RO) water.
It is more difficult to change gH without affecting kH than it is
to change kH without affect gH as you can see.
Conclusions
While distinct, pH, kH and gH interact and affect each
other. If you change one parameter, be sure and
monitor the others to see the affect.
Make changes gradually.
When making changes it is usually best to do it in containers
outside the aquarium, then add the treated water to the
aquarium.
If you have a low kH, increase water changes accordingly and
monitor pH more frequently.
Understand that decorations such as driftwood, bogwood,
limestone, filtering with peat, etc. will affect the kH and pH of
the aquarium.
Saltwater
Salinity and Specific Gravity
As a general rule most saltwater systems are best kept at a
specific gravity 1.020 - 1.025 To discourage parasites - lower
specific gravity to 1.018
The preferred water for marine and reef tanks is RO/DI water, as
it is in a very pure form. The commercial salt mix contains all
the salts and minerals needed.
Salinity describes the content of
these dissolved salts and minerals in the water and is
measured in parts per thousand (ppt).
The easiest and most common instrument to measure the salt
concentration in aquaria is the hydrometer. A hydrometer is a
device that measures the density or specific gravity of a
liquid. The more salt in the water the more dense it
is.
It is important to understand that salinity and specific gravity
are related - but not the same. Salinity can be measured by (a)
boiling down a water sample, (b) measuring conductivity by
electronic means, and (c) other laboratory methods which are
either too complex or too expensive.
Specific gravity indicates density,
while salinity refers to the actual weight of the salt.
The hydrometer works on the principle that a solid body displaces
its own weight of the liquid in which it floats. The
hydrometer is calibrated at 60˚F (15.55˚C) in which distilled water
equals 1.000 as the initial point. The readings will rise with
increasing density of the water.
As the instrument is calibrated at a temperature of 60˚F
(15.55˚C), it requires that the water to be tested will also
have a temperature of 60˚F (15.55˚C) in order to get an accurate
reading.
Water will expand or contract if
temperatures vary; therefore the density fluctuates with temperature
as well. The chart below shows the actual density in relation to
the water temperature.
Actual Specific Gravity
Example:
A marine tank maintained at a temperature of 82˚F (27.77˚C) with
a hydrometer reading of 1.021 translates into an actual specific
gravity of 1.0237
Salinity in ppt
Example:
A marine tank maintained at 80 F and a specific gravity reading
of 1.022 has a salinity content of 31.8 ppt
Stability in specific gravity is an important factor. Any
fluctuation will trigger some effects.
Only freshwater will evaporate
from the tank leaving the salt and minerals
behind. Therefore only freshwater should be used to top off
the aquarium.
Further, the water level is also of importance, as more
freshwater evaporates the density of the remaining water
will increase, thus raising the salinity.
A new batch of salt mix is only required with water changes.
Measurements with the hydrometer should be taken below the
surface, avoiding air bubbles as not to influence the
reading.
The hydrometer should be rinsed with freshwater after use to
avoid any residues.
Ammonia - Nitite -
Nitrate
The Nitrogen
cycle
Here
the Nitrogen cycle is
explained
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