| Introduction
In the first two
articles in this series, I discussed some of the dissolved
components, mostly trace metals, found in the water from a
survey of 23 marine reef aquaria. I chose to examine these
elements for two reasons: first, many reef aquarists seem
very concerned, "obsessed" is not too strong a word,
about trace elements in their systems and, second, the concentrations
of these materials could be analyzed relatively inexpensively.
I have shown that the concentrations of many of these elements
in our reef tanks bear little similarity to what is found
in natural sea water (NSW). Additionally, I have shown that
many of these elements have distributions that are correlated
with one another. After comparing these data with the composition
of the artificial salt mixes as reported in the literature
(Atkinson and Bingman, 1999), it is apparent that some of
the odd, and relatively very high, concentrations are due
to the initial mixtures of the artificial sea water that we
use in our systems. Our systems are very dynamic, however,
and after a very short period bear only a passing similarity
to what is found in either natural or freshly mixed artificial
sea water.
That our systems are dynamic and ever changing
should come as no surprise to any reef aquarist. However,
the magnitude of some of these changes is quite impressive
and the speed with which the systems can accommodate change
is truly awesome. Most, if not all of these changes, are mediated
by the organisms in the reef aquaria, and probably the most
important groups of organisms in this regard are the bacteria
and algae found in the aquaria (Redfield, et al., 1963).
Under appropriate conditions, various bacterial and algal
species will have large populations in our systems, and they
have the capability for rapid metabolically induced changes
of the medium. In natural reefs, about 80 percent of the non-bacterial
biomass is algal (Odum and Odum, 1955). Coral reefs are, in
point of fact, algal reefs with a small animal component layered
over them like the thin frosting on a cheap cake. It is likely
in many of our aquarium systems that the algal component is
equivalently abundant; algae grow on the surfaces of virtually
everything in our tanks, as well as within the rocks, corals,
and sediments. When we set up our aquaria, we are actually
constructing algal culturing vessels of very good design.
Of course, all aquarists, myself included, then gripe loudly
and vociferously about the algae "taking over" our
tanks. Yeah, right... The rapidity of algal growth is amazing,
as demonstrated by the dinoflagellate or diatom blooms we
have had at one time or another.
For most aquarists, an unforeseen or unexpected
side effect of such rapid algal growth is a significant alteration
of the water chemistry; as some elements vanish from solution,
while the abundance of others is hardly changed. Of course,
some of the animals alter the water chemistry as well, but
probably most of the alteration comes from either algae or
bacteria. Such rapid alterations of water chemistry are characteristic
of these two groups in natural systems, and are not at all
characteristic of animals. Most animals use relatively little
in the way of dissolved materials, getting most of the chemicals
they need from their food. One rather peculiar animal, the
reef aquarist, however, does significantly alter the composition
of the fluid in reef aquaria. Aquarists can change the water
chemistry of their systems either actively or passively. In
the former case, they may add or remove materials from the
system. In the latter case, they may simply do nothing, and
in so doing, abet the changes occurring due to the actions
of the various organisms in the system.
Undoubtedly as well, there are many strictly
non-biological chemical reactions occurring in our systems,
but with few exceptions, such as the effects of lime water
or added buffers, these are likely of lesser magnitude and
importance than are the biologically mediated responses.
In an attempt to estimate some of the effects
that aquarists have on their systems, I asked the participants
of "The Tank Water Study" to provide me with a detailed
list of foods they used and their feeding schedule. I also
asked for data on water changes; both if they performed them,
and if so, how much water was changed at each instance and
how frequently these changes were accomplished. By examining
the composition of the foods that go into the aquarium, as
well as the frequency of water removal, I could, rather crudely,
estimate some of the factors influencing the composition of
the materials dissolved in the aquarium water.
Materials, Methods and the Resulting Machinations
The nutrient and
trace element composition of the foods was estimated by calculating
the mass of the food added and comparing the foods to compositions
of comparable foods in what I call "The Food and Additive
Study"(Shimek, 2001). To estimate the mass of food added
to the aquarium, I had to convert from a number of different
odd and wonderfully esoteric measurements into metric units
(Table 1). Most marine animal and plant tissue has a specific
gravity of close to one, and I assumed that one milliliter
of the foods derived from such tissue weighed one gram. This
will introduce some errors, as some foods are a bit denser.
These foods will be undervalued with regard to their contribution.
For some foods there were no available
comparable data, so I estimated their values by using a similar
food. For example, for an addition of mysids, I used brine
shrimp as a surrogate. Likewise, for most of the algae used
by the aquarists in the study, there were no data available.
I used the values for dried Nori (Porphyra spp.) as
a surrogate. This may over-represent the contribution of those
algae, as Nori is a very rich food source. A square inch of
whichever algae were used was estimated to be equivalent to
0.25 g of Nori.
|
Table
1. Measurements and conversions used to estimate
food volumes added.
|
|
Measurement
|
Used
in Calculations
|
Comments
|
|
1/8
teaspoon
|
0.65
ml
|
|
|
1/4
teaspoon
|
1.3
ml
|
|
|
1/2
teaspoon
|
2.5
ml
|
|
|
1
teaspoon
|
5
ml
|
|
|
3
teaspoons = 1 tablespoon
|
0.0148
≈ 15 ml
|
|
|
16
tablespoons = 1 cup
|
0.2365
|
|
|
4
cups = 1 quart =
|
0.9460
liter
|
|
|
1
Frozen food cube =
|
2.83
g
|
Ocean
Nutrition Formula Prime Reef has 70 cubes in the 7oz.
package, therefore each cube is 0.1 ounce; 1 ounce =
28.35 g.
|
|
1
Silverside = 1 to 5 ml
|
2.5
ml
|
Used
the average size (estimated from foods I use).
|
|
Algae
|
0.25
g/square inch
|
Algae
were valued as “Nori” equivalents.
|
|
Sporadic
use
|
0.1
normal value
|
|
|
Phytoplankton
|
0.05
times Tahitian blend
|
Live
or dead phytoplankton is significantly more dilute than
the cryopaste out of the tube which was what was analyzed
in The Food and Additive Study; so I estimated a dilution
factor of 20 times.
|
Every feeding regime
noted by each hobbyist was different, somewhat inconsistent,
and approximate. To be comparable, I needed to bring them
to the same standard, so I divided my estimate of the amount
of food added in one week by seven to give "Average Daily
Ration." This measure was used in all comparisons, even
though many aquarists did not feed on a daily basis. The data
from these calculations were tabulated and graphically compared
to the concentrations of the trace elements found in natural
sea water (Figures
1a - 1f).
To estimate the effect of the added foods
in the tank, I asked each participant to give their system's
size in gallons, and then to estimate the total volume of
the rockwork and the sand. I assumed that the rock and sand
totally displaced water. This is patently false, there is
pore water in any sediment bed and there is water inside of
the rock. The volume of this "internal" water is
difficult to measure and even harder to estimate. However,
in both of these cases, exchange with the main water volume
of the tank will be slow, and these areas may be considered
to be effectively isolated from immediate changes. In any
case, however, the amount of water in each system was probably
somewhat underestimated, maybe by a factor of as much as twenty
percent. Such a reduction has the effect of increasing the
calculated concentrations (Table 2).
|
Table
2. Volumes of the systems of the study.
|
|
|
System Volume
|
Proportional Volume
|
Water
Volume
|
|
Tank
|
Gallons
|
Liters
|
Rockwork
|
Sand Bed
|
Liters
|
|
AC
|
200
|
757
|
0.20
|
0.20
|
454
|
|
AH
|
360
|
1363
|
0.60
|
0.17
|
317
|
|
CC
|
160
|
606
|
0.20
|
0.20
|
363
|
|
DC
|
190
|
719
|
0.20
|
0.00
|
575
|
|
DL
|
225
|
852
|
0.20
|
0.25
|
468
|
|
EB
|
300
|
1136
|
0.20
|
0.20
|
681
|
|
GD
|
55
|
208
|
0.40
|
0.20
|
83
|
|
JD1
|
90
|
341
|
0.40
|
0.20
|
136
|
|
JD2
|
80
|
303
|
0.20
|
0.20
|
182
|
|
JP
|
100
|
379
|
0.20
|
0.20
|
227
|
|
MB
|
36
|
136
|
0.20
|
0.20
|
82
|
|
MM
|
130
|
492
|
0.20
|
0.16
|
315
|
|
RC1
|
200
|
757
|
0.60
|
0.13
|
204
|
|
RC2
|
215
|
814
|
0.60
|
0.05
|
285
|
|
RS
|
220
|
833
|
0.25
|
0.25
|
416
|
|
S1
|
45
|
170
|
0.20
|
0.16
|
109
|
|
S2
|
60
|
227
|
0.05
|
0.16
|
179
|
|
S3
|
55
|
208
|
0.05
|
0.30
|
135
|
|
SC
|
220
|
833
|
0.40
|
0.20
|
333
|
|
SM
|
127
|
481
|
0.40
|
0.20
|
192
|
|
SN
|
65
|
246
|
0.25
|
0.20
|
135
|
|
SS
|
95
|
360
|
0.30
|
0.17
|
191
|
|
WW
|
380
|
1438
|
0.33
|
0.13
|
784
|
|
Average
|
99.3
|
376.0
|
0.16
|
0.16
|
191
|
The composition
of the material fed was estimated by multiplying the components
of the average daily ration by data from "The Food and
Additive Study" (Shimek, 2001). In some cases, I was
able to use the data directly from that study, as some of
the participants indicated that they used foods that were
examined in that study. In other cases, I averaged the values
for a given component of food. For example, to estimate what
was in a "generic" flake food, I used the average
of the dried prepared foods examined in "The Food and
Additive Study" (Shimek, 2001). For each of the foods,
values for about 30 elemental concentrations were estimated.
These were summed over all the foods. This sum was "The
Average Daily Food Ration (Table 3).
For each aquarium, the proportion that
the average daily food ration contributed to a water volume
equivalent to that system was calculated relative to the same
NSW volume (Pilson, 1998) (Table 3). These data are rather
interesting. The average DAILY food ration contains enough
aluminum, if it were totally dissolved in the tank water,
to raise the aluminum concentration of an average tank from
zero to 1.572 times normal. It contains enough iron to raise
the concentration of iron in an average tank from nothing
to 35.141 times the level found in natural sea water. This
bears repeating: each day, each aquarist, added enough iron
to an average tank to raise the iron concentration to over
35 times the normal sea water concentration. And yet, the
tank water contains no detectable iron (Shimek, 2002a, 2002b).
|
Table
3. Average Daily Ration in grams, averaged over
all the tanks and the proportion of NSW concentrations
(Pilson, 1998) averaged over all aquaria that this
ration constitutes. Values = Arithmetic mean ± 1 Sample standard
deviation. Values
of 0.000 in the proportion column indicate that
total proportion was measurable, but less than 0.001.
|
|
A.
Element or Material
|
The Average Daily Ration Contains:
|
Total Daily Additions as a Proportion of
NSW Concentrations
|
|
Aluminum
|
0.000095
± 0.000074
|
1.572 ± 1.347
|
|
Antimony
|
0.000002
± 0.000002
|
0.075 ± 0.079
|
|
Arsenic
|
0.000006
± 0.000008
|
0.018 ± 0.025
|
|
Barium
|
0.000003
± 0.000003
|
0.001 ± 0.001
|
|
Beryllium
|
0.000000
± 0.000000
|
5.219 ± 6.080
|
|
Boron
|
0.000021
± 0.000043
|
0.000 ± 0.000
|
|
Cadmium
|
0.000001
± 0.000001
|
0.037 ± 0.044
|
|
Calcium
|
0.007601
± 0.009062
|
0.000 ± 0.000
|
|
Chromium
|
0.000002
± 0.000002
|
0.049 ± 0.048
|
|
Cobalt
|
0.000001
± 0.000001
|
3.245 ± 3.212
|
|
Copper
|
0.000031
± 0.000045
|
0.547 ± 0.761
|
|
Iodine
|
0.002881
± 0.002880
|
0.265 ± 0.247
|
|
Iron
|
0.000439
± 0.000631
|
35.141 ± 47.969
|
|
Lead
|
0.000002
± 0.000002
|
5.552 ± 5.936
|
|
Lithium
|
0.000001
± 0.000001
|
0.000 ± 0.000
|
|
Magnesium
|
0.001877
± 0.001502
|
0.000 ± 0.000
|
|
Manganese
|
0.000070
± 0.000087
|
11.260 ± 11.823
|
|
Mercury
|
0.000002
± 0.000002
|
26.966 ± 28.881
|
|
Molybdenum
|
0.000004
± 0.000013
|
0.002 ± 0.004
|
|
Nickel
|
0.000002
± 0.000001
|
0.015 ± 0.014
|
|
Phosphorus
|
0.008599
± 0.008582
|
0.564 ± 0.526
|
|
Potassium
|
0.009453
± 0.010747
|
0.000 ± 0.000
|
|
Silicon
|
0.000339
± 0.000277
|
0.001 ± 0.001
|
|
Silver
|
0.000002
± 0.000002
|
4.042 ± 4.277
|
|
Sodium
|
0.008058
± 0.007243
|
0.000 ± 0.000
|
|
Strontium
|
0.000060
± 0.000055
|
0.000 ± 0.000
|
|
Sulfur
|
0.007515
± 0.006823
|
0.000 ± 0.000
|
|
Thallium
|
0.000002
± 0.000002
|
0.936 ± 0.978
|
|
Tin
|
0.000004
± 0.000004
|
40.244 ± 38.782
|
|
Titanium
|
0.000003
± 0.000006
|
1.387 ± 2.059
|
|
Vanadium
|
0.000001
± 0.000001
|
0.004 ± 0.004
|
|
Yttrium
|
0.000000
± 0.000000
|
0.071 ± 0.104
|
|
Zinc
|
0.000208
± 0.000326
|
2.07 5 ± 2.343
|
|
B.
Conventional Nutrients (values in grams; except
for calories).
|
|
Moisture
|
11.64
± 12.13
|
|
|
Ash
|
0.31
± 0.32
|
| |