Bonebrake
03/01/2008, 10:27 PM
These are the values I used for my simulation:
Bromide concentration of natural seawater at 35 ppt: ~0.0674 g / L
Bromide in one kg (1000 g) of Dow calcium chloride: 7 g bromide / kg
In this simulation I chose a relatively high number for supplementation at 1000 grams per week and a 20% weekly water change which would contain 0.0674% bromide for 52 weeks in a 120 gallon system. This amount of calcium supplementation would be substantially higher than even the most demanding SPS and clam loaded tank.
The first column denotes how much bromide per liter would be in the water if there was no removal and the second column denotes the bromide concentration assuming the only source of removal is a 20% water change. (We do not yet have clear data how much bromide may become attached to protein and skimmed out or how much may be consumed by macroalgae and removed.)
0.0674
0.0828
0.0982
0.1136
0.129
0.1444
0.1598
0.1752
0.1906
0.206
0.2214
0.2368
0.2522
0.2676
0.283
0.2984
0.3138
0.3292
0.3446
0.36
0.3754
0.3908
0.4062
0.4216
0.437
0.4524
0.4678
0.4832
0.4986
0.514
0.5294
0.5448
0.5602
0.5756
0.591
0.6064
0.6218
0.6372
0.6526
0.668
0.6834
0.6988
0.7142
0.7296
0.745
0.7604
0.7758
0.7912
0.8066
0.822
0.8374
0.8528
-----
0.0674
0.07972
0.089576
0.0974608
0.10376864
0.108814912
0.11285193
0.116081544
0.118665235
0.120732188
0.12238575
0.1237086
0.12476688
0.125613504
0.126290803
0.126832643
0.127266114
0.127612891
0.127890313
0.12811225
0.1282898
0.12843184
0.128545472
0.128636378
0.128709102
0.128767282
0.128813825
0.12885106
0.128880848
0.128904679
0.128923743
0.128938994
0.128951195
0.128960956
0.128968765
0.128975012
0.12898001
0.128984008
0.128987206
0.128989765
0.128991812
0.12899345
0.12899476
0.128995808
0.128996646
0.128997317
0.128997854
0.128998283
0.128998626
0.128998901
0.128999121
0.128999297
This simulation shows that the concentration of bromide in water essentially doubles relatively quickly, but then stabilizes at approximately ~0.129%.
This calculation can apply to longer intervals for water changes such as every other week or every month, but then you have to stretch out the 1000 grams of supplementation of calcium chloride over two weeks or a month as well.
Therefore, if you would add 1000 grams every two weeks and then do a 20% water change every two weeks then the second column would still apply, likewise, 1000 grams used over a month and a 20% water change every month.
In my humble opinion, I have no data of course, I do not feel that even a doubling of the concentration of this anion in our reefs could have any negative impact. At a natural concentration of 0.0674% how can 0.129% be that bad? For comparison, in the human body our electrolytes are tightly regulated and have a short range of what is considered normal and when they get out of whack bad things happen, but even at this extremely high rate of supplementation and standard water change regimen there is only a slight change.
Bromide can probably be likened to many of the other trace elements in seawater, it is present, may be involved occasionally or accidentally in some reactions, but otherwise just spectates and doesn't make a fuss.
Bromide concentration of natural seawater at 35 ppt: ~0.0674 g / L
Bromide in one kg (1000 g) of Dow calcium chloride: 7 g bromide / kg
In this simulation I chose a relatively high number for supplementation at 1000 grams per week and a 20% weekly water change which would contain 0.0674% bromide for 52 weeks in a 120 gallon system. This amount of calcium supplementation would be substantially higher than even the most demanding SPS and clam loaded tank.
The first column denotes how much bromide per liter would be in the water if there was no removal and the second column denotes the bromide concentration assuming the only source of removal is a 20% water change. (We do not yet have clear data how much bromide may become attached to protein and skimmed out or how much may be consumed by macroalgae and removed.)
0.0674
0.0828
0.0982
0.1136
0.129
0.1444
0.1598
0.1752
0.1906
0.206
0.2214
0.2368
0.2522
0.2676
0.283
0.2984
0.3138
0.3292
0.3446
0.36
0.3754
0.3908
0.4062
0.4216
0.437
0.4524
0.4678
0.4832
0.4986
0.514
0.5294
0.5448
0.5602
0.5756
0.591
0.6064
0.6218
0.6372
0.6526
0.668
0.6834
0.6988
0.7142
0.7296
0.745
0.7604
0.7758
0.7912
0.8066
0.822
0.8374
0.8528
-----
0.0674
0.07972
0.089576
0.0974608
0.10376864
0.108814912
0.11285193
0.116081544
0.118665235
0.120732188
0.12238575
0.1237086
0.12476688
0.125613504
0.126290803
0.126832643
0.127266114
0.127612891
0.127890313
0.12811225
0.1282898
0.12843184
0.128545472
0.128636378
0.128709102
0.128767282
0.128813825
0.12885106
0.128880848
0.128904679
0.128923743
0.128938994
0.128951195
0.128960956
0.128968765
0.128975012
0.12898001
0.128984008
0.128987206
0.128989765
0.128991812
0.12899345
0.12899476
0.128995808
0.128996646
0.128997317
0.128997854
0.128998283
0.128998626
0.128998901
0.128999121
0.128999297
This simulation shows that the concentration of bromide in water essentially doubles relatively quickly, but then stabilizes at approximately ~0.129%.
This calculation can apply to longer intervals for water changes such as every other week or every month, but then you have to stretch out the 1000 grams of supplementation of calcium chloride over two weeks or a month as well.
Therefore, if you would add 1000 grams every two weeks and then do a 20% water change every two weeks then the second column would still apply, likewise, 1000 grams used over a month and a 20% water change every month.
In my humble opinion, I have no data of course, I do not feel that even a doubling of the concentration of this anion in our reefs could have any negative impact. At a natural concentration of 0.0674% how can 0.129% be that bad? For comparison, in the human body our electrolytes are tightly regulated and have a short range of what is considered normal and when they get out of whack bad things happen, but even at this extremely high rate of supplementation and standard water change regimen there is only a slight change.
Bromide can probably be likened to many of the other trace elements in seawater, it is present, may be involved occasionally or accidentally in some reactions, but otherwise just spectates and doesn't make a fuss.