O que realmente acontece quando adicionamos CO2 a um aqua?


gmmartins

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Viva,

 

Encontrei um post muito interessante que nos remete para a parte química da questão. Quem não quiser perder tempo nesta parte, basta ler os resumos que sumarizam as conclusões.

 

Espero que abra os olhos de muita gente que tem terror de injectar CO2...

 

O post está em inglês :( Estive para traduzir mas ainda é para o grandito. Quem tiver dificuldades pode usar o google translate ou então perguntar aqui o que não percebeu e eu tenho traduzir essa parte.

 

O post foi publicado um químico profissional. Melhor é impossível!

 

"So, here we go...

 

When we add CO2 into water, the kH value will technically increase (albeit by a vanishingly small amount);there is no possible mechanism for it to decrease. The pH will drop and the TA (total alkalinity) and gH will necessarily remain unchanged.

 

For example, let's take a litre of pure water (pH = 7; kH = gH = TA = 0)

 

if we add CO2 (g) to a level such that we have 15ppm dissolved CO2:

 

concentration CO2 = [CO2] = 0.015 g/L = 0.015/44 = 3.4 x 10^-4 M

 

Based on the various equilibrium constants (pKa values) for CO2, carbonic acid and bicarbonate:

 

approx 10% of these dissolved CO2 molecules will react with a water molecule to generate a molecule of carbonic acid

 

approx 99% of this H2CO3 will dissociate into H+ & HCO3- ions

 

virtually none of the HCO3-- ions will dissociate into H+ & CO3-- ions

 

in numerical terms:

 

when [CO2] = 3.4 x 10^-4 M; [H2CO3] = 5.7 x 10^-7 M; [HCO3-] = [H+] = 1.2 x 10^-5 M; [CO3--] = 5.6 x 10^-11 M

 

 

So, what effect has this had on pH, kH, gH & Total Alkalinity?

 

We've generated 1.2 x 10^-5 M of protons (H+ ions) so the pH is now:

 

-log 1.2 x 10^-5 = pH 4.9 (we can ignore the negligible number of protons generated from CO3-- formation)

 

We've generated the same number (concentration) of HCO3- ions and these are the only species that contribute to kH (we can once again ignore the CO3-- since it is negligible in comparison).

 

If [HCO3-] = 1.2 x 10^-5 M then the corresponding [CaCO3] hardness (for kH calculation) is:

 

half x 1.2 x 10^-5 = 6.0 x 10^-6 M

 

this equates to an increase of 0.6 ppm or 0.03 kH

 

So, you'd need the best test-kit in the universe to detect the increase in kH... and even then you wouldn't detect a change because kH test-kits actually measure total alkalinity (TA); this has been excellently covered in the sticky-post at the top of this forum board.

 

We can see from the sums above that the various ions we have generated all contribute to total alkalinity (TA), but overall:

 

[HCO3-] + [CO3--] - [H+] = 0

 

and, hence, the TA is necessarily unchanged.

 

 

 

 

Similarly, we haven't added any divalent cations (we've only added a gas to the system), gH is also necessarily unchanged.

 

 

 

So, hopefully you agree with the above? But obviously, our aquaria aren't filled with pure water, so, what difference does all the dissolved sulfate, bisulfate, phosphate, chloride, magnesium, calcium, & potassium make to the calculations above?

 

The answer is: very little.

 

The pH value we calculated above of 4.9 is unlikely to be reached when we add CO2 to our water because the various dissolved anions will have a buffering effect and a lot of the protons generated will be "mopped-up" and the pH reached will typically be more in the region of 6-6.5.

 

What about the kH? It doesn't matter what's dissolved in your aquarium water, the kH will remain essentially unchanged. This is because the only species we're adding that is capable of removing bicarbonate or carbonate is carbonic acid and for every molecule of HCO3- or CO3-- we remove we generate another molecule of HCO3-... and the kH value is restored (in practice it is raised very slightly).

 

And the TA (Total Alklalinity)? Again, we may remove some borate or phosphate ions via the generation of carbonic acid but these are all replaced in stoichiometric fashion with bicarbonate and the TA remains unchanged, although the composition (speciation) may change.

 

The gH is similarly unchanged since (as we stated earlier) we're not adding any divalent cations...

 

 

 

 

In the way of final comments, I would argue that kH and gH are essentially defunct and archaic measurements.

 

The former (kH) is used to express the buffering ability of the aquarium water except it doesn't! You could buffer an aquarium with borate or phosphate and it would be very resistant to pH change but would have a kH of zero. Total alkalinity is a much more sensible measurement... and this is what your kH test kits measure anyway.

 

The latter (gH) is used to express 'hardness' or the total amount of dissolved ionic media... except it only measures divalent cations. Saturated brine solution (aqueous NaCl) has a gH of zero but your freshwater fish certainly won't like it...

 

So, maybe you don't agree with some of the statements I've made or maybe I've made some mistakes; either way I'd be interested to discuss further or listen to alternative suggestions...

 

 

PS- All of the background info is readily availble... Wikipedia is probably the best source if you want something remotely readable. If you look at the articles on Carbonic Acid, Carbonate Hardness, Alkalinity, pKa & Acidity, Water Hardness you'll find pretty much everything you need..."

 

Por: GPHowell

Fonte: http://ukaps.org/for...hp?f=51&t=17744

 

abraço,

 

GM

Gustavo Martins

 

My nano Litopótamus

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Gustavo,

 

Como sempre grandes artigos e informativos :)

 

Eu ainda não como vou medir os parametros da minha agua e ver as compatibilidades entre as faunas, essa era a ajuda que eu gostava de ter.

 

Se os testes the pH, kH e gH não são importantes que parametros e que tipo de compatibilidade devemos procurar.

 

Ou seja se os escalares se dão bem em pH de 6.5 como vamos saber se a nossa agua esta ou não correcta, espero me ter feito compreender :)

 

Pedro Gil

A sair para a poça da Dona Beja :)

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Viva,

 

Epá só agora reparei que tinhas mandado mp...

 

Basicamente o que tens que te preocupar em termos de fauna é com a quantidade de sais (TDS). Testes para TDS comerciais não existem (tens que ir para o laboratório). O que mais se aproxima é o gH. O kH apenas nos diz a capacidade tampão de carbonatos (há outros). Portanto, mede o gH e logo vez se tens

água mole ou dura e fazes as tuas opções de acordo com isso. Se tiveres água muito dura e quiseres escalares e assim podes usar osmose inversa (mas dá uma trabalheira). se quiseres ciclideos africanos mas tiveres água mole, é só pores rochas calcáreas etc lá para dentro.

 

A maior parte dos peixes, se não estiveres a pensar em reprodução, aguenta alguma variação na quantidade de sais desde que as alterações não sejam feitas à pressa. Eles adaptam-se na sua grande maioria.

 

Abraço,

 

GM

Gustavo Martins

 

My nano Litopótamus

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Não faz mal... se quiser o copo ainda vou estar até sábado :)

 

já vi o outro artigo que está nos primeiros passos, muito interessante toda esta informação...

 

Já agora o meu pH é de 7.2 GH 4 e KH 5

 

Pedro

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