Hello.

I have several chemistry questions about tea, water, and oxygen,
which are too technical for the rec.drink.tea group.

A common warning to tea drinkers is that over-boiling water in a
kettle will cause the water to lose its dissolved oxygen, resulting in
"flat-tasting" water that is unsuitable for brewing a decent cup of
tea.  Tea aficionados recommend that water for black tea be heated
just to the boiling point, and the water should then be immediately
removed and poured over the tea.  There is some controversy as to
whether "heated just to the boiling point" means the first bubbles are
appearing or the water has attained a full rolling boil.

The reasoning given for using boiling water for black tea is that the
high temperature increases the rate at which the "good-tasting"
chemicals in the tea diffuse into the water.  Steeping (soaking) the
tea in the water for too long will cause bitter "bad-tasting"
chemicals to dissolve into the water.  The goal then is to maximize
the diffusion of the good chemicals into the tea in the 3 to 5 minutes
before the delayed bad chemicals begin to diffuse.

For oolong and green teas, however, the temperature recommended is
"somewhat cooler than boiling" to prevent "cooking" of the more
fragile leaves.  When pressed, knowledgeable tea drinkers suggest
180-200F (82-93C) as the recommended range for steeping greens and
oolongs, with little explanation.  This is about the temperature that
water attains just after being poured into a room-temperature mug or
teapot.  As a result, for black tea one should warm the pot with
boiling water (and then discard this water) before pouring water into
the pot (or mug) over the tea leaves.

Pouring water over the tea is imagined as partially reoxygenating the
water, especially when the loose tea is used.  (Dunking teabags in
lukewarm water is considered sacrilege.)  Pouring the water over the
leaves is also expected to dislodge air bubbles that might otherwise
adhere to the leaves (thus lessening the surface area between leaf and
water, resulting in a reduced efficiency of the steeping).

In theory, some of the above seems reasonable to me, while other parts
sound less plausible or just likely to be ineffective.  In practice, I
(and many others) have found that following these recommendations
produce good cups of tea, and ignoring these recommendations produces
a poor or only passable drink.  As an engineer and tea lover, I want
to find a more objective way of evaluating how effective these
recommendations are.

Some questions I have are:
1) How does the concentration of dissolved oxygen change as water is
	raised from below room temperature (from the cold water tap)
	to boiling?
2) How does the concentration of dissolved oxygen change as water is
	poured over tea?
3) How does the concentration of dissolved oxygen change as the tea
	is left steeping?  (That is, as more acids and other chemicals
	leach into the water from the tea leaves and as the water slowly
	cools.)
4) What temperatures will be best for the steeping of various types of
	tea?  How important is temperature for making a good cup of tea?

I've speculated on these questions, but only have guesses as to their
answers.  I'm sure I could easily settle the matter if I had an oxygen
probe in my kitchen, but alas I don't, and I'm also interested in an
analytical approach.  One might also ask if it is really a lack of
oxygen (and not, say, a lack of nitrogen) that is responsible for
flat-tasting water.

For question #1, I've checked a CRC (72nd edition) for information on
the solubility of oxygen in water (pg 6-4).  I've plotted the equation
for solubility vs temperature, but the text states that the equation
applies only for temperatures between 273.15K (0C) and 348.15K (75C).
(See http://web.mit.edu/rjbarbal/Tea/oxygen.gif; the green graph is
the range for which the equation is valid.)  Does anyone here know
what happens above 75C?  It appears that most of the dissolved oxygen
will have been lost by the time the water reaches 75C, and that
boiling would cause little additional loss.

Kettles, however, are usually covered (with perhaps a small opening
for a whistling steam release).  Would this nearly fixed volume create
enough of a pressure change within the kettle to alter the solubility
of the oxygen?  Also, how would the change in the partial pressure of
oxygen (mostly trapped inside the kettle) affect the solubility?
Finally, once the kettle lid is removed for pouring the water into the
tea pot, how will the sudden change in pressure affect the solubility?
How fast can substantial changes in dissolved oxygen occur in these
processes?

For question #2, I have studied situations similiar to pouring water
over tea.  Water flowing over a weir will be reoxygenated (due to
entrainment of air bubbles into the stream), with the amount of air
added to the water dependent on many factors including the height of
the water drop, penetration depth of the stream, and amount of
splashing.  I cannot, without experimentation, design a model
appropriate for the scale of water poured into a teapot, but I suspect
the reoxygenation is not significant.  Does anyone have a different
idea about this?

For question #3, I'm really not sure how the addition of solutes would
affect oxygen solubility, or how effective the slow cooling would be
in changing oxygen content.  Can anyone offer advice on this?

For question #4, I'm really not sure how dependent the quality of tea
is on the temperature of the water.  The temperature would certainly
affect how various substances diffuse from the tea leaves into the
water, but so many chemicals are present in tea that evaluating all
the reactions is probably not feasible, and of course there is much
subjectiveness in evaluating how the tea tastes.  I think, however,
that it should be feasible to model how quickly some interesting
chemicals (caffeine, the pigments, bitter tannins) enter the water.
Can anyone provide some direction on this last point?

One reason I'm skeptical of the importance of temperature is that any
difference is subtle, if noticeable at all.  A tea steeped longer at a
cooler temperature tastes much like a tea steeped shorter at a higher
temperature.  In the extreme, iced tea that is made by steeping tea
overnight in a refrigerator tastes as good (to me and my fellow
tea-loving friends) as iced tea that is made from cooling hot tea that
has been prepared regularly.  Yet, heating the refrigerator-made tea
produces a drink which is far less palatable than fresh hot tea.  Why?

I'm also curious about the affect atmospheric pressure has on tea.
I've heard people state that one cannot brew tea as good in Denver as
in Boston, the reason being that in high-altitude Colorado the water
boils at a lower temperature and less oxygen is in the air.  I'm
usually quick to respond that weather maps often show sunny Colorado
with a higher pressure than rainy Massachusetts.  Having had tea in
both locations, I've not been noticed any discernible differences.

It's been a long time since I've studied chemistry, so any help or
advice on these questions and thoughts would be appreciated.  I also
apologize for the length of this post, but those of you who drink tea
can probably appreciate the complexity of the topic.

+ Richard
  <rjbarbal@mit.edu>
----------------------------------------------------------------------
I cannot answer any of your questions, but I can add another. (<:}
What effect does the changing concentration of CO2 have on the brewing
process?

Changes in the concentration of CO2 in the water changes the acidity
of the water, and changes in acidity can have profound effects on
chemical reactions and equilibria.