Today I was reading a paper entitled "Activation of biomass-derived charcoal with supercritical water" by a combined team of French and Spanish scientists about the treatment and (partial) gasification of Arawa stones, the pits of a very common Guyanese palm that is widely eaten in that part of South America. The pit accounts for 80% of the volume of the fruit.
The paper is Daniel Montané et al, and is found in Microporous and Mesoporous Materials 119 (2009) 53–59.
From the paper:
Awara is an edible fruit harvested from a widespread spiny palm tree of the Amazonian basin: Astrocaryum vulgare (Arecaceae), commonly named awara palm. The fruit is especially well known from Guyana. The seed is very big, occupying about 80% of the volume of the fruit itself. Viscous oil having recognized medicinal properties may be extracted from awara stones. In addition, fibers from the leaves are also used for manufacturing fishing nets, bags and hammocks in Peru and Brazilian Amazon. Because of the substantial amounts of awara stones produced by South America, giving added value to this material, like other tropical biomass, is meaningful.
One always has to be a little bit nervous when people start talking about how "useful" tropical biomass is, but no matter. The science is interesting.
The point of the paper was to examine the pore size growth in pyrolysis derived chars of the nuts with a view toward certain materials science applications but there was an interesting discussion of supercritical water - which is water above 373
oC, a temperature beyond which there is no distinction between the liquid and gas (steam) phases of the substance.
While they are well known in inorganic syntheses, pressure methods are seldom used in carbon science. Pressure, through different induced effects, allows the preparation of materials that can generally not be prepared in other ways <1>. Pressure increases both the reaction rate and the homogeneity of the resultant materials, and allows the stabilization of metastable phases. Among the various kinds of pressure methods, hydrothermal ones are those using hot and pressurized water (typically at least above 100C and 1 bar) <2>.
Supercritical water is very remarkable stuff, but what I found interesting - something on which I seldom have thought to reflect - is the change in the self-ionization constant of water, called pK
w which is, for those who haven't taken a chemistry course, a logarithmic term. (The 'p' function is the negative log
10 and accounts for the concept of pH.) The pK
w of normal water is 14, meaning that the pH of normal water is 7. By contrast at 25 bar and 600
oC the pK
w is 8.8 meaning that the pH of water under these conditons,
neutral water, is 4.4.
This accounts for the corrosive nature of supercritical water. (It's not so corrosive that it doesn't have practical application: Many coal fired power plants generate supercritical water for its energy efficiency value.)
Because the ionization is so high, water behaves in some ways as a
salt, a molten salt. From the paper:
...water molecules are more dissociated into H3O+ and OH- ions, thus with an increased trend to behave like a molten salt. Consequently, many reagents are at least partly soluble in such a medium, helping and even making possible a number of reactions that would require much higher temperatures. In a reciprocal way, synthesizing metastable structures is possible in pressurized water at moderate temperatures. Because of the aforementioned peculiarities of supercritical water, it is expected that such a medium has a different activating action towards carbon as compared with standard steam activation. So far, only a few studies were carried out on this subject (see <6> and references. therein). In the present work, a char from awara stone was chosen for conducting the corresponding comparative experiments.
Esoteric maybe, but cool all the same.