Henrik Schulz* and Anita Horn, Archäomertrie-Labor der HAWK ...
Henrik Schulz* and Anita Horn, Archäomertrie-Labor der HAWK ...
Henrik Schulz* and Anita Horn, Archäomertrie-Labor der HAWK ...
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Manuscript, H. Schulz <strong>and</strong> A. <strong>Horn</strong>, Hildesheim, henrik.schulz@archaeometrielabor.com 10<br />
H<br />
O<br />
H H<br />
H O<br />
H<br />
O<br />
H<br />
O<br />
H<br />
Figure 5 Two situations of adsorption of the uncharged imino form of the toluidine blue<br />
onto a wooden surface. Left side: Untreated wooden surface; unspecific<br />
adsorption by interaction with pre-adsorbed water molecules <strong>and</strong> re-reaction<br />
into the charged ammonium form. Right side: Plasma treated wooden surface;<br />
specific adsorption by hydrogen bonding between the alcoholic hydroxy<br />
groups onto the wooden surface <strong>and</strong> the imino form of the dye.<br />
We postulate a simple correlation between the metachromatic shift ∆λ = λ0 − λ1 (indices as<br />
given above) of the shorter absorption b<strong>and</strong> (around 600 nm) <strong>and</strong> the number ∆N of activated<br />
surface groups onto the plasma treated wooden surface. In this manner we connect the change<br />
in adsorption (energy) ∆π = π0,V − π1,V, the metachromatic shift ∆λ <strong>and</strong> the number of<br />
surface groups ∆N by means of the well-known PLANCK relation ∆E = h · ∆ν in which the<br />
quantum energy ∆E respects the energy which is necessary to orientate just one molecule of<br />
the dye that adsorbes at one activated surface group. ∆ν is the frequency shift, h is the<br />
PLANCK constant <strong>and</strong> c the velocity of light.<br />
Straight forward we can write:<br />
∆E ·∆N = ∆π (5)<br />
<strong>and</strong> recalculate the number ∆N as follows:<br />
⎛ 1 ⎞ ⎛ ∆π<br />
⎞<br />
∆N = ⎜<br />
⎟ ⎜ ⎟ λ 0 ⋅ λ 1<br />
⎝ hc<br />
⎠ ⎝ ∆λ<br />
⎠<br />
H<br />
(CH S<br />
3 ) 2N NH<br />
O<br />
C<br />
H 3<br />
H<br />
HN<br />
H<br />
H<br />
O<br />
O<br />
H<br />
O<br />
H<br />
H H<br />
650 pm<br />
N<br />
CH 3<br />
S N(CH 3 ) 2<br />
H<br />
O<br />
CH2 O<br />
O<br />
HO<br />
OH<br />
510 pm<br />
HO<br />
O<br />
CH 2 OH<br />
OH<br />
O<br />
OH<br />
O<br />
O HO<br />
O CH2 O H<br />
H<br />
CH2 O<br />
HO<br />
O<br />
OH<br />
O<br />
(6)<br />
OH<br />
CH2 O<br />
HO<br />
O