1.3.- Data analysis
 
Data analysis is performed on photoacoustic waveforms by comparing the signals obtained for a sample and a reference compound under the same experimental conditions (temperature, solvent, shape of the beam,...).  It is therefore mandatory to leave the laser beam-transducer-cuvette arrangement untouched between sample and reference compounds.
 

Data preprocessing

For evaluation purposes, both for the method of amplitudes and the deconvolution, it is convenient to perform a preprocessing of the experimental data.

Baseline subtraction
Photoacoustic signals are generally small, especially when working with aqueous solutions at low temperatures (below 10 °C).  This requires high gain amplification (normally x100) and it is common to have small offset in the waveforms, resulting either from the amplifiers or from offsetting the trace on the scope in order to achieve maximum vertical resolution.  It is therefore practical to acquire, for each waveform (under the same experimental conditions for both sample and reference compounds), a baseline signal, obtained with no light on the cuvette (by blocking the beam).  This baseline is then subtracted and the offsets (common to, say, the reference signal and its baseline) cancel out.  In this way the photoacoustic waveforms are net signals oscillating around zero (the picture shows energy, absorbance and amplitude normalized data).  Moreover, systematic noise as the noise coming from the laser firing is canceled out in the net waveform.  In practice, however, small offest may survive this procedure, and become important when working with the smallest signals.  A background correction routine may be of help in the data analysis (vide infra).
Signal normalization
 
For several reasons, it is convenient to perform a normalization of the measured signals vs the laser pulse energy E and the absorbance of the solution A. For instance this is extermely convenient when performing deconvolution of experimental waveforms.  However, plots of the measured amplitude Hs vs E or 1-10-A are traditionally used to improve the data analysis when working with the method of amplitudes.
 

Absorbance normalization
In the absence of saturation and in case the interactions between the absorbing chromophore and solutes do not affect the absorbance of the chromophore itself, the measured signal of the solution is proportional to 1-10-A, A being the absorbance of the solution at the excitation wavelength. This relationship is valid only for dilute solutions (A < 1), typical values for the absorbance of the solutions used in photoacoustics experiments range between 0.1 and 0.4. It is important to note that the signal is not directly proportional to A (i.e. to the concentration of the chromophore). After baseline subtraction, the measured signal can be made independent of the absorbance of the solution by dividing the signal by 1-10-A.  Lower absorbances lead to lower S/N ratios, but the extent of the absorbance normalized signal should be essentially unaffected by changing A.  This is only partly true for the shape of the signal, which, due to a small change in the signal generation geometry with A, is essentially unaffected only for variations in A within about 30%.  It is a safe procedure to keep the difference between reference and sample absorbances within 20% of each other. Failure to find independence on A of normalized signals indicates lack of fulfillment of some of the above mentioned conditions.

Pulse energy normalization
The measured signal, after baseline subtraction, is proportional to the energy E of the laser pulses.
In the absence of saturation (e.g. photoequilibria) and non linear phenomena (as, e.g., biphotonic effects) the signal is directly proportional to E. Dividing this signal by E, leads to an energy independent signal.  Typical values of E used in photoacoustics range between 1 and 200 mJ.  Again, failure to find independence on E of the normalized signals indicates the presence of some nonlinear effects that must be taken into account.

Normalization to the maximum of reference signal
Photoacoustic signals are relative values, dependent on several parameters of the experimental system.  Values can be made independent of the detection setup, by scaling waveforms by a factor equal to the amplitude of the reference waveform.  In this way the amplitude of a reference waveform is always 1, and the sample waveform is expressed as a fraction of the amplitude of the reference waveform.  This normalization is not strictly necessary, since the data analysis is performed by comparison of the sample to the corresponding reference and, therefore, scaling factors cancel out.
However, it is very convenient to scale waveforms to the same values (reference are always scaled to 1) because this gives a better feeling of the goodness of the fitting in the deconvolution analysis, as judged by the sum of the residuals (vide infra).

 

Retrieval of thermodynamic and kinetic parameters

Method of amplitudes
In some special cases of interest, the recovery of thermodynamic information from the experimentally measured photoacoustic signals can be simply obtained by using the amplitudes of the waveforms, neglecting its time dependence.
This simple analysis is possible whenever transient lifetimes are either much shorter or much longer than the instrumental response of the photoacoustic setup.  As a rule of thumb, this assumption is valid in case:
short lived transients have lifetimes a factor of 10 below the instrumental response (for a system with a 200 ns risetime, transients with lifetimes below 20 ns are seen as "prompt");
permanent products or transient species have lifetimes ca 5 times longer than the experimentally determined upper limit of the resolution range (i.e. for a system with a 5 ms upper limit, transients with lifetimes of 25 ms can be considered as "long lived").
The amplitude of the photoacoustic signal can be taken in several ways.
The simplest way is to work with signals from which the baseline has been subtracted.  In this case the peak amplitude of the first positive oscillation is a good measure of the photoacoustic signal amplitude.  Alternatively, the difference between the amplitudes of the first positive and the first negative oscillations can be considered.  The advantage of this second estimate is that it compensates for the presence of residual offsets on the waveforms.  When signals are very small and noisy (very dilute samples, very low laser fluences,...) taking the integral of the first positive oscillation may be of help.
Using deconvolution (vide infra) even in the absence of transients with lifetime in the resolution range is an alternative way to reduce the noise and increase accuracy in the recovery of data.
The ratio between the amplitudes of the waveform acquired for the sample under investigation, HSn, and a reference compound, HRn, taken under the same experimental conditions, is then analyzed in terms of the equation (see the phenomenological theory, equation (8)):
 

(8)
 

Deconvolution
When the lifetimes of the transients under investigation are neither much longer than the upper limit of the resolution range nor much shorter than the instrumental response, the method of amplitudes is not practicable any longer and deconvolution must be used instead.
The measured signal Hns(t)  is a numerical convolution of the time derivative of the photoinduced, time-dependent overall volume change (of both structural and enthalpic origin) and the instrumental response, obtained with a compound releasing all of the absorbed energy as heat within a few nanoseconds.
The convolution leads to a distorsion of the output Hns(t) signal both in amplitude an shape.  In order to understand the effect of convolution on the photoacoustic signals, a couple examples are provided, in which either the preexponential factor or the lifetime is held constant, whereas the other parameter is varied.
For short lived transients (lifetime below 1 ns), the effect of changing the preeponential factor is simply scaling the amplitude of the waveform with no change in the time profile.  Negative preexponentials lead to "negative" waveforms, symmetrical with respect to the time axis.
When the amplitude is kept constant ( in the example j is kept constant at 1 for all the waveforms) and the lifetime is changed, both amplitude and shape of the waveform are affected. When the lifetime increases, the resulting amplitude becomes smaller and the position of the maximum shifts towards longer times.  The long lived transients (lifetime above 2 ms) have very small amplitudes (consider that in the example provided the amplitude was kept at 1) and this hinders the recovery of the kinetic information.
 
When multiple exponential decays are considered the analysis is generally perfomed increasing the number of exponentials that are used to fit the data.  The goodness of the fit is judged by the value of the sum of the squares of the residuals, S2, and by visual inspection of the residuals and the autocorrelation function of the residuals.  The autocorrelation function of the residuals gives a good estimate of the randomness of the residuals.  Randomly distributed residuals give autocorrelation functions that are 1 at the first channel and then drop to approximately 0, oscillating randomly around zero.  The addition of a further exponential function is considered to be reasonable, if the S2 improves (becomes smaller) of at least 20 %. The analysis is generally performed using a least squares optimization based on the Levenberg-Marquardt algorithm.  c2 optimization is not used in general, since the evaluation of the errors distribution is too time consuming to be determined for each experiment.
Even for normalized data (divided by E(1-10-A) and reference scaled to 1) the absolute values of the sum of residuals S2 depend on the number of experimental points that are used and the S/N ratio of the signals.  It is therefore not practical to give absolute reference numbers to judge the goodness of S2.
An example is given below, showing signals taken at T = 10 °C for aqueous solutions of bromcresol purple (reference compound) and o-nitrobenzaldehyde in the presence of 20 mM of the Major Urinary Protein (rMUP) at pH 4.5.
Fitting with a single exponential function results in very correlated residuals.  Upon addition of a second decay, the S2 is reduced by a factor 20 and the residuals become randomly distributed.

Background search
When background fluctuations are present, the reference and the sample waveforms may be offset a little bit.  An example is given, for the same data presented above, where an offset has been added.  Although the fit to the sample waveform is reasonable, the residuals are systematically oscillating below zero, whereas the autocorrelation functions shows oscillations not around zero, rather around a finite value. The background search routine allows the optimization of this offset and eliminates the mismatch between sample and convoluted waveforms. Great care must be taken in using the background optimization, especially when long lived (t>2 ms) transients are under investigation.  The addition of an offset may substantially affect the recovered preexponential factor and lifetime and may impair the capability of recovering long lived transients.
 

Shift search
Small changes in temperature or small displacement of the laser beam inside the cuvette (due, for instance, to poiting instability) lead to small time shifts in the signals.  This impairs the capability of recovering the kinetic parameters from the deconvolution.  However, by time shifting the reference and sample waveforms with respect to each other, these small variations can be corrected for. Care must be taken also in optimizing the shift between reference and sample waveforms.  The shifting routine may lead to erroneous evaluations of short (tens of nanosecond) lifetimes.  The presence of a short lived transient (say 30 ns) has effects on the sample waveform which are very similar to time-shifting the sample with respect to the reference of an equal amount.
The shift search is important for evaluation of the structural volume changes in the two-temperatures method. In this case the shifting is due to the change in the speed of sound between the two known temperatures.  However, even in this case, the shifting routine must be used with caution in order to avoid systematic errors in the retrieved parameters.  The time shift between reference and sample waveforms must be carefully evaluated by considering the temperature dependence of the reference waveform in the solvent used in the experiment. Special attention must be paid, especially when working with short lived transients, for which shifting may either mimic or compensate the distorsion introduced by the relaxation, thus introducing a fake transient or "canceling" a true one.


Kinetic schemes

Numerical reconvolution has been performed, so far, assuming multiexponential relaxation functions.
Even in this case, the answer from a multiexponential fitting can be interpreted as resulting from a sequential or a parallel scheme.  For the proper interpretation of ji, it is important to lay down a mechanism. In the case of a sequential reaction scheme:

the amplitudes  derived from the reconvolution analysis are related to the parameters of the elementary steps (i.e., the weight of each step j i and the lifetimes ti ) by the following relations:

It is obvious that for a system with t3 >> t2 >> t1, the equations simplify and ji = jiapp.


 
Temperature dependence of photoacoustic signals

The photoacoustic signal of dilute aqueous solutions depends strongly on the temperature of the solution through the thermoelastic parameter b/Cpr. The temperature dependence of b/Cpr is shown in this figure. As a result, the amplitude of the photoacoustic signals of an aqueous solution of bromcresol purple as a function of temperature varies strongly and, in particular, strongly decreases as the temperature is decreased below room temperature.  In addition, the speed of sound in the solution depends strongly on the temperature and therefore the arrival time of the waveform changes as a function of temperature, resulting in a shift of the waveform when the temperature is changed. This effect is easily seen for the normalized photoacoustic signals of an aqueous solution of bromcresol purple as a function of temperature.
In concentrated aqueous solutions of virtually any kind of solute, this strong temperature dependence is lost and the signal is less affected by changes in temperature.  This is also true for organic solvents.
 
 

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