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 Ludwik Kowalski; 7/10/2006Department of Mathematical Sciences
 Montclair State University, Upper Montclair, NJ, 07043
 
 
 
 This is a continuation of what was in the unit #301. What would happen to the CMNS field if the Mizuno-type excess heat is really shown to be an 
illusion? Not much. Mizuno-type experiments were only a small fraction of the EE (excess energy) sub-field. The CF and CT sub-fields (cold fusion 
and cold transmutations) cannot possibly suffer from an interpretational error in the case of GDPE (glow discharge plasma electrolysis). The only 
negative effect on the entire CMNS field can possibly come from a realization that it took ten years to find a trivial cause of the illusion. 
The fact that dominants researchers, Mizuno and Naudin, decided to remain silent when their conclusions were criticized will be noticed. People might 
generalize that all CMNS scientists are irresponsible. I hope that this will not happen.
 At the beginning of unit #301 I wrote about preliminary results from Scott Little. Last night Scott send me final results. This morning these results 
were posted on the CMNS list (restricted Internet list for CMNS researchers). Three different methods were used to determine the percentage of the 
electrolyte: the method based on weight (already described in unit #301), the method based on concentrations of potassium (K) and the method based on 
concentration of tungsten (W). The XRF (X-Ray Fluorescence) instrument was used to measure the concentrations. How does this method work?
 
 A narrow beam of X-rays is sent on a sample to be analyzed. The atoms in that substance are excited and emit characteristic X-rays. Like in optical 
spectroscope, individual elements can be recognized by unique characteristic X-rays. Scott optimized the instrument for the detection of peaks due 
to K and W. Once this is done he can compare intensities of characteristic rays, for different samples, with the intensity of a standard in which 
concentrations of atoms are known. An example of an XRF spectrum is shown in Figure 1. The abscissa is the wavelength of X ray photons while the 
ordinate is the number of accumulated counts. Characteristic wavelengths indicate presence of specific atoms while heights of peaks are proportional 
to concentrations of these atoms.
 
 
  
 Figure 1
 A typical X-ray fluorescence spectrum. Narrow peaks correspond to specific elements. The rest corresponds to the X-rays with which the sample was 
bombarded. The tail, under narrow peaks, is the background. Heights of peaks do not include that background. Numbers refer to arbitrary units.
 
 
 Suppose, for example, that a particular peak is due K (potassium) atoms, as established by a preliminary calibration. How can this help us to 
determine the percentage of the electrolyte in the liquid lost during a Mizuno-type experiment? This can be done by comparing two spectra (a) that  
due to the sample of the original electrolyte and (b) that  due to a samples of condensed liquid escaping from the cell during an experiment. The two 
samples must have the same volume, for example 27 cubic mm, and be analyzed under identical conditions. Suppose the height of the K peak in (a) is 
8 units (after subtracting the background) while the height of the K peak in (b) is 2 units. Then one would say that concentration of K in (a) is 
4 times higher than in (b). It is easy to consider two extreme cases: the escaping liquid is nothing but H2O vapor and the escaping liquid  
is nothing but original electrolyte. In the first case the height of the peak for (b) would be zero. In the second case the height of the peak in (b) 
would be the same as in (a). The ratio of the peak height in (b) and the peak height in (a), multiplied by 100, is the percentage we are trying to 
establish. For the hypothetical 2/8 ratio the contribution of the electrolyte to the escaping liquid would be 25%. That is the essence of the XRF 
methodology.
 
 
 
 
TABLE 1 Figure 2
 sample   SCA      K       W      % drops   % drops   % drops     %
 conctr. conctr. conctr.   by SCA     by K     by W   3 methods
 #1     0.21    0.063   0.026    7.66       8.70     6.10     7.49
 #2     0.12    0.041   0.026    4.38       5.66     6.10     5.38
 #3     0.18    0.054   0.036    6.57       7.46     8.45     7.49
 #4     2.74    0.724   0.426                              mean = 6.79%
 st.dev=1.21%
 
 Summary of results
 
 
 Figure 2 shows the summary of results. It is based on what was posted by Scott Little last night. He provided numbers in the first four columns, I 
added additional columns to show the main conclusions. Sample # 4 was fresh K2CO3 electrolyte; its concentration was 0.2 M. 
Samples #1, 2, 3 were 
condensed liquids escaping from the electrolytic cell during a Mizuno-type experiment, similar to that in Colorado2. The four samples are identified 
in the first column. The next three columns show results obtained by using three different methods. Note that SCA, in the second column, 
refers to the method described by Scott at the beginning of unit #301. Numbers in that column are weights of solid deposits, in arbitrary units. SCA 
stands for a sensitive scale measuring the weights. Likewise, K in the third column stands for potassium. The numbers in the third columns 
are concentrations potassium atoms, in arbitrary units (heights of potassium peaks in the X-ray spectra). And W in the fourth column stands 
for tungsten. Numbers in the fourth column are concentrations of tungsten atoms in arbitrary units (heights of tungsten peaks in the X-ray spectra).
 
 The columns 5, 6 and 7 show percentages of electrolyte in the escaping liquid inferred from numbers in columns 2, 3 and 4, respectively. That is what 
we really need to calculate the COPs correctly. Let me illustrate this by showing hoe the 8.7% result was obtained for sample #1 by using the K method. 
The concentration of K for the sample 4 was 0.724 arbitrary units. The concentration of K for the sample 1 was 0.063 arbitrary units. The peak ratio 
is 0.063/0.724 is 0.087 and this translates into 8.7%. Is this result consistent with what one finds by using the tungsten method. According to that 
method the percentage of the electrolyte in the escaping liquid is (0.026/0.426)*100 = 6.1%. And what was the percentage of droplets according to the 
weight method? The answer is (0.21/2.74)*100 = 7.7% Ideally all three methods should give the same result for the experiment in which 
sample #1 was collected. But measurements are not ideal. The mean results is (8.7 + 6.1 + 7.7) / 3 = 7.5, as shown in column 8. Results for the samples 
#2 and #3 were obtained in the same way.
 
 The main conclusion is that the escaping liquid is not pure H2O steam; several percents of the lost mass is probably 
removed as droplets of the electrolyte. We did not take this under consideration when COPs were calculated on the basis of data collected in Colorado2 
experiments. All COPs would be significantly lower if percentages of the electrolyte in the escaping liquid was taken under consideration. After posting 
that conclusion on the CMNS discussion list (percentages from columns 5, 6 and 7) I found an interesting tutorial about steam at
 
 http://www.spiraxsarco.com/learn/modules/2_2_01.asp
 
 Here is a quote from it; it shows that the issue of "tiny droplets" is far from being new. ". . . Steam with a temperature equal to 
the boiling point at that pressure is known as dry saturated steam. However, to produce 100% dry steam in an industrial boiler designed to produce 
saturated steam is rarely possible, and the steam will usually contain droplets of water. In practice, because of turbulence and splashing, as bubbles 
of steam break through the water surface, the steam space contains a mixture of water droplets and steam. Steam produced in any shell-type boiler 
(see Block 3), where the heat is supplied only to the water and where the steam remains in contact with the water surface, may typically contain 
around 5% water by mass."
 
 I suppose this is a well known fact. But it is not mentioned in papers or Internet reports with which I am familiar. This can be explained by isolation 
in which CMNS research is done. A normal peer review process would certainly forced the authors to take the tiny drops effect under consideration. But 
reports published at yearly International Conferences on Cold Fusion, or over the Internet, are not scrutinized by selected experts, as papers published 
in mainstream journals. That is one of many undesirable results of exclusion imposed on the CMNS research about 15 years ago. On one hand no evidence 
of the pseudoscientific nature of CMNS was offered and on the other hand the field is not recognized as illegitimate. The situation is tragic; how can 
it be changed? Many think that this will suddenly happen as a result of commercial success; for example after a 100 kW generator, based on the CMNS effect, 
becomes available. I believe that focusing on scientific investigations, rather than on commercial applications, is more appropriate at this time. The CMNS 
field should be allow to evolve in the same way as other areas of science.
 
 Let me return to conclusions drawn for Scotts results. These conclusions are  based on a simplifying assumption which is most likely not valid. 
Ideally one need four samples #4, each removed from the electrolyte (with a pipette) only a moment before the experiment during which the corresponding 
sample (#1, #2 and #3) is condensed. We do not know what concentrations of the electrolyte were at the beginning of these experiments. I simply assumed 
that the concentration in sample #4 was the same as in the original electrolyte, and that fresh original electrolyte was used before each experiment. One 
can imagine several scenarios in which the inferred percentages of tiny droplets would be higher than shown in my table above.
 
 For example, suppose that samples #1, #2 and #3 were extracted after a considerable delay. During that delay a significant fraction of the original 
electrolyte evaporated and replaced by distilled water. Knowing this one would correct concentrations of in sample #4 (for each of methods) , accordingly. 
The values would become smaller than those shown in my table. Suppose they become two times smaller. That would make all percentages two times larger. 
The mean of three means, 6.79% would become 13.58%. The COPs obtained during the three experiments, without accounting for the escaping electrolyte were 
close to 1.1. These values would have to be reduced to less than 1.0 for the 13.58% correction.
 
 The bottom line is that conclusions made in my table are not reliable. Better experiments must be conducted. My suggestion is to use fresh electrolyte 
in each experiment, to extract samples of liquid electrolyte moments before experiments in which samples #1, #2 and #3 are extracted. Actually, three 
samples is hardly enough; we need 5 to 10 samples get reliable means and standard deviations (bars of errors).  Will this be done in Paris3 and Marseilles1 
experiments? I hope so. Will this be done to correct the COPs reported after the Colorado2 experiments (mean 1.24, st.dev = 0.13). It depends on us, 
the authors of the anticipated Colorado2 paper. I think that a simple CLA method of estimating percentages would be sufficient.
 
Appended in 7/13/06):In a message posted today at the CMNS list I wrote that the problem that was labeled tiny droplets is far from being 
resolved. That contradicts what I wrote here earlier.
 
 The mechanisms by which droplets of electrolyte are ejected are certainly worth investigating. But I would not start investigating them at this time, 
except in the context of our main question. That question is "should the total mass, M, lost during a GDPE experiment, be used to calculate thermal 
energy lost via vaporization?" The initial answer was "yes," the COPs were calculated from the uncorrected M in Colorado2. Then the 
question of tiny droplets was raised. We concluded that the mass used to calculate a COP should have been M-m, where m is the mass of escaping droplets 
of the electrolyte. Scott suggested a method for estimating m on the basis of weights of solid residuals, as explained at the beginning of unit #301.
 
 That method was based on the expectation that the major component of solid remains, in two samples (initial electrolyte and condensed steam), would be 
K2CO3. But his XRF method revealed presence of tungsten. The original electrolyte cannot possibly contain a lot of tungsten; presence of W in that 
liquid was a proof that sample 4 was not extracted from the initial electrolyte. That is why another set of samples must be analyzed. But a significant 
amount of W in solid remains from samples 1, 2, and 3 is alarming, as recognized by Peter Gluck. Let me elaborate.
 
 First let me refer to the SCA method (explained by Scott at the beginning of unit #301). My conclusion, for example for Sample 1, was that m was 8.8% 
of M. But that was done by assuming that solid deposit in Sample 1 were chemically the same as in Sample 4 (the original electrolyte). But suppose that 
one half of the solid remains from Sample 1 was tungsten. Knowing this I would conclude that m was 4.4% of M, not 8.8%. And m would become 2.2% of M 
if 75% of the solid mass, in remains from Sample 1, were due to tungsten. To remove the ambiguity I would ask a chemist to extract tungsten from the 
Sample 1, before it is dried and weighted. Would the SCA method become reliable? Not really. It would be reliable only if other elements were not 
present, AND if only tiny droplets were responsible for the removal of the K and W, from the cell. Without these preconditions Scott's SCA method, 
as used in my table (see unit #302), could not be trusted, even if Sample 4 were extracted from the initial electrolyte. To make that method useful 
one must make sure that dominant non-water component, in all samples from condensed steam, is potassium.
 
 But that is not all. How can we be sure that potassium, found in samples 1, 2 and 3, was removed from the beaker by tiny droplets? We simply assumed 
that this was the case. Suppose that K and W are removed from the cell as tiny colloidal particles present in the boiling electrolyte. The particles 
can be either dry or wet. Suppose they are dry. In that case a large concentration of K, found in the solid remains of condensed steam, could not be 
used as an indicator that m was large. One can easily have a situation in which m<<M while the concentration of K in the sample is not negligible. 
In other words, contrary to what I wrote in unit #302, we have no convincing evidence that the actually measured M must be corrected. How can one show 
that colloidal particles are  "nothing to worry about?"
 
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