Abstract—Using a mathematical statistics approach, we review the procedure for type classification of acoustic emission (AE) events into shear, tension, and collapse, proposed by Zang et al. (1998). The procedure is based on counting the signs of first pulses of waves arriving at acoustic sensors and is widely used in rock physics experiments. Under the assumption that the determination errors of first-pulse signs at sensors have uniform and independent distribution , the statistical significance and power of the type separation test are evaluated for a given number of sensors used. We consider and compare three methods of the construction of a statistical test based on the P-value approach and symmetric and asymmetric statistical hypothesis tests. Considering the results of the statistical study, we propose some practical recommendations for selecting a threshold to classify AE event types in experimental studies.
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The study was carried out under the State contract of the Faculty of Physics of the Moscow State University and the Schmidt Institute of Physics of the Earth of the Russian Academy of Sciences. The laboratory experiments initiating this study were conducted in the Center of Shared Research Facilities “Petrophysics, Geomechanics and Paleomagnetism” IPE RAS.
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APPENDIX
APPENDIX
From formula (7),
For convenience, we denote \(m = \left( {{{m}_{0}} + 1} \right)\), then
Let us find the maximum as a function of p. Note that β has a meaning of probability, therefore, \(0 \leqslant \beta \leqslant 1\). At \(p = 0\) and \(p = 1\) , we obtain \(\beta = 0\). As β is not an identical zero at \(0 < p < 1\), from the condition \(\frac{{\partial \beta }}{{\partial p}} = 0\) we can determine the value corresponding to the maximum β as a function of\(p\).
Let us find the respective derivative:
We split the expression into two parts:
Then \(\frac{{\partial \beta }}{{\partial p}} = ~\,\,n!\left( {{{\varphi }_{1}} - {{\varphi }_{2}}} \right)\). In \({{\varphi }_{1}}\) we replace the summation variable \(k{\kern 1pt} ' = k - 1\), so that the form of sum \({{{{\varphi }}}_{1}}\) is as similar as possible to \({{{{\varphi }}}_{2}}\):
It can be seen that the sums in \({{\varphi }_{1}}\) and \({{\varphi }_{2}}\) differ only by the terms with \(k{\kern 1pt} ' = m - 1\) and \(k = n - m\). Since \({{\varphi }_{1}}\) and \({{\varphi }_{2}}\) are present in the formula for \(\frac{{\partial \beta }}{{\partial p}}\) with opposite signs, therefore, in \(\frac{{\partial \beta }}{{\partial p}}\), all the similar terms of sums \({{\varphi }_{1}}\) and \({{\varphi }_{2}}\) are cancelled. Thus, we can record
We use an abridged multiplication formula \({{a}^{n}} - {{b}^{n}} = \left( {a - b} \right)\) \(\left( {{{a}^{{n - 1}}} + {{a}^{{n - 2}}}b + \cdots + a{{b}^{{n - 2}}} + {{b}^{{n - 1}}}} \right)\) to convert the last multiplier in the above formula. This yields
In this formula, at \(0 < p < 1\), only the multiplier \(\left( {\left( {1 - p} \right) - p} \right) = 1 - 2p\) can be zero, which is true at \(p = {1 \mathord{\left/ {\vphantom {1 2}} \right. \kern-0em} 2}\). Thus, \(\frac{{\partial \beta }}{{\partial p}} = 0\) at \(p = \)\({1 \mathord{\left/ {\vphantom {1 2}} \right. \kern-0em} 2}\), therefore, the probability β as a function of \(p\) has a maximum.
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Smirnov, V.B., Isaeva, A.V., Kartseva, T.I. et al. On the Statistical Significance Test for the Procedure of Polarity Classification by Types of Acoustic Emission Sources. Izv., Phys. Solid Earth 59, 49–63 (2023). https://doi.org/10.1134/S1069351323010056
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DOI: https://doi.org/10.1134/S1069351323010056