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De L'indice de Cyrtose des Courbes en Statistique Granulometrique

Dieser Beitrag bringt einen Vorschlag, die Kurtose nach einer neuen Methode zu berechnen. Die Vorteile dieser Methode werden vom statistischen und geologischen Gesichtspunkt aus kurz besprochen. Vielleicht bietet diese neue Berechnung der Kurtose die Möglichkeit, die Sedimente leichter zu differenzieren.

The author show the possibility of computing kurtosis in a manner which parallels Wentworth's computation of skewness. They offer for further consideration various suggestions on the possible statistical and sedimentological advantages of this "new" coefficient. Besides the test or check value, the method permits a greater spread of kurtic value in the central area and in addition would perhaps permit a better differentiation between sediments whose frequency size distribution is close to gaussic.

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