Brief historyGalton <strong>and</strong> McAlister began the study of the lognormal distribution in papers they published togetherin 1879, in which it was related to the use of the geometric mean as an estimate of location. For thisreason, this distribution is sometimes referred to as the Galton distribution. Since then, many others havecontributed to the underst<strong>and</strong>ing <strong>and</strong> development of this distribution, including Wicksell, who introduceda third parameter, known as the threshold, in 1917 to fit the distribution of ages at first marriage.Situations in which to use this distribution<strong>The</strong> log-normal distribution can be applied to a wide variety of situations, such as risk analysis of nuclearpower plants, current gains in transistors, sizes <strong>and</strong> growth of organisms <strong>and</strong> populations, rainfalls, sizesof incomes, <strong>and</strong> many more.Relationships to other distributionsTaking the natural logarithm of the pdf of the lognormal distribution results in a pdf for a Normal distributionwith mean α <strong>and</strong> variance β 2 .<strong>The</strong> <strong>Weibull</strong> DistributionPDFWhere 0 < y < ∞, α > 0, β > 0 <strong>and</strong> α is the ”scale” parameter <strong>and</strong> β is the ”shape” parameterf Y (y) = αβy β−1 e −αyβExpected value <strong>and</strong> varianceE(Y ) = α −1/β Γ(1 + 1/β)V ar(Y ) = α −2/β {Γ(1 + 2/β) − Γ(1 + 1/β) 2 }Graphs with different parameter valuesBrief history2
<strong>The</strong> <strong>Weibull</strong> distribution is named after Waloddi <strong>Weibull</strong> in 1951 who was the first to describe <strong>and</strong> studyit in detail for its application to strength of material. However, this distribution was first discovered byFrechet in 1927 <strong>and</strong> first applied by material scientists Rosin <strong>and</strong> Rammer in 1933 to model the distributionof sizes of pulverized particles. Although it was originally proposed to model objects physical fatigue, itnow has many more applications.Situations in which to use this distribution<strong>The</strong> <strong>Weibull</strong> distribution is most often used to model lifetimes <strong>and</strong> failure times. This may include reliability,failure rates, failure probability. <strong>The</strong> flexibility of this distribution allows for many practicalapplications. It can take into account increasing, decreasing, or constant failure rates. When β > 1 failurerate is increasing over time, <strong>and</strong> when β < 1 failure rate is decreasing over time, <strong>and</strong> β = 1 implies aconstant failure rate. This distribution is interesting because α, or characteristic life is set so 63.21% ofobjects fail at time x = α. For example, to study failure of an aluminum part α = 4, <strong>and</strong> for steel α = 3.<strong>The</strong> smaller the characteristic life is the more scatter of data there is around the model. This distributionis often applied in engineering to model physical degradation, as studied by Waloddi <strong>Weibull</strong>, <strong>and</strong> in seriessystems to model the weakest link. For example, this distribution is used by structural engineers to model<strong>and</strong> predict fatigue <strong>and</strong> resulting cracks in airplanes.Relationships to other distributionsWhen failure rate is constant, i.e. β=1 then <strong>Weibull</strong> (α, 1) = Exponential (α)When β=2 then <strong>Weibull</strong> (α,β) = <strong>Rayleigh</strong> (α) = Chi (2, α) , where n=2<strong>The</strong> <strong>Rayleigh</strong> DistributionPDFf y (y) = y α 2 e −y22α 2 α > 0, 0 ≤ y < ∞= 0 elsewhereExpected value <strong>and</strong> variance√ πE[Y ] = α2Graphs with different parameter valuesBrief historyV ar[Y ] = 4 − π α 22John William Strutt, 3rd Baron <strong>Rayleigh</strong> (1842 - 1919) was a nineteenth- <strong>and</strong> twentieth-century Britishphysicist who discovered the pdf of <strong>Rayleigh</strong> arising in the study of wave motion, which earned him theNobel Prize for Physics. He also discovered <strong>Rayleigh</strong> scattering <strong>and</strong> predicted the existence of the surfacewaves now known as <strong>Rayleigh</strong> waves.Situations in which to use this distribution3