Brought low, the - third record - Whiplash During Low Speed Impact: Fact or Fraud?

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Testing has shown that the maximum loading to a rear-ended car was amplified about two and a half times when it reached the heads of the occupants. The testing also revealed that this occurred about a fourth of a second after impact.
The momentum and loading to cars which are involved in a rear-end impact (of low enough impact velocity so that there is no permanent deformation of the bumpers) can be fairly accurately modeled as a mass-spring system. This enables determination of the loading effects on the cars and heads of the occupants, by input of known quantities (masses of the cars, bumper stiffness, relative velocity between the cars at time of impact).
It is thus possible to determine the likelihood of a claim of whiplash injury being legitimate. Based upon how consistent all incident data is with available research findings and on using as precise a computer model as possible, an engineer with a proper dynamics and biomechanics background can help to determine the viability of a claim.

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The ferroan anorthosite suite consists almost exclusively of the rock anorthosite (>90% calcic plagioclase) with less common anorthositic gabbro (70-80% calcic plagioclase, with minor pyroxene). The ferroan anorthosite suite is the most common group in the highlands, and is inferred to represent plagioclase flotation cumulates of the lunar magma ocean, with interstitial mafic phases formed from trapped interstitial melt or rafted upwards with the more abundant plagioclase framework. The plagioclase is extremely calcic by terrestrial standards, with molar anorthite contents of 94-96% (An94-96). This reflects the extreme depletion of the bulk moon in alkalis (Na, K) as well as water and other volatile elements. In contrast, the mafic minerals in this suite have low Mg/Fe ratios that are inconsistent with calcic plagioclase compositions. Ferroan anorthosites have been dated using the internal isochron method at "circa" Ga.

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