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Exponential Cascade Failure

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reportmonkey | 13:29 Thu 21st Jul 2005 | Science
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I'm running some tests on a series of anomalous materials but seeing some very strange results.

One material seems to have magnetospheric influx ratio of 1.618 much above what I was expecting for non-terrestrial materials.  Biomass results indicated massive megloamoebic structures similar to early bivalve amenos.  Could anyone help me explain where this material might originate from.  I've found no similar details on the internet and i'm concerned that its elemental properties match nothing on the periodic table.

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Ah you have encountered Chemical - X

Take it down to your local primary school and soon you will have:

http://www.cartoonnetwork.com/tv_shows/ppg/index.html

Bru-wah-ha-ha-haaaa!

During periods of northward IMF, as a result of large influx of the magnetosheath ions, the plasma sheet becomes cold and dense. During these periods, a large number of the plasma sheet ions have two components: hot (magnetospheric origin) and cold (magnetosheath origin). Based on their spectral distributions: one-component Maxwellian, two-component Maxwellian, and kappa (k), the characteristics of the plasma sheet ions were studied with DMSP satellites and a method of inferring plasma sheet ion properties from the ionospheric observations. The cold-component constituent of the two-component ions is hotter in the dawn than the dusk sector, consistent with the in situ studies that suggest that the magnetosheath ion is heated upon its entry along the plasma sheet dawn flank. This temperature asymmetry leads to a dawn-dusk asymmetry in the ion spectral distribution. The cold and hot components are closer together in temperature space, which increases the proportion of ions having (apparent) one-component distribution in the dawn flank while, in the dusk flank, the influx of the magnetosheath ions increase the density of the two-component ions. The dawn-dusk asymmetry in the cold magnetosheath ion profile should help determine the roles of various proposed magnetosheath entry mechanisms.  This, I think, explains your problem. Qu'est-ce que vous faites de votre temps libre?
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I've re run the material through the Fusion Mass Implosion Spectrometer and the results are more promising.  By separating out the bi-polor irregularities as suggested by King-Hughes Dimensional Proportions of Elements (1982).  I have managed to extract the chemical make up.  Thank you answerbank you have solved this problem and saved my scientific integrity.

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He was probably distracted by an anomaly in the sub-space continuum
Now try escaping from the Black Mesa Complex.
Is reportmonkey's real name Gordon Freeman by any chance?
Sounds like school custrard.

The magnetospheric influx ratio anomaly is probably caused by Group I bi-polar proton resonance failure.

In other words, the di-lithium crystals cannae handle it, Cap'n.

reportmonkey, your real name is Scottie.
You are dead.
I claim my �5.

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