The inner core.
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The inner core.
Sun, 02/04/2007 - 15:53Do we have a geophysicist in the house!?
Someone call?
Tomography does not have this resolution but good old fashioned seismology does. Probably what is being used here is the reflection from the inner/outer core boundary (PKiKP) and comparison with the P-wave through the outer part of the inner core (PKIKP)
The inner core.
Mon, 02/05/2007 - 18:34Tomography isn't the be all and end all. Like Hypocentre says reflected waves from the inner/outer core boundary could be used to image the boundary, although at those depths I am not sure how that resolution could be acheived.
There has been work done on the irregular D'' layer (just above the outer core IIRC), where diffracted waves from the irregularities, recorded at the surface, can be focused with high precision back to the place where they came from. This is similar to imaging processes used in exploration geophysics.
The inner core.
Mon, 02/05/2007 - 21:49I always liken seismic tomography to trying to look at a member of the opposite sex through a frosted shower screen. You know that there is something quite interesting going on behind there - but you can't quite make out what it is!
The inner core.
Tue, 02/06/2007 - 08:39probably sound stupid here, but i thought that the inner core was hotter than the outer core. so how could the inner core grow by:
small frozen sediments falling onto its surface
Wouldn't the 'frozen sediments' actually have to heat up? and then let pressure solidify them? :?
The inner core.
Tue, 02/06/2007 - 11:34What do they mean by 'frozen' sediments anyway?
I thought 'frozen' just referred to water and would therefore require temperatures of 0C (at 1Atmosphere). Whilst I know the pressure is immense at the inner/outer core boundary so is the temperature.
And just what 'sediments' can sink that far? Surely only the heavy elements can make it to the core - especially given convection cells in the mantle.
Might have to look at the wikipedia article to see the context.
The inner core.
Tue, 02/06/2007 - 14:20but there's no sediment in the mantle or cores. that implies erosion from a solidified rock, namely at the surface.
so that just sounds wrong.
If there's anything going on, maybe some liquid is crystallizing and being moved around because of its denser quality. Or elemental differentiation is still ongoing, so bits of iron and nickle and whatever else are slowly making their way down to the core and joining in, making it larger as the mantle shrinks due to the loss.
The inner core.
Tue, 02/06/2007 - 18:36So it was probably deduced from other more accurate seismic techniques than tomography... thats cleared that up- thanks ![]()
I always liken seismic tomography to trying to look at a member of the opposite sex through a frosted shower screen. You know that there is something quite interesting going on behind there - but you can't quite make out what it is!
Nice analogy!
I really wouldn't be using wikipedia for any reliable geo-information. Especially not for school/university stuff!
Don't worry, this is just from a discussion someone brought up on another website. I wouldn't touch wikipedia with a barge-pole for uni work.
The inner core.
Wed, 02/07/2007 - 13:56Personally I really rate Wikipedia as a free on-line reference service. You just have to critically analyse all that you read (which no doubt everyone does for everything anyway, even peer-reviewed papers). Back in the day when I was a student we searched random homepages for information never having a clue how reliable it was.
To pick on one sentance in an entire article to dismiss the site is a flawed argument. Besides the very essence of Wikipedia is that you can go in and change the article to correct and improve it.
Still, I'd never rely on it as a single source of evidence for uni/work/school. But then again I'd never rely on any single source of evidence - that's the way Creationist thinking works!
PS: No, I don't own shares in wikipedia
The inner core.
Thu, 02/08/2007 - 09:30I am doing various essays for my A-level geology course, and quite often when you search a technical name, guess whats at the top of the list? Wikipedia.
It is useful as there are only a few other sites, GR included, that have good enough technical facts for a-level and above students to use.
But i do agree that if you take a fact from wiki, try to look it up, to make sure it is actually a fact!
Although personally i prefer:
http://uncyclopedia.org/wiki/Main_Page
![]()
The inner core.
Thu, 02/08/2007 - 10:43When I gave my talk recently, I used google as an example of what people find when looking stuff up. My aim was to show how high creationist sites appear, but wikipedia was second on a lot of searches.
There are two problems with wikipedia:
1 - no check on reliability (GR addresses this by editorial means and wikipedia are doing likewise for "controversial" topics)
2 - what you look up today may be different when you check tomorrow (although you can look at the history) because anyone can edit the page.
Having said that, wikipedia is an amazing idea and resource. I've borrowed a lot of ideas from them for GR3 ![]()
inner core
Thu, 08/11/2011 - 20:00OK, so what actually fuels the inner core, anyway? Can anyone comment here? I've heard several different arguments and I would like feedback on them.
The first line of reasoning goes: (a) If it were only gravitational compression the earth would be solidified by now (a la Mars), (b) the heavy, radioactive elements are more dense than iron, therefore (c) heavy metals sink near the center, form nuclear furnaces and a significant amount of heat comes from radioactive decay. (Of course, if it gets too hot, convection can break up the pockets of nuclear material, too.) I think this argument sounds the most plausible.
A second line of reasoning follows: (a) most uranium compounds (with the exception of uranium sulfide) are lighter than iron, (b) therefore they float around in the mantle and don't sink to the core, therefore (c) radioactive decay does not play a major role in keeping the core hot and it's all gravitational contraction.
A third line of reasoning is: (a) solar input nearly matches earth thermal output, so (b) therefore it's all solar. (Gravitational contraction supplied most of the heat until the earth cooled to the point where it was balanced with solar input, and now it's in a state of equilibrium until solar output changes significantly.)
I don't have numbers on any of this so I can't really tell which is right, if any, and which are wrong. The second argument seems wrong to me, though it is also very popular, because I imagine chemistry breaks down (all uranium would be elemental) at temperatures of 7,500 - 10,000 degrees (F) such as are found at the core. Is that not the case, or am I missing something (e.g., the effects of pressure)?
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The inner core.
Submitted by Matt on Sat, 02/03/2007 - 18:30.Little is known about the process of growth of Earth's inner core. Because it is slowly cooling, many expected that the inner core would be very homogeneous and clean. It was even suggested that Earth's inner core may be a single crystal of iron, however, this is at odds with the observed degree of messiness inside the inner core. Seismologists have revealed that the inner core is in fact rather messy and has some large scale structures such that seismic waves pass through it more rapidly in some directions than in others. The surface of the inner core exhibits rapid variations in properties at scales at least as small as 1 km. This is puzzling, since lateral temperature variations along the inner core boundary are known to be extremely small (this conclusion is confidently constrained by magnetic field observations). Recent discoveries suggest that the solid inner core itself is composed of layers, separated by a transition zone about 250 to 400 km thick.[5] If the inner core grows by small frozen sediments falling onto its surface, then some liquid can also be trapped in the pore spaces and some of this residual fluid may still persist to some small degree in much of its interior.
From www.en.wikipedia.org/wiki/inner_core
Do we have a geophysicist in the house!? My understanding was that the best resolution possible from seismic tomography was a couple of hundred km at best, decreasing at lower levels. How was the statement in bold deduced? By another technique? Or is this just another example of why wikipedia isnÂ’t always to be trusted?