Core Inner core

Speculation also continues that the inner core might have exhibited a variety of internCore Inner coreal deformation patterns. This may be necessary to explain why seismic waves pass more rapidly in some directions than in others. Because thermal convection alone appears to be improbable,

The outer core was determined to be liquid from observations showing that compressional waves pass through it, but elastic shear waves do not or do so only very weakly.

of the cooling of the inner core, it is estimated that the current solid inner core formed approximately 2 to 4 billion years ago from what was originally an entirely molten core. If true, this would mean that the Earths solid inner core is not a primordial feature that was present during the planets formation, but a feature younger than the age of Earth (about 4.5 billion years).

However, this prediction was disconfirmed by observations indicating that in ct there is a degree of disorder within the inner core.

in the inner core seismological data. There is a model which explains this by differences at the suce of the inner core melting in one hemisphere and crystallization in the other.

A few years later, in 1940, it was hypothesized that this inner core was made of solid iron; its rigidity was confirmed in 1971.

The Earth was discovered to have a solid inner core distinct from its liquid outer core in 1936, by the seismologist Inge Lehmann,

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is named after Lehmann, this usage still can be found: see for example: . Greenwood Publishing Company. ISBN0-313–8.,and From here to hell, or the D layer, About.com

Based on the relative prevalence of various chemical elements in our solar system, the theory of planetary formation, and constraints imposed or implied by the chemistry of the rest of the Earths volume, the inner core is believed to consist primarily of a nickel-iron alloy known as NiFe: Ni for nickel, and Fe for ferrum or iron.

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any buoyant convection motions will have to be driven by variations in composition or abundance of liquid in its interior. S. Yoshida and colleagues proposed a novel mechanism whereby deformation of the inner core can be caused by a higher rate of freezing at the equator than at polar latitudes,

than pure iron or nickel, even under heavy pressures, it is believed that the core also contains enough gold, platinum and other siderophile elements that if extracted and poured onto the Earths suce it would cover the entire Earth with a coating 0.45 m (1.5feet) deep.

The temperature of the inner core can be estimated by considering both the theoretical and the experimentally demonstrated constraints on the melting temperature of impure iron at the pressure which iron is under at the boundary of the inner core (about 330GPa). These considerations suggest that its temperature is about .

The existence of the inner core also changes the dynamic motions of liquid in the outer core as it grows and may help fix the magnetic field since it is expected to be a great deal more resistant to flow than the outer core liquid (which is expected to be turbulent).

Seismologists have found that the inner core is not completely uniform,new york asian escort model but instead contains large-scale structures such that seismic waves pass more rapidly through some parts of the inner core than through others.

The structure of the EarthThe inner core of the Earth, its innermost part, is a primarily with a radius of about 1,220km (760mi), according to seismological studies.

Growth of the inner core is thought to play an important role in the generation of Earths magnetic field by dynamo action in the liquid outer core. This occurs mostly because it cannot dissolve the same amount of light elements as the outer core and therefore freezing at the inner core boundary produces a residual liquid that contains more light elements than the overlying liquid. This causes it to become buoyant and helps drive convection of the outer core.

and S. Karato proposed that changes in the magnetic field might also deform the inner core slowly over time.

Because the inner core is not rigidly connected to the Earths solid mantle, the possibility that it rotates slightly ster or slower than the rest of Earth has long been entertained.

If the inner core grows by small frozen sediments lling onto its suce, 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.

The pressure in the Earths inner core is slightly higher than it is at the boundary between the outer and inner cores: it ranges from about 330 to 360 gigapascals (3,300,000 to 3,600,000 atm).

. Journal of Statistical Mechanics: Theory and Experiment (iop) 2006 (12): . arXiv:cond-mat/0. . doi:10.1088/1742-5468/2006/12/P. or see preprints , .

In the 1990s, seismologists made various claims about detecting this kind of super-rotation by observing changes in the characteristics of seismic waves passing through the inner core over several decades, using the aforementioned property that it transmits waves ster in some directions. Estimates of this super-rotation are around one degree of extra rotation per year.

The ct that precious metals and other heavy elements are so much more abundant in the Earths inner core than in its crust is explained by the theory of the so-called iron catastrophe, an event that occurred before the first eon during the accretion phase of the early Earth.

(PDF). Earth and Planetary Science Letters (Elsevier) 195 (12): 9198. . doi:10.1016/S0012-821X(01)00568-4.

(This is about 70% of the length of the Moons radius.) It is believed to consist primarily of an iron, and to be about the same temperature as the suce of the Sun: approximately 5700K (5430C).

). Many scientists had initially expected that, because the solid inner core was originally formed by a gradual cooling of molten material, Core and continues to grow as a result of that same process, the inner core would be found to be homogeneous. It was even suggested that Earths inner core might be a single crystal of iron.

The solidity of the inner core had been difficult to establish because the elastic shear waves that are expected to pass through a solid mass are very weak and difficult for seismographs on the Earths suce to detect, since they become so attenuated on their way from the inner core to the suce by their passage through the liquid outer core. Dziewonski and Gilbert established that measurements of normal modes of vibration of Earth caused by large earthquakes were consistent with a liquid outer core.

. Journal of Geophysical Research (American Geophysical Union) 102 (B11): . . doi:10.1029/97JB02125.

Iron can be solid at such high temperatures only because its melting temperature increases dramatically at pressures of that magnitude (see the ClausiusClapeyron relation).

In addition, the properties of the inner cores suce vary from place to place across distances as small as 1km. This variation is surprising, 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 400km thick.

Recent claims that shear waves have been detected passing through the inner core were initially controversial, but are now gaining acceptance.

who deduced its presence from observations of earthquake-generated seismic waves that reflect off the boundary of the inner core and can be detected by sensitive seismographs on the Earths suce. This boundary is known as the Bullen discontinuity,

The Earths inner core is slowly growing as the liquid outer core at the boundary with the inner core cools and solidifies due to the gradual cooling of the Earths interior (about 100 degrees Celsius per billion years

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