What is a chondrule? How do we know they were not formed by the ambient heat of the solar nebula?

Short Answer

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Chondrules are small, spherical rocks found in meteorites mainly consisting of silicate minerals. They were not formed by the ambient heat of the solar nebula due to the higher temperature required for their formation (up to 2000 K), their glassy structure and rapid cooling, which is inconsistent with the lower temperature and slow cooling rate of the solar nebula.

Step by step solution

01

Definition of Chondrule

A chondrule is a round grain found in a meteorite. They are between 0.1 and 10 mm in diameter and are typically composed of silicate minerals, principally olivine and pyroxene.
02

Contrasting Chondrule Formation to the Solar Nebula Hypothesis

Chondrules are believed to have formed by flash heating of dust particles in the protoplanetary disk surrounding the young Sun. This process must have reached temperatures up to 2000 K to cause the silicate to melt and subsequently cool, a temperature significantly higher than the ambient temperature of the solar nebula, which was lower and not sufficient to melt silicate (below 1500 K). In addition, the crystal structure of chondrules indicates that they were rapidly cooled, on the order of hours to days, which is inconsistent with the slow cooling rate at the ambient temperature of the solar nebula.
03

Acceptance of Chondrule Formation Theory

Even though the exact process of chondrule formation remains unclear, the high-temperature, short-duration flash heating event hypothesis is widely accepted in the scientific community and is strongly evidenced by characteristics of chondrules.

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