A Heidelberg-designed dust detector on Cassini space probe – ie cosmic dust analyser (CDA) – has identified several extremely rare and minuscule particles of interstellar dust from outside our solar system, and examined their chemical composition. Surprisingly it turns out that the different dust particles are very similar in composition and have collected the whole element mix of the cosmos. They suspect that dust is continually destroyed, reformed and thereby homogenised in the “witch’s cauldron” of outer space.
“Interstellar dust is one of the last bastions of the unknown in space, its individual particles being only about 200 nanometres in size and very hard to find,” explains Prof. Dr. Mario Trieloff, earth scientist from Heidelberg University. The dust is part of the interstellar material consisting of gas and helium, as well as heavy metals, and which can arise from the condensation processes of stars and planets. These particles are the raw material that were the main building blocks for Earth and other terrestrial planets.
The Stardust space probe was already able to capture particles of the very weak flux crossing our solar system. “But these particles were unusually large, so the research findings are possibly not representative,” Prof. Trieloff says. By contrast, Cassini probe could identify 36 particles of interstellar dust among millions of planetary dust particles. Furthermore the CDA is in a position to analyse them on the spot precisely with mass spectrometry.
Mass spectrometric measurements can now be made for the first time on “a statistically significant quantity of such dust particles.” This process had only become possible through a complex series of tests in Heidelberg to calibrate lab models of CDA. To achieve this aim, silicate dust had to be accelerated to ~40 km/s, roughly the speed of interstellar dust.
“The result of the measurements was truly amazing,” Dr. Postberg reports. “The 36 particles of interstellar origin, that are very similar in their composition, contain a mix of the most important rock-forming elements – magnesium, iron, silicon and calcium – in average cosmic abundance. Although a dust particle has a mass of less than a trillionth of a gram, the whole element mix of the cosmos is collected there, with the exception of very volatile gases. Such particles cannot be found in our solar system.” Most scientists had expected dust populations with different compositions, corresponding to the different processes of origin in atmospheres of dying stars. These differences are also found in the stellar dust of meteorites, which is highly individual in its isotope composition. “Our data tells a completely different story,” he underlines.
The dust has lost its individuality as it was homogenised. It contains gigantic, million-degree hot bubbles of supernova explosions, whose edges arise from shock fronts expanding at 100s of km/second. It is theorized interstellar dust can survive this energy-rich environment for only a few hundred million years and very few “lucky survivors” succeed in reaching newly forming planetary systems as intact stellar dust. Research now confirm most particles are destroyed and reformed in molecular clouds, i.e. cool, dense regions of outer space. Interstellar winds bring these particles as homogenised dust into our solar system. http://www.uni-heidelberg.de/presse/news2016/pm20160414_heidelberg-researchers-analyse-chemical-composition-of-dust-from-beyond-the-solar-system.html
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