Monthly Archives: June 2016

Today in Chemistry History – Emil Erlenmeyer’s Birthday

The Erlenmeyer flask is a piece
of glassware most of us have likely used at some point. The tapered sides and
narrow neck of this flask allow the contents of the flask to be mixed by
swirling, without risk of spillage, making them suitable for titrations. By
placing it under the buret and adding solvent and the indicator in Erlenmeyer
flask. Such features similarly make the flask suitable for boiling liquids. Hot
vapors condense on the upper section of the Erlenmeyer flask, reducing solvent
loss. Erlenmeyer flasks’ narrow necks can also support filter funnels.

As Compound Interest notes “The
Erlenmeyer flask’s popularity lies in its utility. Its flat base means it isn’t
easily toppled, unlike the round-bottomed flasks which can also be found in the
laboratory. Its tapered, cone-like shape, coupled with its narrow neck, means
that liquids inside it can be swirled without spilling easily. Additionally,
the sides minimise loss of liquids from the flask when they are heated, as
vapours condense on the sides. The narrow neck can also be plugged with a
rubber or glass stopper.”

Who was Erlenmeyer?

Erlenmeyer was the son of Dr.
Friedrich Erlenmeyer, a Protestant theologian. He enrolled in the University of
Giessen to study medicine, but after attending lectures of Justus von Liebig
changed to chemistry. In the summer of 1846 he went to Heidelberg for one year,
and studied physics, botany and mineralogy, returning to Giessen in 1847. After
serving as assistant to H. Will and then to Carl Remigius Fresenius, Erlenmeyer
decided to devote himself to pharmaceutical chemistry. For this purpose he
studied in Nassau, where he passed the state pharmaceutical examination, and
shortly afterwards acquired an apothecary’s business, first at Katzenelnbogen
and then in Wiesbaden. He became dissatisfied with pharmacy and returned to
chemistry, finishing his doctorate at Giessen in 1850.

In 1855 he moved to Heidelberg
and there converted a shed into a private laboratory. In 1857 he became
privatdocent and his habilitation thesis “On the manufacture of the
artificial manure known as superphosphate” contained a description of several
crystalline substances which greatly interested Robert Bunsen. It was while at
Heidelberg that Erlenmeyer was brought under the influence of August Kekulé,
whose theoretical views he was one of the first to adopt. He was the first to
suggest, in 1862, that double and triple bonds could form between carbon atoms,
and he made other important contributions to the development of theories of
molecular structure.

In 1863 he became associate
professor at the University of Heidelberg. In 1868 he was hired as full
professor in Munich to take charge of the laboratories of the new Munich
Polytechnic School, a post which he held until his retirement from teaching in
1883.

His work mostly focused on
theoretical chemistry, where he suggested the formula for naphthalene and
formulated the Erlenmeyer rule: alcohols in which the hydroxyl group is
attached directly to a double-bonded carbon atom become aldehydes or ketones.

Erlenmeyer’s practical
investigations were concerned mostly with aliphatic compounds. In 1859 he
synthesised aminohexoic acid and proceeded to study the general behaviour of
albuminoids on hydrolysis. He worked out methods to determine the relative
amounts of leucine and tyrosine, which are produced during the degradation of
several substances of this class, and was the first (1860) to understand the
nature of glycide and to suggest that this substance is related to glycerol in
the same way as is metaphosphoric acid to orthophosphoric acid. In the
following year he studied the action of hydroiodic acid on glycerol, and showed
that the product was isopropyl- and not propyl iodide. His investigations of
the higher alcohols produced during fermentation yielded the important proof
that these alcohols do not belong to the normal series.

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Ultra-thin slices of diamonds reveal geological processes

Diamonds are not only
beautiful and valuable gems, they also contain information of the geological
history. By using ultra-thin slices of diamonds, Dorrit E. Jacob and her
colleagues from the Macquarie University in Australia and the University of
Sydney found the first direct evidence for the formation of diamonds by a
process known as redox freezing. In this process, carbonate melts crystallize
to form diamond. The slices were prepared by Anja Schreiber of the GFZ German
Research Centre for Geosciences in Potsdam, Germany. The work is published in
Nature Communications. The study shows that the reduction of carbonate to
diamond is balanced by the oxidation of iron sulphide to iron oxides.

Siberia’s Udachnaya diamond mine, by Stepanovas (Stapanov Alexander). (Own work) [GFDL (http://ift.tt/KbUOlc) or CC-BY-SA-3.0 (http://ift.tt/gc84jZ)%5D, via Wikimedia Commons
The researchers used the new
nano-scale technique of Transmission Kikuchi Diffraction to discover rims of
the iron oxide mineral magnetite just a few ten thousandths of a millimetre
thick around sulphide minerals inside the diamonds. The GFZ’s Anja Schreiber
prepared these slices using a focussed beam of charged atoms (ions) to ablate
the surface. The already ultra-thin slices were re-thinned after being mounted
on a carbon-coated copper grid. This process was carried out for the first time
successfully on a grid and yielded the data set used for the study.

The results also solve a
puzzle that has occupied diamond researchers for decades, namely the
over-abundance of sulphide occurring as inclusions in diamond. Iron sulphides
are the most common inclusions in diamond even though there is only about 0.02%
of sulphur in the mantle: it now appears that the oxidation of the iron
sulphides directly causes the formation of the diamonds that include them.

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Dagger in Tutankhamun’s tomb was made with iron from a meteorite

A dagger entombed with King Tutankhamun was made with iron from a meteorite, a new analysis on the metal composition shows.

In 1925, archaeologist Howard Carter found two daggers, one iron and one with a blade of gold, within the wrapping of the teenage king, who was mummified more than 3,300 years ago. The iron blade, which had a gold handle, rock crystal pommel and lily and jackal-decorated sheath, has puzzled researchers in the decades since Carter’s discovery: ironwork was rare in ancient Egypt, and the dagger’s metal had not rusted.

Italian and Egyptian researchers analysed the metal with an x-ray fluorescence spectrometer to determine its chemical composition, and found its high nickel content, along with its levels of cobalt, “strongly suggests an extraterrestrial origin”. They compared the composition with known meteorites within 2,000km around the Red Sea coast of Egypt, and found similar levels in one meteorite.

That meteorite, named Kharga, was found 150 miles (240km) west of Alexandria, at the seaport city of Mersa Matruh, which in the age of Alexander the Great – the fourth century BC – was known as Amunia.

The researchers published their findings on Tuesday in the journal Meteoritics & Planetary Science.

Although people have worked with copper, bronze and gold since 4,000BC, ironwork came much later, and was rare in ancient Egypt. In 2013, nine blackened iron beads, excavated from a cemetery near the Nile in northern Egypt, were found to have been beaten out of meteorite fragments, and also a nickel-iron alloy. The beads are far older than the young pharaoh, dating to 3,200BC.

“As the only two valuable iron artifacts from ancient Egypt so far accurately analysed are of meteoritic origin,” the team that studied the knife wrote, “we suggest that ancient Egyptians attributed great value to meteoritic iron for the production of fine ornamental or ceremonial objects”.

The researchers also stood with a hypothesis that ancient Egyptians placed great importance on rocks falling from the sky. They suggested that the finding of a meteorite-made dagger adds meaning to the use of the term “iron” in ancient texts, and noted around the 13th century BC, a term “literally translated as ‘iron of the sky’ came into use … to describe all types of iron”.

“Finally, somebody has managed to confirm what we always reasonably assumed,” Thilo Rehren, an archaeologist with University College London, told the Guardian.

Rehren, who studied the nine meteoritic beads, said “there never has been a reason to doubt this outcome but we were never really able to put this hard data behind it”.

He added that other objects from Tutankhamun’s tomb, including jewelry and miniature daggers, are believed to made from meteorite iron.

“Yes, the Egyptians referred to this stuff as metal from the heaven, which is purely descriptive,” he said. “What I find impressive is that they were capable of creating such delicate and well manufactured objects in a metal of which they didn’t have much experience.”

An iron meteorite, by James St. John (Flickr: Murnpeowie Meteorite) [CC BY 2.0 (http://ift.tt/o655VX)%5D, via Wikimedia Commons

The researchers wrote in the new study: “The introduction of the new composite term suggests that the ancient Egyptians were aware that these rare chunks of iron fell from the sky already in the 13th [century] BCE, anticipating Western culture by more than two millennia.”


Egyptologist Joyce Tyldesley, of the University of Manchester, has similarly argued that ancient Egyptians would have revered celestial objects that had plunged to earth.

“The sky was very important to the ancient Egyptians,” she told Nature, apropos of her work on the meteoritic beads. “Something that falls from the sky is going to be considered as a gift from the gods.”

The high quality of the blade suggests that Tutankhamun, who lived during the latest stage of the Bronze Age, was supported by ironworkers who were skilled despite the relative rarity of the material.

The blade may not be the only item derived from falling rocks on Tut’s person.

In 2006, an Austrian astrochemist proposed that an unusual yellowish gem, shaped as a scarab in King Tut’s burial necklace, is actually glass formed in the heat of a meteorite crashing into sand.

“It would be very interesting to analyse more pre-Iron Age artifacts, such as other iron objects found in King Tut’s tomb,” Daniela Comelli, of the physics department at Milan Polytechnic, told Discovery News. “We could gain precious insights into metal working technologies in ancient Egypt and the Mediterranean.”

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Rosetta’s comet contains ingredients for life

Ingredients crucial for the origin of life on Earth, including the simple amino acid glycine and phosphorus, key components of DNA and cell membranes, have been discovered at Comet 67P/Churyumov-Gerasimenko.

The possibility that water and organic molecules were brought to the early Earth through impacts of objects like asteroids and comets have long been the subject of important debate.

While Rosetta’s ROSINA instrument already showed a significant difference in composition between Comet 67P/C-G’s water and that of Earth, the same instrument has now shown that even if comets did not play as big a role in delivering water as once thought, they certainly had the potential to deliver life’s ingredients.

ESA/Rosetta/NAVCAM, CC BY-SA IGO 3.0 [CC BY-SA 3.0-igo (http://ift.tt/1wBCVB0)%5D, via Wikimedia Commons
While more than 140 different molecules have already been identified in the interstellar medium, amino acids could not be traced. However, hints of the amino acid glycine, a biologically important organic compound commonly found in proteins, were found during NASA’s Stardust mission that flew by Comet Wild 2 in 2004, but terrestrial contamination of the collected dust samples during the analysis could not be ruled out. Now, for the first time, repeated detections at a comet have been confirmed by Rosetta in Comet 67P/C-G’s fuzzy atmosphere, or coma.

The first detection was made in October 2014, while most measurements were taken during the perihelion in August 2015 – the closest point to the Sun along the comet’s orbit while the outgassing was strongest. “This is the first unambiguous detection of glycine in the thin atmosphere of a comet,” says Kathrin Altwegg, principal investigator of the ROSINA instrument at the Center of Space and Habitability of the University of Bern and lead author of the study. The results are now being published in Science.

Glycine is very hard to detect due to its non-reactive nature: it sublimates at slightly below 150°C, meaning that little is released as gas from the comet’s surface or subsurface due to its cold temperatures. “We see a strong correlation of glycine to dust, suggesting that it is probably released from the grains’ icy mantles once they have warmed up in the coma, perhaps together with other volatiles,” says Altwegg. At the same time, the researchers also detected the organic molecules methylamine and ethylamine, which are precursors to forming glycine. Unlike other amino acids, glycine is the only one that has been shown to be able to form without liquid water. “The simultaneous presence of methylamine and ethylamine, and the correlation between dust and glycine, also hints at how the glycine was formed,” says Altwegg.

Another exciting detection by ROSINA made for the first time at a comet is of phosphorus. It is a key element in all living organisms and is found in the structural framework of DNA and RNA.

“The multitude of organic molecules already identified by ROSINA, now joined by the exciting confirmation of fundamental ingredients like glycine and phosphorus, confirms our idea that comets have the potential to deliver key molecules for prebiotic chemistry,” says Matt Taylor, Rosetta project scientist of the European Space Agency ESA. “Demonstrating that comets are reservoirs of primitive material in the Solar System, and vessels that could have transported these vital ingredients to Earth, is one of the key goals of the Rosetta mission, and we are delighted with this result.”

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The above post is reprinted from materials provided by University of Bern. Note: Materials may be edited for content and length.

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