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The Earth Story

@earthstory / earthstory.tumblr.com

This is the blog homepage of the Facebook group "The Earth Story" (Click here to visit our Facebook group). “The Earth Story” are group of volunteers with backgrounds throughout the Earth Sciences. We cover all Earth sciences - oceanography, climatology, geology, geophysics and much, much more. Our articles combine the latest research, stunning photography, and basic knowledge of geosciences, and are written for everyone!
We hope you find us to be a unique home for learning about the Earth sciences, and we hope you enjoy!
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Eudialyte syenite

Isn’t that a delightful color? The mineral with the strong color is Eudialyte, a fairly rare mineral found in igneous rocks with a unique composition. Eudialyte’s crystal structure has a number of rare elements in it, typically including zirconium and some of the rare earth elements, in addition to the silica species that make up the backbone of the mineral.

To form Eudialyte, the first step is concentrating zirconium, rare earth elements, and sodium in a molten rock. These concentrations are only commonly found in magmas that have crystallized a lot – molten rock generated by directly melting the mantle will be very dilute in those elements. Forming this mineral requires concentrating those elements by crystallizing out other components and removing them from the magma, concentrating elements that only form rare minerals like this one – sort of like distilling alcohol to higher concentrations (sometimes the magma will also exchange elements with the rocks that surround the magma chamber holding it, enhancing the concentrating effect).

Eudialyte also forms from magmas that are “silica undersaturated”, meaning they don’t have enough silicon in them to form quartz. There are too many other atoms – sodium, rare earth elements, zirconium, etc., in the magma to allow quartz to form.

In this rock, the Eudialyte is surrounded by feldspars, biotite, and aegirine, which require aluminum, potassium, and sodium to form, in addition to the silicon backbone. This rock was found in Brazil and formed as part of a slow-cooling magma with that interesting composition.

-JBB

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Island of the Rare Earths

In the 1700s, there was a mine on an island called Resarö, about 15 km north of Sweden’s capital city of Stockholm. At the time, the mine was pulling a type of feldspar out of the ground for making porcelain, useful for stoves and furnaces in Sweden. The mine was named for the local community, the Ytterby mine.

In 1787, a Swedish Army Lieutenant named Carl Axel Arrhenius who had a background in chemistry recognized that there was something odd about one of the dark black rocks at this site. He collected a sample of the rock, named it “ytterbite” since it was discovered at the Ytterby quarry and sent it off to several professors including Johan Gadolin at Åbo University.

Professor Gadolin isolated some components from the rock and realized that he was dealing with an element that had not been previously characterized. He named the compound “Ytterbia” and published its discovery as a newly-characterized element.

However, this rock was more complicated. Half a century later, another scientist named Carl Gustav Mosander worked on the same material and realized that there was more than 1 element t here. He was able to split the ytterbite into 4 different elements at the time, each with slightly different properties.

As this was before the periodic table of elements was created, they had no way of knowing that they were dealing with the Rare Earth Elements – the uppermost of the rows at the very bottom of the periodic table. These elements are very similar in their chemistry – they make the same type of ions and their sizes are only slightly different, so the elements follow each other quite well. The original ytterbite rock collected by Arrhenius was rich in all the rare earth elements; they just had to be isolated.

Eventually those four piles of elements were broken up again and a total of 10 different chemical elements were isolated from this single rock sample. Today, the legacy of this mine is buried within the names on the Periodic Table. Ytterbium comes directly from the name of the mine, and terbium, erbium, and yttrium were all split by Mosander. Gadolinium was later named for professor Gadolin, Holmium is named after Stockholm, and scandium and thulium were named after Scandanavia (Thule).

So, the next time you struggle to pronounce the name of one of the elements at the bottom of the periodic table, pause for a moment and think about Sweden. Our modern society uses those elements heavily in batteries and electronics, so they both made the electronics age possible and made a small part of it a little bit difficult for me to memorize.

-JBB

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Glowing Minerals

In 1852, George Gabriel Stokes noticed something unique in a sample of fluorite. When he held the mineral under UV light, it appeared to ‘glow’ a brilliant blue-violet colour. Stokes named this phenomenon fluorescence. Fluorescence is the ability of a mineral to temporarily absorb a small amount of light energy and then instantaneously release the energy again in the form of light. When a light ray with the correct wavelength (generally ultraviolet light, 10 – 400nm) hits the mineral, electrons in the mineral’s atomic structure absorb the light’s energy causing them to jump up an energy level. When the electrons fall back down an energy level they release the energy in the form of light. The colour that the mineral fluoresces depends on the wavelength of the energy released, but is often in the visible spectrum (400 – 700nm).

Fluorescence is caused by the presence of certain elements in a mineral’s chemical structure. Common fluorescence causing elements include tungsten, molybdenum, lead, boron, titanium, manganese, uranium, chromium, and some rare earth elements. These elements are called ‘activators’ and are usually present as impurities in the chemical structure. In very rare cases, pure minerals do fluoresce and these are called ‘self-activated’ minerals. Scheelite, powellite, and several uranium minerals have self-activated fluorescence. In some cases, crystal structure defects or organic impurities can also cause minerals to fluoresce. Interestingly, the presence of certain elements like copper or ferrous iron supresses fluorescence in minerals. These elements are aptly named ‘quenchers’.

Fluorite (pictured) is one of the most strongly fluorescent minerals, and produces a spectacular blue-violet glow under UV light. In fact, fluorite can fluoresce so strongly that in some samples it can be seen by viewing the sample outside on a bright sunny day. Yttrium, europium, or samarium impurities in the chemical structure is thought to be the cause of its fluorescence. Calcite can fluoresce many different colours depending on the impurities present. Lead and manganese cause pink or red fluorescence, uranyl ions cause green fluorescence, and mercury causes pink fluorescence under longwave UV and blue fluorescence under shortwave UV light.

Fluorescence can be used as an indicator of certain minerals. Several valuable gemstones like diamond, ruby, opal, kunzite, and scheelite display fluorescence. Prospectors have used this to their advantage by searching out these minerals from sedimentary deposits at night with UV lamps. In the dark, the brightly glowing minerals are much easier to pick out.

  • CD

Sources http://bit.ly/1xJDrk7 http://bit.ly/2vKyVGg http://bit.ly/1T1uLSC Dyar MD, Gunter ME, and Tasa D (2008) Mineralogy and Optical Mineralogy. Mineralogical Society of America, 708 pp, ISBN 978-0-939950-81-2

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Rare Earth Elements

Rare Earth Elements (REEs) consist of 17 elements on the periodic table. They are made up of the lanthanides (lanthanum, cerium, praseodymium, neodymium, promethium, samarium, europium, gadolinium, terbium, dysprosium, holmium, erbium, thulium, ytterbium, and lutetium), scandium and yttrium. This group is sometimes referred to as rare earth metals or rare earth oxides, due to the fact that they are usually sold as oxide compounds.

This group of elements have similar enough properties that they are often found together in the earth’s crust, and can often be difficult to separate from one another. Despite their name, they are not that uncommon in nature, just scattered. In fact, the rarest of the REEs is still 200 times more common than gold. However, large, concentrated deposits are difficult to locate, and are thus not easily extracted from the Earth.

Why do we wish to extract them in the first place? That device in your hand or in your pocket is made from metals or alloys containing REEs. With the advance of the mobile phone and other electrical devices, the demand for REEs have exploded in the last twenty or so years. Not only are they in computers, cameras, TVs and other common household equipment, they are also in green technology, such as wind turbines and electrical vehicle engines. They are also used in weaponry and other military technologies, such as night vision goggles.

The demand for these metals shows no sign of slowing down. As the average global GDP rises, so does the demand for REE-rich products. Currently, China supplies 97% of the world’s REEs, although there are efforts to mine REEs elsewhere in the world, particularly in Brazil, Russia and Australia.

-GG

Sources: http://bit.ly/1mJ36Gj http://bit.ly/2cioOgJ http://bit.ly/2cLN11j Previous posts: https://tmblr.co/Zyv2Js28WNz33 https://tmblr.co/Zyv2Js1kYFbvw Image: http://bit.ly/2cLMPiE http://bit.ly/2cUc2ts

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Rare Earth Elements: Not really rare

If you’ve paid attention to the popular press over the last few years, you’ve probably heard various stories about “Rare Earth Elements”. These elements, which I’ll abbreviate REEs from now on, have gained importance as applications have developed for them in high powered magnets, lasers, renewable energy generation, and other high-tech gadgets. The laptop I’m typing this on probably contains a fair amount of them, as does the smartphone sitting to my side.

Go find a periodic table; I’ll wait (http://webelements.com/). The REEs are found in one of those rows at the bottom of the periodic table; the row labeled the “lanthanides”. They are mostly heavy elements, with atomic weights between 57 and 70, and therefore also have large electron clouds around them. 2 other elements, Scandium and Yttrium, are generally included with REEs due to similar chemical properties. There are a number of unique properties of certain elements, such as low melting points, strong magnetic fields, and even radioactive decay that can make REE very interesting to scientists. They generally shrink from left to right across the row, so the properties of each element are a little different from the nearby elements.

REEs have been mined for industrial applications for decades. For a long time, the Mountain Pass mine in California’s Mojave Desert (just across the border from Nevada) was the worlds’ largest producer of REEs, and it appears in this photo. That changed, however, in the 1990’s, when production from mines in China began increasing.

That’s the general story of these elements. They’re called Rare, but they’re only sort of rare. There are lots of deposits of REEs around the globe, but many have only recently been recognized. For decades, there was really no need to evaluate these type of deposits; REEs were only used in rare applications and the price was generally low.

The real story of REEs is not that they’re rare, but instead that it’s really hard to get them. Almost all of them are more abundant than silver in the Earth, and Cerium (the most abundant REE) is actually more abundant than copper. The problem is they are only concentrated in certain stable phases and stay in those phases unless they are dissolved. Extracting them involves large amounts of caustic acids, which can both kill people and render areas uninhabitable if they’re spilled. The waste products can contain other heavy metals like barium, lead, and uranium, which can render water undrinkable.

The low REE price through the 1990’s and 2000’s was, to some extent, maintained by Chinese government policy. The Chinese production of REEs in the 1990’s ramped up so fast that the prices of the elements dropped, and in 2002 the Mountain Pass mine closed, unable to maintain profitability against Chinese competition. The country made a decision to support this industry decades ago and was willing to tolerate substantial pollution as a consequence.

Over the last decade, however, demand for REEs in products such as electronics, windmills, solar panels, and hybrid cars has grown substantially, and at the same time, in the late 2000’s there was a major price spike as China curtailed its own production to begin to deal with the environmental consequences. The main mine is close to the Gobi desert, so the nearby population is low, but dust and pollution from the mine can reach all the way to Beijing, across the entire country. Thus, supply suddenly became constricted just as demand was skyrocketing, leading to a price spike.

The environmental issues with REE mining are not confined to China. The Mountain Pass mine, for example, has had multiple wastewater spills during its lifetime that have contaminated surrounding areas, and releases dust that can impact communities including Las Vegas.

China was able to corner the market on REEs by tolerating these issues, but as pollution of their cities becomes an increasing problem, their willingness to tolerate the environmental impacts has declined. But, since the price has risen substantially, deposits that would not have been worth developing a few years ago have suddenly become economical.

For that reason, recent press reports have included reports of large, billions-to-trillions of dollar REE deposit finds, in environments such as the mountains of Afghanistan and the seafloor off the coast of Japan. Production has also recently restarted at the Mountain Pass mine in the U.S. And occasionally, people will even cite REE abundances as reason to begin mining asteroids.

Really though, these reports of huge amounts of money depend on the market price. If the market was flooded with REEs again from new production, as happened in the 1990’s, the price would plummet and the value of deposits in difficult to reach places like the ocean floor would drop as well. There are strategic reasons for countries to develop these resources as defense industries are heavy users of REEs as well, but readers should have some skepticism when a new trillion dollar valued find is discovered; that deposit is only worth trillions of dollars if prices don’t change upon the start of production, which they always do.

Demand for these elements is going to continue growing with time as countries transition to high-tech industries and move to renewable energy sources. These mines are the downside of that transition. They can be kept clean by strong regulation, but that costs money. For several decades, the Chinese population effectively subsidized the world by tolerating the pollution themselves, but that’s a situation which can’t continue forever.

New developments of REEs are going to come on line in the next few years, and as the price has skyrocketed, people have started looking for deposits they would otherwise have ignored. A few years ago, China had >50% of the world’s proven reserves of REEs, today that number has dropped to less than 25%, entirely because other countries have started actually looking for new deposits. But the downside is that, like much mining, this is a messy industry. It produces a lot of waste and the byproducts can be very toxic. Eventually, some balance will have to be struck between REE price, REE demand, and the technology of the industry to operate these mines safely and cleanly. REEs will become more important in the lives of people with time, but if nothing else, the problems with their extraction should be understood as well.

-JBB

Image credit: ELEMENTS Magazine: http://elements.geoscienceworld.org/content/8/5/369/F1.expansion.html

REE Mining and Exploration in North America: http://elements.geoscienceworld.org/content/8/5/369.full

Diversity of Rare Earth deposits: http://elements.geoscienceworld.org/content/8/5/361.full

Rare Earth Element mining at Mountain Pass: http://www.docstoc.com/docs/140923732/Rare-Earth-Mining-At-Mountain-PassWriting-A-New----Desert-Report

Congressional Research Service Report: http://www.fas.org/sgp/crs/natsec/R41347.pdf

REE In Afghanistan : http://www.scientificamerican.com/article.cfm?id=afghanistan-holds-enormous-bounty-of-rare-earths

TES article on REE’s on seafloor near Japan: http://tinyurl.com/d754vpq

Rare Earth Elements: Not So Rare http://technorati.com/politics/article/rare-earth-elements-not-so-rare/

Rare Earth Elements Not Rare, Just Playing Hard to Get http://blogs.smithsonianmag.com/science/2010/11/rare-earth-elements-not-rare-just-playing-hard-to-get

China's Ace in the Hole: Rare Earth Elements http://www.ndu.edu/press/chinas-ace-in-the-hole.html

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Japanese overcome against China’s stranglehold over rare earth elements!

Since the 1990s, China had a near monopoly over rare Earth metals. These rare Earth metals, such as europium (http://on.fb.me/14VqvLo), dysprosium, ytterbium, and terbium, are important in use for raw materials in hi-technologies & advanced weapon systems. Controlling nearly 97% of the global supply, China started restricting exports in 2009.

Japan, as the third largest consumer of these minerals, found the restriction of the exports as a call for urgency on finding their own source of these elements. They took immediate actions by dispatching their own team of marine scientists to explore the seabed of the Pacific Ocean for their own source of metals. Two years later in 2011, Japan hit the jackpot as they discovered a large quantity of the metals near Hawaii and Tahiti. Then again, last month near the same region of the first findings. The latest find is located in the deep-sea mud around the island of Minami-Torishima. It sits at 5.7 km below sea level.

Leading the team is Professor Yasuhiro Kato of Tokyo University. Professor Kato claims the extraction of the minerals to be a low costly venture. With just the use of pressurized air and a minimal disturbance of the seafloor, he believes that they can extract enough minerals to force China to lift their restrictions. Professor Kato will continue his research for the next two years.

Other countries such as the U.S. and parts of Europe are also building a case against China while also opening up their own mining explorations. The use of these metals can also extend out to green technology, health care, etc.

~era

Sources: [Japanese found metals in 2011] http://www.telegraph.co.uk/finance/commodities/8616623/Rare-earth-minerals-find-in-Pacific-could-spark-Japan-Hawaii-stand-off.html [Japanese Finds metal in March 2013] http://www.telegraph.co.uk/finance/comment/ambroseevans_pritchard/9951299/Japan-breaks-Chinas-stranglehold-on-rare-metals-with-sea-mud-bonanza.html [China’s announced restriction on exports] http://www.telegraph.co.uk/finance/china-business/8022484/China-blocked-exports-of-rare-earth-metals-to-Japan-traders-claim.html [Overall information] http://www.eaglespeak.us/2013/03/breaking-chinas-monopoly-japan-says-its.html

More info on the minerals from our page: http://on.fb.me/14VqvLo [Europium] http://on.fb.me/10HLPwB [Industrial mining]

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Island of the Rare Earths

In the 1700s, there was a mine on an island called Resarö, about 15 km north of Sweden’s capital city of Stockholm. At the time, the mine was pulling a type of feldspar out of the ground for making porcelain, useful for stoves and furnaces in Sweden. The mine was named for the local community, the Ytterby mine,

In 1787, a Swedish Army Lieutenant named Carl Axel Arrhenius who had a background in chemistry recognized that there was something odd about one of the dark black rocks at this site. He collected a sample of the rock, named it “ytterbite” since it was discovered at the Ytterby quarry and sent it off to several professors including Johan Gadolin at Åbo University.

Professor Gadolin isolated some components from the rock and realized that he was dealing with an element that had not been previously characterized. He named the compound “Ytterbia” and published its discovery as a newly-characterized element.

However, this rock was more complicated. Half a century later, another scientist named Carl Gustav Mosander worked on the same material and realized that there was more than 1 element t here. He was able to split the ytterbite into 4 different elements at the time, each with slightly different properties.

As this was before the periodic table of elements was created, they had no way of knowing that they were dealing with the Rare Earth Elements – the uppermost of the rows at the very bottom of the periodic table. These elements are very similar in their chemistry – they make the same type of ions and their sizes are only slightly different, so the elements follow each other quite well. The original ytterbite rock collected by Arrhenius was rich in all the rare earth elements; they just had to be isolated.

Eventually those four piles of elements were broken up again and a total of 10 different chemical elements were isolated from this single rock sample. Today, the legacy of this mine is buried within the names on the Periodic Table. Ytterbium comes directly from the name of the mine, and terbium, erbium, and yttrium were all split by Mosander. Gadolinium was later named for professor Gadolin, Holmium is named after Stockholm, and scandium and thulium were named after Scandanavia (Thule).

So, the next time you struggle to pronounce the name of one of the elements at the bottom of the periodic table, pause for a moment and think about Sweden. Our modern society uses those elements heavily in batteries and electronics, so they both made the electronics age possible and made a small part of it a little bit difficult for me to memorize.

-JBB

Image credits: https://flic.kr/p/91kyGh

http://bit.ly/1cwN5Av

Read more: http://bit.ly/1Pvq250

http://www.vanderkrogt.net/elements/rareearths.php

http://pubs.acs.org/doi/pdf/10.1021/ed078p1343

http://slate.me/1cwNumt

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