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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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Dragon rock Hivitserkur is a 15 metre high volcanic plug, the eroded remains of magma frozen on its way up a volcanic conduit towards the vent at the surface. Located in Iceland's Gulf of Hunafloui, it resembles a grazing dragon or dinosaur. The local legend says that it is a frozen troll, caught by the rising sun on its way to raid a nearby abbey. The name means white shirt, and comes from the guano stains from fishing birds running down it. The foundations were shored up with concrete to save the monument from the Atlantic ocean. Loz Image credit: Stephan Rebernik http://ourworldinpictures.net/world/223-icelandic-dinosaur-hvtserkur.html http://www.mymodernmet.com/profiles/blogs/hvitserkur-dinosaur-rock http://www.atlasobscura.com/places/hvitserkur

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The secrets of Roman concrete

This building is nearly 2000 years old. The structure you’re looking at is Trajan’s market in the city of Rome, built around 100 a.d. The presence of structures like this one nearly two millennia later is a testament both to Roman engineering skills and to the concrete they used in constructing their empire.

Even in modern construction, concrete exposed to the elements or the ocean often does not survive as well as Roman concrete. New research led by a team from UC Berkeley makes an effort to explain why that is the case.

They took a core of Roman concrete found just offshore in the Bay of Naples and subjected it to modern analytical techniques, going down to the atomic structure to see where every atom was sitting. In a paper just published in the journal American Mineralogist, they identify a specific atomic structure that might make all the difference, one called Al-tobermorite.

In traditional concretes, a key part of the mixture is a calcium-silicate-hydrate “glue”, a mixture of elements that hardens and binds together the sand and gravel used in the mix. Other modern mixtures will include an additional component – alumina, which adds strength to the mix.

This mixture, C-A-S-H, has all the ingredients and a similar molecular formula to the Al-tobermorite found in Roman concretes but it doesn’t form the same mineral. Experiments showed that this tobermorite mineral can only be produced in modern concretes if they are heated to over 100 °C, which typically does not happen during construction. Thus, Roman construction achieved a mineral that strengthened their concretes against alteration and weathering to a degree uncommon in modern concrete.

The main ingredients of the Roman concrete were pyroclastic ash and rock taken from the Plegrean fields near Naples and Mount Vesuvius along with coarser grained aggregate and pumice from the surrounding area. These particles were mixed with calcium oxide (lime) from other areas around Rome and then submerged in seawater.

Descriptions from Roman writers cited in the paper suggest that when this mixture was immersed in seawater, it would heat up on its own from an exothermic reaction between the ingredients (the reaction between lime and water).

The final trick for Roman construction noted by the authors was that it took place on a large scale. Without active systems to remove heat, Roman concretes would have taken years to cool completely after they were set, and the larger buildings would have heated from this reaction to a greater degree. The size of Roman construction therefore could have helped trap heat in, allowing high enough temperatures for the Al-tobermorite reaction to take place, and developing that mineral seemingly added strength and longevity to their concrete products.

This research sheds some new light on the source of the longevity in Roman structures and may eventually lead to application of some of these techniques in modern construction as well.

-JBB

Image credit: Alessio Nastro Siniscalchi http://en.wikipedia.org/wiki/File:Traiano_mercati.jpg

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reblogged

Geologists Make Stupid Jokes and Steven Universe Fans Can't Handle It

My brother is a geology major and apparently all geologists make the same joke when they see asphalt or concrete and refer to it as"Urbanite" (a parking lot is an urbanite deposit)

Me, being a Steven Universe fan, really wants to see someone design a gem based on that joke….

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earthstory

I always use anthropomorphite.

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Moon Hill

Moon Hill is a mountain with a natural arch just outside of Yangshuo in southern China. It is named for a wide almost perfect semicircular hole in the hill. The hole is approximately 50 meters wide and 50 meters tall. It is all that remains of what was once a limestone cave.

The area is known for its karst formations and is made up of compact carbonate rocks which became uplifted and transformed by erosion. The rocks started out as sea floor sediments and were pushed up during the collision of India with Asia. Afterwards, the warm and wet Monsoon climate of southern China created the well-known karst formations we can see today. The naturally-occurring acid rains of Yangshuo’s subtropical climate caused the dissolution of limestone and caused caves and sinkholes to form.

Moon Hill has a concrete path passing through the arch and several rock climbing routes. It also offers great panoramic views of the surrounding knobby karst hills found throughout the region.

Xandi Image Credits: http://bit.ly/2mXUOxS http://bit.ly/2mFLe0A Sources: http://bit.ly/2n4xVdJ http://bit.ly/2n4iRN9

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This is rather awesome and a bit depressing. The Los Angeles River used to be a wild, ephemeral river - moving across a large floodplain as it flowed from the mountains north of L.A. to the Pacific Ocean. However, a migrating river doesn’t work well in an urban area of 10 million inhabitants and in the 1930s the river was almost entirely paved. You’ve seen it in a variety of movies, I promise. Today, the river still flows in these concrete channels, built with levees to prevent flooding of the nearby structures. This video explores aerial views of that concrete river, including both dry and flowing sections.

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The Greenest Street in America of 2013

The verdict is in and as of April 1st 2013, Cermak Road in Chicago, IL is named the greenest street in America. What makes this road so green? Well, its ability to be a self-sustaining and sufficient road is what puts it ahead of the competition. As part of a big effort to working towards a better future, the Windy city jump-started a $14 million project in redoing the industrial Pilsen neighborhood. Not only did they prove that it can be done in such a busy area but they were able to do it with a smaller budget than a traditional road-resurfacing project along with the expectancy of a lower cost for future maintenance.

Fed up with waiting for the federal government to take action, Chicago decided to take the matter in their own hands. The Chicago Department of Transportation (CDOT) has chosen Cermak Road and Blue Island Avenue in the Pilsen neighborhood because of its busy industrial environment and for its frequent visit from trucks. Those challenging factors made the two streets the ideal situation for the new project to tackle. The project targeted on reducing waste, energy, smog, cost, and run offs. It also inspired major innovation and unique ideas such as the smog-eating pavement.

The smog-eating paving was developed by an Italian company called, Italcementi, and its main use was to protect the Catholic churches from the growing pollution in Rome. The Catholic churches are typically white and if exposed enough to the smog, it will turn dark and dirty. This cement, TioCem, is made up of titanium dioxide and it reacts with the Sun’s UV light to produce OH, which reacts with the Nitrogen Dioxide in the air. The Nitrogen Dioxide reacts with the hydroxide and forms Nitrogen Oxide, which then lays dormant in the cement until it is dissolved by water. Unfortunately, TioCem is more costly than the traditional pavement, but Chicago is determined to use it in practice. They laid down a thin layer of TioCem on the road for bicycle and parking lanes.

Here are some other ways that made Cermak Road the greenest street in America in 2013:

· Streetlights are run by solar and wind power.

· Plants and trees are planted to capture more carbon dioxide.

· The sidewalks are made of recycled concrete.

· More bicycle lanes are added to encourage more people to ride bikes and to cut down on emissions.

· More trees, shrubs, and grasses are being planted to form a bioswales, which help prevent the rainwater from overfilling the sewer system.

~era

Photo Courtesy of CDOT

References: http://phys.org/news/2013-04-smog-eating-pavement-greenest-street-america.html http://www.ases.org/smog-eating-pavement-on-chicagos-greenest-street-in-america/ http://www.smartplanet.com/blog/bulletin/chicago-debuts-smog-eating-street/3284 http://www.heidelbergcement.com/NR/rdonlyres/7DEA23C8-7023-46FD-8BEE-5AA11CF4FC33/0/Sonderdruck_TioCem.pdf http://www.picada-project.com/domino/SitePicada/Picada.nsf?OpenDataBase

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Anonymous asked:

Hello, Can the sand produced in the Grand Canyon be used for construction? Thanks, Nathalie

Sand, particularly river-transported sand, is a key component of concrete. Basically in concrete you take something solid, sand grains, and add something that solidifies and holds them together. It doesn’t matter as much what the sand grains are made of as it does that they’re angular, broken up sand grains.Sand in the Colorado River is picked up from mountains in Colorado and the plateaus in Arizona and Utah as it winds its way down the river. Today, most of the sand carried from Colorado is getting dumped at the start of Lake Powell, gradually forming a delta where the river flow slows down. Some additional sand enters the Grand Canyon in the tributary channels below lake Powell, including the Little Colorado River. A few years ago, the US opened the floodgates on the Glen Canyon Dam to stir this sand up, allowing it to reform sand bars in the Grand Canyon area - an environment important to life there.So the Grand Canyon and the Colorado system has plenty of sand. It’s the kind of sand useful in making concrete, but getting it out of there would be difficult as you have to lift it up a mile-deep canyon and that’s more than a little expensive. Sand in a mountain setting like the Colorado Plateau is probably fairly poorly sorted, so it would be useful in concrete but it isn’t that useful in fracking, which is currently one of the main uses of sand in the eastern US (much of that comes from Wisconsin - https://tmblr.co/Zyv2Js1Znr1CV). You could also in theory dredge that sand and use it to fill in an eroded beach, but the Grand Canyon is pretty far from beaches. 

Between there not being a lot of construction in the Grand Canyon area, the presence of other sand sources in most areas of the US, the difficulty of getting it out, the fact that the sand isn’t going to be that pure/well sorted and thus can’t be used for everything, and the fact that it is a national park and people like me will get really annoyed if you mess with it, there’s plenty of reasons why it wouldn’t be used for that. But in theory, probably could be.For more, here’s a worth-reading Wired piece on sand mining around the world from last year: http://www.wired.com/2015/03/illegal-sand-mining/

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The Creeping Imperial Fault

Southeast of the Los Angeles basin and due East from San Diego lies California’s Imperial Valley. It is heavily irrigated, as you see from the small irrigation ditch featured in this photo. The land is quite flat and has been filled in with sediment from the Colorado River. Thanks to irrigation channels leading from the Colorado, the area has become a rich area for growing plants and vegetables.

But, many unseen geological features lurk beneath the surface of the Imperial Valley. The San Andreas Fault enters the northwestern tip of this Valley, but then breaks off into a couple different segments along the coastline of the Salton Sea. South of the Salton Sea, the fault reorganizes into a system that travels into Mexico known as the Imperial Fault.

In this photo of what appears to be a simple Imperial Valley irrigation ditch, you’ll notice that the concrete has cracked and there are plants growing through the concrete along these fractures.

This irrigation ditch sits directly atop of the Imperial Fault. This picture was taken from the “North American” plate side of the fault, looking across at the Pacific plate, so the land to the top of this image is moving to the right relative to the viewer (the San Andreas system being a right-lateral fault).

The fault hasn’t had a major earthquake since a magnitude 6.4 event in 1979, which happened before this channel was built, but it’s still there and still slowly creeping. Concrete doesn’t handle shear stress very well, so here it’s cracking due to that slow motion. The Fault hasn’t had large motions since 1979, but it still creeps along, allowing very subtle motions to take place while the stress builds up that will eventually drive a larger earthquake.

This fault also offsets a nearby rail line and telephone poles, some of which were built before the 1979 quake and are offset by a meter or more. There is also, for some reason, a buried high pressure gas line at this location.

-JBB

Image credit: Me, image owned by the author of this post.

1979 Earthquake details: http://www.data.scec.org/significant/imperial.html

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Major flooding in Chennai

The City of Chennai on the eastern coast of India is, by population, the 4th largest urban area in the country and the 36th largest urban area in the world. Like the rest of the city, its airport has undergone major expansion over the past 15 years. However, as of right now, that airport is a lake.

This photograph was taken by an Indian Air Force helicopter surveying the damage to the area after a hundred-year rain event brought 50 cm of rain (half a meter/a foot and a half) in only two days following a month of November that featured 3x the typical rainfall for that month.

At present, no casualty estimates are available from the most recent rainfall, although reports from November established 269 deaths throughout the surrounding province associated with weather and flooding.

These floods in Chennai serve as an example of the type of disaster that can follow rapid urbanization in a small area. The Adyar River runs through the heart of this city and there is a long historic record of floods in this area associated with typhoons and other severe rain events (as could also be triggered by the yearly Monsoon, combined with this eyar’s record breaking El Niño). However, the former river system has been dramatically altered by construction.

For example, a large marshland used to sit at the mouth of this river, where it reached the Bay of Bengal. Marshlands commonly can hold large amounts of water; protecting marshlands along river shores is a common method of limiting the impact of floods. However, over 90% of the area once occupied by that marshland is now developed.

Urbanization also makes floods worse on its own. When heavy rainfall strikes an undeveloped region, some portion of the rainfall is absorbed by the soil and can even recharge local groundwater. However, urban areas typically have their soils covered by roads and buildings that are impermeable. Water that used to absorb into soil instead is forced to run over the surface by paved surfaces, forcing even more water into surface channels. If systems aren’t built to handle the extra water, urbanization therefore will make the flooding after a large rainstorm dramatically worse.

On top of that, if storm drains aren’t regularly kept clear of debris, even existing storm sewers may not be able to do their job, and local reports say this has been an issue in the Chennai flooding as well.

It’s possible to deal with some of these issues using modern green building techniques and construction of flood maintenance systems, but those cost money and in rapidly urbanizing countries the money to build adequate systems is commonly not available. The city of Chennai has years of reports stating that its development was increasing flood risk, but development has continued with limited response to those reports.

Perhaps the best example of the interaction between urban planning and flooding I can give goes back to this airport. This airport is literally a concrete strip built directly on the river’s floodplain. It is so integrated with the river that one runway of the airport literally crosses the river using a bridge. Building an airport on that site basically requires that the airport is going to regularly flood, and systems have to be built that can deal with those floods. Otherwise, thousands of people will have to be evacuated, as reportedly happened at the Chennai airport during this flood.

-JBB

Image credit: Indian Air Force/MIB India https://twitter.com/MIB_India/status/672328771123339264

References: http://bit.ly/1lYBSx1 https://twitter.com/maitri/status/672237294204510209 http://bit.ly/1m05JFk http://bit.ly/1lwcXAs http://apne.ws/1XL6EFl http://bit.ly/1MW8eRS

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An urban flood

The Blanco River runs through central Texas and was one of the worst parts of the disastrous floods that hit the state this week, with 3 people confirmed dead and 9 others currently missing after that river broke through its banks.

A disaster like this has many different stories to tell. The rainfall amounts in Texas recently are enormous and solid cases can be made linking them to both a developing El Nino event and climate change (directly linked through unusually warm waters in the Gulf of Mexico and the Pacific Ocean). However, in this post I’m going to focus on an issue we have more direct control over: development.

Human development makes floods worse. That’s a strong statement and it is very well scientifically supported – in fact you can go outside and do the experiment yourself. Take 2 pitchers of water, pour one on some open grass, and pour another on a paved surface. The water poured on the grass may flow for a little bit, but eventually it’s going to enter the soil. On the other hand, none of the water poured on a paved surface will enter the soil at first. It will flow downhill until it reaches a trap: a storm drain or a low spot nearby.

Now look around and ask, “how much of the surface area around me is paved?” That includes building roofs, streets, sidewalks, parking lots, etc. In undeveloped areas, the ground surface is generally “permeable” meaning rainwater can infiltrate into the soil and move downwards. Paved surfaces on the other hand are mostly impermeable; water must flow over them and cannot penetrate downwards.

Even a moderately developed area can see the amount of impermeable surface increased to 25% just by roads and buildings, but in urban city cores the amount of impermeable surface can top 90%. When a surface is made impermeable, rainwater is either concentrated in area that is permeable or it is pushed into manmade storm drains; the capacity of both can easily be overwhelmed in a large rain event. A paved city with 10% permeability has to find a place to put 90% of the rain that falls on it; otherwise the end result will look like this photo.

Paving surfaces isn’t the only part of development that impacts flooding; wetlands have a large capacity to absorb floodwaters and prevent damage downstream, but people can develop wetlands as farming and riverfront property. Soils generally have good infiltration rates, but farming practices can also reduce those, further increasing storm runoff. Finally, developing in floodplains puts people’s lives and property directly at risk since they’re living in those areas.

The Blanco River is outside of Austin, Texas, one of the fastest growing urban areas in the United States. The population of the county where the most severe flooding occurred has literally doubled within less than a decade – it is rapidly urbanizing. This not only puts more people at risk from the same flood, it will make floods worse. This rainstorm would have still caused major flooding throughout Texas, but every few centimeters of water height at the peak of the flood winds up causing more damage and putting more people in jeopardy.

The end result of this problem can’t be “don’t build cities” because people do want to live places. Instead, there are a variety of other solutions to these issues. Many cities are developing flood control infrastructure – large reservoirs or open spaces where storm drain overflow can be pushed during a storm. Chicago, for example, has developed a system to use a gigantic open-pit limestone mine on the city’s south side as a location where storm overflow can be pushed during a storm to limit major flooding.

Other types of green infrastructure can help too. Small things, such as rain barrels that collect water off of roofs, can make a difference if they’re deployed over a large area. Green infrastructure can help too – designing parks or landscapes such that water can enter the ground and migrate slowly downhill within them rather than pouring rapidly over the surface and into flooding rivers can reduce the peak flood magnitudes.

However, that topic brings us back to Texas, because those projects cost money. Texas in general puts very few restrictions on development and thus does not have organized plans to deal with these risks. Major cities may have some flood control measures, but the state does not fund flood control infrastructure development and there is no plan for managing floodplains or limiting development in at-risk areas. A single city can only do so much if the floodplain upstream is developed.

The state has several thousand dams that can help limit flooding, but many of them are privately owned and not regularly inspected. On those that are managed by the state, quality control is low due to high costs and an average of 4 fail per year. As a consequence, when these types of storms hit Texas, the damage they do is maximized – people are permitted to develop on floodplains and that development both makes the flood worse and puts more people at risk.

The U.S. Government manages the National Flood Insurance program as private insurers pulled out decades ago when they were unable to assess flood risks. Outside of large events such as Hurricane Katrina, Texas is the leader in receiving flood damage payments per year. Furthermore, when a huge disaster like this storm strikes, Texas will receive disaster response and rebuilding assistance from the federal government as well.

Because of these policies, the people who live in the flood plains are put at risk and the U.S. taxpayer is put at risk, but that alone will not be enough to lead to more sensible development or integrated flood-control policies.

-JBB

Image credit: Drew Anthony Smith/Getty Images http://huff.to/1AybaBw

Read more/References: http://t.co/8OtIYbIec5 https://www.hcfcd.org/ http://bit.ly/1AyGeB4 http://bit.ly/1Q8QgdW http://nyti.ms/1AyGjVo http://on.mash.to/1HwSlfk http://nyti.ms/1cjOU2C

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The International Year of Soils 2015 has been declared the International Year of Soils (IYS) by the United Nations General Assembly. Governments and organizations around the world will join together to increase global awareness about the importance of soils, and the need to protect them from degradation. We tend to associate soils with agriculture, but we also depend on them to cycle nutrients, sequester carbon, provide habitat for a quarter of Earth’s biodiversity, and supply clean water. They can even be used as a building material, such as mud homes and clay bricks. Unfortunately, soils are a finite resource, meaning we don’t have an endless supply. They are considered nonrenewable on a human timescale; requiring more than a lifetime to form. Soil scientists say that it takes an average of 100 years to get 1 millimeter of new topsoil, although the actual rate depends on parent material (rock, ash, peat, etc.), topography, climate, and the organisms present. Bottom line, it takes longer for new soils to form than it does for humans to destroy them using common agricultural and construction practices. Estimates state that we are losing soils 10 to 40 times faster than they are created, even as human populations, and the corresponding demand for land and crops, are increasing. Most of the losses come from accelerated erosion due to disruption of the protective vegetative cover. We are also polluting our soils, covering them with concrete, and reducing the productivity of croplands through overuse.  Only a fraction of all soils are suitable to meet human needs, and civilizations have reportedly fallen because their land became too degraded to grow food. IYS aims to raise awareness about the way we depend on soils, and about how we are using, or even abusing, them, so we’ll do more to protect the soils we depend on. - RE Photo Credit: "Dead Sea Coastal Erosion March 2012" by Wilson44691 http://en.wikipedia.org/wiki/Erosion#mediaviewer/File:Dead_Sea_Coastal_Erosion_March_2012.JPG Read More:  http://www.fao.org/soils-2015/en/ https://www.soils.org/iys http://www.nrcs.usda.gov/wps/portal/nrcs/site/national/home/ http://www.globalchange.umich.edu/globalchange2/current/lectures/land_deg/land_deg.html

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Diverting Lava Flow. It may seem like something out of a bad Hollywood Movie, think "Volcano", but in 1992 a Hollywood style village rescue occurred on the slopes of Mt Etna. Volcanologists, with the aid of the military used concrete blocks (thrown into the lava from helicopters) to attempt to divert the flow away from Zafferana, a local village on the slopes of the Volcano. But before the concrete blocks were used, an “Earth Barrier” was constructed, 21m high and over 230m long, it managed to contain the lava for around about a month, before the flow breached the embankment on the 9th April 1992. 3 Smaller barriers were built to gain time whilst volcanologists “figured out a plan”. Their plan was to block the channels, by blasting the solidifying lava flows, as well as dropping concrete blocks into the flows. This still didn't quite work, and the lava front was still advancing towards Zafferana. Finally a successful plan was hatched, between the 27th and 29th May 1992 an artificial channel was dug coming away from the lava flow, and the natural dam between them blasted away, the result was that two thirds of the lava ended up flowing into to artificial channel, and Zafferana was saved, although the flow was stopped only 850m from the village. To read more head to the links below -LL Image by Martin Rietze Links; http://news.bbc.co.uk/2/hi/europe/676327.stm http://www.slideshare.net/whiskeyhj/case-study-volcanic-eruption-mt-etna http://www.photovolcanica.com/VolcanoInfo/Etna/Etna.html

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