Carbon Cycle

Carbon is part of the oceans, air, rocks, soil, and all other living things. It is always moving from place to place. Carbon moves from the air to plants. In the atmosphere, carbon is attached to oxygen in the form of carbon dioxide. With the process of photosynthesis, the plants use the carbon dioxide and sunlight to make food for it. Then the carbon moves from the plants to the animals. It moves to the animals when they eat the plants. Animals that eat other animals get carbon from the animals that eat the plants. When the plants and animals die, their bodies decay and bring the carbon into the ground. Some animals, buried deep underground, form fossil fuels after millions of years. Carbon also moves from living things into the atmosphere. Every time people exhale, carbon dioxide gas is released into the atmosphere. Carbon moves from fossil fuels to the atmosphere when the fuels are burned. When the fuels are burned, they return to the atmosphere as carbon dioxide gas once again.  Carbon dioxide is moved from the atmosphere to the oceans. The oceans and other bodies of water pick up carbon from the atmosphere when it rains and also through absorption.

 

http://www.windows2universe.org/earth/Water/co2_cycle.html,

November 6, 2012 2:16 pm

Carbon Essentials

  • Name: Carbon
  • Symbol: C
  • Atomic number: 6
  • Atomic weight: 12.0107
  • Standard state: Solid
  • Group in the periodic table: 14
  • Period in the periodic table: 2
  • Block in the periodic table: p-block
  • Color: In graphite form, carbon is black. In diamond form, it is colorless
  • Classification: non-metallic

A new form, aside from the common graphite and diamond forms, of carbon called buckminsterfullerene or C60 was discovered. It is of high interest to scientists and is being researched in laboratories. Carbon is also present in the atmosphere as carbon dioxide and is also dissolved in all natural waters. It is bar of rocs as carbonates of calcium, magnesium and iron. Ninety-six percent of the atmosphere of Mars is carbon dioxide.

 

Hydrocarbons, another form of carbon bonds, are coal petroleum and natural gas. Carbon is unique among other elements because of the amount of bonds it is able to form with other elements. Organic chemistry is the study of carbon and its compounds. Silicon can take the place of carbon in forming many compounds, but it is not able to currently form stable compounds with long chains of silicon atoms.

 

http://www.webelements.com/carbon/

November 1, 2012, 1:07 pm

Isotopes

Carbon Isotopes

Carbon has three naturally occurring isotopes (isotopes have in their nuclei equal numbers of protons but different numbers of neutrons), with 12C and 13C being stable; carbon 14C is a radioactive isotope decaying with a half-life of about 5,730 years (half-life tells time isotope falls to half of its original radioactivity).

Radiocarbon dating, invented in 1949 by Willard Libby (the 1960 Nobel Prize) is a 14C-based radiometric method of estimating the age of materials aged up to 58,000–62,000 years. Older samples contain too small number of remaining intrinsic 14C carbon. Carbon dating allows estimate the age of organic remains and artifacts, objects of cultural or historical value, if they contain carbon. Scientists collected wood of the same age (based on the tree ring analysis) to increase accuracy of the technique. They have also measured radiocarbon in stalactites and stalagmites (called speleothems) using both 14C carbon dating method and the uranium-thorium dating to obtain radiocarbon calibration curves (Hoffman et al., 2010).
Ancient fossilized animal and human footprints in Acahualinka, Nicaragua has been first estimated as 5,000 years old and later determined as 2,100 years old.

The Chauvet-Pont-d’Arc Cave in the southern France, discovered in 1994, contains the rock art, a treasure trove of Paleolithic masterwork paintings, prints, charcoal drawings of different animal species such as horses, lions, rhinos and bears, etched into the cave’s walls, and also fossilized remains, and markings of animals, some of which are now extinct (Herzog, 2012). Findings based on an analysis called geomorphological and chlorine-36 dating (36Cl Cosmic Ray Exposure) show that most of the art works were created by people who lived 28,000 to 40,000 years ago, in the Aurignacian culture of the early stages of the Upper Paleolithic, Late Stone Age; later on, an overhanging cliff began collapsing 29,000 years ago and did so repeatedly over time, definitively sealing the entrance to humans around 21,000 years ago. “This study confirms that the Chauvet cave paintings are the oldest and the most elaborate ever discovered, challenging our current knowledge of human cognitive evolution” (Sadier et al., 2008; Agence France-Presse, 2012). Bon et al. (2008) wrote, “We collected bone samples from the Paleolithic painted cave of Chauvet-Pont d’Arc (France), which displays the earliest known human drawings, and contains thousands of bear remains. We selected a cave bear sternebra, radiocarbon dated to 32,000 years before present, from which we generated overlapping DNA fragments assembling into a 16,810-base pair mitochondrial genome. … our study establishes the Chauvet-Pont d’Arc Cave as a new reservoir for Paleogenetic studies.“

A German film director Werner Herzog created in 2010 a documentary film about Chauvet Cave, Cave of Forgotten Dreams (2012) and won Best Documentary Award by several film critics groups. He rendered in 3D the curvature of the rocks to enhance the texture and depth of the art works on the cave walls. As described on his webpage, Herzog had been mesmerized, as a boy in Germany, by a book about cave paintings that he saw in a store window. He wrote, “The deep amazement it inspired in me is with me to this day. I remember a shudder of awe possessing me as I opened its pages.” (Werner Herzog, 2012). Cave of Forgotten Dreams was triggered by a Judith Thurman’s article in The New Yorker based on photos and interviews. Herzog became the first filmmaker permitted by the French Ministry of Culture to enter the cave, however under heavy restrictions. All people had to wear special suits and shoes that have had no contact with the exterior, stay on a two-foot-wide walkway, using only a small 3D-camera rig and three battery-powered light sources. Because of near-toxic levels of CO2 and radon in the cave, the crew could enter the cave for only a few hours each day. The cave explorers found, among rock paintings on a cave wall, some hand imprints with one finger shorter than others. This could be considered the first signature in art. In his film “Roma (1972) awarded at Festival de Cannes, BAFTA (British Academy of Film and Television Arts), and other festivals, an Italian film director and scriptwriter Federico Fellini devoted one episode to a sudden discovery of ancient Roman frescoes and sculptures that would conceivably happen during digging a tunnel for an underground metro. When the workers stunned by the majesty of the portraits on the frescoes pointed their flashlights toward the paintings in the newly discovered chambers, the faces on the walls became slowly bleach, whiten by exposure to light, and finally they disappeared.

The radiocarbon dating provided a key marker for the disastrous volcanic eruption (Minoan eruption of Santorini) that devastated the island of Santorini (also called Thera) close to the coast of Crete, and implications for the chronology of the Eastern Mediterranean cultures from the Bronze Age in the second millennium BC. The radiocarbon dating analysis of an olive tree buried beneath a lava flow from the volcano indicate, that the eruption occurred between 1627 BC and 1600 BC with a 95% degree of probability (Friedrich et al., 2006; Manning et al, 2006).

Occurrence

Carbon is the fourth most common chemical element by mass in the universe. Hydrogen, helium, and oxygen are the first three most common. Carbon can be found in the sun, the stars, comets, and also in atmospheres of most planets. Some meteorites also contain tiny diamonds that were formed when the solar system was still gas surrounding a new-formed star. These tiny diamonds might also be formed when the meteorite impacts and the immense pressure and temperature that creates.

 

Along with most other planets, carbon is found in Earth’s atmosphere along with carbon dioxide and oxygen. We can also find it on Earth in the water dissolved. It is estimated that 36,000 gigatonnes of carbon is in the bodies of water on earth. About 1900 gigatonnes of carbon are in the biosphere. Carbon in the form of hydrocarbons such as coal, petroleum, and natural gas has about 900 gigatonnes on Earth. Oil reserves amount to about 150 gigatonnes. Carbon is also in abundance in the form of “unconventional” gases. The individual allotropes of carbon make up another large amount of substance. Graphite is very commonly found in the U.S., Russia, Mexico, Greenland and India. Diamonds are found in volcanic pipes. Most of these deposits are in Africa, however there are some in Arkansas, Canada, Russia, Brazil and Australia. Though most diamonds are found naturally, about 30% of diamonds in the United States are being made synthetically.

 

http://en.wikipedia.org/wiki/Carbon,

October 30, 2012, 1:17 pm

November 1, 2012 1:07 pm

November 6, 2012 1:02 pm

Allotropes

There are three different allotropes (forms) of carbon that are commonly known. There are amorphous carbon, graphite, and diamond. There are also several fullerenes (substances made completely of carbon), which include carbon nanotubes and carbon Nano buds and Nano fibers. These things were once considered rare, but now are made commonly for use in research. There are also less well know and hard to find types of allotropes such as carbon nanofoam and glassy carbon, among others.

 

Amorphous carbon is a set of carbon atoms in an irregular, “glassy” state which is the basics of graphite except for the fact that it is not in a crystal-like structure at the Nano level. Its main form is a powdery substance and is the main substance in things like charcoal, soot and activated carbon (a form of carbon that has small holes that increase the surface area and make it easier for it to absorb other substances or chemical reactions).

 

Graphite is formed when carbon is at normal pressures. When it takes the form of graphite, the atoms of the carbon are bonded triagonally to three others in a “plane composed of fused hexagonal rings”. This leaves a network of 2-dimentional atoms and these sheets of flat carbon atoms are stacked and bond together. This is what makes carbon so soft and malleable.

 

The diamond form of carbon is formed when carbon is put under high pressures. Diamond has almost twice the density of graphite because of its compacted form. In diamonds, the atoms are bonded tetrahedrally to four other atoms, which makes it a “3-dimenstional network of puckered six-membered rings of atoms”. Silicon and germanium both have the same cubic structure as diamond. Also, because of the strength of the carbon-to-carbon bonds, diamond is one of the hardest naturally occurring substances when it comes to resistance to scratching. Under normal conditions, diamonds are thermodynamically unstable and will transform to graphite. The transition to graphite from a diamond state at room temperature is so slow that it is unnoticeable.

 

Fullerenes have a structure very similar structure to graphite, but instead of hexagonal bonding, they also contain pentagons and sometimes heptagons. This will turn the sheet of atoms into spheres, ellipses or cylinders. The fullerenes haven’t been fully analyzed yet. There is a lot of research to go before we fully understand what they can do. Buckyballs, a type of fullerenes, are large molecules formed out of carbon-bonded triagonally, which forms the spheroids (such as the buckminsterfullerene which is soccer ball shaped). Carbon nanotubes are bonded in also triagonally but form a cylinder shape.

 

http://en.wikipedia.org/wiki/Carbon,

October 30, 2012, 1:17 pm

November 1, 2012 1:07 pm

November 6, 2012 1:02 pm