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An Old Science Experiment On The Moon

The most famous thing Neil Armstrong left on the moon 35 years ago is a footprint, a boot-shaped depression in the gray moondust. Millions of people have seen pictures of it, and one day, years from now, lunar tourists will flock to the Sea of Tranquility to see it in person. Peering over the rails ... 'hey, mom, is that the first one?' Will anyone ...

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AnOldScienceExperimentOnTheMoon
Astronomy

Black Hole Sound Waves

Astronomers using NASA's Chandra X-ray Observatory have found, for the first time, sound waves from a supermassive black hole. The 'note' is the deepest ever detected from any object in our Universe. ... Continue reading

BlackHoleSoundWaves
Physics

X-Rays - Another Form of Light

A new form of radiation was discovered in 1895 by Wilhelm Roentgen, a German physicist. He called it X-radiation to denote its unknown nature. This mysterious radiation had the ability to pass through ... Continue reading

XRays
Biology

The Rapid Movement of the Soybean Rust Pathogen

Soybean rust, caused by the fungus Phakopsora pachyrhizi, results in soybean yield losses of up to 80%. Rust diseases are named for the orange powdery spores produced in leaf pustules. They are easily ... Continue reading

SoybeanRustPathogen
Science

Benjamin Franklin, Science Founding Father

While popularly known for his role as one of the United States' founding fathers, Benjamin Franklin was also a renowned scientist who made a number of substantial contributions in the field of Earth ... Continue reading

BenjaminFranklin

Carbon Dating

CarbonDatingAs isotopes break down, or decay they give off radiation. Materials that decompose in this way are said to have a 'half-life'. As the quantity of material present decreases, so does the actual rate at which the material decays. The process of dating artifacts by radioactive C-14 measurement depends strictly upon this condition. Using C-14 measurement and analysis it is possible to obtain a reasonably accurate estimate of the age of materials, given certain conditions.

Carbon-based materials such as wood, bone, and other organic materials, come from sources that were once living and in a dynamic relationship with their environment. Organic fibers that come from sourcessuch as trees, flax, cotton, and wool, grow through or depend on the process of photosynthesis. In photosynthesis, carbon dioxide is incorporated with water to produce the structural fiber cellulose and related compounds. Due to the influx of background radiation from terrestrial sources and 'cosmic rays', there is a fairly constant percentage of carbon dioxide in which the carbon atom is radioactive C-14 rather than non-radioactive C-12. While the plant is alive, this radioactive carbon dioxide is incorporated into the photosynthetic process at a constant corresponding rate, providing a baseline composition ratio of C-14 to C-12.

When the plant is killed, photosynthesis ceases and the relative amount of C-14 in the material begins to decrease from the baseline quantity. By relating the amount of C-14 remaining in the artifact material to the baseline amount of C-14 in living systems, a fairly accurate estimate can be had of the amount of time that has passed since the artifact was produced, according to the number of half-lives that have transpired. An invaluable tool for archeologists.