ScienceIQ.com

What is Haze?

Haze is caused when sunlight encounters tiny pollution particles in the air. Some light is absorbed by particles. Other light is scattered away before it reaches an observer. More pollutants mean more absorption and scattering of light, which reduce the clarity and color of what we see. Some types of particles such as sulfates, scatter more light, ...

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Haze
Biology

Batesian Mimicry

If you ever got stung by a wasp you would probably avoid all flying insects which resemble the brightly-colored yellow and black wasp. If you were a bird and certain types of butterflies gave you a ... Continue reading

BatesianMimicry
Biology

Life In The Extreme

Lowly microbes just may be the toughest living things on Earth. They have learned to survive, and indeed flourish, in the harshest environment imaginable, deep-sea rifts. These rifts are chains of ... Continue reading

Microbes
Chemistry

Knocking the NOx Out of Coal

Nitrogen is the most common part of the air we breathe. In fact, about 80% of the air is nitrogen. Normally, nitrogen atoms float around joined to each other like chemical couples. But when air is ... Continue reading

KnockingtheNOxOutofCoal
Geology

Antarctica and Climate Change

Because of its influence on world weather and climate patterns, Antarctica lies at the heart of the debate on climate change and has become the premier location in which to study the effects of global ... Continue reading

AntarcticaandClimateChange

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.