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What Are Aerosols?

Aerosols are tiny particles suspended in the air. Most occur naturally, originating from volcanoes, dust storms, forest and grassland fires, living vegetation, and sea spray (Figure 1). Human activities, such as the burning of fossil fuels and the alteration of natural surface cover, also generate aerosols. Averaged over the globe, aerosols made by ...

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Aerosols
Biology

Electricity and the Brain

A child's electric train and our brains have something in common. They both require electricity for any activity to take place. But the brain uses electricity in a much different way than a toy train. ... Continue reading

BrainElectricity
Chemistry

What Is pH?

Anyone who is the least bit familiar with vinegar, nausea, sodium bicarbonate, and ammonia-based cleaning solutions probably has a very good 'feel' for the different natures of acidic and basic ... Continue reading

WhatIspH
Geology

Haleakala Crater

Modern geology indicates that the Hawaiian Islands are situated near the middle of the Pacific Plate, one of a dozen thin, rigid structures covering our planet like the cracked shell of an egg. Though ... Continue reading

HaleakalaCrater
Geology

A Great Sunset Takes A Few Clouds

Although the twilight sky can certainly inspire awe even when it is devoid of clouds, the most memorable sunsets tend to be those with at least a few clouds. Clouds catch the last red-orange rays of ... Continue reading

AGreatSunsetTakesAFewClouds

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.