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Seed of the Week: Sorghum or Milo

Our mystery seeds from last week arose from a simple question:  What is in the bird seed we are feeding our birds?

With some detective work, we found out that the smaller, shiny white or light-colored seeds are white proso millet, Panicum miliaceum.

The bigger, red or orangish seeds are from sorghum (also called milo), Sorghum bicolor.

Both plants are monocots.

Sorghum has broad leaves that may resemble those of corn plants.

The sorghum seeds start pale and then darken with time.

Studies have shown that different birds prefer different sizes and types of seeds. In our yard, most of the ground feeding species, such as mourning doves, inca doves, white-winged doves and sometimes curved-bill thrashers, will eat the millet and sorghum.

Refer to Birdzilla for more information and pictures of different types of bird seed.

Sorghum was thought to have come from northern Africa and it grows remarkably well in dry areas. In fact, it can grow where there is too little moisture for corn to grow. Although the leaves are large, it has an extensive root system and the leaves are waxy, to prevent water loss. It also can go dormant during periods of drought.

Apparently the leaves can contain too much prussic acid (hydrogen cyanide), and can be toxic. The foliage is converted into silage before being fed to animals to prevent prussic acid poisoning.

What an interesting plant!

What kinds of seeds to you feed your birds?

Weekend Science Fun: Dust Storms

This week let’s take a look at a weather phenomena that has been in the news in the Southwest:  dust storms.

On July 5, 2011 a huge dust storm hit Phoenix. It was a wall of rapidly blowing dust 5,000 feet high in some places.

This time-lapse video shows how it looked as the curtain of dust approached.

(In inside look at how the video was made.)

Dust storms occur most frequently in arid regions, such as the southwestern United States, the dry areas of Australia, the Middle East (see a similar dust storm that happened in April in Kuwait), China and the Sahara Desert. Here in Arizona we have them most frequently in the summer, typically in late June and July, although sometimes into September if the summer rains fail to materialize.

Why summer? The dust storms are fueled by the intense heat that causes air to rise, just like happens with thunderstorms. The rising updrafts eventually begin to cool when the air gets high enough and a rush of air starts down. Under certain conditions, the thunderstorms collapse and the down rushing air can be intense. Huge gusts of wind pick up any loose soil particles as they flow by. Where there are large areas of exposed soil -such as in deserts- the amounts of dust picked up can be extremely high.

Plants the day after the dust storm in Phoenix

To give you an idea what dust in the air was like during the recent storm, let’s take a look at the records from the weather stations that record the amount of particulates in the air. On a normal day, the average amount of particulates is 38 micrograms per cubic meter of air. On July 5th the readings ranged from 2,576 to 5,190 micrograms of particulate per cubic meter. (Source:  The Arizona Republic, July 24, 2011). That’s a lot of dust!

For some related hands-on activities, try the Wind Power post.

Bug of the Week: Squash Bug

My son found this in a friend’s garden.

What’s that blur?

See it better this way?

An accident?

No, the squash bug gave off an odor when my son touched it. The fly was attracted to the odor, probably thinking it might find a free meal.

I don’t have 4D on the blog, so you’ll have to find a squash bug for yourself to see what it smells like 🙂

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