Soil, the living world beneath our feet

Everyone is curious about the life in the soil and the food web, 

yet we can’t see the "microbiome" in the soil. Gardeners love soil and have so many questions about it – how to test it, how to compost, how to enhance soil structure and fertility. For those in the "growing" world, we wonder if the difference between dirt and soil is just semantics. Turns out, it's not just semantics! Soil is a living environment...whereas dirt is basically dead soil, according to scientists. Soil is the earth’s delicately structured biological skin(video). Every terrestrial ecosystem and the food you eat sprouts from soil. (95% of food comes from soil).

• Soil anchors and feeds forests, prairies, and farmed fields.
• The amazing difference between dirt and soil is that soil contains mycorrhizae, a beneficial fungi, which lives beneath our feet. Click here for Dr. Linda Chalker-Scott photos and description of this beneficial fungi.
• Soil is habitat for many burrowing animals and harbors an amazing biodiversity of microbes, insects, arthropods, and worms, many yet to be scientifically described. 

Growing a Revolution

• Soil is essential to the water cycle as it filters and gradually releases water year-round to streams, rivers, and lakes.  

• Soil decomposes fallen leaves, feces, dead animals and plants into soil organic matter while recycling the nutrients that plants need to grow. Increasing soil organic matter is one way to sequester atmospheric carbon dioxide and address climate change.
• David Montgomery talks about bringing our soil back to life, and with one third of the arable land laying dormant, soil is a lifeline to healing the planet and feeding the hungry.
• Whether one is a serious scientist, or food activist, a farmer or a backyard gardener, the following references and link resources will open a new world, one going on right under our feet. 

To understand how Canyon County soils influence plant growth, check out this class  https://bit.ly/2cSoils    offered on Zoom.

Further links: 
Great videos, interactive games from Smithsonian Environmental Research Center http://forces.si.edu/soils/ 

Soil Health Awareness: Sponsored by the US Government, this site provides information for educators. USDA Natural Resources link

Frost, Freeze, or Hard Frost? It's that time of year...!

 According to the National Weather Service, here are the definitions of a Frost, Freeze and Hard Freeze.

Frost:  Frost occurs when there is a solid deposition of water vapor from the air. Frost will form when solid surfaces are cooled below the dew point. An air temperature range of 33°- 36°, along with very light winds, is usually needed to initiate frost formation. At least minor damage is possible to plants. One must keep in mind that a frost is not guaranteed at these temperatures if moisture in the air is lacking and/or winds are strong.

Freeze:  Freeze occurs when the air temperature drops to 32°-or-lower. A freeze will result in significant damage to many unprotected plants, especially if the temperature remains at-or-below the freezing mark for several hours.

Hard Freeze:  Hard freeze occurs when the temperature reaches 28°-or-lower for at least a few hours. It usually means that many types of plants and most seasonal vegetation will be destroyed.

Mark Longstroth with Michigan State University Extension posted the following information explaining the differences more clearly than just a definition.

A frost is when we get a visible frost. A freeze is when the air temperature drops below freezing. Sometimes we get frost when the temperatures are above freezing and we often have a freeze without frost. It all has to do with the amount of water in the air.

At the dew point, water vapor in the air condenses on the ground and other surfaces as dew. If the dew point is below freezing, the water vapor condenses as ice, freezing as frost. So the air can be above freezing and the surface of your car (or the roof of your house) can be colder than the air and colder than freezing causing a frost even though the air temperature is above freezing. That is how we get a frost without a freeze. If the dew point is much below freezing then we can get freezing temperatures cold enough to freeze plants without any frost. This is also called a black frost, a freeze without a frost. When frozen plants thaw they have a water-soaked, black appearance as they die.

Sometimes we get a freeze under windy conditions. This is caused by the movement of a cold air mass into the area with subfreezing temperatures. These freezes are called wind freezes.

Idaho Average First Frost Date Map will give you accurate information for your county.

Steps to take to help your plants survive as long as they can.

1.    Of course cover your plants with a frost fabric or sheets or plastic.

2.    Bring what plants you can indoors

3.    Water extra with warm water

4.    Keep water running at a trickle if possible for a few days.  Be careful not to over water.

5.    Wrap the trunks of young trees.

6.    Wrap pots that cannot be moved indoors.

Your plants are counting on you...Protect them!