What’s going on under our feet And in our gardens. Score Four Program, Interstate Commission on the Potomac River Basin, July 2015.

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What’s going on under our feet And in our gardens. Score Four Program, Interstate Commission on the Potomac River Basin, July 2015.

 Nutrients  Minerals  Water  Oxygen Soil provides plants with -- Interstate Commission on the Potomac River Basin (301) │ │

Graphic: MEA Learning Center, moisture-monitoring/learning-centre/what-is-soil-structure?vm=r Soil consists of:  Mineral particles – sand silt, or clay  Organic matter – decomposing plants, animal matter and droppings  Small organisms – worms and insects and microorganisms, such as bacteria and fungi  The space between mineral particles (pore space) Interstate Commission on the Potomac River Basin (301) │ │

Three minerals comprise soil:  Sand  Silt  Clay Interstate Commission on the Potomac River Basin (301) │ │

These minerals are classified by size. You can see –  Sand with your eye or magnifying glass  Silt with microscopes  Clay with electron microscopes Interstate Commission on the Potomac River Basin (301) │ │

Particle size influences soil texture. The particles feel differently, due to their sizes and structure. The minerals in a soil define its texture. We can tell the general composition of soil from its texture. Interstate Commission on the Potomac River Basin (301) │ │

 The spaces between soil particles are called pore spaces.  Pore spaces house water, oxygen, and microorganisms.  Plant roots grow into and make pore spaces. Interstate Commission on the Potomac River Basin (301) │ │

Interstate Commission on the Potomac River Basin (301) │ │ Graphic: Earth Science Australia Different types of minerals have different sized pore spaces.

Which type of mineral has the largest pore spaces?  Sand?  Silt?  Clay? Interstate Commission on the Potomac River Basin (301) │ │

Infiltration: water passing into the soil. Porosity: the amount of pores in soil.  Which soils are the most porous?  Which soil would rain infiltrate into the fastest? Interstate Commission on the Potomac River Basin (301) │ │

 Bacteria and protozoa  Algae and fungi  Microscopic nematodes and arthropods  Worms, insects, animals  Plants  Interestingly, these organisms cleanse our water and air Graphic: Soil and Water Conservation Society (SWCS) Soil Biology Primer. Rev. ed. Ankeny, IA: Soil and Water Conservation Society Interstate Commission on the Potomac River Basin (301) │ │

 What are some factors that cause pore spaces in soil?  Which would retain water the best – a sandy soil or a clayey soil?  What types of organisms do you think you will find in your school soil? Interstate Commission on the Potomac River Basin (301) │ │

 Plants need nutrients, oxygen, and water from the soil.  Rain gardens are meant to let large amounts of storm water percolate slowly through the soil.  Which mix of soils would work best in a rain garden? Think about this question during your soils experiments. Interstate Commission on the Potomac River Basin (301) │ │

 Flow diagram for Texture by Feel. Commonly used in the field. Provided by the USDA Natural Conservation Resources Service. (Click here for a high-resolution version of the graphic.) Flow diagram for Texture by Feelhere  Soil Science Society of America provides an excellent bank of soils lessons for multiple grades covering texture, biology, chemistry, forensics, and more. activities#General9 Soil Science Society of America activities#General9  Basic Hydrologic Science Course Runoff Processes Section Four: Soil Properties. In depth explanations with public domain graphics. graz.at/meted/hydro/basic/Runoff/print_version/04- soilproperties.htm?vm=r#12http://wegc uni- graz.at/meted/hydro/basic/Runoff/print_version/04- soilproperties.htm?vm=r#12 Interstate Commission on the Potomac River Basin (301) │ │