Varoius Soil Tests Pro & Con
TAKING A SOIL PROFILE
If you have serious soil drainage, compaction or structural prob­lems, it may pay you to take a soil profile. This is done simply by digging a pit into a "central" area of the garden to get an over-all idea of what lies underneath the topsoil. The pit ought to be at least two feet deep and wide enough so you can get down in it to "read" the soil profile.

At the top of the profile you will see the dark layer of topsoil (unless a building contractor got rid of clay from an excavation by spreading it over your lot, in which case a layer of hard, stiff, light-colored strata will overlay the darker topsoil). Sometimes, in semi-arid regions, topsoil may be lighter than layers underneath but this is rare in any soil where garden plants will grow.

The depth of the topsoil usually shows how deeply roots of grasses and shallow-rooted weeds have penetrated. In prairie soils where bluegrasses often penetrate as deep as two to three feet, a surface layer of that depth is often found. The darker color of the topsoil indicates where perishable plant tissue has decayed, leaving behind a residue of humus and carbon.

In the soil scientist's language, this upper layer is called the A horizon. In many soils, just below it is another darker layer, but separated from it, which is called the A1 horizon. In some soils, where organic matter is tightly held by the topsoil, no well-defined A1 hori­zon develops. In such cases the next lower layer is the B horizon or subsoil. The science of pedology makes a great deal of these hori­zons. From them, earth scientists can read the history of soil forma­tion. However, our interest is in checking depth and condition of the topsoil and the subsoil.

WASH TESTS
I am often asked whether a wash test cannot be used by the home gardener to see what materials make up a given soil. A direct yes or no answer is not possible. Light sandy soils containing little clay are easy to check in this way. The heavier the soil, however, the less accurate a wash test will be. The difficulty lies in breaking the bond between the acid clay particle and its cluster of alkaline particles. However, I find that if two tablespoonfuls of sodium nitrate are added to the soil sample, some of the electrical charge holding clay and lime together can be neutralized.




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