Oroville Mercury-Register

Clay, sand, silt, loam: How different soils affect gardens

- By Lee Reich

By now, you probably know what kind of soil you have out there in your “back 40.” If planting that rose bush brought up wads of gummy goo, you know to call it clay. If instead you scooped up gritty particles that didn’t clump together, you have the other extreme, a sand.

Both extremes in soil have their advantages and shortcomin­gs.

These soils act the way they do mostly because of the size of the particles that make them up. Sand particles are relatively large ( by definition from 2- to 5-hundredths of a millimeter across). At the larger end of this range, you can easily see them with your naked eye and feel them between your fingers. Clay particles are very small ( by definition less than 2-thousandth­s of a millimeter across).

It’s all about pores

Tiny clay particles have tiny spaces between them — small enough to draw in water and cling to it by capillary action. That can be a bad thing this time of year, when you’re likely waiting for the soil to dry enough to become crumbly for planting, or anytime if there’s not enough pore space open for roots to get air. Don’t let clay soil get too dry before planting, though, or it becomes rock-hard.

The way clay slurps up and holds water makes it a good thing as summer weather turns dry. Some of that water, though, is held so tightly that even roots cannot get at it.

In sandy soils, the larger spaces don’t hold water. This makes for pleasant digging in spring mud season, but has plants gasping for water in dry summer weather.

Another asset to many kinds of clay particles is that they are negatively charged on their surface. That means that positively charged plant nutrients like potassium and calcium can latch onto those clay particles instead of being washed below the roots by rainfall or watering.

Sand particles are uncharged, letting plant food just wash right through and leaving these soils naturally infertile.

The cure-all

You can cure the ills of either clay or sandy soils in basically the same way: with plenty of organic matter. That includes compost, manure, leaves, peat moss, straw, hay, grass clippings, wood chips, and anything else that is or once was living.

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