We’ve gone over quite a few things in this mini-section on soil structure as we zoomed closer and closer in on the structure of soil! I do hope it’s becoming clearer as to why a good soil structure is so important, and how even poor soils… more »
Archives for: "June 2019"
Last week ended with a brief mention of cation exchange being the activity that occurs on the very large surface areas of clay and humus colloids. But before we get to cation exchange, first some very simple chemistry to get up to speed on what a cation… more »
Clay and humus are the two smallest particles in soil, and together they make up the colloidal fraction of soil. A colloid is a particle able to stay suspended in a solution for very long periods of time, without settling to the bottom —you can see this… more »
Last week we covered the five ped types, of which the granular type is the one best for plant growth. This type is synonymous with soils of good fertility, drainage, aeration, friability, and tilth. Not all soils are this good unfortunately, and you may… more »