In plain English, the presentation explains what can and cannot be done to mitigate the effects of clay content in soil. It includes some basic irrigation terms and their definitions, within the context of soil texture.
12. Used with permission: Bradshaw, M and R. Weaver. 1995. Foundations of Physical Geography. W.C. Brown Communications, Inc. Dubuque, IA. Subduction zone
13. Fact #4: Same volume, different surface area . Surface area = 2X2X6X8 = 192 sf Do the math and prove it to yourself! 4’ 4’ Surface area = 4X4X6 = 96 sf
14. Small particles, enormous surface area. Big particles, small surface area.
23. Fact #6: A plant taking up water is playing tug of war with the soil. Clayey soils hold water tightly. Sandy soils have limited storage capacity. Image used with permission from the BBC’s Schools Website Evaporation
27. Fact #7: Unavailable Water As soil dries out, it holds on to water more tightly. capillarity not connected
28. Fact #8: Soil’s water storage depends on texture. stored water more less clay sandy loam silt loam sand loam clay loam soup water available to plants unavailable water field capacity permanent wilting point
38. Linda J. Brewer Extension Horticulture Extension Small Farms [email_address] 541-737-1408
Editor's Notes
Kaolin Clay
Think about taking the clay soil model to the library?
I’m going to show you a series of slides that show how water moves through coarsely and finely textured soils. I filled mylar “ant farms” (hold one up) with sand, and started water slowly dripping into the sandwich. I traced the path of the water onto the plastic surface with a marker – this is what you’re seeing here.
Cation Exchange is trading: Plants trade what they cannot use for what they can. The soil acts as like the old drive-in movie theater.