I took a class last Thursday with the Marin Master Gardeners and the guest speaker and UC Berkeley Soil Scientist, Steve Andrews. Steve took us through a wonderful and most entertaining review of soil morphology and additional insights into soil ecology and plant nutrition. -Truly a a divine experience! This was a longer version of the class he presented to the Bay Friendly Landscape Professional class I attended last year. Steve told us that there may be an advanced soil class in the near future. While at Cal Poly, SLO, I took the soil science classes, and all the topics Steve brought up were reminders of those classes, but that was back in the late 80's and Cal Poly was still somewhat stuck in the old agribusiness mentality of soil as a sterile medium, fertilizers being measured out by the acre and recommendations based on economic returns on investment -without comment about the soil ecology and how it might be affected. It is so nice to hear a modern soil educator so passionate about our most precious resource, our LIVING soils.
Which is more precious? Fresh Water, or Soil?... that's a hard one. We need both. They are intertwined in the web of life. One creates the other. As our species has evolved on Earth, our various civilizations have thrived and crashed primarily based on how we have treated these two resources. Their interaction along with the ecologies they support give rise to the world we hold so dear. Our understanding of these interactions will be the basis of our survival. Learning about soil is one of the first steps in learning about life, a big step towards our species making the changes necessary in our practices, and a huge leap towards any individual's concept of where they fit into the web of life - a strong dose of awe that can lead to a better intellectual and even spiritual questioning of how and why we are here. Perhaps our greatest calling is to be good soil stewards.
A good resource for soil can be found at the WSS, the Web Soil Survey. This is information provided by the National Cooperative Soil Survey operated by the USDA natural Resources Conservation Service. Maps and data are available for more than 95% of our nation's counties! Amazing to type in an address and get so much information: soil complex percentages, elevation, slope, mean annual precipitation, temperature, and frost free period plus depth to water table, etc. Then you can search for a use and see the results.
During our class we got to do a textural ribbon test. This is done by getting a soil sample damp and pressing it between the thumb and fingers and pushing it through into a ribbon, the length of which determining the relative amounts of sand, silt, and clay. This exercise, along with rubbing a smaller, wetter sample in the palm of the hand to determine it's grittiness or smoothness can be a good indicator of the soil textural class as depicted on the Soil Pyramid. The Sand, Silt, and Clay are the "Soil Separates".
The relative sizes of these are:
Sand: 2mm -.05mm
Silt: .05mm - .002mm
Clay: smaller than .002mm. (Cant be seen by the unaided human eye!)
"Garden Nirvana!" - the area in the middle of the pyramid (this sounds almost masonic!) where the concentrations of the three soil separates find their sweet spot in the textural class of LOAM.
Several insights I gleaned is that in most soils, soil pore space, roughly 50% by volume in soil, is filled with air and water, always in flux, and is where the concept of "field capacity" as it relates to water saturation occurs. This is also where gas exchange occurs and most of soil chemistry. 5% of most soils is comprised of organic matter and humus which, consisting of relatively 80% of that 5%, is the magical "glue" that binds soil into aggregates and peds, the macro structures of soil conglomerates. The ability of humans to enhance or destroy soil structure is key to the survival of civilization. These concepts: soil texture, a constant in an anthropocentric time frame, and soil structure, a fragile system that can take thousands of years to create ("pedogenesis") -or destroyed in a very short time frame, form the basis of modern soil classification.
Clay is also where all the action is. Clay, being .002mm or smaller in size, has both chemical properties an electrical properties. The negative charge of clay particles allows soils to hold onto cations -important plant nutrients. The negative clay surface also allows the soil to interact with active nutrient absorption systems that plants (and a plethora of other organisms) have evolved. The sheer mind boggling expanse of this surface area is hard to comprehend. Clay particles, which are so small they are not visible to the naked human eye, are comprised of layers, 1:1 or 2:1 of tetrahedral and octahedral layers. This layering allows an amazing surface area. Steve pointed out in our class that a single teaspoon of clay can have the relative equivalent surface area of a football field.
Clay can also be the source of life as we know it on this planet. A.G. Cairns-Smith, in a paper in 1966, postulated that clay was the scaffold upon which life arose. Clay affords the protection, the repeating layers, the proper distances between those layers, the chemical charge, and the structure to create repeating compounds as well as the affinity for organic compounds and an ability to organize them. Chemist James Ferris and colleagues at Rensselaer Polytechnic Institute, during research sponsored by NASA, created an experiment where they "induced clays to act as scaffolds in the formation of RNA, the polymer that carries the genetic message enabling protein synthesis". Harvard University geneticist Jack Szostak, who later mixed clays, RNA nucleotides, and lipids was able to show that the clay not only absorbed the RNA, but quickly formed lipid vesicles. "This spontaneous self-assembly of RNA-containing vesicles, though a long, long way from synthesizing life, is perhaps the closest anyone has come to forming a cell-like entity from scratch". (p.158, Gen-e-sis, Robert M. Hazen, 2005)
The miracle of life may well have evolved in the chemically charged, too-small-to-be-seen, layers of clay. This concept lends a new perspective to the idea that soil supports life. Other impressive soil life concepts from the present day include: a gram of soil contains a population of between 100 million to 3 BILLION bacteria, roughly a million fungi, perhaps miles of mycelium... and a plethora of virus, anthropods, isopods, etc. -a truly wonderous soil food web with feedback loops and interactions with the macroecology of vertebrates and plants. -too much to go into in this little blog!
We also briefly looked at the Munsell color chart, an expensive and very accurate color system created by Albert H. Munsell and adopted by the USDA for soil research in the 1930's. It uses Hue, Value, and Chroma to determine the exact color- based on human visual perception. Soil color can show us clues to mineral concentrations, especially in the B soil horizon where soil elements accumulate due to leaching over time. As Steve pointed out, the color of soils can also have a legal application in the process of saving our wetlands from overdevelopment.
Soil as it relates to gardens and gardeners -agriculture- is a huge topic. I will explore more of this awe inspiring topic and how we fit into the soil web in later blogs. Fertilizers and their use being the next topic of discussion for the Sloat Garden Center Seminar series (Feb. 20 in Kentfield and Feb 27 in Mill Valley, Miller) and the Marin Garden and Landscape Meet Up group meeting.
That having been said, I can't express enough my main take-away from the class, and almost every gardening class I've ever been involved with: The magic bullet: Compost. Compost adds life, it adds buffers, it adds humus. Compost can take almost any soil ill and correct it over time, creating a more complex (and thus stable) food web, maintaining better water holding capacity while improving drainage, water infiltration and filtration, soil nutrient availability through chemical and biological actions, as well as a myriad of other benefits including the breakdown of toxins. As our Co-Horts pointed out, one of the main MMG mantras is " Compost Compost Compost - Mulch Mulch Mulch!" This is truly the key to improving humus content and soil life.
Steve Andrews also pushed another take-away: Don't fall into the media-driven trap of regular fertilizing without proper soil testing and taking the plants needs, the season, and climate into account. This falls right into place alongside the practices of IPM - using the synergistic approach and monitoring before taking action, knowing the biotic and abiotic situation and the possible affects of those actions.
So go forth and spread the good word of Compost, Mulch, and the wonder of Life; in, from, and dependent on -our precious Soil.
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