Clay, silt, and sand layers - failure
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david52 Zone 6
9 years agogrubby_AZ Tucson Z9
9 years agoRelated Discussions
6 acres of silt soil over gray clay
Comments (25)You need to get a book called "Hands-On Agronomy" by Neal Kinsey. Or you can get the DVD short version of that info, but it's not as comprehensive. They tell the how and why of getting your soil nutritionally balanced. Going blind into your soil improvement is usually a waste of money. Find out what's wrong, what's right, and how you need to tweak it with a GOOD lab test. Just adding compost or cover crops isn't going to solve the problem. If your soil nutrients aren't in balance, your pH will be wrong and you're going to have nothing but problems. Too much of one nutrient can tie up the availability of others. Some areas of the country are totally lacking necessary elements, and you'll have to add them. Both the book and the video are in the library systems. If your local library doesn't have them, request an interlibrary loan. I don't have anything to do with these people, but the book and DVD make so much sense that I'm going to get my soil tested by them. They will test it and give recommendations on how much of what you need to add or change. Sue Here is a link that might be useful: Kinsey Agricultural Services...See Moresilt and clay as amendment
Comments (37)I'm not sure exactly what part you're saying is mythical. From what you've posted: "Coarse Sand or Gravel Subsoil Fine soil overlaying coarse sand or gravel subsoil must become very wet before water will move down through the large pours of the subsoil. Under these conditions, the overlying soil holds up to two or three times as much water as it would if the course subsoil were not present" And that's exactly what I was talking about. The water "perches". It's not actually 100% saturated but it is water that is perched until you apply enough for gravity to suck it down into the subsoil. With proper irrigation management, you can perch the water where you want it and use that effect to your advantage. Of course, that saturated zone (not actually 100% saturation but close enough for the girl's I go with, as my grandfather use to say) Will be bigger in a fine soil over gravel due to greater capillary action but it will still be there in a sand over gravel. You might have a 5 or 6 inch layer of saturation in a heavy soil over gravel and a 1 or 2 inch layer in a sand over gravel. In the paragraph above that, your reference states (when placing a find soil over sand): "When water passes through a fine layer and reaches a layer of coarse sand, it stops until enough water accumulates to nearly saturate the fine soil" Note the use of the word "stops". Again, this happens when going from a sand to a gravel due to a difference in capillary action of the two different layers. Again, this is the effect that we use to "perch" water where we want to so the roots can get to it. As far as a clay layer goes, you're right. You can perch water that way too. "Clay Layer When water reaches the clay, the very fine pores of this layer resist water flow. Although water does pass through the clay, it's penetration is so slow that water tables often build up above the clay." In that condition, note that water actually moves but slowly rather than coming to a dead stop like it does when you put a finer material over a coarser material as discussed previously. However, your zone of saturation will be larger and you can't "push" water into the subsoil when you need to by applying a bigger head of water. It will just perc as slow as the clay will allow it to move and no faster. It's harder to control soil moisture that way. Both of these conditions become less and less important the deeper in the profile the textural interface is but when the interface exists relatively near the surface, either by accident or design, it can be an advantage or a liability depending on intent and management practices. ("Or so the legends of yore go.", I suppose I should say)...See Moreroses on clay vs sand in hot climates and cold climates
Comments (51)Came back to this thread to check on Comte de Chambord, yes, Val grows it, and I agree that needs loamy soil, lots of rain, and healthier if alkaline. Comte is rooting easily in my wet baggie, and rooted easily in heavy out-door rain, while other cuttings rot. Comte has aggressive root and can root easily in alkaline sand, but I need to make my rooting-medium more acidic for the cuttings which are harder to root. Pink Pet definitely likes dry/loamy soil and warmer climate (Val's pic. is awesome). But died in my soaking wet clay last winter....See MoreProblem! Clay + sand = concrere
Comments (23)You'd need an ungodly amount of silt to significantly impact the proportions. Hauling and tilling that in sounds like a backbreaker. If you can get the SFW going strong, you aren't looking at a huge amount of years to get usable results, a year or so of very heavy mulch will have noticeable results underneath. Some of it will be your mulch breaking down, some will be your soil broken up, it's enough to work with in seasons while you're waiting for change to go deeper. Again I gotta mention dandelions as possible helpers to get this plot into shape. They do well in hard pan clay soil (they grow out of accumulated crud in cracks in pavement, too), and drill big strong tap roots down. The leaves, roots, and flowers are edible. They attract pollinators and some beneficial predator insects. And they can seed hundreds more of themselves, which makes for very easy spread as a pioneer plant. You are probably going to need some very tough, stubborn, hard-working helpers for this rehabilitation; plants and bugs that put up a fight instead of rolling over and dying. It might be worth your while to look up beneficial weeds in general, and cross reference your findings against what grows in your area. Changing the soil structure completely can be done, natural processes and human activities both do it. "Clay" and "sand" just refer to the dominant sizes of rock fragments in the area; there is a lot more in soil than just rock. You'd be amazed at the differences that can happen when the SFW starts moving rock up and organic material down, breaking some bonds and building others. Gross shape, fine texture, air flow and drainage can all change dramatically....See MoreUser
9 years agoUser
9 years agoUser
9 years agokimmq
9 years agoGary in Riverside Ca (USA) USDA Zone 9b; Sunset Zone 18
9 years agolast modified: 9 years agorhizo_1 (North AL) zone 7
9 years agolast modified: 9 years agotoxcrusadr
9 years agoGary in Riverside Ca (USA) USDA Zone 9b; Sunset Zone 18
9 years agolast modified: 9 years agokimmq
9 years agoGary in Riverside Ca (USA) USDA Zone 9b; Sunset Zone 18
9 years agolast modified: 9 years agoNil13 usda:10a sunset:21 LA,CA (Mount Wash.)
9 years agolast modified: 9 years agokimmq
9 years agoGary in Riverside Ca (USA) USDA Zone 9b; Sunset Zone 18
9 years agolast modified: 9 years agoUser
9 years agoUser
9 years agoUser
9 years agoUser
9 years agoUser
9 years agoUser
9 years agoGary in Riverside Ca (USA) USDA Zone 9b; Sunset Zone 18
9 years agolast modified: 9 years agoUser
9 years ago
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Gary in Riverside Ca (USA) USDA Zone 9b; Sunset Zone 18Original Author