Soil improvement findings
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6 years ago
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Nevermore44 - 6a
6 years agoRelated Discussions
Improving Soil Structure of Sandy Soil
Comments (23)ibuzzard - yes, constantly adding organic matter after harvest before the next crop. To speed things up bring in a lot of organic matter as manure + bedding to compost in piles set aside from the current gardening beds. Then after harvest rake those on to the beds if you let some lay fallow or put what is crumbling & dark brown on beds you plan to replant right away. It takes awhile to build enough compost to cover all the beds at all times, but with diligence you can do it. The small animal manures like chicken & rabbits are potent, but not the quantity you'd need. Get a hold of some horse manures and you'll be able to speed up the process. Ten years of using chicken, duck & rabbit manures from our backyard animals (Plus liberal amounts of used coffee grounds + shredded leaves mown over on the lawn in fall. Plus our kitchen waste compost bin contents.)... didn't up the soil organic matter content as much as when we started adding horse manure as well composting first in piles or spreading in fall on fallow beds. Volume made a huge difference though I was quite skeptical in the beginning, afraid of weeds & then learned about the herbicide residue in some hay fed to livestock. I made sure we used manure from horses fed alfalfa hay instead. Now after at least 3 years of horse manures we no longer need 6-12 inches of it added in the fall to break down. The soil is light, fluffy and diggable with hands rather than pickaxe like before....See MoreBest way to improve soil
Comments (40)Hi Everybody,,,Funny you should talk about composting. I'm in a master gardener program in my county right now and just yesterday our lecture was all about soils, fertilizers and composting. Here are some helpful hints to "correct" or trouble shoot your compost heap if these things occur. Problem: Cause: Ammonia smell: Too many greens Solution: Add more browns,mix and turn Pile has rotten odor 1.too wet 2.pile compacted 3. food scraps exposed Solution: mix in browns 2.turn pile to aerate 3.bury food scraps in middle of pile Pile doesn't heat up - low temp 1.Not enuf greens 2.not enuf air 3. lack of moisture 4. pile too small Solution: mix in greens, 2.turn pile more frequently 3. add small amounts of water 4.Build pile to be (symbold is the "v" turned so that the open mouth is on the left, don't which character to use on keyboard) greater than 1 cubic yard. Pile attracting flies or rodents Attracted by food remains Solution: Don't use meats or fat, bury fruit/veg scraps. This all comes from the Univ of Calif Cooperative Extension. There isn't a website for this brochure but there is a hotline that will answer your questions at ucmastergardeners@yahoo.com,,,,Hope this helps. Nicole Just a great program!! I'm lucky to have one of the choosen.... :)...See Moresoil improvement
Comments (1)Improving Soil for Better Lawns and Gardens By Don Comis November 9, 2010 U.S. Department of Agriculture (USDA) scientists in West Virginia are finding ways to improve soil on degraded land so it can be used for sports fields and other uses. Researchers with USDA's Agricultural Research Service (ARS) at the agency's Appalachian Farming Systems Research Center (AFSRC) in Beaver, W.Va., are developing constructed or replacement subsoils and topsoils to build better and less-costly sports fields, raingardens and lawns on former landfills, mine lands and other degraded land. ARS is USDA's principal intramural scientific research agency. The constructed soil research project is in its fourth year. ARS is conducting the research in cooperation with the National Turfgrass Research Initiative, Inc., a joint turfgrass industry-ARS program created in 2007. The initiative draws on the expertise of scientists with ARS and at universities, according to lead scientist Rich Zobel at AFSRC. The turfgrass industry has set a high priority on improving degraded soils by constructing soils that include readily available rural, urban and industrial byproducts that can be mixed with local soils. These byproduct mixes are being tailored to not only reduce rain runoff and erosion, but also to remove or neutralize pollutants before they reach storm drains. With lower costs through using inexpensive local byproducts, schools and local parks have a better chance of being able to afford soil replacement for better turfgrass survival. Eliminating compacted soil is the first step toward growing good, robust grass. The most promising mixture so far includes quarry byproducts and composted chicken litter. It has met predetermined requirements such as the ability to transmit stormwater. Zobel and his colleagues develop recipes for constructing designer soils from various materials in Ohio, Kentucky, Tennessee, West Virginia, Virginia and southern Pennsylvania. For the future, Zobel envisions new turfgrass varieties, possibly perennial ryegrass and tall fescue, that will penetrate compacted soil and renovate fields without the need to tear up fields and till compacted soil. Read more about this research in the November/December 2010 issue of Agricultural Research magazine, available online at: http://www.ars.usda.gov/is/AR/archive/nov10/gardens1110.htm. Findings from this research have been published in the Journal of Soil Science and Environmental Management and in USGA Turfgrass and Environmental Research Online....See MoreMulching for long-term soil improvement?
Comments (13)Randall, based on your location, here's the government poop on your soil (see below the demarcation). I'm guessing it's not red clay, but rather has some yellow clay in it. Does it look like the picture at the bottom of this post (farm near Raleigh)? I'd recommend fescue if you want a year-round green lawn. If your soil doesn't crust and get hard during the summer, you can use lime. Otherwise, use gypsum to break up the hard clay surface and Milorganite when it comes time to plant fescue seed. You should never have to dethatch, but aerating once or twice a year can help OM get deeper and work faster after you have a lawn going. You actually can top dress with granular lime right after seeding and don't worry about the nitrogen reaction. it won't matter that much. I have used peat moss or vermiculite as a top dressing also, but I have a commercial level Hunter irrigation system to keep that moist with regular spritzes. Fescue doesn't like to be covered too much, and even good seed can take three weeks to germinate (sprout). Straw helps, but I sometimes use a very lightweight insect cloth in 100-foot rolls to cover seed for the first three weeks. As soon as the grass is popping up, pull that off so the new sprouts don't "damp off." Look for the freshest seed you can find, direct from Oregon. Several sources on the internet when it comes to buying seed. Meanwhile, yes by all means find worms. I can't tell you how nice it is to see piles 4-inches in diameter of wormcastings in my yard this time of year, all over the place. One worm near a Pro-Spray head was about 10-inches long. He was a monster. We have little "cocoons" or egg thingees all over the raised vegetable garden, which has tons of azaleas, camellias and mountain laurels interspersed around additional raised beds for those good ol' veggies. We actually had tomatoes still two weeks ago! Anyway, the cocoons are future worms. Google earthworm images on the net so you can learn to recognize them. If you find them in the woods or anywhere, grab them and put them in your yard. Worms will find a way to organic material, even in clay soils, and they are indispensable. Good luck. ================================================= DURHAM SERIES The Durham series consists of deep, well drained moderately permeable soils formed in loamy residuum from acid crystalline rock. They are nearly level to sloping soils on broad ridges of the Piedmont. TAXONOMIC CLASS: Fine-loamy, siliceous, semiactive, thermic Typic Hapludults TYPICAL PEDON: Durham loamy sand--cultivated. (Colors are for moist soil unless otherwise stated.) Ap--0 to 8 inches; light brownish gray (10YR 6/2) loamy sand; weak coarse granular structure; very friable; medium acid; clear smooth boundary. (6 to 10 inches thick) BA1--8 to 13 inches; pale brown (10YR 6/3) loamy sand; weak coarse granular structure; very friable; strongly acid; clear smooth boundary. (4 to 10 inches thick) BA2--13 to 16 inches; pale brown (10YR 6/3) sandy loam; weak medium granular structure; friable, slightly brittle; strongly acid; clear smooth boundary. (0 to 4 inches thick) Bt1--16 to 25 inches; brownish yellow (10YR 6/6) sandy clay loam; moderate medium subangular blocky structure; friable, slightly sticky, slightly plastic; thin continuous clay films; strongly acid; clear smooth boundary. (8 to 10 inches thick) Bt2--25 to 36 inches; yellowish brown (10YR 5/8) heavy sandy clay loam, few fine and medium distinct (7.5YR 5/6) strong brown and yellowish red (5YR 4/6) mottles; moderate medium subangular blocky structure; friable, slightly sticky, slightly plastic; thin continuous clay films; strongly acid; gradual smooth boundary. (10 to 14 inches thick) Bt3--36 to 42 inches; mottled yellowish brown (10YR 5/8), strong brown (7.6YR 5/8), and yellowish red (5YR 5/8) sandy clay loam; weak medium subangular blocky structure; friable, slightly sticky, slightly plastic; thin patchy clay films on vertical faces of peds; few fine flakes of mica; strongly acid; gradual wavy boundary. (0 to 8 inches thick) BC--42 to 48 inches; mottled yellowish brown (10YR 5/4), strong brown (7.5YR 5/6), and yellowish red (5YR 5/8) sandy clay loam; weak medium subangular blocky structure; friable; few fine flakes of mica; few bodies of sandy loam; strongly acid; gradual wavy boundary. (5 to 12 inches thick) C--48 to 60 inches; mottled yellow, yellowish red, and pale brown saprolite that crushes to sandy loam; rock structure; friable; strongly acid. TYPE LOCATION: Wake County, North Carolina; five miles south of Rolesville, North Carolina, on county road 2227, 1/4 mile east of Bethany Baptist Church at junction of county road 1003; 50 feet north of road in cultivated field. RANGE IN CHARACTERISTICS: The thickness of the loamy horizons over saprolite range from 40 to more than 60 inches below the surface. Depth to bedrock is more than 5 feet. Coarse fragments range from 0 to 5 percent throughout. The soil is strongly acid or very strongly acid except where the surface has been limed. The A or Ap horizons have hues of 7.5YR, 10YR, and 2.5Y, value of 4 to 6, and chroma of 1 to 3. The BA horizon as hue of 10YR and 2.5Y, value of 6 to 8, chroma of 1 to 4. The A horizon is loamy coarse sand, loamy sand, sandy loam, or fine sandy loam. Where present, BA and BE horizons of sandy loam are pale brown, brownish yellow, brown, or light yellowish brown. The Bt horizon has hue of 7.5YR, 10YR, or 2.5Y, value of 5 to 8, and chroma of 4 to 8. It has few to common reddish, brownish, or yellowish mottles. Mottles in chroma of 2 or less are below the upper 20 inches of the Bt horizon. It is sandy clay loam or clay loam. Some pedons have lower Bt horizon of sandy clay, but the textural control section averages less than 35 percent clay. The BC horizon is similar in color to the Bt horizon except where the mottles are more contrasting. It is sandy loam, sandy clay loam, or clay loam. The B3 horizon contains weatherable minerals such as mica and feldspar. The C horizon is mottled or varicolored saprolite of acid crystalline rock. It is sandy loam or loamy sand. COMPETING SERIES: These are the Apison, Cahaba, Cowarts, Emporia, Euharlee, Granville, Hartsells, Kempsville, Linker, Marvyn, Nauvoo, Nectar, Pirum, Spadra, and Suffolk series. Apison, Hartsells, Linker, and Pirum soils have bedrock at depths less than 40 inches. Cahaba, Nauvoo, and Nectar soils have redder hue. Cowarts, Emporia, Kempsville, Marvyn, Spadra, and Suffolk soils lack weatherable minerals in the lower solum and have C horizons of Coastal Plain or old alluvial sediments. Euharlee soils contain more silt. Granville soils are higher in exchangeable aluminum. GEOGRAPHIC SETTING: Durham soils are on nearly level to sloping Piedmont uplands. Slopes are commonly 2 to 5 percent and range from 0 to 10 percent. Durham soils formed in residuum weathered from acid crystalline rocks, chiefly granite and gneiss. Mean annual precipitation is about 47 inches and the mean annual temperature is about 60 degrees F. near the type location. GEOGRAPHICALLY ASSOCIATED SOILS: These are the Appling, Cecil, Helena, Louisburg, Pacolet, Vance, Wedowee, and Worsham series. Appling, Cecil, Helena, Pacolet, Vance, Wedowee, and Worsham soils contain more clay and Louisburg soils contain less clay. Helena and Worsham soils have mottles with chroma 2 or less in the upper 20 inches of the control section and occupy lower positions on the landscape. DRAINAGE AND PERMEABILITY: Well drained; medium runoff; moderate permeability in upper subsoil and moderately slow permeability in lower subsoil. USE AND VEGETATION: About two thirds of the total acreage is in cultivation or pasture. The remainder is in mixed hardwood and pine. Common crops grown are corn, soybeans, tobaco, cotton, small grain, and vegetables. Native tree species include loblolly pine, short leaf pine, Viginia pine, sweetgum, whiteoak, red oak, post oak, hickory, and yellow-poplar. Understory species include flowering dogwood, persimmon, sourwood, red maple, eastern redbud, eastern redcedar, and common sassafras DISTRIBUTION AND EXTENT: Piedmont of North Carolina, Alabama, Georgia, South Carolina, and Virginia. The series is of moderate extent. MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Raleigh, North Carolina SERIES ESTABLISHED: Raleigh to New Bern Area, North Carolina, 1900. REMARKS: Durham soils were formerly placed in the Red-Yellow Podzolic great soil group. They ranged in texture of the B horizon from moderately-fine to fine, and in drainage from well drained to moderately well drained. This revision restricts the texture of the argillic horizon to fine-loamy and the drainage class to well drained. Here is a link that might be useful: Cecil soil (probably what you have)...See Morekimmq
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