On-Farm Benefits of Soil Organic Matter - Discovery LINKS connecting science to the farm
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Discovery LINKS connecting science to the farm Summer 2013 ARDF Bulletin 5 On-Farm Benefits of Soil Organic Matter Neal Mays I f one soil characteristic were to be nutrients, as well as water, as SOM named which most affects soil quality, levels increase. health, and productivity, it would prob- ably be soil organic matter. The physical, • Soil organic matter is approximately chemical, and biological condition of soil 58% carbon. may be enhanced or degraded by land • Soil organic matter is the substance management practices which either create that gives most rich, productive soils or destroy soil organic matter. Increasing their dark color. soil organic matter content on ordinary crop or pasture land often takes years to accomplish, and if the soil surface is left Soil Organic Matter: Cropping Benefits exposed during a heavy rain, productive • Improves water infiltration and reduces topsoil can be gone in a matter of hours, the likelihood of runoff, soil crusting, even minutes. and soil erosion. • Improves soil air flow and increases General Facts about Soil Organic Matter plant available water, which can reduce (SOM) drought stress. • Soil organic matter arises primarily • Decreases soil bulk density and pene- from decomposed plant matter, but tration resistance, improving the ability decomposed animal and soil microbial of root systems to grow and develop. tissues also contribute. • Increases the content of water stable • The soil microbial community is aggregates in soil. Most soils are crumb- responsible for converting plant and like after cultivation and have high animal tissue into humus, another levels of SOM. name for stable forms of soil organic matter. • Improves soil fertility by adding nutri- ents to soil as residues decompose, and • In order to increase SOM, soil nitro- by supporting a healthy soil microbial gen (N), phosphorus (P), and sulfur community, which converts some (S) concentrations must be sufficient to nutrients to plant-available forms. Arkansas Discovery support a healthy soil microbial Farms Program community. • May reduce the need for pesticide Department of applications as the soil food web Crop, Soil, and • As SOM increases, soil N diversifies and populations of beneficial Environmental Sciences concentration normally increases, as 115 Plant Sciences Bldg. organisms increase do levels of other nutrients required University of Arkansas • Improves ground and surface water Fayetteville, AR 72701 for plant growth. There is greater soil storage capacity for these valuable quality by improving the filtering Phone: (479) 575-2354 Fax: (479) 575-3623 capacity of soil.
Crop residues decompose and build SOM, while protecting the soil surface from crust formation and reducing erosion. Photo by Gene Alexander, USDA Natural Resource Conservation Service. Soil organic matter probably has as much impact on soil Increasing Grassland Productivity fertility and productivity as any measured soil property. Maintaining or increasing its level in your soils is akin to • Creating or enhancing mixed grass/legume stands using coupons at the grocery store or keeping your enhances soil microbial diversity and soil health, vehicle running properly. These prac-tices either rendering the soil more capable of cycling nutrients directly save money now or limit how much you spend between soil and plant and increasing productivity later on, and managing SOM is also a money-saving of the land. Soil microorganisms obtain much of endeavor. In grazed pastures and grassland, SOM may their energy from SOM. increase more rapidly than on hayed land, because of • Pay attention to manure deposits. Heavy manure nutrient redistribution in the field. deposits in a loafing area are not an efficient return of nutrients to the pasture. Valuable N and P Increasing Soil Organic Matter Increases may accumulate to extreme levels and be lost due Soil Fertility to leaching through the soil or as runoff during storms. Significant amounts of N can also be lost as • SOM effectively works like a bank for plant nutri- a gas into the atmosphere when N is over-applied ents. The higher its content, the more potential for and soils remain wet. nutrient “investments,” and the more “tell-ers” there are to distribute nutrients to plants as they • Creating a grazing plan in which you control where need them. On soil test reports, this activity is the cattle spend their time, and in turn deposit their referred to as CEC (cation exchange capac- manure, is an effective nutrient management and ity). Mineral soils with high SOM generally have a redistribution plan. higher CEC. • Maintain an appropriate stocking rate. A classic • Organic forms of N and P naturally found in SOM forages textbook recommends “take half and leave are routinely changed to plant available forms by half” of the forage produced. Overgrazing damages soil microorganisms. The SOM to N ratio for many and can kill established grasses and legumes. soils is around 20:1, and the top 6 inches of an acre • Fence cattle out of ponds and streams, while of soil is often estimated to weigh around 2,000,000 providing alternative sources of clean water. This pounds. Using these estimates, increasing SOM practice can help prevent erosion and degradation content from 2% to 3% could yield an additional of adjacent grazing land. 1000 pounds of total N per acre, some of which would be plant available. In cropland, conservation tillage and other SOM- building practices have been the backbone of some • Some studies show intensive grazing techniques can farm management plans for years. In a series of essays, improve pasture SOM, as much as 0.35% each year. 2
U.S. and Canadian farmers explained their commit- Economic Benefits of No-Till or Reduced Till: ment to land management practices that increase • fewer and smaller tractors required, SOM and soil carbon. The following are direct obser- vations made by these individuals, regarding both the • less wear on equipment; fewer trips across field, challenges and benefits associated with limited tillage1. • both of the above yield reduced fuel consumption, Challenges Created by No-Till or Reduced Till: • reduced labor cost, • weed control; shift to perennial weed species, • reduced time in the field, • increased soil compaction initially, • can enter wet fields earlier, • reduced yield between years 2 and 5 after changing • more consistent yields; dry years are better, and to no-till, • crop stubble protects seedlings. • increased tire wear, particularly with corn and bean stubble, Soil and Environmental Benefits of No-Till • cooler soils; affecting planting date, variety selec- or Reduced Till: tion, and creating pest problems (animals, insects, • increase in soil organic matter, of up to 0.5% each year, disease), • reduction in bulk density, • heavy residue can limit creating a good seedbed, and • greater water infiltration, • starter fertilizer program needed to ensure seedling vigor • reduced soil crusting, runoff, and erosion, • improved soil condition, • moisture conservation and reduced irrigation needs, • long term fertility programs become more stable, • improved wildlife habitat, and • water quality can be improved, as long as nutri-ent management is adapted to avoid accumulation of phosphorus, particularly at the soil surface if fertilizer and/or manure continues to be broad-cast. Injection or shallow incorporation of added fertilizer nutrients should be encouraged to avoid nutrient enrichment of surface runoff. Soils with high SOM do not readily slake (fall apart) when wetted. Soil aggregates are stabilized by the C-based compounds in hu- mus, which is a “glue” holding soil particles together. The soil on the right would be more likely to crust after a heavy rain, whereas the soil on the left would retain much of its granular appearance. Photo courtesy of USDA-NRCS. 3
Conclusions Implementing farm management strategies which allow plant residues to remain on the soil surface or in the root zone have been shown to increase SOM levels. Soil quality is improved as SOM increases, resulting in increased soil productivity, and increases in SOM enhance cropping sustainability, resulting in a soil whose physical, chemical, and biological condition favors crop growth with each new season. “The success of generational farming relies solely on the stewardship of the present generation. Soil health is our primary concern, and we are constantly look- ing for methods of ‘growing’ our soils to higher levels of biodiversity. In other words, to work in harmony with natural processes, versus trying to subdue and control them with commercial heavy iron, will keep more of our natural resources in place for the next generation.” — Kenneth J. Cain, Darlington, Indiana1 Vigorous pasture growth satisfies the nutritional needs of grazing livestock. The extensive root system of pasture grasses 1 On-farm Benefits of Carbon Management: the Farmer’s release carbon-rich compounds into soil and eventually die and Perspective, p. 45-65. In: Soil Carbon Management: Economic, decompose , thereby increasing SOM levels. Overgrazed, sparsely Environmental and Societal Benefits, 2007, CRC Press, Boca vegetated pastures tend to have lower SOM. Photo by Lynn Raton, FL. Betts, USDA Natural Resource Conservation Service.
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