Soil - Sarasota County Extension

sarasota.ifas.ufl.edu

Soil - Sarasota County Extension

Community GardeningOrganic Vegetable Gardening*Soil Management*Robert KlusonAg/NR Extension AgentUF/IFAS Sarasota County Extension


Syllabus of Presentation Series• Introduction to Organic VegetableGardening• Soil Management• Crop Management• Pest Management• Water Management• Cover Crops• Advanced Composting


Introduction• Goals of Presentation Series– Food for your freshest nutrition– Food for expanded community benefits– Food for thought– Food for your soul


Introduction• Approach of this presentation– Provide the concepts, and science fromagroecology of soil management practicesused in organic vegetable gardening– Provide resources in the managementpractices of soils and plant nutrition, inaddition to our text “Vegetable Gardening inFlorida” by James Stephens, UF/IFAS


Soil Appreciation Through History• “Soil Is The Mother Of All Things” . . .Chinese proverb• “Mother Earth” . . . similar expressions inmany cultures• Bierman, OSU; http://www.ag.ohio-state.edu/~prec/soil/slides/• “Feed the soil, not the plants” . . . organicfarming adagehttp://newfarm.rodaleinstitute.org/columns/research_paul/2005/1105/feedsoil.shtml


Food For The Soul"If fresh food is necessary tohealth in man and beast, thenthat food must be providednot only from our own soil butas near as possible to thesources of consumption."-Lady Eve Balfour


Soil Ecosystem & Plant Growth


Organic Vegetable Garden EcologyGarden Agroecosystem Examplecropspestssoil• Soil ecosystems have functional properties &subsystems (e.g., nutrient cycling,etc) from biodiversity


Agroecosystem Concept• An approach that looks at your vegetablegarden as a functional whole of interactingliving and non living components•• Analogy to the human body and its interactinglevels of molecules, cells, tissues, organs, andsystems.• Properties include:– Structural & functional levels– Hierarchical and temporal scales– Emergent properties - i.e., “whole is more than•sum of parts”Gliessman, S., 1999. Agroecology: Ecological Processes in Sustainable Agriculture


Soil Ecosystem ‘Emergent’Property Examples• Aggregation• Soil profile development• Nutrient cycling• Biotic mutualisms• Organic matter• Soil ‘quality’ and ‘health’Gliessman, S., 1999. Agroecology: Ecological Processes in Sustainable Agriculture


Aggregation Example• Soil structure– how components are held together not justcomposition– Indicator of good “tilth”– improved by root growth and organic matter– reduced by compaction and increased densityGershuny &Smillie, 1995,Soul of Soil.


Water Stable Aggregates• Formed by the aggregation of non-living(e.g., clay) and living (e.g., gluing togetherof macro-aggregates with bacterialsecretions, fungal hyphae, and root hairbonding) components.


Soil Profile Example• Arrangements oflayers or “horizons” ofsoils with particularcharacteristics.• Product of living andnon-living factors• Indicator of soil types,landscapes & ecosystemsExample: “Myakka fine sand”


Soil Survey Resource• Soils information for land use planning• Highlights soil capabilities/limitationsfor many different users• Intended for a general level application• Available at county level• Accessible onlineGo to http://websoilsurvey.nrcs.usda.gov/app/


Soil Nutrient Cycle Example


Biotic Mutualism Example: Mycorhizae Myco (fungi) + rhizae (root) Serves as an expanded root system thatprovides water and nutrient benefits to plant hostPfleger and Linderman, 1994, Mycorrhizae and Plant Health.


Biotic Mutualism Example:Nitrogen-Fixing Bacteria• Nodulesformed whereRhizobiumbacteriainfected rootsof legumecrops• Convertsatmosphericnitrogen forplant uptake


Organic Matter• Influences almost all importantproperties that contribute to soilquality!• Range of values– Temperate soils have higher OM levels(5-10%)– Tropical soils generally have 0.5-1.0%(e.g., FL upland soils in native condition)


Soil Organic Matter• Composition– all living organisms(microorganisms,earthworms, etc),– fresh residues (oldplant roots, cropresidues, recentlyadded manures),– well-decomposedresidues (humus).Soil Resource Webpage, Univ. of MNhttp://www.soils.umn.edu/academics/classes/soil2125/


Soil Organic Matter Ecology• OM additions startrapid multiplicationof bacteria, fungi,and actinomycetes• As most readilyavailable energysources are used up,microorganismsagain becomerelatively inactive,• Leaving behind adark mixture usuallyreferred to ashumus – a stableorganic compoundSoil Resource Webpage,Univ. of MN, http://www.soils.umn.edu/academics/classes/soil2125/


Humusa mixture of compounds and complex lifechemicals of plant, animal, or microbial originthat are resistant to decomposition and include:Fulvic AcidsHumic Acids


Function of Humus• increases water holding capacity• sticks together & helpsestablish and maintain a strongcrumb structure & aidsinfiltration• provides some nutrients (N & P)as it is slowly decayed bymicrobial activity at the rate of2.5% per year• buffers pH changes• creates good soil “ Tilth”• holds nutrients by increasingcation & anion exchangecapacity, and chelating capacityHumus =HighMediumLow


Composting• Art & science of producing stableorganic matter soil amendment by:– mixing organic materials properly– monitoring resultant biological activity• Types– aerobic– anaerobic digestion– worm (vermicomposting)


Composting Literature• Walt Whitman, “Behold This Compost” (1855)– A celebratory poem in his seminalbook ‘Leaves of Grass’“Something startles me where I thought I was safest,I withdraw from the still woods I loved . . .How can you be alive you growths of spring?How can you furnish health you blood of herbs, roots, orchards, grain?Are they not continually putting distemper'd corpses within you?Is not every continent work'd over and over with sour dead?Where have you disposed of their carcasses? . . .Behold this compost! behold it well!Perhaps every mite has once form'd part of a sick person--yet behold!The grass of spring covers the prairies,The bean bursts noiselessly through the mould in the garden,The delicate spear of the onion pierces upward, . . .What chemistry! . . .”http://classiclit.about.com/library/bl-etexts/wwhitman/bl-ww-thiscompost.htm


Composting Literature• Sir Albert Howard, “An AgricultureTestament” (1943)– Introduced Indore Compost MakingProcess– Foundation of organic gardening/farming• J.I Rodale, “Complete Book ofComposting” (1960)– Father of US organic gardening/farming


Aerobic Composting• Organic materials– carbon:nitrogen ratio = 30:1– less than 2-3 inches particle size– moisture (40-60 %)• Pile building and management– layers– aeration– volume (3’x3’x3-6’)• Monitoring– temperature rise (minimum 131 o F for 3 days)• Management– mixing/turning– finishing/curing– screening– maturity testsGo to http://compostinfo.com/


Aerobic Composting


Aerobic Composting


Aerobic Composting


Aerobic Composting


Soil Quality DefinitionSoil FertilityPhysical PropertiesBiological Activity“The ability of soil to function; to supplyplants with adequate nutrients, have gooddrainage and aeration, promote root growthand biological activity.”


Soil Health Definition• Definitions– Interactions between soil qualityand plant/animal/human quality– Sustaining and improving soilquality over the long term


What Is Soil?Soil will be studied as an ecosystemKourik, 1986, Designing & maintaining edible landscape naturally.


What is Soil?• 2 MAJOR PERSPECTIVES• Pedological (holistic) - a product of naturebased on– climate– living organisms– nature of parent material– topography of area– time• Edaphological (reductionistic) – a habitat forplants (e.g., for food/fiber production &landscapes)Brady, N.C. & R.R. Weil, 2003, Nature and Properties of Soils


What is Soil?• A Mixture of Components• Pore Space 50% (v) Solids 50% (v)– water - minerals– air - organic matterBrady,1974,Nature andPropertiesof Soils


Soil Mineral Components• Sand: largeparticles,0.05-2.0 mm indiameter.• Silt: mediumparticles, 0.002-0.05 mm. Settleswithin 48 hours.• Clay: extremelysmall particles,less than 0.002mm.


• MineralcompostiondeterminesSoil TextureClass• Florida gardensoils aretypically indifferent sandtextureclassesSoil Triangle


Textures Affect CapacitiesSand -Clay -Low LowHigh High


Soil pH• The measure of acidity or alkalinity ofthe soil• Determines the concentration ofnutrients in solution in the soil water(availability of nutrients for the plant)


Soil pH and Nutrients Availability


Adjusting Soil pH• To raise soil pH (make more alkaline): applylime (calcium carbonate) or dolomite(magnesium carbonate) - carbonatecompounds• To lower soil pH (acidify) temporarily: applyelemental sulfur compounds.• To add calcium or magnesium withoutchanging soil pH: use sulfate compounds(ex.: gypsum = calcium sulfate)


Plant Nutrition Concepts


• Principle of Limiting Factors–Justus von Liebig (1803-1873)• The research of the “father of the agricultural fertilizer industry”also acknowledged the importance of soil organic matter


Plant Nutrition Deficiencies


UF/IFAS Plant NutritionalDeficiencies WebsiteNitrogenMagnesium• User-friendly “decision tree” database• Ornamental plant examples primarily• Online at http://hort.ifas.ufl.edu/nutdef/


Plant Nutrition DeficiencyIdentification Caveats• Changes can be normal part of aplant’s cycle, e.g., iris foliage diebackor fall leaf colors• Often related to other problems– Pesticides– Disease– Insects– Soil factors– Environment (rainfall, wind, cold, etc)• In order to treat the problem, firstnecessary to diagnosis it correctly


Soil Chemistry & Plant NutritionPotassium(K)Example


Rhizosphere and Plant NutritionOMRoot TipRoot tip & OM contactRhizosphere OM decomposition Rhizosphere & protozoa Protozoa N wastes Clarhom, M.C., 1985Root uptakeof N wastes


Soil Life And Plant RootsCurl, E.A. & B.T. Truelove, 1986, The Rhizosphere.


Soil Life in Soil ProfileKourik, 1986, Designing & maintaining edible landscape naturally.• Protect topsoil as habitat for optimum soil life


Soil As Habitat for Biodiversity


EARTHWORMS• Earthworms dramatically alter soil propertiesfor growing conditions favorable for crop plants


Earthworm Benefits• Stimulate microbial activity• Mix and aggregate soil• Increase infiltration• Improve water-holding capacity• Provide channels for root growth• Bury and shred plant residue


Soil Testing• Program that includes:– nutrient analyses and interpretation– fertilizer & amendment recommendations– other considerations• salinity• elemental toxicity• Soil Testing Labs– UF/IFAS Soil Lab(http://soilslab.ifas.ufl.edu/)– Alternative Soils Labs(http://attra.ncat.org/attra-pub/soil-lab.html


Soil Sampling• Representative sample = goal• Sample separately distinct areas


Soil Sampling


Soluble Salts Testing• Soil soluble salt levels are generallyclassified as damaging in the followingways:– 2100 ppm = very damaging levels, tolerableonly by the most salt-tolerant plants• As reference:– Fresh water (


Alternative Soil Test Example• Soils, crops and livestock require balanced nutrition for health, justas people need a balanced diet to stay healthy. Organic farmersstrive to provide a 'balanced diet" for their farms by adding a varietyof organic materials and natural mineral amendments to the soil.M. Schonebeck, Soil Cation Nutrient Balancing in Sustainable Agriculturehttp://www.vabf.org/infosht.php


Alternative Soil Test Example“The Solvita® soil-life test kit provides animportant new tool for gardeners, farmers andscientists to evaluate soil microbial respiration ratein an efficient and cost-effective manner. Soilrespiration is an important aspect of soil qualityand a good indicator of soil fertility.”“The Solvita test enables you to:•estimate annual nitrogen release based on soilbiological activity•evaluate organic matter sufficiency of soils•make overall judgements to fit into "soil quality"interpretation•achieve accuracy comparable to and less expensivethan Dräger tubes”


Soil Respiration Rate –the reality• More CO2 (carbon dioxide) coming off thesoil means the soil is respiring (breathing)more. This indicates either a high rate ofrespiration of existing organisms, or highnumbers, or both.• Having more organisms is a good thing, but ahigh respiration rate also means your soilsystem is burning off carbon…which lowersyour organic matter levels, which is a badthing.• High respiration rate is a result of optimaltemperatures, moisture, and aeration,sometimes as a result of tillage.


Alternative Soil Test ExampleHumus Testing[using LaMottehumus index test.]Newer garden soil withmulch = 1.0Improved garden soil =3.0Fresh worm compost = 5Near-by ag field (withsubsoil) = 0


Alternative Soil Test Example


AlternativeSoil TestExample


Summary• Organic vegetable gardeningfundamentally depends ondeveloping a functional soilecosystem• Practices are designed toenhance soil quality and health• “Feed the soil so that the soil canfeed the plant”


• Cornell Soil HealthAcknowledgementshttp://www.hort.cornell.edu/soilhealth/• Janke, R., Sustainable Cropping Systems, KSU– Soil qualitywww.oznet.ksu.edu/rff/Soil%20Quality%20NEW.ppt– Soil tests interpretationswww.oznet.ksu.edu/rff/Soil%20Test%20Interpretation.ppt• Stromberger, M. Composting Organisms, CSUhttp://www.extsoilcrop.colostate.edu/Soils/powerpoint/compost/CompostingOrganisms.pdf• USDA NRCS Soil Quality Institutehttp://soils.usda.gov/sqi/index.html

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