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Content and lab derived from the USDA-NRCS Guides for Educators. Go to www.nrcs.usda.gov/soils for the Guides and additional pictures and diagrams. This lesson plan was adapted for South Dakota from the University of Nebraska Institute of Agriculture and Natural Resources, CROPWATCH. South Dakota Natural Resources Conservation Service South Dakota FFA January 2018 Approximately 180 minutes Objectives By the end of the lesson, students will know or be able to: • Define soil respiration and soil microbes • Explain the role of soil respiration in determining soil health • Diagram the role of soil respiration in the cycle of life on earth • List and explain inherent factors that affect soil respiration • List and describe soil respiration management processes • Interpret management impacts on soil respiration and soil organic matter • Measure soil respiration and interpret data Materials • Lab materials (see Lab Guided Notes) • Baggie that seals • Plant cutting Preparatory Work • Place a plant cutting in a plastic baggie several hours prior to teaching this lesson so that respiration is visible Soil Biology Respiration Soil biology respiration refers to the production of carbon dioxide when soil organisms respire. This includes respiration of plant roots, the rhizosphere, microbes and fauna. Soil biology respiration is a key ecosystem process that releases carbon from the soil in the form of CO 2 . CO 2 is acquired from the atmosphere and converted into organic compounds in the process of photosynthesis. Plants use these organic compounds to build structural components or respire them to release energy. When plant respiration occurs below-ground in the roots, it adds to soil respiration. Over time, plant structural components are consumed by the biota in the soil which then releases CO 2 . When this CO 2 is released by below-ground organisms, it is considered as soil respiration. The amount of soil respiration that occurs in an ecosystem is controlled by several factors. The temperature, moisture, nutrient content and level of oxygen in the soil can produce extremely disparate rates of respiration. These rates of respiration can be measured in a variety of methods. Soil biology respiration rates can be largely affected by human activity. This is because humans have the ability to and have been changing the various controlling factors of soil respiration for numerous years. Tillage and fertilization by humans also has the potential to affect respiration rates.

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Page 1: Soil Science Curriculum€¦ · Soil Biology Respiration 2 Label the Information (Approximately 4 minutes) Direct students to their Guided Notes and encourage them to capture the

Soil Science CurriculumContent and lab derived from the USDA-NRCS Guides for Educators. Go to www.nrcs.usda.gov/soils for the Guides and additional pictures and diagrams. This lesson plan was adapted for South Dakota from the University of Nebraska Institute of Agriculture and Natural Resources, CROPWATCH.

South DakotaNatural Resources Conservation Service South Dakota FFA

January 2018

Approximately 180 minutes

ObjectivesBy the end of the lesson, students will know or be able to:

•Definesoilrespirationandsoilmicrobes•Explaintheroleofsoilrespirationindeterminingsoilhealth

•Diagramtheroleofsoilrespirationinthecycleoflifeonearth

•Listandexplaininherentfactorsthataffectsoilrespiration

•Listanddescribesoilrespirationmanagementprocesses

• Interpretmanagementimpactsonsoilrespirationandsoilorganicmatter

•Measuresoilrespirationandinterpretdata

Materials•Labmaterials(seeLabGuidedNotes)•Baggiethatseals•Plantcutting

Preparatory Work•Placeaplantcuttinginaplasticbaggieseveralhourspriortoteachingthislessonsothatrespirationisvisible

Soil Biology Respiration

Soilbiologyrespirationreferstotheproductionofcarbondioxidewhensoilorganismsrespire.Thisincludesrespirationofplantroots,therhizosphere,microbesandfauna.

SoilbiologyrespirationisakeyecosystemprocessthatreleasescarbonfromthesoilintheformofCO2.CO2isacquiredfromtheatmosphereandconvertedintoorganiccompoundsintheprocessofphotosynthesis.Plantsusetheseorganiccompoundstobuildstructuralcomponentsorrespirethemtoreleaseenergy.Whenplantrespirationoccursbelow-groundintheroots,itaddstosoilrespiration.Overtime,plantstructuralcomponentsareconsumedbythebiotainthesoilwhichthenreleasesCO2.WhenthisCO2 isreleasedbybelow-groundorganisms,itisconsideredassoilrespiration.

Theamountofsoilrespirationthatoccursinanecosystemiscontrolledbyseveralfactors.Thetemperature,moisture,nutrientcontentandlevelofoxygeninthesoilcanproduceextremelydisparateratesofrespiration.Theseratesofrespirationcanbemeasuredinavarietyofmethods.

Soilbiologyrespirationratescanbelargelyaffectedbyhumanactivity.Thisisbecausehumanshavetheabilitytoandhavebeenchangingthevariouscontrollingfactorsofsoilrespirationfornumerousyears.Tillageandfertilizationbyhumansalsohasthepotentialtoaffectrespirationrates.

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Label the Information (Approximately 4 minutes)DirectstudentstotheirGuidedNotesandencouragethemtocapturethefollowinginformation.

•Soilrespirationisameasureofthecarbondioxidereleasedfromthesoilbymicrobesdecomposingsoilorganicmatterandfromtherespirationofplantroots.

•Soilrespirationindicatessoilhealth(soilorganicmattercontent,soilorganicmatterdecompositionandthelevelofmicrobialactivity).

• SoilMicrobes:Soilorganismsthatareresponsibleforsoilrespirationandmanyimportantsoilprocessessuchasnutrientcycling.

• Respiration:Releaseofcarbondioxidefromseveralsources(decompositionofsoilorganicmatterbysoilmicrobes,andrespirationfromplantroots).

• Mineralization:Organicmatterdecompositionreleasingnutrientsinaplantavailableformthatoccursduringrespiration.

• Ammonification:Productionofammoniumfromsoilorganicmatterdecomposition.• Denitrification:Anaerobicconversionandlossofnitrate-nitrogentonitriteandnitrogenvarieties ofgases.• Nitrification:Anaerobicmicrobialprocessconvertingsoilammoniumnitrogentoplant availablenitrate.

Provide the Experience – Key Terms and Soil Health (Approximately 5 minutes)Separatestudentsintosmallgroupsofthreeorfour.

Provideeachsmallgroupwithasoilsample.(Itwillbehelpfulifsomeofthesampleshavebugs,worms,cropresidueorotherlivingorganismsinthem.)

Instructsmallgroupstoinvestigatetheirsoilanddeterminewhatinthesoilaffectstherespirationthatoccursinthesoil.Elicitstudentresponses.

Enroll the Participants (Approximately 4 minutes)Showorpassaroundthesealedbaggiewiththeplantcuttinginsideofit.Inquiretostudentsastowhattheyknowaboutwhythewaterdropletsformedinsideofthebaggieeventhoughyouplacedonlyaplantcuttinginsideofthebaggie.

Holdupthesecond(empty)plasticbaggieandbreatheintoittodemonstratetheformationofwaterdropletsbecauseofyourbreath.Again,inquireaboutwhatstudentsknow.

Contenttoshare:

•Livingorganismsconducttheprocessofrespiration.•It’seasytoseesignsthatahumanisbreathing (arisingchestorabdomen,soundofbreathing,feelofbreath,etc.)•Wecanseethatplantsarebreathingthroughthecuttinginthebaggie

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Demonstrate the Relevance (Approximately 7 minutes)Instructstudentstotalktogetherandformulateideasabouthowsoilorganicmatterandrespirationaffectsoilhealth.

Elicitresponses,fillinginthefollowinginformation.

•Respirationratecanbebasedontheamountofsoilorganicmatterpresent.- Soilorganicmatterisafoodsourceformicrobesandwhenmicrobesarepresentandworking,respirationishigher.

- Whensoilorganicmatterisabsentorlow,thereislessdecomposingactivity.- Soilmicrobesareresponsibleforsoilrespirationandmayimportantsoilprocesses(suchasbacteria,fungi,protozoa,algae).

- Oneheapingtablespoonofsoilcancontainoverninebillionmicrobes,morethanallthepeopleonearth.

Sharethefollowingdiagram.Encouragestudentstocompletethediagramintheirguidednotes.

Provide the Experience – Factors Affecting Soil Respiration (Approximately 5 minutes)Instructstudentstoworkinsmallgroups.Provideeachsmallgroupwithoneofthefollowingfactorsthataffectsoilrespiration.Instructstudentstodiscusshowtheirgroup’sfactormightaffectsoilrespiration.

Factors: Climate/Weather Biologicalactivity Soilmoisture Amountandhealthofsoilorganicmatter Soil texture

Plants

Food+OxygenSunWater+CarbonDioxoide

Soil

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Label the Information (Approximately 7 minutes)SoilRespirationManagementPractices

1.Leavecropresiduesonthesoilsurface.a.ResidueswithlowC:NratiosdecomposefasterthanthosewithhighC:Nratiosb.Highresiduecrops+addedNitrogen=higherdecompositionratesandaccrualoforganicmatter

2.Useno-tillpractices.a.Tillingdecreasessoilbiologywhichthenslowsdecompositionoforganicmatterb.Minimizeequipmentuseinfieldsc.Minimizefarmequipmentuseingeneralwhensoilsarewetd.Usedesignatedlocationsforequipmenttraffic

3.Usecovercrops.a.Rootsproviderespiration

4.Addorganicmatter.a.Nourishesmicrobes

5.Plantlongseasoncrops.a.Providesalivingrootfortheentiregrowingseasontomaximizesoilbiology

Demonstrate the Relevance (Approximately 5 minutes)Facilitateadiscussionwithyourstudentsaboutthelargereconomiceffectsofpoorsoilrespiration.Dependingonthedemographicsofyourstudents,usereferencesthatmakesensetothem–farmingorfromthestandpointofaconsumer.Considerusingthefollowingquestionsasaguide:

Howcanpoorsoilrespirationaffectafarmerwhoseincomedependsonthecropgrowninthatsoil?Howcanpoorsoilrespirationaffectthepricesweseeforourfoodinthegrocerystore?

Provide the Experience – Soil Respiration Management (Approximately 3 minutes)Continuethefacilitateddiscussionbyaskingthefollowingquestion:

Whatdoyouthinkwecandoasproducersandconsumerstoensureaproductivesoilrespirationrate?

Label the Information (Approximately 10 minutes)•Climate/Weather

-Cannotbechanged-Affectstemperature,moistureandindirectlyaffectsbiologicalactivity

•Biologicalactivity-Varieswiththeseasonsandtimesofday

•Soilmoisture-Asmoistureincreases,respirationratesincreaseuntiltheporesareoverlysaturated,resultinginloweroxygencontentandlowersoilorganismrespiration-Sixtypercentporespacesaturation(fieldcapacity)isidealforrespiration-Drysoilshavelowrespirationratesbecauseoflesssupportforbiologicalactivities

•Amountandhealthofsoilorganicmatter-Affectsmicrobeactivity

• Soil texture-Clay–soilorganicmatteris“protected”fromdecomposition-Sand–toolittleorganicmatter-Mediumtexture(siltandloam)–favorableforsoilrespiration

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Demonstrate the Relevance (Approximately 15 minutes)DirectstudentstothefollowingchartintheirGuidedNotesandinstructthemtolistsomeshorttermandlongtermimpactstheycanthinkofforeachmanagementpracticeandapplication.Usethekeybelowtofacilitatethediscussionafterashorttime.

Management Practice

Application Short Term Impacts Long Term Impacts

Solidmanureororganicmaterialapplication

Provide additional carbonandnitrogensourceformicrobestobreakdownandincreasebiomassproduction.

HighresiduecropsorcovercropsusedinrotationwithhighC:Nratio

HighC:Nratiocropsandaddednitrogenincreasedecompositionandaccrualofsoilorganicmatter.

Tillagesuchasannualdisking,plowing,etc.

Stirsthesoilprovidingatemporaryincreaseinoxygenformicrobestobreakdowncarbonsources.

Cropresiduemanagement

Leave residue on the surfaceincreasinggroundcovertoprotectthesoil.

Nitrogenfertilizerormanureapplication

Providesnitrogen(energy)sourceformicrobestobreakdownhighC:Nratioresiduequicker.

Vehicleorfarmequipmenttraffic

Compactssoildecreasingporespace,watermovement,oxygenformicrobesandnitrogenlossfromdenitrification.

Table 1.InterpretingmanagementimpactsonsoilrespirationandSoilOrganicMatter(SOM).

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Management Practice Application Short Term Impacts Long Term Impacts

Solidmanureororganicmaterialapplication

Provideadditionalcarbonandnitrogensourceformicrobestobreakdownandincreasebiomassproduction.

Increasedrespirationwhenmanurebeginstobreakdownandincreasedbiomassproduction.

Positiveimpactonsoilstructure,fertilityandsoilorganicmattercontent.

HighresiduecropsorcovercropsusedinrotationwithhighC:Nratio

HighC:Nratiocropsandaddednitrogenincreasedecompositionandaccrualofsoilorganicmatter.

HighC:Nratiocropresiduetieupnitrogentemporarilyinordertobreak down residue, increasedsoilmoisture,decreasederosion.

Positiveimpactonlongtermsoilhealth,fertilityandsoilorganicmattercontent.

Tillagesuchasannualdisking,plowing,etc.

Stirsthesoilprovidingatemporaryincreaseinoxygenformicrobestobreakdowncarbonsources.

Providesaflushofnitrogen,othernutrientsandcarbondioxidereleaseimmediatelyaftertillage.Increaseserosionrates,decompositionrate of residue, and other carbonsources.

Declinesinsoilorganicmatter,soilhealth,soilfertility.

Cropresiduemanagement

Leave residue on the surfaceincreasinggroundcovertoprotectthesoil.

Increasedcropresiduecovercantieupnitrogentemporarilyinordertobreak down residue, increasedsoilmoisture,decreasederosionandcoolersoiltemperatures.

Positiveimpactonlongtermsoilhealth,fertilityandsoilorganicmattercontent.

Nitrogenfertilizerormanureapplication

Providesnitrogen(energy)sourceformicrobestobreakdownhighC:Nratioresiduequicker.

Temporaryincreaseinrespirationduetoincreasedrateofbreakdownoforganicmaterials.

Whenmanagedcorrectly,hasanoverallpositiveimpactonsoilorganicmatterandsoilhealthbyincreasingproductionlevels and residue amounts.

Vehicleorfarmequipmenttraffic

Compactssoildecreasingporespace,watermovement,oxygenformicrobesandnitrogenlossfromdenitrification.

Decreasesrespiration,yields,waterinfiltrationandincreasesrunoff.

Productiondeclines,increasedsoilerosionandrunoff,decreasedsoilhealth,compactedsoilsandreducedmicrobialactivity.

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Provide the Experience – Measure and Interpret Soils Respiration(Approximately 90 minutes)

Introduceeachofthelaboratorysuppliestothestudentsandreviewthelaboratoryprocessesandprocedureswiththeclass.SeetheGuidedNoteslabforinformation.

Studentsengageinthelabactivity.

Label the Information (Time varies)Studentsrecordinformationandanswerlabquestions.

Demonstrate the Relevance (Time varies)Discusswithstudentshowtheiractivitiesaffectsoilrespirationrates.

Review the Content (Approximately 7 minutes)Instructstudentstoworkinsmallgroupstocreateajinglethatincludesaminimumofthreefactstheylearnedduringthesoilrespirationlessonandlaboratoryactivity.Studentssharetheirjinglewiththeclass.

Celebrate Student Success (Approximately 3 minutes)Thankstudentsfortheirengagementandparticipation.

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Guided Notes: Soil RespirationNotescompletedby___________________________

SoilMicrobes:

Respiration:

Mineralization:

Ammonification:

Dentrification:

Nitrification:

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•Climate/Weather

•Biologicalactivity

•Soilmoisture

•Amountandhealthofsoilorganicmatter

• Soil texture

Factors Affecting Soil Respiration Soil Respiration Management Practices

1.Leavecropresiduesonthesoilsurface.

2.Useno-tillpractices.

3.Usecovercrops.

4.Addorganicmatter.

5.Plantlongseasoncrops.

6.Drainwetsoil.

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Table 1.InterpretingmanagementimpactsonsoilrespirationandSoilOrganicMatter(SOM).

Management Practice

Application Short Term Impacts Long Term Impacts

Solidmanureororganicmaterialapplication

Provide additional carbonandnitrogensourceformicrobestobreakdownandincreasebiomassproduction.

HighresiduecropsorcovercropsusedinrotationwithhighC:Nratio

HighC:Nratiocropsandaddednitrogenincreasedecompositionandaccrualofsoilorganicmatter.

Tillagesuchasannualdisking,plowing,etc.

Stirsthesoilprovidingatemporaryincreaseinoxygenformicrobestobreakdowncarbonsources.

Cropresiduemanagement

Leave residue on the surfaceincreasinggroundcovertoprotectthesoil.

Nitrogenfertilizerormanureapplication

Providesnitrogen(energy)sourceformicrobestobreakdownhighC:Nratioresiduequicker.

Vehicleorfarmequipmenttraffic

Compactssoildecreasingporespace,watermovement,oxygenformicrobesandnitrogenlossfromdenitrification.

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Guided Notes: Soil Respiration LaboratorySoil Respiration Scenario

TomandMollyaretroubledabouttheperformanceafieldtheyrecentlypurchasedandplantedtocorn.Thefieldwashighlytilledwithlittlecropresidue.Theequipmentusedonthefieldbythepriorownerhadverynarrowtires,andthereisnoconsistentpathusedfortravelingtotheirrigationpad.Theyarecuriousaboutwhatmightbetheproblemandplantotestthesoilrespirationratetoday.

Laboratory Supplies

•Solvita®samplejarforcorrectvolumeofsoilora3-inchdiameteraluminumcylinderandlid•Foil-packcontainingaspecialgelpaddle•Solvita®keyforreadingresults•Solvita®interpretationguidetoestimatedifferencesinsoilhealth,respirationandpotentialnitrogenrelease

•Aluminumfoilorcapwhenaluminumcylinderisused•Solvita®soilliferespirationtest(paddles)•Soilthermometerorcontrolledroomtemperature•Smallplasticbucketforeachgroupofstudents•Baggieswithazipperclosure

Laboratory Steps

Whensoilsaremixed,respirationtemporarilyincreasesbecauseoftheaerationcausedbymixing.Thisissimilartothetemporaryincreaseinrespirationcausedbytillage.Asoxygenavailabilityincreases,organicmatterbreaksdownquicker.

Considerusinganintactsoilcoreinthe3-inchdiameteraluminumcylinderratherthanmixingsoil.Anintactcorebetterreflectsrespirationforno-tillapplications,whileamixedsamplewillbetterreflectrespirationeitherimmediatelyaftertillageorposttillage(atleastonedayaftermixing).Togetanaccuratecomparisonofdifferentmanagementsystems,severalsoilsamplesrepresentingdifferentmanagementsystemscanbecompared.

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Step-by-Step Procedure 1.SoilSampling-Gatheraminimumof10smallsamplesfromanareathatrepresentssimilarsoiltypeandmanagementhistorywithaprobefromthesurface0-6inchdepth.Placethesamplesinthesmallplasticbucket.Repeatthisstepforeachsamplingarea.

(Soilrespirationisvariable,bothspatiallyandseasonally,andisstronglyaffectedbyorganicmatter,manureapplications,oxygenlevels,soilmoisture,salinityandsoiltemperature.Usefreshsoilsamples,gatheredjustbeforethetest.)

2.Mixing-Mixsoilintheplasticbucketjustwellenoughtobehomogeneousandremoveroots,residue,largestonesandresiduesfromsampleandplaceinalabeledplasticzipbag.

3.AddWaterifNeeded-Thesampleshouldhaveidealmoisture(nearfieldcapacity)forgrowingconditions.Iffieldconditionsaredryitisbesttoaddwater24hourspriortosampling.Ifneeded,watercanbeaddedpriortostartingthetestintheclassroom.

4.PutSampleIntoSolvita®Jar-ShortlyaftersamplingputmoistmixofsoiluptofilllineintheSolvita®jar.Asyoufill,tapthebottomofthejaronahardsurfacetoensuretherearenovoids.

5.UsetheColorGel-Insertcolorgelpaddleintosoilwiththegelfacingoutnexttotheclearsideofthejar.Becarefulnottojostleortipthejar.Screwthelidonverytightlyandrecordthetimeonthelid.Keepthejarintheclassroomatacontrolledtemperatureof68-75degreesFahrenheitandoutofsunlightfor24hours.

6.ReadandRecordResults-Readgelcolorafter24hoursandrecordresultsonTable3. 7.AnswerdiscussionquestionsandcompleteinterpretationssectionofTable3.RefertoSolvita®soiltestinstructionsforadditionalinformationandinterpretations.

Interpretations

Respirationlevelsreflectsoilhealthbasedonthelevelofcarbondioxiderespiration.Ratesareimpactedbythehealthofsoil,soilorganicmattercontent,andcanbeusedtoapproximatequantityofnitrogenreleasedperyearinanaverageclimate.TherateofcarbondioxidereleasedisexpressedasCO2-Clbs/acre-3”/day.

Highsoilrespirationratesareindicativeofhighbiologicalactivity.Thiscanbeagoodsignofahealthysoilthatreadilybreaksdownorganicresiduesandcyclesnutrientsneededforcropgrowth.Solvita®responsemaygofromaninactivecondition(0-1blue-gray)toaveryactivestate(3.5-4.0green-yellow)assoilrespirationincreasesfromdesirablemanagementmeasuressuchasdiversecroprotations,andno-till.

Insomecases,heavilymanuredsoilsorsoilshighinorganiccontentcanattainaveryhighrate(5yellow).Thiscanbedetrimentalwhendecompositionofstableorganicmatteroccurs.Itisgenerallydesirabletohaveatleastgreencolor3.Ittypicallytakesseveralyearsforasoiltoimprovefromalowbiologicalstatustoamoreactiveone.Withproperresiduemanagement,diversecroprotations,organicmatteradditionsandavoidanceofdestructivetillagepractices,thetimetoreachamoreoptimumconditionisshortened.

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Table 2.Basicsoilbiologicalhealth

Solvita Test - Color/Colorimetric Number

0-1Blue-Gray

1.0-2.5Gray-Green

2.5-3.5Green

3.5-4.0Green-Yellow

4-5Yellow

Soil Respiration Activity

VeryLowSoilActivity

Moderately Low Soil Activity

MediumSoilActivity IdealSoilActivity UnusuallyHighSoilActivity

Associatedwithdrysandy soils, and littleornoorganic

matter

Soilismarginalintermsofbiologicalactivityandorganic

matter

Soil is in a moderately

balancedconditionand has been

receivingorganicmatteradditions

Soiliswellsuppliedwithorganicmatterandhasanactivepopulationof

microorganisms

High/Excessiveorganicmatter

additions

*Approximate Level of CO2 - Respiration

<300mgCO2/kgsoil/wk

300-500mgCO2/kgsoil/wk

500-1000mgCO2/kgsoil/wk

1000-2000mgCO2/kgsoil/wk

>2000mgCO2/kgsoil/wk

<9.5lbsCO2-C/acre-3”d

9.5-16lbsCO2-C/acre-3”d

16-32lbsCO2-C/acre-3”d

32-64lbsCO2-C/acre-3”d

>64 lbsCO2-C/acre-3”d

Approximate Quantity of Nitrogen (N) Release Per Year (Average Climate)

<10lbs/acre 10-20lbs/acre 20-40lbs/acre 40-80lbs/acre 80->160lbs/acre

*Source:Doran,J.(2001)USDA-ARSSoilHealthInstitutecorrelationofSolvita®andfieldsoilrespiration.Calculationsbasedona3-inchsoilcore(7.6cm).

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Table 3. Soilrespirationlevelsandinterpretations.

Sample Site

Median 24-hr Soil or Room

Temp.

Time-frame

Start Time

End Time

Gel Color & Colorimetric

Number

Soil Activity Rating

(Table 1)

Avg. Respiration

Level lbs CO2-C/acre-

3”/d

Quantity of N

Released lbs/ac/yr

Whatdidyouexpectintermsofthesoilrespirationlevels?

Whatsurprisedyouaboutthesoilrespirationlevels?

Whatdoyouexpecttohappentothesoilorganicmatterbasedonthesoilrespirationrates?(improve,decline,remainthesame)Why?