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7-Predicting soil loss RUSLE
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20Mar2017

1

PredictingSoilLossfrom

WaterErosion(notgully)

Lecture7

Reading:Chapter6-1thru6-4(esp.6-1

and6-3),7-2.1andsection19-2.7thru2.8

1

Whyisthereaneedtomeasure

soilerosion?

?Todetermineerosionpotentialwith

presentmanagement.

?Toevaluatealternativemethodsofcrop&

soilmanagement.

–Makewisedecisions

?Economic&Environmentalincentives

–Costshareprograms

2

USLE

?UniversalSoilLossEquation.

–1950s

–USDAARS(AgricultureResearchService)

andSCS(SoilConservationService,now

calledtheNRCS)

?A=RxKxLSxCxP.

?Designedforcroplandintheeastern

U.S.A.

?Laterappliedtomanykindsofcrops

throughouttheUSAandothercountries.

?Didnotaccuratelymeasuresoilloss.3

RUSLE

?RevisedUniversalSoilLossEquation.

?Usedforestimatingsoillossesfrom

pasture,range,forestlandandcropland.

?Computerizedprogramorbyhand.

?FirstreleasedbytheUSDA-ARSin1992.

?Plotrunoffstudies,rainfallsimulation

?“RUSLE2”releasedin2003

–Computer-based

–Thecurrentagencystandard4

RUSLE

?A=RxKx(LS)xCxP

“adjusted”Kf

?Factorsdon’treallyhaveunits

?Highertheindividualfactors,moresoilloss.

?Requiresuseoftablesorchartsorcomputer

software

?Usefulformanagementdecisions,i.e.weshould

askthequestion“Howcanthesenumbersbe

changed(reduced)?”

5

A

Predictedaverageannualsoilloss(sheet

andrillerosion)intonsperacreperyear.

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2

R

?Therainfallfactor.

?Measureofrainfallamount,energyand

intensityofstorms.

–Historicalweatherstationdata

?Staticnumber

?Missourirangesfrom175to270.

?Floridarangesfrom450to600.

?Dryerpartsofwest=10.

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“R”

8

9

Example

?A=255x…

R

Keepinmindthatalargerresult(i.e.a

larger“A”product)meansmore

averageannualsoilloss…soifyou

startwithalargenumberyouneedto

domoretoreducepredictederosion.

10

K

?Soilerodibilityfactor.

?Measureofrelativeresistanceofasoilto

detachmentandtransportbywater.

?Reality:erodibilityvariesduringtheyear

duetoseasonalchangesintemperature

andrainfall.

?Valuesrangefrom0.02to0.60.

–Higherthenumber,moreerodible.

11

K(continued)

?Evaluatestexture(silt,veryfinesands,

sands),organicmatter,permeabilityof

soil,structure

–Determinedviaalaboratoryprocedure

?Numberschangewithdepth.

–Forsoillosscalculations,surfacelayeronly

?Staticnumberbutinrealitycanchangeby

makingsoillesserodible(increase

structuralstability),butneedlabto

measure.

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3

Fromsoilsurveytables:

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Kf

?Indicatestheerodibilityofthefineearth

fractionoftexture.

?2mmandlessindiameter.

–Rocksdonoterodeundernormalrainfall

?Numbersrangefrom0.05to0.70.

?Rockysoil:KfwillbehigherthanK

?Soilwithlittlerockatsurface:Kf=K

14

AdjustedKf

?RUSLE

?Adjustmentsforseasonalchanges–

freezing/thawing,moisture,consolidation

?Variesaroundcountry.

?FindKf,thenusetheRUSLEtableto

adjust.

–TheadjustedKfisthe“K”usedinRUSLE

formula

1516

Example

?IfKfwas0.32inthesoilsurvey

?AdjustedKf=0.28

?Sofar:

A=255x0.28x…

RK

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LS

?Slopeandslopelengthfactorcombined.

?Itisaratioofsoillossfromagivenfield

slopetothatfromaslopethathasalength

of72.6ft.and9%slope(theindexlength

andslope).

9%

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4

?Slope:%verticaldropoverahorizontal

distance

?Length:Horizontaldistancefromtheorigin

ofoverlandflowtothepointwheresoil

depositionoccursorrunoffisconcentrated

inadefinedchannel.

19

LS(con)

?Measureslopewithlevelorclinometer.

?Measurelengthwithtape,pacing,GPS

?UsetablestocomeupwithLSvalue.

?Steepertheslope,thehighertheLS

?Thelongertheslope,thehighertheLS

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LS(con)

?CanchangetheLSofahillsideby

breakingthelength(L)with:

–Terraces

–Stripcropping

–Onlywithcertainterracescanyouchangethe

%slope(S).

21

TerracesaffectLS

broadbased

grassedback

22

(annualcropswithtillage)

Notethatyoucaninterpolatetoseethattheindexslopeof76’at9%is1.00

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5

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Example

?5%slope;200’slopelength(rowcrops

withtillage)

?LS=0.85

?Sofar:

A=255x0.28x0.85x…

RKLS

26

C

?Coverandmanagementfactor.

?Ratioofsoillossfromlandcroppedunder

specifiedconditionstothelossfromclean-

tilled,continuousfallow.

?Rangefrom0.01to0.48.

27

C(con)

?Throughcalculationofanaverage,Cestimates

thecombinedeffectofallinterrelatedcoverand

managementvariables.

–Differentcroprotations

–Differenttillagesystems(i.e.residuelevels,timing)

?Cropyieldsimpacttheactualresult(becauseyieldisrelated

tothebiomassofresidueleftbehind)buttablesusesone

yield.

–Covercrops

–Useofcrop(grainvssilage)

?Considersgroundandcanopycover.

–Considersdistributionof“R”throughyear

28

?Averageofallcrops/tillageand

managementforthelengthoftherotation

–Forexample:corn-soybean-wheatrotation

–Anumberforeachcrop,addup,divideby3

?Continuouspermanentgrass.

?Cfactoristheeasiestandmost

manageablefactortochangetoreduce

soilloss.

29

Example

?Corn-Soybeanrotation(2yearrotation)

–Cornforgrain

–Soybeans(widerow)

–Tillage

?Soybeanresiduetilledinspring,cornplanted(20%)

?Cornresidueprimarytillageinfall,secondarytillage

inspring,soybeansplanted(30%)

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20Mar2017

6

JFMAMJJASONDJFMAMJJASOND

Corn-Soybeanrotation(2yearrotation)

Tillage

tools

Plant

corn

(20%)

Growcorn

Harvestcorn

Chisel

plow

corn

residue

Sec.

tillage

tools

CORNYEARSOYBEANYEAR

Plant

soybeans

(30%)

Growbeans

Harvestbeans

31

Example

CornSoytotallengthaverage

0.23+0.12=0.35/2years=0.175

C=0.175

Sofar:

A=255x0.28x0.85x0.175x…

RKLSC

32

P

?SupportPracticefactorisaproductof

multiplyingthreefactorstogether.

?Ratioofsoillosswithaspecificsupport

practicetothecorrespondingsoillosswith

uphillanddownhilltillageoperations.

?Includesthreedifferentsupportpractices

–contouring

–strip-cropping

–terracing

33

P(con)

?Contouring(Pc)

?Stripcropping(Ps)

?Terraces(Pt)

?PcxPsxPt=P

?Ifpracticenotinplacesuchas:no

contouring(up/downhill),nostrip

cropping,noterraces;P=1(multiply

anythingby1andnothingchanges)

34

?Pc(Contouring)verycomplicated.

–Considersmanagementofcover,ridge

heights,rowgrade,10yearstormerosion

index,soilhydrologicgroup(A-D)

–MostMOcontouringaround0.8(Depends!)

?Crossslopefarmingconsideredbeneficial

?Pt(Terraces)

–Considerswhether“open”outlets

(waterways),“closed”outlets(underground

outlets),interval,gradeofterracechannel.

–Rangesfrom0.5to1.0

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7

?Ps(Stripcropping)complicated

–Considersslope,numberofstrips,amountof

grassstripsversuscropstrips,widthofstrips.

–Rangesfrom0.64to1.0

37

Example

?P=0.89(Pcwithnoterracesorstrips)

?Sofar:

A=255x0.28x0.85x0.175x0.89

RKLSCP

38

ExamplesofRUSLE

A=RxKxLSxCxP

255x0.28x0.85x0.175x0.89=9.5t/A/yr

Isthisgoodorbad?

Highorlow?

39

Double-checkfor“feedback”

?Buildingterracesorstripcropping(P

factors)willchangeLSandPc

?Usingcontinuousno-tillwillchangeLS

table,andCvalueswillchange

40

Tolerable(T)rates

?“themaximumlevelofsoilerosion(sheet

andrill)thatwillpermitahighlevelofcrop

productivitytobesustainedeconomically

andindefinitely”

?Trangesfrom1to5t/A/y

–Gasconadesoilseries=1.0t/a/y.

–Captinasoilseries=3.0t/A/y.

–Newtoniasoilseries=5.0t/A/y.

41

“T”considerstheentiresoilprofile.

–Depthofsoil.

–Parentmaterial.

–Relativeproductionpotential.

–Amountofpreviouserosion.

Farmingto<“T”shouldbethegoal.

42

“Conservation…doesthatsimplymeanwedestroy

somethingoveralongerperiodoftime?”

20Mar2017

8

Backtothesoilsurveytables

43

A=

255x0.28x0.85x0.175x0.89=9.5t/A/y

IfT=4t/A/y…Bad!

44

Whatcanbechangedtogetto“T”?

R=no

K=nofortheequation,yesinrealityifmanage

forimprovementoverextendedtime

S=no,unlesscertainterraces

L=yes,withterraces,bufferstrips/strip

cropping

C=absolutely!Uselesstillage(timing),add

lesserosivecropstorotation

P=yes,betterjobofcontouring,addstripsor

terraces.

45

Someexamplechanges

?UseaCorn-Corn-Soybeanrotation

–Notill(drill)soybeansinsteadofwiderow(

–Nofalltillageforcorn(springmulchtillage,

30%coveratplanting)

?Addterraces

–Closedoutlets(undergroundoutlets)@125

footspacing

46

Corn-Corn-Soybean

?CornafterSoybean:0.14(notilldrill,20%cover)

?CornafterCorn:0.13(springmulchtill,30%)

?SoybeanafterCorn:0.04(50%cover)

CaftSCaftCSaftCtotalyrsaverage

0.14+0.13+0.04=0.31/3=0.103

WhyisSoybeanafterCornsolow?

47

HowmuchdidchangingChelp?

A=255x0.28x0.85x0.103x0.89=5.6t/A/y

Soillossestimatereducedby4t/A/y(40%)

Goodstart!

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20Mar2017

9

Addingterraces

Willprobablychangethreenumbers:

1.Terracefactor(Pt)

2.ReduceLS;lengthgoesfrom200’to125’.

3.Terracesareclosedwithunderground

outlets.Contourfarmingoperationsfollow

terraces,givingabetterPcvalue

4950

x

InterpolatetogetanLSestimateof~0.7151

RKLSCP

255x0.28x0.71x0.103x0.48=2.5t/ac/yr

0.8(Pc)x0.6(Pt)x1(Ps)

T=4t/ac/yr

Soilloss=2.5t/ac/yr

GOOD!

52

ConservationCompliance

?AgriculturalResourcesand

EnvironmentalIndicators.USDA,

EconomicResearchService,NaturalResources

andEnvironmentDivision.Agricultural

HandbookNo.705.

?ConservationandEnvironmentalPrograms

?Conservationcomplianceandsodbuster

?http://www.ers.usda.gov/media/871561/arei6-3.pdf

(1994)

?http://www.ers.usda.gov/media/872940/eib16.pdf

pp.184-191(2006)

53

About10yrsaftertheenactmentofthe1985

FoodSecurityAct(“FarmBill”thatrequired

conservationcomplianceinordertobe

eligibleforfederalprogramsandcost-

shares),USDAconductedareviewofHighly

ErodibleLands:

“Forthe98millionacrescurrently[1994]in

fullcompliance,[NRCS]estimatesthat

averageannualerosionhasbeenreduced

from19.8tonsperacreto5.9tons.”(AREI)

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20Mar2017

10

ConservationCompliance

?Isreducingerosionbyafactorof3

enough?

?Whatdoesittaketobein“compliance”in

termsofT?

55

ExampleandImpactof

improperpasture

management

(SeethePastureC-factortable

forMOonBlackboard)

56

Poorsite

57

SHEET&RILLEROSON:RUSLE

50%groundcover,10%canopycover,lowvigor/production/fertility

7%slope,150’slopelength

averageOzarksoil(e.g.Wilderness)(T=3)inGreeneCounty

RKLSCP

A=___X_____X___X____X1.0=____t/ac/yr

58

Bettersite

59

SHEET&RILLEROSON:RUSLE

80%groundcover,10%canopycover,mediumvigor/production/fertility

7%slope,150’slopelength

averageOzarksoil(e.g.Wilderness)(T=3)inGreeneCounty

RKLSCP

A=____X____X____X_____X1.0=____t/ac/yr

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20Mar2017

11

InfiltrationandRunoffUnderGrazing

Condition

LighttoModGrazing

HeavyGrazing

0.33”1.00”0.66”

0.29”

0.11”0.00”

0.09”

0.60”

0.33”

SansarcShallowClayRangeSite

5%Slope(Spaethetal.,1991)

61

Moreinformation

?RUSLE

–K.G.Renard,etal.1994.RUSLErevisited:

status,questions,answers,andthefuture.

JournalofSoilandWaterConservation.

49(3):213-220.

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