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<br /> <br />- <br /> <br />- <br /> <br />- <br /> <br />- <br /> <br />- <br /> <br />- <br /> <br />- <br /> <br />- <br /> <br />- <br /> <br />- <br /> <br />- <br /> <br />- <br /> <br />- <br /> <br />- <br /> <br />- <br /> <br />- <br /> <br />- <br /> <br />- <br /> <br />"""" <br /> <br />nemR/ "::'" l,mM'" I~~/- "'''"'''''>IT /":""D'/ UNO ;:;~-' =,,~;;f: "'''i,:''''''j'':''''ATW", <br />OFF COVER USE AND FIEIJ) OF AND <br />SOILS ER.O- SErlDlENJ: DATA SOLUTION APPLICABILITY <br />SIaN TRANSPORT <br /> <br />l/llJldfilJllllillllfjjjflll18/ <br /> <br />o <br />Q <br />..... <br />...,.. <br />..... <br />N <br /> <br />BRYAN <br /> <br />X <br />D <br /> <br />x <br />, <br /> <br />x <br />, <br /> <br />x <br />, <br /> <br />x <br /> <br />NO PREDICTIVE EQUATION. DATA <br />RELATES SOIL ERODIlHLITf TO <br />WATER. SOLUBLE AGGREGATES) 3_ <br />EQUATION UNIVERSALLY APPLIC_ <br />ABJ.,E IF COEFFICIENTS ARE <br />DETERMINED. <br /> <br />FOSTER AND MEYER <br /> <br />x <br />, <br /> <br />x <br />, <br /> <br />X <br />D <br /> <br />X <br />D <br /> <br />x <br /> <br />~ <br />~ <br />ffl <br />" <br />" <br />" <br />" <br />, <br />~ <br /> <br />MEEU'.IIG <br /> <br />x X X X <br />D D , <br /> <br />x <br />, <br /> <br />x <br />, <br /> <br />X <br />D <br /> <br />x <br /> <br />EQUATIONS nF:J:ERMINE RELAilllE <br />ERODIBILITY Bur AT A CONStANT <br />RATE OF PRECIPITATION. <br /> <br />MEYER AND WISCIlMEIR <br /> <br />, x <br />, , <br /> <br />X <br />D <br /> <br />x <br />, <br /> <br />x <br />, <br /> <br />x x <br />, D <br /> <br />x <br /> <br />EQUATION lJNlYERSALLY APPLIC- <br />ABLE BUT COEFFIC'LENTS lHl'F- <br />lCULT TO DETERMINE. <br /> <br />'" <br /> <br />MUSGRAVE <br /> <br />x <br />, <br /> <br />x X <br />D , <br /> <br />x <br />, <br /> <br />x <br />, <br /> <br />, <br />, <br /> <br />x <br />, <br /> <br />, <br /> <br />EQUATION UNIVERSAllY AFPLIC- <br />ARLEBUTLIMITEDIOSLOPES <br />LESS TIIAl'l 20 PERCENT. <br /> <br />WlSCllMEIR ANn SMlTIl <br /> <br />x <br />, <br /> <br />x x x x <br />" , <br /> <br />x <br />, <br /> <br />x <br />, <br /> <br />x <br />, <br /> <br />x <br /> <br />. . <br /> <br />EQUATION UNlVERSl\LLY APPLlC- <br />ABLE BlJT LIMITED TO SLOPES <br />LESS THAN 20 PERCENT. <br />EQUATION APPLICABLE MAINLY <br />IN LARGE WATERSHEDS BUT llEEDS <br />SEDIMENT TRANSPORT DATA. <br /> <br />ANDERSON <br /> <br />, <br /> <br />, <br /> <br />x <br />, <br /> <br />x <br />, <br /> <br />x X <br />D <br /> <br />x <br />, <br /> <br />X <br />D <br /> <br />x <br /> <br />X <br />D <br /> <br />x <br />, <br /> <br />x <br />, <br /> <br />x x <br /> <br />x <br /> <br />x <br /> <br />X <br />o <br /> <br />BRANSON AND OWEN <br /> <br />, <br /> <br />, , <br /> <br />, <br />, <br /> <br />X <br />o <br /> <br />x , <br />D <br /> <br />, . <br /> <br />EQUATlON UNIVERSALLY APPtIC- <br />ABLE BUT CORRELATION COEFFI_ <br />C!EN'rS FOR UCH MU!A lillSi BE <br />DETERMINED. <br />EQUATION UNI'lEltSA1.l..'lll?PLlC_ <br />ABLE ESPECIALLY IN WESTERN <br />UNITED STATES. <br /> <br />~ <br />" <br />~ <br />~ <br />ffl <br /> <br />'''''"'' <br /> <br />, <br />o <br /> <br />x <br />, <br /> <br />x x , <br />" D <br /> <br />x . <br /> <br />. <br /> <br />NEGEV <br /> <br />x <br /> <br />, <br /> <br />, <br /> <br />, <br /> <br />EQUATION UNIVERSALLY APPLIC- <br />ABLE BUT NEEDS PIU:CIPtTAnON <br />AlID RUNOFF DATA. <br /> <br />RENARD <br /> <br />x x x <br />, , , <br /> <br />x <br />, <br /> <br />x , x <br />, <br /> <br />* EQUATION APPLICABLE UNlVERS_ <br />ALLY IF RUNOFF GENERATION <br />ME'rWJn AVhllJUlLE. Y <br /> <br />TM1JI1 <br /> <br />x <br />, <br /> <br />, <br />D <br /> <br />X <br />o <br /> <br />, <br />D <br /> <br />x <br />, <br /> <br />x <br /> <br />. <br /> <br />EQUATtoN ll'P"LTCALLE TO SDl.1TIl- <br />mHr.h2l}!6~D &S~M:iSEFF~WS <br />DATA. <br /> <br />X DATA NEEDED TO FORMULATE l1ETHOD <br />o DATA USED TO SOL.VE DERIliED MEnIOn <br />" MISCELLANEOUS INFORMATION ON COST AND DATA QUTFUT <br />1/ C1l.ANNEL SLOPES ARE NEEDED FOR RENARD'S METHOD <br />11 USED WITH EPIlEMERAL STREAM MODEL IN SOUTHWESTERN UNITEP STATES <br /> <br />Table l.-Sunnnary table of on-site erosion and sediment yield methods <br /> <br />