Determining soil erodibilities for the USLE-MM rainfall erosion model

P. I.A. Kinnell

    Research output: Contribution to journalArticle

    4 Citations (Scopus)

    Abstract

    The USLE-MM is a rainfall erosion model which predicts soil loss using an erosivity index which is given by the QREI30 index to a power > 1.0. In the USLE modelling environment, soil erodibility is defined as the soil loss per unit quantity of the erosivity index. With the USLE-MM model where event soil loss = KUMM (QREI30)b1, using KUMM as the erodibility factor does not conform with the requirement that the erodibility factor has units that are consistent between soils and locations. The alternative is to use the model event soil loss = KUM a1 (QREI30)b1 where KUM is determined from dividing the total amount of soil loss from a large number of events by the total value of QREI30 associated with those events because this model isolates the soil erodibility effect from the effect of b1 on KUMM. The effect of b1 on a1 is demonstrated in this paper for bare fallow plots at 15 locations in the USA and plots at Sparacia, Sicily.

    Original languageEnglish
    Pages (from-to)424-426
    Number of pages3
    JournalCatena
    Volume163
    DOIs
    Publication statusPublished - 1 Apr 2018

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    Universal Soil Loss Equation
    erodibility
    erosion
    rainfall
    soil
    erosivity
    fallow
    loss

    Cite this

    Kinnell, P. I.A. / Determining soil erodibilities for the USLE-MM rainfall erosion model. In: Catena. 2018 ; Vol. 163. pp. 424-426.
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    abstract = "The USLE-MM is a rainfall erosion model which predicts soil loss using an erosivity index which is given by the QREI30 index to a power > 1.0. In the USLE modelling environment, soil erodibility is defined as the soil loss per unit quantity of the erosivity index. With the USLE-MM model where event soil loss = KUMM (QREI30)b1, using KUMM as the erodibility factor does not conform with the requirement that the erodibility factor has units that are consistent between soils and locations. The alternative is to use the model event soil loss = KUM a1 (QREI30)b1 where KUM is determined from dividing the total amount of soil loss from a large number of events by the total value of QREI30 associated with those events because this model isolates the soil erodibility effect from the effect of b1 on KUMM. The effect of b1 on a1 is demonstrated in this paper for bare fallow plots at 15 locations in the USA and plots at Sparacia, Sicily.",
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    Determining soil erodibilities for the USLE-MM rainfall erosion model. / Kinnell, P. I.A.

    In: Catena, Vol. 163, 01.04.2018, p. 424-426.

    Research output: Contribution to journalArticle

    TY - JOUR

    T1 - Determining soil erodibilities for the USLE-MM rainfall erosion model

    AU - Kinnell, P. I.A.

    PY - 2018/4/1

    Y1 - 2018/4/1

    N2 - The USLE-MM is a rainfall erosion model which predicts soil loss using an erosivity index which is given by the QREI30 index to a power > 1.0. In the USLE modelling environment, soil erodibility is defined as the soil loss per unit quantity of the erosivity index. With the USLE-MM model where event soil loss = KUMM (QREI30)b1, using KUMM as the erodibility factor does not conform with the requirement that the erodibility factor has units that are consistent between soils and locations. The alternative is to use the model event soil loss = KUM a1 (QREI30)b1 where KUM is determined from dividing the total amount of soil loss from a large number of events by the total value of QREI30 associated with those events because this model isolates the soil erodibility effect from the effect of b1 on KUMM. The effect of b1 on a1 is demonstrated in this paper for bare fallow plots at 15 locations in the USA and plots at Sparacia, Sicily.

    AB - The USLE-MM is a rainfall erosion model which predicts soil loss using an erosivity index which is given by the QREI30 index to a power > 1.0. In the USLE modelling environment, soil erodibility is defined as the soil loss per unit quantity of the erosivity index. With the USLE-MM model where event soil loss = KUMM (QREI30)b1, using KUMM as the erodibility factor does not conform with the requirement that the erodibility factor has units that are consistent between soils and locations. The alternative is to use the model event soil loss = KUM a1 (QREI30)b1 where KUM is determined from dividing the total amount of soil loss from a large number of events by the total value of QREI30 associated with those events because this model isolates the soil erodibility effect from the effect of b1 on KUMM. The effect of b1 on a1 is demonstrated in this paper for bare fallow plots at 15 locations in the USA and plots at Sparacia, Sicily.

    KW - Erosion plots

    KW - Soil loss prediction

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