SciELO - Scientific Electronic Library Online

vol.42Nitrous Oxide Emissions in a Wheat/Corn Succession Combining Dairy Slurry and Urea as Nitrogen SourcesMineralogy and Concentration of Potentially Toxic Elements in Soils of the São Francisco Sedimentary Basin índice de autoresíndice de assuntospesquisa de artigos
Home Pagelista alfabética de periódicos  

Serviços Personalizados




Links relacionados


Revista Brasileira de Ciência do Solo

versão impressa ISSN 0100-0683versão On-line ISSN 1806-9657


CASSOL, Elemar Antonino; SILVA, Tiago Stumpf da; ELTZ, Flávio Luiz Foletto  e  LEVIEN, Renato. Soil Erodibility under Natural Rainfall Conditions as the K Factor of the Universal Soil Loss Equation and Application of the Nomograph for a Subtropical Ultisol. Rev. Bras. Ciênc. Solo [online]. 2018, vol.42, e0170262.  Epub 14-Maio-2018. ISSN 0100-0683.

Erodibility represents the intrinsic susceptibility of the soil to the erosion process, represented by the K factor in the Universal Soil Loss Equation (USLE). In Brazil, there are few field experiments determined with a series larger than ten years of data, which are the most reliable for quantifying the K factor. The aim of this study was to determine the K factor of the USLE by the direct method, relating soil losses determined in the field under standard conditions to erosivity of rains, and by the analytic method, applying the Wischmeier nomograph. The data on soil loss by water erosion were obtained in a field experiment under natural rainfall conditions from 1976 to 1989 in an Ultisol at the Agronomic Experimental Station in Eldorado do Sul, RS, Brazil. The value of the K factor by the direct method was 0.0338 Mg ha h ha-1 MJ-1 mm-1, which is high, showing considerable susceptibility of the soil to erosion. From the analytical method, the K factor obtained was 0.0325 Mg ha h ha-1 MJ-1 mm-1, a value very close to that determined experimentally. Thus, the Wischmeier nomograph proved to be valid for determination of the K factor of the Ultisol under study. This method proved to be valid for this type of soil. These results can be used for calibration models based on the USLE.

Palavras-chave : water erosion; soil loss; soil properties; erosion modeling; surface runoff.

        · texto em Inglês     · Inglês ( pdf )