Testing simple scaling in soil erosion processes at plot scale

Vito Ferro, Vincenzo Bagarello, Jesús Rodrigo Comino, Manuel Pulido, Artemi Cerdà, Saskia Keesstra

Risultato della ricerca: Articlepeer review

22 Citazioni (Scopus)


Explaining scale effects for runoff and erosion improves our understanding and simulation ability of hydrologicaland erosion processes. In this paper, plot scale effects on event runoff per unit area (Qe), sediment concentration(Ce) and soil loss per unit area (SLe) were checked at El Teularet-Sierra de Enguera experimental site in EasternSpain. The measurements were carried out for 31 events occurring in the years 2005 and 2007 in bare ploughedplots ranging from 1 to 48m2. The analysis established the scaling relationship by dimensional analysis and selfsimilaritytheory, and tested this relationship at different temporal scales ranging from event to annual scale. Thedimensional analysis and the incomplete self-similarity condition allowed us to establish a power scaling relationshipwhich was found to also be usable for the moments of k (1, 2, 3, 4) order. The power scaling relationshipwas theoretically deduced applying a boundary condition which is based on the hypothesis thatsediment delivery processes do not occur at the selected plot scale. The simple scaling invariance condition wasalways verified (i.e. for each temporal horizon) for runoff and soil loss while the same hypothesis was notperfectly acceptable for sediment concentration. The analysis of the scaling relationships at event temporal scaleshowed that the spatial scale effects were less frequent for the composite variable (soil loss=sediment concentration×runoff)than the constituting variables. For 48% of the events, a statistically significant scale effectwas detected for all tested variables. With reference to the statistically significant relationships, both runoff andsoil loss always decreased and sediment concentration always increased in the passage from the reference area(1m2) to the largest one (48m2). The analysis at aggregated temporal scales suggested that annual scale effectsfor soil loss per unit area should be temporally more stable than those for both runoff and sediment concentration.Finally, at mean event scale the three investigated variables have a similar behaviour in terms ofsimple scaling invariance.
Lingua originaleEnglish
pagine (da-a)171-180
Numero di pagine10
Stato di pubblicazionePublished - 2018

All Science Journal Classification (ASJC) codes

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