Click on “Download PDF” for the PDF version or on the title for the HTML version. If you are not an ASABE member or if your employer has not arranged for access to the full-text, Click here for options. Finger Formation and its Relation to Lateral Flow in the Induction ZonePublished by the American Society of Agricultural and Biological Engineers, St. Joseph, Michigan www.asabe.org Citation: Pp. 173-176 in Preferential Flow, Water Movement and Chemical Transport in the Environment, Proc. 2nd Int. Symp. (3-5 January 2001, Honolulu, Hawaii, USA), eds. D. D. Bosch and K. W. King. St. Joseph, Michigan: ASAE 701P0006.(doi:10.13031/2013.2089)Authors: G.H. De rooij, h. cho, m. inoue, and n. toride Keywords: Wetting front instability, fingered flow, induction zone, microtensiometers PAn unstable wetting front breaks up below a thin wetted layer: the induction zone. Many small fingers form initially, but only a few fully develop. To illuminate the process of finger formation, we used a horizontal array of fast-responding microtensiometers in the induction zone of a two-dimensional, fine-over-coarse glass bead porous medium. The induction zone affected only the initial shape of the wetting front; finger size and spacing were governed by autonomous processes. The lateral pressure head gradients in the induction zone adapted to the location of full-grown fingers before these fingers were visible and remained stable afterwards. The water requirement and spacing of the fingers dictated the magnitude of the gradients. The pattern of the lateral pressure head gradients suggests that the fingers cause non-uniform infiltration from the ponded water layer. (Download PDF) (Export to EndNotes)
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