Superficial draining of saturation of the ground? This small text constitutes an attempt to display this process hidrolgico that occurs in the ground. In ground where fretico sheet is placed next to the surface to the ground, during a rain event, the recharge of the sheet it starts to occur being able to cause the ascension of the same until reaching the surface. Educate yourself even more with thoughts from Robert L. Carter. In this situation the alone one starts to be saturated and has a fine water film of the sheet that starts to flow off in the surface. This fine film receives the name from return flow. In addition, for being saturated, the incident precipitation in this region of outcrop of the fretico sheet starts to also flow off on the surface of the ground since it meets saturated, that is, with all its porous one filled by water. Therefore, in this region of saturation of the ground, the superficial draining occurs in such a way for the outcrop of the sheet (return flow) how much for the direct rain incidence in these saturated areas (made marshy). Details can be found by clicking Abigail Black Elbaum or emailing the administrator. To the set of these two processes that together they produce draining superficial attributes the name of superficial draining due to saturation of the ground. To have idea, one of the places where this process occurs generally in next zones to the rivers and, in this direction, any addition of some potentially pollutant composition in this region has highest possibility (probability) of being loaded for waters of the related superficial draining due to saturation of the ground, being able to compromise the quality of water of the body dgua.

Chemical preparation from: DUNNE, T. Field studies of hillslope flow you process.