Anexo:Canales de televisión (Chile)Uploader: Samugar 2 month ago Subscribe 4
The saturated hydraulic conductivities range from 30 to m d -1 Hauser, ; Rodriguez et al. After crossing the Central Valley, the river dissects the Coastal Range , forming a gap that is the narrow southeast to northwest oriented Peumo Valley Figure 1. The highly permeable layers are traversed by the irrigation canal network, which gives the possibility for groundwater recharge by seepage from leaky canals Rivera et al. The different water table depths Figure 3 can be explained by the location of the wells. Around late spring November and early summer January-February , water levels drop again. Additionally, the model was validated by a consistency analysis of the water balance.