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system act as low points attracting groundwater outflow. The distribution of groundwater The time distribution of the particles (longest in the system first) is illustrated in Figure heads then approximates the topography, with higher heads in the hinterland surround- ing the river valleys and the salars. The initial set of parameters were adjusted so as to ensure that the distribution of groundwater heads was sensible, i.e., not above the ground surface. Further calibration can be undertaken once observed groundwater heads are Remote Sens. 2022, 14, x FOR PEER REVIEW 14 of 21 Figure 11. MODFLOW modelling. (a) Modell setup with HUs (see Appendix A), model extent, and rivers; (b) long-term average rainfall. Figure 12. MODFLOW modelling output. Steady-state groundwater heads. Figure 12. MODFLOW modelling output. Steady-state groundwater heads. Remote Sens. 2022, 14, 1383 13 of 22 available. Groundwater flow occurs to the rivers in the base of the valleys and then onto the Salar de Uyuni, reaching it via the main river channel Rio Grande de Lipez. 5.2. MODPATH Model 5.2. MODPATH Model The MODPATH model (Version 7.2.001) was developed by inheriting most of its The MODPATH model (Version 7.2.001) was developed by inheriting most of its data data from the MODFLOW model described above. The main extra dataset was porosity from the MODFLOW model described above. The main extra dataset was porosity based based on the zonation from the geology distribution (see Appendix A). The particle tracks on the zonation from the geology distribution (see Appendix A). The particle tracks were produced for the southern part of the Uyuni watershed developed for the prototype work- flow and are shown in Figure 13a. They mainly enter the river system or find their way to the salar itself. The latter is a low point in the system from a groundwater head perspective (see Figure 12) and so will attract any particles that are not captured by the river network.PDF Image | Lithium Brine Deposit Formation
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