Rice cultivation. The (Figure 16). Both aquifers in lowlands in lowlandsfor rice
Rice cultivation. The (Figure 16). Both aquifers in lowlands in lowlandsfor rice cultivation. The development on the piezometric piezometric important within the alterites the alterites S19 than by S19 than in development of thelevel is more level is far more vital in captured by captured PHA-543613 site inside the fractured the fractured reservoir captured by fourThe 1st events (156 July) did not July) did not reservoir captured by S5. The first S5. rainfall 4 rainfall events (156 affect the pieaffect the piezometricfractured reservoir. The piezometric level increased in the end of at zometric degree of the degree of the fractured reservoir. The piezometric level improved the the finish of your despite a considerable drop in rainfall. This rainfall. This could be explained bya rainy season rainy season in spite of a important drop in is usually explained by the fact that the truth that a rainfall event can resultthe floodingseveral region forweeks. In S19,ordecrease rainfall occasion can lead to flooding of in region for of the days or a number of days a weeks. In S19, a decrease in electricalobserved at the beginning of the rainy season. This lower in electrical conductivity was conductivity was observed at the starting of your rainy season. This lower in electrical conductivity of dueaquifermixingwith low mineralized in electrical conductivity is because of the mixing will be the towards the water from the aquifer water with low mineralized water.of August, starting of conductivity electrical conductivity water. In the starting In the the electrical August, the increases until Septemincreases electrical conductivity from the deep basal aquiferof the deep basal aquifer water ber. The till September. The electrical conductivity water collected by piezometer S5 collected bycontinuously from the beginning on the rainy the starting of the rainy season decreased piezometer S5 decreased continuously from season until mid-September when till mid-September whenstatic untilremained virtually staticThis behavior is believed to become its value remained pretty much its value the end of the season. till the end from the season. This behavior is thought toinduced by a sizable influx of water with aalow chemical load. on account of intensive leaching be as a consequence of intensive leaching induced by huge influx of water using a low chemical load.Water 2021, 13, 3216 Water 2021, 13, x FOR PEER REVIEW16 of 22 16 ofFigure 16. Groundwater hydrographs versus electrical conductivity in relation to rainfall in the outFigure 16. Groundwater hydrographs versus electrical conductivity in relation to rainfall in the outlet let of your catchment. of the catchment.4.four. Discussion Discussion The distribution of hydraulic conductivity values shows reasonably higher values the The distribution of hydraulic conductivity values shows fairly high values inin central valley (S1, S1Bis, S2, S2, and SA). Evaluation of hydrographs with the aquifers within the the central valley (S1, S1Bis, and SA). Evaluation of your the hydrographs of the aquifers location region shows an instantaneous response on the aquifers aquifers to key rainfall within the shows an almostalmost instantaneous response with the to major rainfall events (Figure 13). This really is the result of superior of great hydraulic continuity the permeable soils and events (Figure 13). This is the outcome hydraulic continuity betweenbetween the permeable the saturated zone on the region. Pumping tests Pinacidil custom synthesis performed by [48,65] [48,65] recommended soils and also the saturated zone of the location. Pumping tests performed by recommended a larger a pe.