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Articles 6871 - 6900 of 29939
Full-Text Articles in Geology
Mgrre_Thinsections_Mgrre-78a_10, Mgrre
Mgrre_Thinsections_Mgrre-78a_12, Mgrre
Mgrre_Thinsections_Mgrre-78a_14, Mgrre
Mgrre_Thinsections_Mgrre-78a_17, Mgrre
Mgrre_Thinsections_Mgrre-78a_18, Mgrre
Mgrre_Thinsections_Mgrre-78a_20, Mgrre
Mgrre_Thinsections_Mgrre-78a_21, Mgrre
Mgrre_Thinsections_Mgrre-78a_22, Mgrre
Mgrre_Thinsections_Mgrre-78a_23, Mgrre
Mgrre_Thinsections_Mgrre-78a_24, Mgrre
Mgrre_Thinsections_Mgrre-78a_3, Mgrre
Mgrre_Thinsections_Mgrre-78a_4, Mgrre
Mgrre_Thinsections_Mgrre-78a_19, Mgrre
Mgrre_Thinsections_Mgrre-78a_5, Mgrre
Mgrre_Thinsections_Mgrre-78a_6, Mgrre
Mgrre_Thinsections_Mgrre-78a_7, Mgrre
Mgrre_Thinsections_Mgrre-78a_1, Mgrre
Mgrre_Thinsections_Mgrre-78a_8, Mgrre
Mgrre_Thinsections_Mgrre-78a_10, Mgrre
Mgrre_Thinsections_Mgrre-78a_11, Mgrre
Mgrre_Thinsections_Mgrre-78a_12, Mgrre
Mgrre_Thinsections_Mgrre-78a_13, Mgrre
Mgrre_Thinsections_Mgrre-78a_14, Mgrre
Mgrre_Thinsections_Mgrre-78a_16, Mgrre
Mgrre_Thinsections_Mgrre-78a_18, Mgrre
Mgrre_Thinsections_Mgrre-78a_20, Mgrre
Mgrre_Thinsections_Mgrre-78a_22, Mgrre
Mgrre_Thinsections_Mgrre-78a_24, Mgrre
Baseflow And Water Resilience Variability In Two Water Management Units In Southeastern Brazil, Lucas Vituri Santarosa, Didier Gastmans, Troy E. Gilmore, Jan Boll, Sebastian Balbin Betancur, Vitor Fidelis Monteiro Gonçalves
Baseflow And Water Resilience Variability In Two Water Management Units In Southeastern Brazil, Lucas Vituri Santarosa, Didier Gastmans, Troy E. Gilmore, Jan Boll, Sebastian Balbin Betancur, Vitor Fidelis Monteiro Gonçalves
Conservation and Survey Division: Faculty and Staff Publications
Changes in climate and water demand in densely populated regions increasingly affect hydrological systems, and, in turn, impact socioeconomic conditions. In this case study, we identify how the hydrogeological frameworks of two water resource management units, Tietê-Jacaré (TJ) and Piracicaba-Capivari-Jundiaí (PCJ) in Sao Paulo state (Brazil), control the baseflow processes and resilience in the face of streamflow fluctuations in response to anthropogenic activities and climate variation. The results reveal between 40% and 75% contributions of baseflow to total streamflow in basins overlying crystalline and sedimentary aquifers. The basins in PCJ which mostly overly crystalline aquifers, have shorter water residence times …