Caracterização fisiográfica e vazão de duas bacias hidrográficas do sítio PELD TURF na Chapada do Couto, Serra do Espinhaço Meridional

Abstract

Watersheds are the basic unit for hydrological studies, as they allow the spatial and temporal compartmentalization of water fluxes within the hydrological cycle. e hydrological response of watersheds varies according to numerous factors, such as size and form, drainage network and relief characteristics, among others, what demands the physiographical characterization of watershed in relation to these parameters. e aim of the present study was to characterize two experimental watersheds that are being monitored in the Long-Term Ecological Research Site Peatlands from Southern Espinhaço Mountain Range (PELD TURF) installed in the Chapa do Couto plateau, at the easternmost Southern Espinhaço Mountain Range, Minas Gerais state, Brazil. Both watersheds were characterized according to parameters related to shape and size, parameters related to the drainage network and parameters related to relief. e water discharge from both watersheds was measured on two different years (2021 and 2022) during the dry season (June) and the rainy season (December). e physiographical characterization pointed that the watershed located within the conservation unit of the Rio Preto State Park (RP watershed) was more likely to generate surface runoff, given its more compact shape, less extensive drainage network and higher slope. Nevertheless, the watershed impacted by anthropization (ARA watershed) presented lower water discharge during the dry season and higher discharges during the rainy season than the RP watershed, possibly indicating that its hydrological response is being affected by the conditions of the recharge area, subject to fires and grazing by cattle