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(Reference retrieved automatically from SciELO through information on FAPESP grant and its corresponding number as mentioned in the publication by the authors.)

Hydrological response of hydrographic sub-basins in the Piracicaba River Basin - Southeast Region of Brazil

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Author(s):
Ana Claudia Pereira Carvalho [1] ; Reinaldo Lorandi [2] ; José Augusto Di Lollo [3] ; Eduardo Goulart Collares [4] ; Luiz Eduardo Moschini [5]
Total Authors: 5
Affiliation:
[1] Universidade Federal de São Carlos - Brasil
[2] Universidade Federal de São Carlos - Brasil
[3] Universidade Estadual Paulista Júlio de Mesquita Filho - Brasil
[4] Universidade do Estado de Minas Gerais - Brasil
[5] Universidade Federal de São Carlos - Brasil
Total Affiliations: 5
Document type: Journal article
Source: Sociedade e Natureza; v. 34, 2022-03-16.
Abstract

Abstract The use of water for several human needs, associated with climate change, indicates how important it is to understand the response of watersheds, in order to provide adequate planning and management of water resources. This study was carried out in two pairs of hydrographic watersheds, in the Piracicaba River Basin, southeast of Brazil, analyzing water response, integrating in-situ collected precipitation and flow data, natural environmental attributes, and anthropic environmental data. To support the analysis, Surface Runoff Potential Charts (SRPC) were made. The evaluation of the physical characteristics of the sub- watersheds (SW(A) and SW(B)) shows that these areas present very low to low potential, indicating greater infiltration capacity. The use and coverage of the soil partially justifyies flow changes in pair 1, since SW(A) has a larger extent of agricultural areas that can use irrigation. SW(B), even with a greater variety of crops, has a smaller cultivated area and tends to demand less water. As for pair 2, the low runoff potential was mainly due to the predominance of flat relief in the sub-basins. Their soils present a higher fraction of silt and clay, with thicknesses > 5m in SW(C) and varying from 0.5m, reaching depths above 5m in SW(D). The physical properties of these soils do not provide a low flow rate, but when associated with the low slope of the land, geological characteristics and low drainage density are configured in regions where the flow flows more slowly, contributing to the evaporation and infiltration process. The use and coverage of the soil also partially justifyies the flow oscillations, due to anthropic activities in SW(C) and SW(D), such as irrigation and spraying of citrus, fertirrigation of sugarcane, irrigation of seedling nurseries, directly interfering with the availability of surface water. (AU)

FAPESP's process: 18/14145-4 - Spatial analysis of the water availability in sub-basins of the Piracicaba River (SP) for the proposition of water resources planning and management instrument
Grantee:Reinaldo Lorandi
Support Opportunities: Regular Research Grants