Estudo do nivel piezometrico por analise geoestatistica


Autoria(s): Sturaro, J. R.; Landim, P. M B
Contribuinte(s)

Universidade Estadual Paulista (UNESP)

Data(s)

27/05/2014

27/05/2014

01/12/1988

Resumo

160 groundwater bores in the Ribeirao Preto region were used to study the behaviour of the piezometric surface of the Botucatu Formation aquifer by geostatistical methodology. The semi-variogram showed the following results: nugget = 50 m2; sill = 450 m2 and range = 4.5 km. The piezometric surface, obtained by punctual kriging in a 100 x 100 knot grid, revealed two lowered zones: one in a southwest to north-northeastern trend, indicating the groundwater flow north toward the Rio Pardo; and the other in the central part due to the high concentration of holes in the urban region of Ribeirao Preto city. -from English summary

Formato

201-210

Identificador

Geociencas, v. 7, p. 201-210.

http://hdl.handle.net/11449/63879

2-s2.0-0024253260

Idioma(s)

por

Relação

Geociencas

Direitos

closedAccess

Palavras-Chave #geostatistical method #groundwater flow #piezometric surface #Brazil, Rio Pardo
Tipo

info:eu-repo/semantics/article