INVESTIGADORES
PICCOLO Maria Cintia
congresos y reuniones científicas
Título:
The Quequen Salado river overflows in its upper basin.
Autor/es:
MARINI, M.F.; SCHWALLER, D.; PICCOLO, M.C.
Lugar:
Bahía Blanca
Reunión:
Congreso; 4th LOICZ Open Science Meeting; 1999
Institución organizadora:
LOICZ
Resumen:
The Quequen Salado River is very important in the central zone of the southeast of the Buenos
Aires Province because it flows over a large hinterland. Its basin is located in a region where
the agricultural and farming activities, in general, are essential. The river is characterized in
some sectors of its watercourse by steep riverbanks. The main objective of this study is to
investigate the consequences of the river floodings over some regions of its basin. Maps in
different scales from the Military Geographic Institute were used in the study and several
surveys performed in the area provided material for this investigation.
The mean annual rainfall in the basin is 700 mm. However, in the last few decades, there have
been events of intense precipitation. In some extraordinary events more than 150 mm of
precipitation have fallen during two or three days. These circumstances cause overflows in the
basin affecting some towns that are not even in the area of the river basin. This is the case of
Copetonas, located to the east of the basin. The town is limited by El Gaucho Creek, which has
a basin area of 887 km2. During the 20th century, the town was threatened by flooding from the
creek due to the entrance of the water. The El Gaucho overflows are caused by the entrance of
Quequen Salado River water into the creek during these intense precipitation events. After
analyzing the problem, several possible solutions of the Copetonas floodings are presented and
discussed. One of them is the construction of a channel that will divert the waters towards a
steep riverbank sector of the Quequen Salado River.2. During the 20th century, the town was threatened by flooding from the
creek due to the entrance of the water. The El Gaucho overflows are caused by the entrance of
Quequen Salado River water into the creek during these intense precipitation events. After
analyzing the problem, several possible solutions of the Copetonas floodings are presented and
discussed. One of them is the construction of a channel that will divert the waters towards a
steep riverbank sector of the Quequen Salado River.