Relación entre el cambio de uso del suelo en la cuenca del Aconcagua y su litoral arenoso correlativo: Chile central

Authors

  • María Victoria Soto Bäuerle Universidad de Chile
  • Joselyn Arriagada González Universidad de Chile
  • Carmen Paz Castro Correa Universidad de Chile
  • Michael Maerker Universität Potsdam
  • Giuliano Rodolf Universidad de Florencia

DOI:

https://doi.org/10.4067/S0718-34022011000300011

Keywords:

Land use change, sediment input, coastal sand dunes

Abstract

In the Aconcagua basin the modernization and intensification of land use have resulted both in an agricultural conversion, and the increase in area cultivated. This process has been very intense as far that have entered new areas beyond the limits of the valley and towards sloping ground. This signals changes in land use over the vegetation coverage models. The analysis of the geomorphology of the coastline in detail, accounts for the occurrence of transformations on the beach and dunes that are spatially less significant, but evolutionarily important, since they show a sediment feeding, which could be correlated with changes in vegetation cover in the basin.

 

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Author Biographies

María Victoria Soto Bäuerle, Universidad de Chile

Departamento de Geografía, Universidad de Chile (Chile). 

Joselyn Arriagada González, Universidad de Chile

Departamento de Geografía, Universidad de Chile (Chile). 

Carmen Paz Castro Correa, Universidad de Chile

Departamento de Geografía, Universidad de Chile (Chile). 

Michael Maerker, Universität Potsdam

Institut für Geoökologie, Universität Potsdam (Alemania). 

Giuliano Rodolf, Universidad de Florencia

Universidad de Florencia (Italia).   

Published

2011-12-31

How to Cite

Soto Bäuerle, M. V. ., Arriagada González, J. ., Castro Correa, C. P. ., Maerker, M. ., & Rodolf, . G. . (2011). Relación entre el cambio de uso del suelo en la cuenca del Aconcagua y su litoral arenoso correlativo: Chile central. Revista De Geografía Norte Grande, (50), 187–202. https://doi.org/10.4067/S0718-34022011000300011

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