Author/Authors :
Rahmati, M. Department of Soil Science and Engineering - Faculty of Agriculture - University of Maragheh, Iran , Neyshabouri, M.R. Department of Soil Science - Faculty of Agriculture - University of Tabriz, Iran , Mohammadi-Oskooei, M. Faculty of Mining Engineering - Sahand University of Technology, Tabriz, Iran , Fakheri-Fard, A. Department of Water Engineering - Faculty of Agriculture - University of Tabriz, Iran , Ahmadi, A. Department of Water Engineering - Faculty of Agriculture - University of Tabriz, Iran
Abstract :
Characterizing soil infiltration parameters is time consuming and costly. We carried out
the current research to predict different parameters of soil infiltration using field/laboratory
measured and remotely-sensed data. The investigated parameters included infiltration rates
at different time intervals and the parameters of the three well-known infiltration models.
We employed soil sampling and field measurements on late spring 2012 and acquired
ETM+ data for the correspondent dates. We measured several soil properties as well as
infiltration. Then, we developed several pedo-transfer functions (PTFs) from the collected
field/laboratory measured and remotely sensed data to predict the intended infiltration
parameters. Results showed that field/laboratory measured data were able to predict soil
infiltration rates and parameters of the investigated models with reasonably high accuracies
(E value up to 0.961). The results also revealed that, although there was no significant and
robust relationship between soil surface reflectance and the investigated parameters, the
developed PTFs had reasonable accuracies (E value up to 0.634) in estimating the intended
infiltration parameters using soil characteristics (moisture content, soil separates, and
organic carbon) which are predictable from remotely sensed data.
Keywords :
Lighvan watershed , Remote sensing , Soil infiltration , Pedo-transfer functions