Including topography and vegetation attributes for developing pedotransfer functions
Sharma, S.K., Mohanty, B.P. , Zhu, J. Including topography and vegetation attributes for developing pedotransfer functions. Soil Science Society of America Journal Volume 70, Issue 5, September 2006, Pages 1430-1440
Sharma, S.K., Mohanty, B.P. , Zhu, J. Including topography and
vegetation attributes for developing pedotransfer functions. Soil
Science Society of America Journal Volume 70, Issue 5, September
2006, Pages 1430-1440
Abstract - With the advent of advanced geographical informational
systems (GIS) and remote sensing technologies in recent years,
topographic (elevation, slope, aspect, and flow accumulation) and
vegetation attributes are routinely available from digital
elevation models (DEMs) and normalized difference vegetation index
(NDVI) at different spatial (remote sensor footprint, watershed,
regional) scales. Based on the correlation of soil distribution and
vegetation growth patterns across a topographically heterogeneous
landscape, this study explores the use of topographic and
vegetation attributes in addition to pedologic attributes to
develop pedotransfer functions (PTFs) for estimating soil hydraulic
properties in the Southern Great Plains of the USA. The extensive
Southern Great Plains 1997 (SGP97) hydrology experiment database
was used to derive these functions by using artificial neural
networks. Eighteen models combining bootstrapping technique with
artificial neural networks were developed in a hierarchical manner
to predict the soil water contents at eight different soil water
potentials (θ at 5, 10, 333, 500, 1000, 3000, 8000, and 15000
cm) and the van Genuchten hydraulic parameters (θr, θs,
α, n). The performance of the neural network models was
evaluated using the Spearman correlation coefficient between the
observed and the predicted values and root mean square error
(RMSE). Although variability exists within boot-strapped
replications, improvements (of different levels of statistical
significance) were achieved with certain input combinations of
basic soil properties, topography and vegetation information
compared with using only the basic soil properties as inputs.
Topography (DEM) and vegetation (NDVI) attributes at finer scales
were useful to capture the variations within the soil mapping units
for the SGP97 region dominated by perennial grass cover.



