
A. Castrignanò
Related Authors
Ilias Kounatidis
The Open University
Bilgili Volkan
Harran University
Mogens Humlekrog Greve
Aarhus University
Gaetano Robustelli
University of Calabria
simone pascucci
Consiglio Nazionale delle Ricerche (CNR)
Per Stenborg
University of Gothenburg
Christian Isendahl
University of Gothenburg
Theofanis Gemtos
UNIVERSITY OF THESSALY, GREECE
Uploads
Papers by A. Castrignanò
The aim of this study is to describe a method to optimize the spatial sampling scheme, taking physics constraints and preliminary information into account. The method is based upon a spatial simulated annealing algorithm. Spatial sampling schemes can be optimised for minimal kriging variance or distance between observations. Three case studies are presented in different pedoclimatic conditions (mountain, plane, hill) to locate 100 samples.
In Val Chiavenna (mountain, SO) minimal distance between observations criterion was used. Lithology, aerial photographs and two pedological profiles were preliminary information. In Lodi (plane) preliminary information was soil use and 158 soil samples. The optimization process was carried out in two steps: 50 samples were located with the minimal distance between observations criterion while additional 50 samples were located with the variance kriging criterion. In Mustigarufi (hill, CL) 50 samples were located with the minimal distance between observations criterion without take preliminary information into account. Additional 50 samples were located with the minimal distance between observations criterion and soil electrical conductivity variability, 6 pedological profiles and the earlier 50 observations as preliminary information.
The aim of this study is to describe a method to optimize the spatial sampling scheme, taking physics constraints and preliminary information into account. The method is based upon a spatial simulated annealing algorithm. Spatial sampling schemes can be optimised for minimal kriging variance or distance between observations. Three case studies are presented in different pedoclimatic conditions (mountain, plane, hill) to locate 100 samples.
In Val Chiavenna (mountain, SO) minimal distance between observations criterion was used. Lithology, aerial photographs and two pedological profiles were preliminary information. In Lodi (plane) preliminary information was soil use and 158 soil samples. The optimization process was carried out in two steps: 50 samples were located with the minimal distance between observations criterion while additional 50 samples were located with the variance kriging criterion. In Mustigarufi (hill, CL) 50 samples were located with the minimal distance between observations criterion without take preliminary information into account. Additional 50 samples were located with the minimal distance between observations criterion and soil electrical conductivity variability, 6 pedological profiles and the earlier 50 observations as preliminary information.