
This work is licensed under a Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License.
The soil physical properties show spatial variability due to the intrinsic characteristics and the changes  generated by soil management. Since this is important for agriculture, a research was carried out in order  to evaluate that variability by the deterministic and geostatistical method in two plots of soils coming from volcanic ash and located in the Department of QuindÃo–Colombia. In each farm, 1.0 ha was delimited  and soil samples were taken in a grid pattern every 10 m. Sand, silt and clay, humidity retention to field capacity (FC) and wilting point (WP), particle density (DP) and bulk density (DB), aggregates stability  (AS), hydraulic conductivity (HC) and penetration resistance (PR) were evaluated. Most of the properties  showed normal distribution and coefficients of variation from low to intermediate. The spatial variability of the properties was different in both plots, which was attributed to the influence of the geomorphology because in the plot with heterogeneous geomorphology, 5 properties showed spatial tendency, 2 showed  Nugget effect, and in 2 the prediction was not reliable. In the most homogeneous plot, 3 properties showed spatial tendency and the remaining 7 were adjusted to  theoretical models with reliable results. Therefore,  the sampling grid system in plots with heterogeneous topography was not the most appropriate for studies with geostatistical purposes. Besides, the IDW method was useful to expose the spatial variability of the  properties that did not meet the geostatistical assumptions.