GEOSTATISTICAL CHARACTERIZATION OF SOIL-MOISTURE PATTERNS IN THE TARRAWARRA A CATCHMENT

Spatial soil moisture patterns have been measured in the 10.5 ha Tarra warra catchment in temperate south-eastern Australia on 13 occasions u sing time domain reflectometry (TDR). Measurements are made on regular grids of between 500 and 2000 points for each occasion. The spatial c orrelation structure of these soil moisture patterns is analysed. Samp le variograms are found to have a clear sill and a nugget. Exponential variogram models, including a nugget, fit the sample variograms close ly. The geostatistical structure is found to evolve seasonally. High s ills (5-25 (% v/v)(2)) and low col relation lengths (35-50 m) are obse rved during the wet winter period. During the dry summer period sills an smaller (5-15 (%v/v)(2)) and correlation lengths are longer (50-60 m). This seasonal evolution is explained on the basis of the importanc e of lateral redistribution of moisture during different seasons. Both a nugget effect due to measurement error and variability at small sca les contribute to the variability at the 10 m scale, which is the smal lest scale in most of the data sets, For one occasion four soil moistu re patterns containing 514 samples were collected on 10 x 20 m grids. These patterns are offset by 2 m in an easterly and/or a northerly dir ection. Variograms for these four patterns are similar which indicates that variograms used for the structural analysis are highly reliable. An analysis based on transects subsampled from typical summer and win ter soil moisture patterns indicates that a substantial number of data points (more than about 300) are needed to obtain meaningful sample v ariograms. (C) 1998 Elsevier Science B.V.