Research Article
A GIS-Enabled Approach for Assessing Damage Potential of Levee Systems Based on Underlying Geology and River Morphology
Table 13
Parameters from the ordinary kriging semivariograms of identified soil layers in the study areas.
| |||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
Units of these elements is the “square of the corresponding parameter unit”. bNo kriging estimate could be done due to limited number of data points available for the parameter of this layer. cThe low value of the range for the deep Sacramento River as compared to the other sand layers is due to limited number of data points at large distances for this particular layer. |