The temporal and spatial distribution of salinity in the field is usually expressed by simple averaging of the data. The high values of standard deviation that usually exceed 50% of the average salinity make it impossible to reach valid conclusions. A method that normalizes soil salinity data was developed and its advantages are presented.
|Number of pages||3|
|Journal||Journal of Irrigation and Drainage Engineering - ASCE|
|State||Published - Jan 2003|
- Subsurface drainage