| Summary: | Soil and groundwater salinity poses a serious problem in Khon Kaen Province of Thailand and causes major reductions
to crop productivity. In this study, aerial photo interpretation, field studies, and borehole lithology log data were analyzed to
explore the spatial relationship between geological structure and the distribution of salinity. The results show that geological
structures play an important role in determining the salinity distribution. Slight and moderate salinity are generally found over
syncline structures and rock formation boundaries, whereas severe salinity is generally found over anticline structures and around
depressions containing rock salt. All three categories of salinity (slight, moderate, and severe) are encountered along fractures
associated with braided streams and faults associated with meandering streams. The electrical resistivity tomography results
showed that the depth of saline groundwater was between 5 and 30 m and its distribution was related to geomorphology. Salinity
distributions are natural occurrences controlled by subsurface geological structures and geomorphology.
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