The load-flow relationship of salt in drainage water was studied using
drainage water flow and salinity data from an irrigation district on
the west side of the San Joaquin Valley of California. Flow and salini
ty data were collected from the main district drain, individual draina
ge sumps, and two field sites. Linear regression was used to describe
the salt load-flow relationship at each drainage site. The slope of th
e regression line for the salt flow in the main drain was different co
mpared to the subsurface drainage sites because of the inclusion of su
rface runoff from irrigation in the main drain. The EC in the water fr
om the subsurface drains was not correlated with the flow rate. Cluste
r analysis of the load-flow relationships of 45 individual drainage su
mps indicated that the load-flow relationship for flow from the distri
ct could be characterized by one of three relationships.