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<br />1968 <br /> <br />6 <br /> <br />SPATIAL VARIABILITY <br /> <br />X-SALTY <br />-t-FRESH <br /> <br />/1\ <br />/ \ <br />J '\ <br /> <br />/{ \1\ <br /> <br />/ '\ / <br />/ '\ / <br />)< 'X-- -X <br />/ <br />/ <br />/ <br /> <br />... <br />"X.... <br /> <br />......1\ <br />...K-" \ <br />\ <br />\ <br />'X,.... <br />'-X <br /> <br />L <br />U <br />"- <br />(f) <br />o <br />I <br />:L <br />L <br /> <br />4 <br /> <br />u <br />w <br /> <br />2 <br /> <br />, <br /> <br /> <br /> <br />o <br /> <br />1 2 <br />SOUTH <br /> <br />3 <br /> <br />4 <br /> <br />5 <br /> <br />6 <br /> <br />6 <br /> <br />5 <br /> <br />4 <br /> <br />321 <br />NORTH <br /> <br />IRRIGATION LEVEL <br /> <br />Figure A-6. Soil electrical conductivity (Ee) from saturated extract for the 30-60 cm <br />(1-2 ft) depth collected August 4, 1981 as part of the field variability <br />study. <br /> <br />w <br />w <br /> <br />