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48: 107-118. W i l l i a m s , J . and C o v e n t r y , R . J . , 1979. The c o n t r a s t i n g s o i l hydrology of red and y e l l o w e a r t h s in a landscape of low r e l i e f . I n : The hydrology of a r e a s of low precipitation. IAHS P u b l . No. 128, pp. 385-95. W r o n s k i , E . B . , 1980. Hydrometeorology and water r e l a t i o n s of Pinus radiata. P h . D . T h e s i s . F l i n d e r s U n i v . of South A u s t r a l i a , 317 pp. 35 TRANSPORT OF SALTS IN SOILS AND SUBSOILS E.

Volumetric Water Content, 0(cm cm"3) 3 F i g . 4 . S o i l w a t e r s u c t i o n head ( h ) as a f u n c t i o n of s o i l water c o n t e n t ( θ ) f o r 4 v a l u e s of s o l u t i o n c o n c e n t r a t i o n ( C ) . Computed r e s u l t s ( s o l i d l i n e s ) a r e compared w i t h measured c u r v e s (dashed l i n e s ) . 10 i s s h i f t e d and data a r e t r a n s l a t e d along θ a x i s . (After Russo and B r e s l e r , 1980). From d i f f u s e double l a y e r t h e o r y t h e d i s t a n c e 2d between a d j a c e n t q u a s i c r y s t a l s can be c a l c u l a t e d as a f u n c t i o n ential v a l u e s f o r mixed systems.

7 shows the r e l a t i v e anion e x c l u s i o n c o n c e n t r a t i o n function of b c , where the l a t t e r 2 v a r i e s between 200 and 20 000. f data a r e obtained from the r e l a t i o n s h i p f o r experimental (ν θ χ ) d a t a , v a l u e s of b, Α or t h e e x c l u s i o n w a t e r c o n t e n t Measured = V ^ e x * It = 6 ex / ( b A ex b' p ( f ) as a θ χ (θ ^ c a , p , b -| c u -| ted a = r ~/( b c )- T Theoretical o calculate f and e i t h e r the e x c l u s i o n volume ) must be known.

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