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NOTE: To get off this list, send email to majordomo@aqua.ccwr.ac.za with the body of the message containing the line: unsubscribe sowacs > Reply to Ginny Carrera > > A sand, particularly a pure sand of dune origons will have a very > uniform grain size. That means it also has a uniform pore size which > in turn means that if a column of saturated sand is subjected to > higher and higher suctions (raised further above the water table) , it > will not change water content very much at all until a particular > suction is reached, then nearly all the water drains at once. I have a > sand which drains at 49.5cm suction precisely leaving the sand water > content virtually zero.. As the silt and clay content increase, the > material will drain slowly over a wider range of suctions and will not > drain completely. > > The suction at which it wets will also be very precise - but it is > unlikely to be the same suction as that at which it drains. > cliff.hignett@soilwater.com.au > > owner-sowacs@aqua.ccwr.ac.za wrote: > > > NOTE: To get off this list, send email to majordomo@aqua.ccwr.ac.za > > with the body of the message containing the line: > > unsubscribe sowacs > > > > Jiny Carrera asks > > > > In a sand (free of osmotic suction) what is the > > relationship between matric suction and the height of > > the soil with respect to the water table? > > > > Is this relationship the same for both, wetting and > > drying process? > > > > __________________________________________________ > > -- > Cliff Hignett > Soil Water Solutions > 45a Ormond Ave > Daw Park > South Australia 5041 > pH 61 (08) 8276 7706 > WWW.SOILWATER.COM.AU > > > > >