Publication Date

1989

Description

The purpose of this study is to examine the structure of macroporous soils which allows better aeration, water reten­tion and drainage. Previous investigations of macroporous soils have dealt with drainage (McIntyre and Sleeman, 1982), void forms (Tippkotter, 1983; Walker and Trudgill, 1983) and X-ray radiography (Rogaar, H. and R.A.H. Thiadens, 1975). Analyses of these studies have not proved sucessful to explain the effect of the soil structure as regards water retention and drainage. Therefore, the present study was designed to deter­mine the structure of macroporous soils by use of soft X-ray radiography and soil physical properties. Tokunaga et al.,(1984, 1986, 1988), found contrast media suitable for X-ray radiography on soil pore structures. The contrast media were infiltrated into soil samples and X-ray radiography was performed. The present investigation was undertaken to exam­ine the structure of a 14 year old grassland soil for macropore composition.

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Studies on the Macropores Structure of Grassland's Soil

The purpose of this study is to examine the structure of macroporous soils which allows better aeration, water reten­tion and drainage. Previous investigations of macroporous soils have dealt with drainage (McIntyre and Sleeman, 1982), void forms (Tippkotter, 1983; Walker and Trudgill, 1983) and X-ray radiography (Rogaar, H. and R.A.H. Thiadens, 1975). Analyses of these studies have not proved sucessful to explain the effect of the soil structure as regards water retention and drainage. Therefore, the present study was designed to deter­mine the structure of macroporous soils by use of soft X-ray radiography and soil physical properties. Tokunaga et al.,(1984, 1986, 1988), found contrast media suitable for X-ray radiography on soil pore structures. The contrast media were infiltrated into soil samples and X-ray radiography was performed. The present investigation was undertaken to exam­ine the structure of a 14 year old grassland soil for macropore composition.