Characterization And Spatial Variability of a Phosphate Minesoil in Central Florida
Characterization And Spatial Variability of a Phosphate Minesoil in Central Florida
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The figure did show roughly, however, the relationship between sampling points and spoil islands. It was evident that the long rows of spoil of uneven height were already partially covered with ST, forming spoil islands. It was impossible to identify precisely all the spoil islands or determine how much of the spoil remained above the ST at the end of the filling stage.
3ased on the measurements of depth to spoil-capped ST taken in the medium-sized grid, it appears that the spoil ridge underlyi...ng the eastern 2/3 of the medium grid largely was buried by the ST prior to leveling. The ST was closer to the surface on the northern half (Fig. 12) and deeper to the south.
On tne southeastern edge of the medium grid, it was common to find a thin (3 to 30 cm) layer of ST somewhere in the profile. These layers usually contained more clay (field textures ranging from sand to sandy loam) than was found in ST elsewhere. This characteristic of higher clay content in ST just above spoil was observed elsewhere on the study site.
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To quickly assess the difficulty of the text, read a short excerpt:
The figure did show roughly, however, the relationship between sampling points and spoil islands. It was evident that the long rows of spoil of uneven height were already partially covered with ST, forming spoil islands. It was impossible to identify precisely all the spoil islands or determine how much of the spoil remained above the ST at the end of the filling stage.
3ased on the measurements of depth to spoil-capped ST taken in the medium-sized grid, it appears that the spoil ridge underlyi...ng the eastern 2/3 of the medium grid largely was buried by the ST prior to leveling. The ST was closer to the surface on the northern half (Fig. 12) and deeper to the south.
On tne southeastern edge of the medium grid, it was common to find a thin (3 to 30 cm) layer of ST somewhere in the profile. These layers usually contained more clay (field textures ranging from sand to sandy loam) than was found in ST elsewhere. This characteristic of higher clay content in ST just above spoil was observed elsewhere on the study site.
What to read after Characterization And Spatial Variability of a Phosphate Minesoil in Central Florida?
You can find similar books in the "Read Also" column, or choose other free books by Gensheimer, Gregory J. to read onlineMoreLess
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