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To test this hypothesis, flow experiments were conducted on experimental soil columns with different spatial architecture of soil collected from the Norman Landfill site.
The implications that the architecture of soil pore system evolution could have on the capacity of these constructed soils as well as "natural" soils to carry out their basic functions are also discussed.
Because of its ability to visualize the 3D architecture of soil non-destructively, X-ray computed tomography (CT) is becoming a widespread tool for studying soil pore network structure.
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Over the last decade, X-ray computed tomography (CT) has been used increasingly to characterise the microscale architecture of soils.
The objective of this study was to quantify the architecture of soils beneath the shrub canopy and in the adjacent interspace grass area following the establishment of a shrub Caragana microphylla Lam.
The objective of this study was to quantify the architecture of soils beneath Alpine Kobresia meadow, Farmland, and Sand using computed tomography in the Qinghai Lake Watershed of northeastern Qinghai-Tibet Plateau.
The objective of this study was to quantify the architecture of soils beneath Alpine Kobresia meadow, Achnatherum splendens steppe, and Potentilla fruticosa shrubs using computed tomography in the Qinghai Lake Watershed of northeastern Qinghai Tibet Plateau.
Further studies are needed to investigate the potential effects of root architecture on soil detachment capacity by overland flow under different conditions.
The stabilisation of organic materials in soils by the soil matrix is a function of the chemical nature of the soil mineral fraction and the presence of multivalent cations, the presence of mineral surfaces capable of adsorbing organic materials, and the architecture of the soil matrix.
However, the soil architecture of different land uses is not well understood elusive in Alpine region.
Soil microstructure is an important component of soil architecture.
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