CSS :: Soils and Topography
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The development of soil structure from single grained or massive states conditions:
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[A]. |
Single grained: Where each soil particles function as an individual e.g. Sandy soil | [B]. |
Massive: Clay fills the spaces and pores so that the soil becomes dense and forms clods
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[C]. |
Both (a) & (b) | [D]. |
None of these |
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