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- W1972912199 abstract "Quartz particles in sediments become flatter with decreasing size; a cleavage mechanism may operate below the critical size of about 100 microns. Flat particles would tend to form a more open packing than spherical particles, and this may contribute to the collapse of loess and similar soils and the sudden loss of strength observed in sensitive clay soils." @default.
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- W1972912199 date "1973-06-22" @default.
- W1972912199 modified "2023-09-30" @default.
- W1972912199 title "Shape and Nature of Small Sedimentary Quartz Particles" @default.
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- W1972912199 doi "https://doi.org/10.1126/science.180.4092.1277" @default.
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