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A sheetlike phase could be produced by subjecting a suspension simultaneously to a uniaxial field and steady or oscillatory shear–a known magnetohydrodynamic instability. Such a material would be quite interesting; the two-dimensional sheets would be nearly structurally equivalent in the plane that includes the uniaxial field direction and the direction of shear, yet the easy axis of the particles would align with the field, leading to a material with different magnetic properties along the three principal axes
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A sheetlike phase could be produced by subjecting a suspension simultaneously to a uniaxial field and steady or oscillatory shear–a known magnetohydrodynamic instability. Such a material would be quite interesting; the two-dimensional sheets would be nearly structurally equivalent in the plane that includes the uniaxial field direction and the direction of shear, yet the easy axis of the particles would align with the field, leading to a material with different magnetic properties along the three principal axes.
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