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Online proceedings - EDA Publishing Association

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BACKGROUND<br />

11-13 <br />

May 2011, Aix-en-Provence, France<br />

represented in Fig. 3 and its nominal dimensions and<br />

<br />

III. THEORETICAL<br />

material properties are listed in Table I.<br />

pyrolytic graphite density ρ 2200 kg/m 3 1⁄ 2 <br />

. (10)<br />

The measurements were performed by the optical The magnetic properties of materials are identified by the<br />

strategy; the laser sensor Keyence LK-G82 (50kHz parameters described below. The induced magnetization <br />

sampling frequency, 0.2µm±0.05% accuracy) was used to persists in the permanent magnets even if the external<br />

measure the static configuration of the system. The real magnetic field is removed; generally, it is given by<br />

thickness of every levitating mass was estimated as the<br />

<br />

average of 9 detections (1.707·10 -3 (1)<br />

average variance among<br />

where <br />

all the masses); the levitation height was also measured in<br />

is the magnetic susceptibility. The magnetic flux<br />

the different configurations of the system.<br />

density is related to by the equation<br />

(2)<br />

where is the magnetic permeability of free space<br />

(4 · 10 ⁄ ). Under the hypothesis of 1, valid<br />

for diamagnetic materials, the combination of Eqs. (1) and<br />

(2) gives the relations<br />

(3)<br />

1 (4)<br />

where 1 is the relative magnetic permeability<br />

and is the magnetic permeability.<br />

Diamagnetic materials are characterized by very small<br />

negative (that means slightly smaller than 1),<br />

paramagnetic materials have very small positive ( <br />

slightly higher than 1) and are weakly attracted by magnetic<br />

Fig. 1. Application of the magnetic suspension to real devices [8]. fields, ferromagnetic materials have large positive ( <br />

much larger than 1) and are strongly attracted by magnetic<br />

fields. Thanks to their properties, diamagnetic materials are<br />

able to generate a weak opposite field when inserted into an<br />

external magnetic field; consequently, in particular<br />

conditions, the magnetic force acting on the diamagnetic<br />

mass may balance the gravity force and produce levitation.<br />

To estimate the magnetic force, the single dipole of the<br />

diamagnetic material (e.g. atoms, molecules, ions, etc.) has<br />

Fig. 2. Image of the levitating system.<br />

to be considered. Each dipole has an individual<br />

y<br />

characteristic magnetization . The unit of volume ∆ has<br />

a magnetization<br />

z<br />

∑ <br />

∆ . (5)<br />

w<br />

The single dipole immerged in the magnetic field with<br />

o x flux density has the potential energy<br />

(6)<br />

o x l<br />

then, the elementary diamagnetic force acting on the dipole<br />

can be calculated as<br />

. (7)<br />

The diamagnetic force per unit volume is<br />

Fig. 3. Configuration of the levitating system.<br />

∑ <br />

∆ (8)<br />

and, from Eq. (3), it results<br />

TABLE I<br />

NOMINAL DIMENSIONS AND MATERIAL PROPERTIES<br />

1⁄ 2 (9)<br />

Description Symbol Value Unit<br />

IV. MODELING<br />

NdFeB magnets side w 20 mm<br />

NdFeB magnets thickness t’ 3 mm<br />

The static levitation distance of the proof mass can be<br />

NdFeB magnets layers N 1-2-3 -<br />

predicted by considering the diamagnetic force for unit<br />

NdFeB coercive force H c 860÷995 kA/m volume in the vertical direction as expressed by Eq. (9);<br />

χ<br />

NdFeB mag. susceptibility x,y -85·10 -6 -<br />

instead, the horizontal contributions are opposite in<br />

χ z -450·10 -6 -<br />

pyrolytic graphite side l 10 mm direction and self balanced. For orthotropic materials, it<br />

pyrolytic graphite thickness t 0.3-0.5-0.7-0.9-1.0 mm results<br />

98

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