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JPH0638367B2 - permanent magnet - Google Patents
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JPH0638367B2 - permanent magnet - Google Patents

permanent magnet

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Publication number
JPH0638367B2
JPH0638367B2 JP60007357A JP735785A JPH0638367B2 JP H0638367 B2 JPH0638367 B2 JP H0638367B2 JP 60007357 A JP60007357 A JP 60007357A JP 735785 A JP735785 A JP 735785A JP H0638367 B2 JPH0638367 B2 JP H0638367B2
Authority
JP
Japan
Prior art keywords
magnet
peripheral portion
inner peripheral
anisotropic
permanent magnet
Prior art date
Legal status (The legal status is an assumption and is not a legal conclusion. Google has not performed a legal analysis and makes no representation as to the accuracy of the status listed.)
Expired - Lifetime
Application number
JP60007357A
Other languages
Japanese (ja)
Other versions
JPS61168210A (en
Inventor
昭彦 井端
Current Assignee (The listed assignees may be inaccurate. Google has not performed a legal analysis and makes no representation or warranty as to the accuracy of the list.)
Panasonic Holdings Corp
Original Assignee
Matsushita Electric Industrial Co Ltd
Priority date (The priority date is an assumption and is not a legal conclusion. Google has not performed a legal analysis and makes no representation as to the accuracy of the date listed.)
Filing date
Publication date
Application filed by Matsushita Electric Industrial Co Ltd filed Critical Matsushita Electric Industrial Co Ltd
Priority to JP60007357A priority Critical patent/JPH0638367B2/en
Publication of JPS61168210A publication Critical patent/JPS61168210A/en
Publication of JPH0638367B2 publication Critical patent/JPH0638367B2/en
Anticipated expiration legal-status Critical
Expired - Lifetime legal-status Critical Current

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Description

【発明の詳細な説明】 (産業上の利用分野) 本発明は、永久磁石に関するものであり、さらに詳細に
は、多結晶マンガン−アルミニウム−炭素系(Mn-Al-C
系)合金磁石の改良に関するものである。
TECHNICAL FIELD The present invention relates to a permanent magnet, and more particularly, to a polycrystalline manganese-aluminum-carbon system (Mn-Al-C).
System) alloy magnets.

(従来の技術) Mn-Al-C系合金磁石は、主として強磁性相である面心正
方晶(τ相、L10形規則格子)の組織で構成され、Cを
必須構成元素として含むものであり、不純物以外に添加
元素を含まない3元系および少量の添加元素を含む4元
系以上の多元系合金磁石が知られている。また、このMn
-Al-C系合金磁石は、主として強磁性相である面心正方
晶の組織で構成され、前記の面心正方晶の〔001〕軸
(磁化容易軸)の統計的分布の相違によって等方性磁石
と各種の異方性構造を有する異方性磁石(たとえば、特
定の方向または特定の平面に磁化容易方向をもつ異方性
磁石)が知られている。
(Prior Art) An Mn-Al-C alloy magnet is mainly composed of a face-centered tetragonal structure (τ phase, L1 0 type ordered lattice) which is a ferromagnetic phase, and contains C as an essential constituent element. There are known ternary alloy magnets containing no additional element other than impurities and quaternary or more multi-component alloy magnets containing a small amount of additional elements. Also this Mn
-Al-C alloy magnets are mainly composed of a face-centered tetragonal structure, which is a ferromagnetic phase, and are isotropic due to the difference in the statistical distribution of the [001] axis (easy axis of magnetization) of the face-centered tetragonal crystal. A magnetic magnet and an anisotropic magnet having various anisotropic structures (for example, an anisotropic magnet having an easy magnetization direction in a specific direction or in a specific plane) are known.

多極着磁の分野で用いられる異方性磁石としては、特定
の方向に磁化容易方向を有する径方向異方性磁石、特定
の平面に平行な任意の方向に磁化容易方向を有した異方
性磁石(面異方性磁石、特開昭56-111203号公報)およ
び、前記特定の平面内で特定の方向に磁化容易方向を有
するようにし、内周部では径方向に磁化容易方向を有す
るか、または外周部では弦方向に磁化容易方向を有する
かの少なくともどちらかを満足する異方性磁石(特開昭
58-189355号公報)などが知られている。
As anisotropic magnets used in the field of multi-pole magnetization, radial anisotropic magnets having an easy magnetization direction in a specific direction, anisotropic magnets having an easy magnetization direction in an arbitrary direction parallel to a specific plane. Magnetic magnet (plane anisotropic magnet, JP-A-56-111203) and an easy magnetization direction in a specific direction within the specific plane, and an easy magnetization direction in the radial direction at the inner peripheral portion Or an anisotropic magnet satisfying at least one of the directions of having an easy magnetization direction in the chordal direction at the outer peripheral portion (Japanese Patent Laid-Open No. Sho 61-96).
No. 58-189355) is known.

(発明が解決しようとする問題点) 多極着磁の分野で用いられる磁石の形状としては、一般
には軸対称の形状であり、一例として円筒体がある。円
筒体の磁石の内周に多極着磁(内周着磁)した場合の磁
石内部での磁路の形成を模式的に第2図に示した。同図
において破線が磁路を示し、一つの径方向(γ方向)に
対する弦方向(θ方向)も示している。前述したように
円筒の径方向(γ方向)と円筒の軸方向にそれぞれ直交
する方向を弦方向(θ方向)とする。
(Problems to be Solved by the Invention) The shape of a magnet used in the field of multi-pole magnetization is generally axisymmetric, and a cylindrical body is an example. FIG. 2 schematically shows the formation of a magnetic path inside the magnet when the inner circumference of the cylindrical magnet is multi-pole magnetized (inner circumference magnetized). In the figure, the broken line indicates the magnetic path, and also indicates the chord direction (θ direction) with respect to one radial direction (γ direction). As described above, the direction orthogonal to the radial direction of the cylinder (γ direction) and the axial direction of the cylinder are the chord directions (θ direction).

第2図に示したように、磁路は、内周部ではほぼ径方向
に沿い、外周部ではほぼ弦方向に沿い、外周部と内周部
の中間部では径方向から弦方向に順次変化している。前
述したように、磁石の形状を円筒体とした場合に内周部
というのは磁路がほぼ径方向に沿っている部分をさし、
外周部というのは磁路がほぼ弦方向に沿っている部分を
さし、さらに中間部というのは磁路が径方向から弦方向
に順次変化している部分をさす。
As shown in FIG. 2, the magnetic path changes along the radial direction at the inner peripheral portion and along the chordal direction at the outer peripheral portion, and changes from the radial direction to the chordal direction at the intermediate portion between the outer peripheral portion and the inner peripheral portion. is doing. As described above, in the case where the magnet has a cylindrical shape, the inner peripheral portion means the portion where the magnetic path is substantially along the radial direction,
The outer peripheral portion refers to a portion where the magnetic path is substantially along the chord direction, and the intermediate portion refers to a portion where the magnetic path sequentially changes from the radial direction to the chord direction.

前述した内周部が径方向に磁化容易方向を有するか、ま
たは外周部が弦方向に磁化容易方向を有するかの少なく
ともどちらかを満足する異方性磁石では、どちらも満足
する異方性構造を有する異方性磁石であるとしても、前
述した内周中間部(磁路が径方向から弦方向に順次変化
している部分)に適した異方性構造を有していない。
In the anisotropic magnet satisfying at least one of the inner peripheral portion having the easy magnetization direction in the radial direction and the outer peripheral portion having the easy magnetization direction in the chord direction, an anisotropic structure satisfying both Even if it is an anisotropic magnet having the above, it does not have an anisotropic structure suitable for the above-mentioned inner peripheral intermediate portion (the portion where the magnetic path sequentially changes from the radial direction to the chord direction).

(問題点を解決するための手段) 以上述べてきた問題点を解決するために本発明の永久磁
石は、内周部では径方向に磁化容易方向を有し、外周部
では弦方向に磁化容易方向を有し、さらに外周部と内周
部の境界に第3の部分(中間部)として径方向から弦方
向に磁化容易方向が順次変化する領域を有する新規な異
方性構造をもったものである。
(Means for Solving the Problems) In order to solve the problems described above, the permanent magnet of the present invention has an easy magnetization direction in the radial direction at the inner peripheral portion and an easy magnetization direction in the chord direction at the outer peripheral portion. Having a direction, and having a novel anisotropic structure having a region where the easy magnetization direction sequentially changes from the radial direction to the chordal direction as a third portion (intermediate portion) at the boundary between the outer peripheral portion and the inner peripheral portion. Is.

(作用) 前述したように、第3の部分(中間部)を有するため、
第2図に示した内周着磁を施した場合、優れた磁気特性
を示す異方性磁石となる。
(Operation) As described above, since the third portion (intermediate portion) is included,
When the inner circumferential magnetization shown in FIG. 2 is applied, the anisotropic magnet exhibits excellent magnetic characteristics.

(実施例) 本発明は、前述した背景のもとに、内周部が径方向に磁
化容易方向を有するか、または外周部が弦方向に磁化容
易方向を有するかの少なくともどちらかを満足する異方
性磁石を改良した多極着磁に適した新規な異方性構造を
もった永久磁石をMn-Al-C系合金磁石の改良によって提
供するものである。
(Example) The present invention satisfies at least one of the inner peripheral portion having the easy magnetization direction in the radial direction and the outer peripheral portion having the easy magnetization direction in the chord direction based on the background described above. The present invention provides a permanent magnet having a novel anisotropic structure, which is an improved anisotropic magnet and is suitable for multi-pole magnetization, by improving the Mn-Al-C alloy magnet.

多極着磁の分野で用いられる磁石の形状は、一般には軸
対称の形状であるため、磁石の形状を軸対象の形状とし
て、第1図に基づいて本発明の永久磁石を説明する。
Since the shape of a magnet used in the field of multi-pole magnetization is generally an axially symmetrical shape, the permanent magnet of the present invention will be described with reference to FIG.

これまでに知られている異方性磁石は内周部が径方向に
磁化容易方向を有し、外周部が弦方向に磁化容易方向を
有しているが、本発明の永久磁石はさらに外周部と内周
部の境界に第3の部分(中間部)として磁化容易方向が
径方向から弦方向に順次変化する領域を有している。
In the anisotropic magnets known so far, the inner peripheral portion has the easy magnetization direction in the radial direction and the outer peripheral portion has the easy magnetization direction in the chord direction. A third portion (intermediate portion) has a region where the easy magnetization direction sequentially changes from the radial direction to the chordal direction at the boundary between the portion and the inner peripheral portion.

第1図に本発明の永久磁石を対称軸の方向からみた図を
示す。説明のために各部分を破線で区分けして模式的に
各領域を表わしている。1は内周部で磁化容易方向が径
方向に沿っている部分である。2は中間部で磁化容易方
向が中心に近づくにつれて弦方向から径方向に沿って変
化している部分であり、各凹部の表面から近傍の部分の
みをさし、同心円状のすべての部分をさすのではない。
3は外周部で磁化容易方向が弦方向に沿っている部分で
あり、中間部2と同様に、同心円状のすべての部分をさ
すのではない。本発明の永久磁石では、言い変えると、
内周面の凹部の表面に沿って磁石の外周への向きに磁化
容易方向の変化をみると、凹部の表面の近傍ではまず最
内周部(中心から最も近い、部分)では径方向に平行で
あり、外にいくにつれて順次弦方向に近づく方向に変化
し、凹部の最も外周に近い部分で弦方向に平行になるよ
うに変化している。第1図では模式的に3つの部分に分
けたが、前述したように連続的に変化している。
FIG. 1 shows a view of the permanent magnet of the present invention viewed from the direction of the axis of symmetry. For the sake of explanation, each part is divided into broken lines to schematically represent each region. Reference numeral 1 denotes an inner peripheral portion in which the easy magnetization direction is along the radial direction. In the middle part, 2 is a part in which the direction of easy magnetization changes from the chordal direction to the radial direction as it approaches the center, and refers to only the part in the vicinity of the surface of each recess, and all the concentric parts. Not of.
Reference numeral 3 denotes a peripheral portion where the easy magnetization direction is along the chord direction, and like the intermediate portion 2, does not refer to all concentric portions. In other words, in the permanent magnet of the present invention,
Looking at the change of the easy magnetization direction toward the outer circumference of the magnet along the surface of the recess on the inner peripheral surface, first in the vicinity of the surface of the recess, the innermost peripheral portion (closest to the center, part) is parallel to the radial direction. That is, the distance gradually changes toward the chord direction toward the outside, and changes so as to be parallel to the chord direction at the portion closest to the outer periphery of the recess. Although it is schematically divided into three parts in FIG. 1, it is continuously changed as described above.

第1図に示した例では、内周面の凸部が6個あるため、
内周に6極の多極着磁を施して用いるのに適した異方性
構造を有している。すなわち極数に合わせて凸部の数が
変化する。また内周着磁した場合の極の位置は内周面の
凸部である。
In the example shown in FIG. 1, since there are six convex portions on the inner peripheral surface,
It has an anisotropic structure suitable for being used by magnetizing the inner circumference with 6 poles. That is, the number of convex portions changes according to the number of poles. The position of the pole when the inner circumference is magnetized is the convex portion on the inner circumference.

本発明の永久磁石は、前述したような異方性構造をもっ
ているため、第2図に示したような内周着磁を施した場
合に優れた磁気特性を示すのである。
Since the permanent magnet of the present invention has the anisotropic structure as described above, it exhibits excellent magnetic characteristics when subjected to inner circumferential magnetization as shown in FIG.

第2図に示したような内周に多極着磁を施した場合、磁
路に沿うように、前記の面心正方晶〔001〕軸(磁化容
易軸)を配列させた構造を有するためである。
When multi-pole magnetized on the inner circumference as shown in FIG. 2, it has a structure in which the face-centered tetragonal [001] axis (easy axis of magnetization) is arranged along the magnetic path. Is.

一般に、多結晶体における結晶方位の優先配向の状態を
極密度Pで表現する。τ相は正方晶であるから、〔00
1〕軸の配向は(001)極密度分布として捉えることができ
る。多結晶のある方位での(001)極密度は、その方位に
X線回折方線を置いたときの(00n)面回折積分強度の等
方性材料の場合に対する比として測定される。等方性磁
石では全ての立体方位に対して極密度は1である。本発
明の永久磁石は換言すれば、磁石内の特定の平面に平行
な特定の方向でP>1であり、しかもその平面の垂線方
向でP<1である。
In general, the state of preferential orientation of crystal orientation in a polycrystal is represented by the pole density P. Since the τ phase is tetragonal, [00
The 1) axis orientation can be understood as a (001) pole density distribution. The (001) pole density in a certain orientation of a polycrystal is measured as the ratio of the integrated intensity of the (00n) plane diffraction when the X-ray diffraction line is placed in that orientation to that in the case of an isotropic material. In isotropic magnets, the pole density is 1 for all three-dimensional orientations. In other words, the permanent magnet of the present invention has P> 1 in a specific direction parallel to a specific plane in the magnet, and P <1 in the direction perpendicular to that plane.

発明者が試作した本発明の永久磁石について、両方向
(特定の方向と垂線方向)間の(001)極密度の相違は全
ての試料について3倍以上であった。また、前記平面に
平行な方向での(001)極密度は特定の方向と直角な方向
との比で、1.1以上であるが、その比を大きくする方が
磁気特性上有利である。
Regarding the permanent magnet of the present invention prototyped by the inventor, the difference in the (001) pole density between both directions (specific direction and perpendicular direction) was three times or more for all the samples. Further, the (001) pole density in the direction parallel to the plane is 1.1 or more in the ratio of the specific direction and the direction perpendicular to the specific direction, but it is advantageous in terms of magnetic properties to increase the ratio.

本発明の永久磁石は、前記の面異方性磁石において同等
に〔001〕軸を配列させた平面内でさらに外周部、中間
部および内周部で特定の方向に優先的に配列させたもの
である。磁気特性的にみれば、内周部では径方向(γ方
向)異方性で、外周部では弦方向(θ方向)異方性でさ
らに中間部では径方向から弦方向に順次異方性方向が変
化する。発明者らが試作した本発明の永久磁石について
は特定の方向とそれに直交する方向の残留磁束密度の比
が、1.1以上であった。
The permanent magnet of the present invention is one in which the plane anisotropic magnets are preferentially arranged in a specific direction at the outer peripheral portion, the intermediate portion and the inner peripheral portion within the plane in which the [001] axes are arranged in the same manner. Is. In terms of magnetic properties, the inner circumferential portion has radial (γ direction) anisotropy, the outer circumferential portion has chord direction (θ direction) anisotropy, and the middle portion has radial direction to chordwise anisotropic direction. Changes. With respect to the permanent magnet of the present invention prototyped by the inventors, the ratio of the residual magnetic flux density in the specific direction to the direction orthogonal thereto was 1.1 or more.

本発明の永久磁石は、公知のMn-Al-C系磁石用合金、た
とえば、68重量%ないし73重量%(以下単に%で示す)
のMnと(1/10Mn-6.6)ないし(1/3Mn-22.2)%のCと残部の
Alからなる合金を530ないし830℃の温度域で押出加工等
の公知の方法によって一軸性の均質微細な〔001〕繊維
組織としたのち、たとえば一つの製造法としては、軸方
向に圧縮加工を施し、圧縮加工によって試料の内周面を
凹凸上に形成することによって得ることができる。
The permanent magnet of the present invention is a known alloy for Mn-Al-C magnets, for example, 68% by weight to 73% by weight (hereinafter referred to simply as%).
Of Mn and (1 / 10Mn-6.6) to (1 / 3Mn-22.2)% C and the balance of
An alloy made of Al is formed into a uniaxial homogeneous fine [001] fiber structure by a known method such as extrusion in a temperature range of 530 to 830 ° C, and, for example, one manufacturing method is compression processing in the axial direction. It can be obtained by forming the inner peripheral surface of the sample on the concavo-convex portion by applying and compression processing.

次に本発明の具体的な実施例について説明する。Next, specific examples of the present invention will be described.

配合組成で69.5%のMn、29.3%のAl、0.5%のCおよび
0.7%のNiを溶解鋳造し、直径70mm、長さ50mmの円柱ビ
レットを作製した。このビレットを1100℃で2時間保持
したのち、室温まで放冷する熱処理を行なった。次に潤
滑剤を介して、720℃の温度で直径45mmまでの押出加工
を行なった。さらに潤滑剤を介して680℃の温度で直径3
1mmまでの押出加工を行なった。この押出棒を長さ20mm
に切断し、切削加工して、外径30mm、内径24mm、長さ20
mmの円筒ビレットを作製した。このビレットを用いて、
第3図および第4図に示した金型を用いて圧縮加工を行
なった。第3図においてDK(外径5の内径)=30mm、XA
=8mm、RS(ポンチ凸部のR)=2.5mm,DP(ポンチ
径)=16Zであり、ポンチ凸部は8個ある。第4図は第
3図と直交する方向からの断面図を示す。同図において
4はビレット、5は外型であり、6および7はポンチ
で、凹凸面がかみあうような表面を有し、図の上下方向
に移動することができる。このような金型を用いて、高
さ12mmまで圧縮加工を行なった。
69.5% Mn, 29.3% Al, 0.5% C and
0.7% Ni was melted and cast to form a cylindrical billet having a diameter of 70 mm and a length of 50 mm. After holding this billet at 1100 ° C. for 2 hours, it was heat-treated by allowing it to cool to room temperature. Next, through a lubricant, extrusion processing was performed at a temperature of 720 ° C. to a diameter of 45 mm. Further through the lubricant a diameter of 3 at a temperature of 680 ° C
Extrusion processing up to 1 mm was performed. This extruded rod is 20 mm long
Cut into pieces, cut and processed, outer diameter 30 mm, inner diameter 24 mm, length 20
A cylindrical billet of mm was produced. With this billet,
Compression processing was performed using the mold shown in FIGS. 3 and 4. In Fig. 3, D K (outer diameter 5 inner diameter) = 30 mm, X A
= 8 mm, R S (R of punch protrusion) = 2.5 mm, D P (punch diameter) = 16 Z , and there are 8 punch protrusions. FIG. 4 shows a sectional view taken in a direction orthogonal to FIG. In the figure, 4 is a billet, 5 is an outer mold, and 6 and 7 are punches, which have a surface in which uneven surfaces are engaged with each other and can be moved in the vertical direction of the figure. Using such a die, compression processing was performed to a height of 12 mm.

圧縮加工後のビレットを内径20mmまで切削加工し、8極
の内周着磁を施した。着磁は2000μFのオイルコンデン
サーを用い1500Vでパルス着磁した。内周面の表面磁束
密度をホール素子で測定した。比較のために、直径18m
m、長さ20mmの円柱ビレットを680℃の温度で円柱軸方向
に自由圧縮加工した。なお、圧縮加工後のビレットの高
さは12mmであった。加工後のビレットは表面異方性磁石
であり、前記と同様に切削加工し、着磁し、表面磁束密
度を測定した。
The billet after compression processing was cut to an inner diameter of 20 mm and magnetized with an inner circumference of 8 poles. The magnetization was pulsed at 1500 V using a 2000 μF oil condenser. The surface magnetic flux density of the inner peripheral surface was measured with a Hall element. 18m diameter for comparison
A cylindrical billet of m and 20 mm in length was freely compressed in the axial direction of the cylinder at a temperature of 680 ° C. The height of the billet after compression processing was 12 mm. The billet after processing was a surface anisotropic magnet, which was cut and magnetized in the same manner as described above, and the surface magnetic flux density was measured.

以上の両者の値を比較すると、本発明の方法で得た磁石
の表面磁束密度の値は、面異方性磁石のそれの約1.6倍
であった。
Comparing the above two values, the value of the surface magnetic flux density of the magnet obtained by the method of the present invention was about 1.6 times that of the surface anisotropic magnet.

前記と同様な方法で得た本発明の永久磁石の外周部およ
び内周部から一辺が3mmで、それぞれの辺が軸方向、径
方向および弦方向に平行である立方体を切り出し、各方
向の磁気特性を測定した。
From the outer and inner circumferences of the permanent magnet of the present invention obtained by the same method as described above, a cube having a side of 3 mm and each side parallel to the axial direction, the radial direction and the chord direction was cut out, and the magnetism in each direction was cut. The properties were measured.

外周部の弦方向では、Br=5.9kG,Hc=2.7kOe,(BH)max=
6.2MG・Oeであり、径方向では、Br=3.1kG,Hc=2.3kOe,
(BH)max=2.0MG・Oe、軸方向ではBr=2.6kG,Hc=1.9kOe,
(BH)max=1.4MG・Oe、また内周部ではBr=3.0kG,Hc=2.0
kOe,(BH)max=1.7MG・Oeであり、径方向では、Br=5.6k
G,Hc=2.5kOe,(BH)max=5.4MG・Oe、軸方向ではBr=2.6k
G,Hc=1.9kOe,(BH)max=1.4MG・Oeであった。
In the chord direction of the outer circumference, Br = 5.9kG, Hc = 2.7kOe, (BH) max =
6.2MG Oe, and in the radial direction, Br = 3.1kG, Hc = 2.3kOe,
(BH) max = 2.0MG ・ Oe, Br = 2.6kG, Hc = 1.9kOe, Axial direction
(BH) max = 1.4MG ・ Oe, and Br = 3.0kG, Hc = 2.0 in the inner circumference
kOe, (BH) max = 1.7MG ・ Oe, and radial direction Br = 5.6k
G, Hc = 2.5kOe, (BH) max = 5.4MG ・ Oe, axial direction Br = 2.6k
G, Hc = 1.9 kOe, (BH) max = 1.4 MG · Oe.

さらに、磁気トルク測定の結果、磁石内周面の凹部の近
傍部分では、凹部の表面にほぼ沿った方向に磁化容易方
向を有していることが判明した。
Further, as a result of measuring the magnetic torque, it was found that the portion of the inner peripheral surface of the magnet near the recess had an easy magnetization direction substantially along the surface of the recess.

(発明の効果) 本発明によれば、内周多極着磁に適した異方性構造を有
するため優れた磁気特性を示す永久磁石をうることがで
きる。
(Effect of the Invention) According to the present invention, it is possible to obtain a permanent magnet exhibiting excellent magnetic properties because it has an anisotropic structure suitable for inner circumferential multipole magnetization.

【図面の簡単な説明】[Brief description of drawings]

第1図は本発明の一実施例の永久磁石を異方性構造の違
いの区分けを模式的に示す図、第2図は円筒状磁石の内
周面に多極着磁を施した場合の磁石内部での磁路の形成
を模式的に示す図、第3図および第4図は、実施例にお
ける本発明の永久磁石を得るのに用いた金型の一部の断
面図である。 1……内周部、2……中間部、3……外周部、4……ビ
レット、5……外型、6,7……ポンチ。
FIG. 1 is a diagram schematically showing the classification of permanent magnets according to an embodiment of the present invention by the difference in anisotropic structure, and FIG. 2 is a diagram showing a case where multi-pole magnetization is applied to the inner peripheral surface of a cylindrical magnet. FIGS. 3 and 4 are schematic cross-sectional views of a mold used to obtain the permanent magnet of the present invention in Examples, showing the formation of a magnetic path inside the magnet. 1 ... inner peripheral part, 2 ... middle part, 3 ... outer peripheral part, 4 ... billet, 5 ... outer mold, 6,7 ... punch.

Claims (1)

【特許請求の範囲】[Claims] 【請求項1】主として面心正方晶の組織で構成される多
結晶マンガン−アルミニウム−炭素系合金磁石であっ
て、前記磁石の形状が軸対称であり、前記面心正方晶の
〔001〕軸が前記軸に垂直な平面に平行な任意の方向
に、前記軸方向に比して優先的に配列されていて、しか
も前記平面内の内周部では磁気的に径方向に異方性であ
り、外周部では磁気的に弦方向に異方性であり、さらに
前記外周部と内周部の間に中間部として中心に近づくに
つれて順次、磁気的な異方性の方向が弦方向から径方向
に変化する領域を有することを特徴とする永久磁石。
1. A polycrystalline manganese-aluminum-carbon alloy magnet mainly composed of a face-centered tetragonal structure, wherein the shape of the magnet is axisymmetric, and the face-centered tetragonal [001] axis is used. Are preferentially arranged in an arbitrary direction parallel to a plane perpendicular to the axis in comparison with the axial direction, and moreover, the inner peripheral portion in the plane is magnetically anisotropic in the radial direction. , The outer peripheral portion is magnetically anisotropic in the chord direction, and the magnetic anisotropy direction is gradually increased from the chord direction toward the radial direction as the center portion is closer to the center as an intermediate portion between the outer peripheral portion and the inner peripheral portion. A permanent magnet having a region that changes to.
JP60007357A 1985-01-21 1985-01-21 permanent magnet Expired - Lifetime JPH0638367B2 (en)

Priority Applications (1)

Application Number Priority Date Filing Date Title
JP60007357A JPH0638367B2 (en) 1985-01-21 1985-01-21 permanent magnet

Applications Claiming Priority (1)

Application Number Priority Date Filing Date Title
JP60007357A JPH0638367B2 (en) 1985-01-21 1985-01-21 permanent magnet

Publications (2)

Publication Number Publication Date
JPS61168210A JPS61168210A (en) 1986-07-29
JPH0638367B2 true JPH0638367B2 (en) 1994-05-18

Family

ID=11663706

Family Applications (1)

Application Number Title Priority Date Filing Date
JP60007357A Expired - Lifetime JPH0638367B2 (en) 1985-01-21 1985-01-21 permanent magnet

Country Status (1)

Country Link
JP (1) JPH0638367B2 (en)

Also Published As

Publication number Publication date
JPS61168210A (en) 1986-07-29

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