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JPH0791564B2 - Rare earth containing alloy powder - Google Patents
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JPH0791564B2 - Rare earth containing alloy powder - Google Patents

Rare earth containing alloy powder

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Publication number
JPH0791564B2
JPH0791564B2 JP60275875A JP27587585A JPH0791564B2 JP H0791564 B2 JPH0791564 B2 JP H0791564B2 JP 60275875 A JP60275875 A JP 60275875A JP 27587585 A JP27587585 A JP 27587585A JP H0791564 B2 JPH0791564 B2 JP H0791564B2
Authority
JP
Japan
Prior art keywords
atomic
less
rare earth
powder
alloy
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
JP60275875A
Other languages
Japanese (ja)
Other versions
JPS61270304A (en
Inventor
尚幸 石垣
隆樹 浜田
節夫 藤村
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.)
Proterial Ltd
Original Assignee
Sumitomo Special Metals Co Ltd
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Filing date
Publication date
Application filed by Sumitomo Special Metals Co Ltd filed Critical Sumitomo Special Metals Co Ltd
Publication of JPS61270304A publication Critical patent/JPS61270304A/en
Publication of JPH0791564B2 publication Critical patent/JPH0791564B2/en
Anticipated expiration legal-status Critical
Expired - Lifetime legal-status Critical Current

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  • Manufacture Of Metal Powder And Suspensions Thereof (AREA)
  • Powder Metallurgy (AREA)
  • Hard Magnetic Materials (AREA)

Description

【発明の詳細な説明】 〔産業上の利用分野〕 本発明は希土類R−鉄Fe−コバルトCo−ホウ素B系の永
久磁石原料としてのR−Fe−Co−B系合金粉末に関す
る。工業的量産規模において安価にR1−R2−Fe−Co−B
系の合金粉末を提供しようとするものである。
DETAILED DESCRIPTION OF THE INVENTION [Field of Industrial Application] The present invention relates to an R-Fe-Co-B based alloy powder as a raw material for a rare earth R-iron Fe-cobalt Co-boron B-based permanent magnet. R 1 −R 2 −Fe−Co−B at low cost on an industrial mass production scale
It is intended to provide a system alloy powder.

〔従来の技術〕[Conventional technology]

最近サマリウム−コバルト系希土類磁石に代ってR−Fe
−B系希土類磁石が注目されている(特開昭59−46008
号等)。
Recently, samarium-cobalt rare earth magnets have replaced R-Fe
-B rare earth magnets have been attracting attention (Japanese Patent Laid-Open No. 59-46008).
Etc.).

しかし、このR−Fe−B合金磁石のキュリー温度は310
℃と比較的低く、常温以上の使用条件に対して安定性に
欠けるため、Feの一部をCoに置換し、キュリー温度を上
昇せしめて、温度に対する安定性の向上が計られてい
る。(特開昭59−64733号) 〔発明により解決すべき問題点〕 本出願人はさらにR−Fe−Co−B系磁石の改良としてNd
やPrなどの軽希土類成分をGd,Tb,Dy,Ho,Er,Tm,Ybの少な
くとも1種以上の重希土類元素で5原子%以下置換する
ことによって(BH)max=20MGOe以上の高エネルギー積
を有したまま、保磁力(iHc)を10kOe以上に飛躍的に向
上し、室温以上の100〜150℃の温度環境においても使用
可能なR1−R2−Fe−Co−−B系希土類磁石(ここでR1
Gd,Tb,Dy,Ho,Er,tm,Ybの重希土類元素のうち1種以上、
R2はNd及び/又はPrが80原子%以上で残りがR1以外のY
を含む希土類元素の少なくとも1種である)を開発して
いる。(特願昭58−141850号)。
However, the Curie temperature of this R-Fe-B alloy magnet is 310
Since it is relatively low at ℃, and lacks stability under operating conditions above room temperature, it has been attempted to improve the stability against temperature by substituting a part of Fe with Co and raising the Curie temperature. (Japanese Patent Laid-Open No. 59-64733) [Problems to be solved by the invention] The present applicant has further proposed Nd as an improvement of the R-Fe-Co-B magnet.
Energy content of (BH) max = 20MGOe or more by substituting 5 atomic% or less of at least one heavy rare earth element of Gd, Tb, Dy, Ho, Er, Tm, Yb for light rare earth elements such as Pr and Pr. while having the coercive force (iHc) drastically improved over 10 kOe, above room which can also be used in 100 to 150 ° C. in a temperature environment R 1 -R 2 -Fe-Co - B based rare earth magnet (Where R 1 is
One or more of the heavy rare earth elements of Gd, Tb, Dy, Ho, Er, tm, Yb,
R 2 is Nd and / or Pr of 80 atomic% or more and the rest is Y other than R 1.
Which is at least one of the rare earth elements including). (Japanese Patent Application No. 58-141850).

このR1−R2−Fe−Co−B系希土類磁石を製造する出発原
料は電解法あるいは熱還元法によって作られた純度99.5
%以上の希土類金属、純度99.9%以上の電解鉄、電解コ
バルト、ボロンなどの不純物の少ない高価な金属塊が使
用される。したがっていずれの原料もあらかじめ鉱石か
ら精製された不純物の少ない高品質のもので、これらの
原料を用いた製品磁石価格は非常に高価となる。とくに
希土類金属原料の生産には高度な分類精製技術を要し、
その生産効率も悪いのでその価格はきわめて高い。
The starting material for producing the R 1 -R 2 -Fe-Co-B rare earth magnet is a purity of 99.5 produced by an electrolytic method or a thermal reduction method.
% Or more rare earth metals, purity 99.9% or more of electrolytic iron, electrolytic cobalt, and expensive metal lumps with few impurities such as boron are used. Therefore, all of the raw materials are high-quality ones that have been purified from ore in advance and have few impurities, and the price of the product magnet using these raw materials becomes very expensive. In particular, the production of rare earth metal raw materials requires advanced classification and refining technology,
Its production efficiency is poor and its price is extremely high.

そこでR1−R2−Fe−Co−B系永久磁石はiHcが高く高性
能を有し、実用永久磁石材料として非常に有効ではある
が、その磁石価格は相当に高くなってしまう。
Therefore, the R 1 -R 2 -Fe-Co-B system permanent magnet has a high iHc and high performance and is very effective as a practical permanent magnet material, but the magnet price will be considerably high.

本発明は上述の諸問題点を解消し、希土類元素を含有し
て安価でしかも品質のすぐれた磁石材料用希土類含有R
(R1−R2)−Fe−Co−B系合金粉末を工業的量産規模で
安価に提供することを目的とする。
The present invention solves the above-mentioned problems and is a rare earth element-containing R for a magnet material which contains a rare earth element and is inexpensive and excellent in quality.
It is an object to provide (R 1 -R 2 ) -Fe-Co-B based alloy powder at a low cost on an industrial mass production scale.

〔発明による解決手段及び作用効果〕[Means for Solving the Invention and Effects]

すなわち本発明の第1の視点においては、希土類Rの化
合物を含む原料の還元剤として用いられるカルシウムを
微量含有して、希土類R、B、Fe、及びCoを主成分とす
る下記組成のカルシウム還元粉であって、R:12.5〜20原
子%(RのうちR1:0.05〜5原子%)、B:4〜20原子%、
Fe:45〜82原子%、及びCo:35原子%以下(但し0%を除
く)、(ここでR1は重希土類元素Gd、Tb、Dy、Ho、Er、
Tm、Ybの内の1種以上、R2はNd及び/又はPrが80原子%
以上で、残りがR1以外のYを含む希土類元素の少なくと
も1種とし、R=R1+R2(原子%)とする)、酸素含有
量10000ppm以下、炭素含有量1000ppm以下、及び、カル
シウム含有量2000ppm以下とし、かつ、主相(特定の相
が80vol%以上)が正方晶であることを特徴とする希土
類含有合金粉末である。
That is, in the first aspect of the present invention, a calcium reduction having the following composition containing rare earth R, B, Fe, and Co as the main components, contains a trace amount of calcium used as a reducing agent for a raw material containing a compound of rare earth R. Powder, R: 12.5 to 20 atomic% (R 1 : 0.05 to 5 atomic% of R), B: 4 to 20 atomic%,
Fe: 45 to 82 atomic% and Co: 35 atomic% or less (excluding 0%), (wherein R 1 is a heavy rare earth element Gd, Tb, Dy, Ho, Er,
One or more of Tm and Yb, R 2 has Nd and / or Pr of 80 atomic%
As described above, the rest is at least one kind of rare earth element containing Y other than R 1 and R = R 1 + R 2 (atomic%)), oxygen content is 10000 ppm or less, carbon content is 1000 ppm or less, and calcium content The rare earth-containing alloy powder is characterized in that the amount is 2000 ppm or less and the main phase (specific phase is 80 vol% or more) is tetragonal.

第2の視点においては、希土類Rの化合物を含む原料の
還元剤として用いられるカルシウムを微量含有して、希
土類R、B、Fe、及びCoを主成分とする下記組成のカル
シウム還元粉であって、R:12.5〜20原子%(Rのうち
R1:0.05〜5原子%)、B:4〜20原子%、Fe:45〜82原子
%、及びCo:35原子%以下(但し0%を除く)、(ここ
でR1は重希土類元素Gd、Tb、Dy、Ho、Er、Tm、Ybの内の
1種以上、R2はNd及び/又はPrが80原子%以上で、残り
がR1以外のYを含む希土類元素の少なくとも1種とし、
R=R1+R2(原子%)とする)、酸素含有量10000ppm以
下、炭素含有量1000ppm以下、及び、カルシウム含有量2
000ppm以下とし、かつ、主相(特定の相が80vol%以
上)が正方晶であり、前記Feに部分的に代わり、5.0原
子%以下のA1、3.0原子%以下のTi、5.5原子%以下の
V、6.0原子%以下のNi、4.5原子%以下のCr、5.0原子
%以下のMn、5.0原子%以下のBi、9.0原子%以下のNb、
7.0原子%以下のTa、5.2原子%以下のMo、5.0原子%以
下のW,1.0原子%以下のSb、3.5原子%以下のGe、1.5原
子%以下のSn、3.3原子%以下のZr、3.3原子%以下のH
f、及び5.0原子%以下のSiのうち少なくとも1種を添加
含有させることを特徴とする。
In a second aspect, there is provided a calcium-reduced powder having the following composition, which contains a small amount of calcium used as a reducing agent for a raw material containing a compound of rare earth R and has rare earths R, B, Fe, and Co as main components. , R: 12.5 to 20 atom% (of R
R 1 : 0.05 to 5 atomic%), B: 4 to 20 atomic%, Fe: 45 to 82 atomic%, and Co: 35 atomic% or less (excluding 0%) (where R 1 is a heavy rare earth element). At least one of Gd, Tb, Dy, Ho, Er, Tm, and Yb, R 2 is at least 80 atomic% of Nd and / or Pr, and the remaining is at least one rare earth element containing Y other than R 1. age,
R = R 1 + R 2 (atomic%)), oxygen content 10,000 ppm or less, carbon content 1000 ppm or less, and calcium content 2
000ppm or less, and the main phase (specific phase is 80vol% or more) is tetragonal, partially replacing Fe, 5.0 atomic% or less A1, 3.0 atomic% or less Ti, 5.5 atomic% or less V, 6.0 atomic% or less Ni, 4.5 atomic% or less Cr, 5.0 atomic% or less Mn, 5.0 atomic% or less Bi, 9.0 atomic% or less Nb,
7.0 at% or less Ta, 5.2 at% or less Mo, 5.0 at% or less W, 1.0 at% or less Sb, 3.5 at% or less Ge, 1.5 at% or less Sn, 3.3 at% or less Zr, 3.3 H less than atomic%
At least one of f and Si of 5.0 atomic% or less is added and contained.

なお両視点において、上記勝カルシウム還元粉とは、希
土類酸化物等の希土類化合物を含む原料にカルシウムを
添加して、このカルシウムを還元剤として還元された希
土類Rを、主成分のひとつとする希土類含有合金粉末で
ある。カルシウムは単体又は化合物の状態を含む。
Note that, from both viewpoints, the above-mentioned reduced calcium powder is a rare earth whose main component is a rare earth R reduced by using calcium as a reducing agent by adding calcium to a raw material containing a rare earth compound such as a rare earth oxide. Contains alloy powder. Calcium includes a simple substance or a compound.

本発明のR1−R2−Fe−Co−B合金粉末(本発明の第2の
視点に係る、Feに部分的に代わり所定元素を所定量含有
するものを含む)を用いることによって(BH)max20MGO
e以上、iHc10kOe以上の磁石特性を維持したままで磁石
のキュリー温度を上昇させて、残留磁束密度(Br)の温
度係数(α)を、従来のR−Fe−B又はR1−R2−Fe−B
磁石合金(α=約0.14%/度、但し室温〜150℃)より
も改良された永久磁石がえられる。Co5原子%以上でBr
の温度係数αは約0.1%/度以下となる。
By using the R 1 -R 2 -Fe-Co-B alloy powder of the present invention (including the one containing a predetermined amount of a predetermined element in place of Fe partially according to the second aspect of the present invention) (BH ) Max20MGO
The temperature coefficient (α) of the residual magnetic flux density (Br) is increased from the conventional R-Fe-B or R 1 -R 2 -by increasing the Curie temperature of the magnet while maintaining the magnet characteristics of e or more and iHc10kOe or more. Fe-B
An improved permanent magnet can be obtained over the magnet alloy (α = about 0.14% / degree, but at room temperature to 150 ° C). Br of 5 atomic% or more of Co
Has a temperature coefficient α of about 0.1% / degree or less.

また本発明によりR1−R2−Fe−Co−B系希土類磁石を安
価に提供できる。
Further, according to the present invention, the R 1 -R 2 -Fe-Co-B rare earth magnet can be provided at low cost.

この合金粉末は希土類金属を製造する前段階の中間原料
である価格の安いNd2O3やPr6Ol 1などの軽希土類酸化物
およびTb3O4やDy2O3などの重希土類酸化物とFe粉、Co
粉、および純ボロン粉、Fe−B粉またはB2O3粉末を出発
原料とし、還元剤として金属カルシウム及び/又は水素
化カルシウム、還元反応生成物の崩壊を容易にするため
の塩化カルシウム(CaCl2)を用いる工程によって製造
される。そのため、種々の金属塊原料を用いるよりも安
価に品質のすぐれた合金粉末が工業的量産規模において
容易にえられる。またこの合金粉末を用いることによっ
て磁石の製造工程の短縮も可能となり、価格の安いR1
R2−Fe−Co−B系希土類磁石を提供することが可能とな
ってその経済的効果が非常に大きい。
This alloy powder is an intermediate raw material before the production of rare earth metals.Light rare earth oxides such as inexpensive Nd 2 O 3 and Pr 6 O l 1 and heavy rare earth oxides such as Tb 3 O 4 and Dy 2 O 3 which are inexpensive. Thing and Fe powder, Co
Powder, pure boron powder, Fe-B powder or B 2 O 3 powder as a starting material, metal calcium and / or calcium hydride as a reducing agent, and calcium chloride (CaCl 3) for facilitating the decomposition of the reduction reaction product. It is manufactured by the process using 2 ). Therefore, alloy powders of excellent quality can be easily obtained on an industrial mass production scale at a lower cost than using various metal ingot raw materials. The shortening of the magnet manufacturing process by the use of this alloy powder also becomes possible, cheap price R 1 -
Since it is possible to provide an R 2 —Fe—Co—B rare earth magnet, its economic effect is very large.

ここで希土類酸化物とFe粉やFe−B粉などの金属粉末と
の混合粉末を出発原料にして金属Caによって還元・拡散
反応させると、反応温度において溶融状態のCaで還元さ
れた希土類金属がただちにFe粉、Co粉やFe−B粉ときわ
めて容易にしかも均質に合金化して希土類酸化物からR1
−R2−Fe−Co−B合金粉末が歩留りよく回収され、希土
類酸化物原料を有効に利用できる。還元剤としては金属
Caの代わりに水素化カルシウムを用いることもできる。
Here, when a mixed powder of rare earth oxide and metal powder such as Fe powder or Fe-B powder is used as a starting material and a reduction / diffusion reaction is performed with metallic Ca, the rare earth metal reduced by the molten Ca at the reaction temperature becomes Immediately and very easily and homogeneously alloy with Fe powder, Co powder, and Fe-B powder to form R 1 from rare earth oxides.
-R 2 -Fe-Co-B alloy powder is good yield recovered can be effectively used a rare earth oxide raw materials. Metal as a reducing agent
It is also possible to use calcium hydride instead of Ca.

また原料粉末中のB(ボロン)成分の含有はR1−R2−Fe
−Co−B合金粉末を生成する際の還元・拡散反応温度の
低下に有効で、本系合金粉末の還元・拡散反応を容易に
する。またCo成分の含有は、この永久磁石に不可欠な
(正方晶構造を有する)金属間化合物の一部となり、合
金粉末の耐酸化性を著しく向上させる効果がある。
The content of B (boron) component in the raw material powder is R 1 -R 2 -Fe.
-Effective for lowering the reduction / diffusion reaction temperature when producing a Co-B alloy powder, and facilitating the reduction / diffusion reaction of the present alloy powder. Further, the inclusion of the Co component becomes a part of the intermetallic compound (having a tetragonal structure) indispensable to this permanent magnet, and has the effect of significantly improving the oxidation resistance of the alloy powder.

したがって安価な希土類酸化物から工業的規模において
大量にR1−R2−Fe−Co−B磁石用の原料合金粉末をうる
ためには今日大量に生産され安価なFeとBとの合金粉末
を製造することが最も有効であるとして本発明の特定組
成範囲のR1−R2−Fe−Co−B合金粉末を発明するに至っ
たものである。
Therefore, in order to obtain a large amount of raw material alloy powder for R 1 -R 2 -Fe-Co-B magnets from an inexpensive rare earth oxide on an industrial scale, an inexpensive alloy powder of Fe and B, which is produced in large quantities today, is used. The present invention has led to the invention of the R 1 -R 2 -Fe-Co-B alloy powder in the specific composition range of the present invention, considering that production is most effective.

〔好適な実施の態様〕[Preferred Embodiment]

本発明による希土類含有合金粉末は以下の工程によって
製造される。
The rare earth-containing alloy powder according to the present invention is manufactured by the following steps.

Nd酸化物(Nd2O3)やPr酸化物(Pr6Ol 1)などの軽希土
類(R2)酸化物の少なくとも1種と、Tb酸化物(Tb
4O7)やDy酸化物(Dy2O3)などの重希土類(R1)酸化物
の少なくとも1種、鉄(Fe)粉、コバルト(Co)粉およ
び純ボロン粉,フェロボロン(Fe−B)粉,三酸化ボロ
ン(B2O3)粉のうち少なくとも1種の原料粉末を R :12.5〜20原子%(そのうち R1:0.05〜5原子%)、 B :4〜20原子%、 Fe:45〜82原子%、及び Co:35原子%以下(但し、0%を除く) (ここでR1は重希土類元素Gd,Tb,Dy,Ho,Er,Tm,Ybのうち
1種以上、R2はNd及び/又はPrが80原子%以上で、残り
がR1以外のYを含む希土類元素の少なくとも1種としR
=R1+R2(原子%)とする)の組成となるように配合
し、原料混合粉末とする。さらに希土類酸化物の還元剤
として金属Ca及び/又は水素化カルシウムを使用し、還
元後の反応生成物の崩壊を促進させるためにCaCl2粉末
を添加する。Caの必要量は原料混合粉末中に含まれる酸
素を還元するのに必要な化学量論理的必要量の1.2〜3.5
倍(重量比)、好ましくは1.5〜2.5倍、さらに好ましく
は1.6〜2.0倍とし、CaCl2の量は希土類酸化物原料の1
〜15%(重量比)(好ましくは2〜10%、さらに好まし
くは3〜6%)とする。
At least one light rare earth (R 2 ) oxide such as Nd oxide (Nd 2 O 3 ) or Pr oxide (Pr 6 O l 1 ) and Tb oxide (Tb
4 O 7 ) and at least one heavy rare earth (R 1 ) oxide such as Dy oxide (Dy 2 O 3 ), iron (Fe) powder, cobalt (Co) powder and pure boron powder, ferroboron (Fe-B) ) powder, the three least one raw material powder of the boron oxide (B 2 O 3) powder of R: 12.5 to 20 atomic% (of which R 1: 0.05 to 5 atomic%), B: 4 to 20 atomic%, Fe : 45 to 82 atom% and Co: 35 atom% or less (excluding 0%) (wherein R 1 is one or more of heavy rare earth elements Gd, Tb, Dy, Ho, Er, Tm, Yb, R 2 is 80 atomic% or more of Nd and / or Pr, and the remainder is at least one rare earth element containing Y other than R 1 and R
= R 1 + R 2 (atomic%)) to obtain a raw material mixed powder. Further, metallic Ca and / or calcium hydride is used as a reducing agent for the rare earth oxide, and CaCl 2 powder is added to accelerate the decomposition of the reaction product after reduction. The required amount of Ca is 1.2 to 3.5 of the stoichiometrically required amount required to reduce the oxygen contained in the raw material mixed powder.
Double (weight ratio), preferably 1.5 to 2.5 times, more preferably 1.6 to 2.0 times, and the amount of CaCl 2 is less than that of the rare earth oxide raw material.
-15% (weight ratio) (preferably 2-10%, more preferably 3-6%).

以上の希土類酸化物粉末,Fe粉,Co粉,フェロボロン粉な
どの各原料粉末およびCa還元剤などからなる混合粉末を
アルゴン不活性ガス雰囲気中において950〜1200℃(好
ましくは950〜1100℃)の温度範囲で所定時間(好まし
くは1〜5時間)の還元・拡散処理を行い、室温まで冷
却して還元反応生成物をえる。これを適当な粒度、好ま
しくは8mesh(2.4mm)以下に粉砕して水に接触させる
(投入する)と反応生成物中の酸化カルシウム(CaO),
CaO・2CaCl2および過剰なカルシウムは水酸化カルシウ
ム(Ca(OH))などとなり、反応生成物は崩壊して水
との混合スラリーとなる。このスラリーを水を用いてCa
分を十分に除去して粉末粒径凡そ10〜500μmの本発明
の希土類含有合金粉末がえられる。10μm以下では合金
中に酸素量が多くなり優れた磁石特性が得られない。ま
た、500μm以上では還元時の拡散反応が十分でないこ
とが多く、α−Fe相などが磁石中に出現するためiHcが
低下し減磁曲線の角形性を低下させる。本発明の好まし
い粒径は後続の磁石化工程における作業性および磁石特
性の点で20〜300μmが好ましい。えられた合金粉末は R :12.5〜20原子%(Rのうち R1:0.05〜5原子%)、 B :4〜20原子%、 Fe:45〜82原子%、及び Co:35原子%以下(但し、0%は除く) (ここでR1は重希土類元素Gd,Tb,Dy,Ho,Er,Tm,Ybのうち
の1種以上、R2はNd及び/又はPrが80原子%以上(〜10
0%)で、残り(20〜0%)がR1以外のYを含む希土類
元素の少なくとも1種としR=R1+R2(原子%)とす
る)からなり、主相(合金の80vol%以上)が正方晶
で、酸素含有量10000ppm以下、炭素含有量1000ppm以
下、カルシウム含有量2000ppm以下となる。
The mixed powder consisting of the above raw material powders such as rare earth oxide powder, Fe powder, Co powder, ferroboron powder, and Ca reducing agent was heated to 950 to 1200 ℃ (preferably 950 to 1100 ℃) in an argon inert gas atmosphere. The reduction / diffusion treatment is performed within a temperature range for a predetermined time (preferably 1 to 5 hours), and then cooled to room temperature to obtain a reduction reaction product. When this is crushed to an appropriate particle size, preferably 8 mesh (2.4 mm) or less and brought into contact with water (input), calcium oxide (CaO) in the reaction product,
CaO · 2CaCl 2 and excess calcium become calcium hydroxide (Ca (OH) 2 ), etc., and the reaction product disintegrates and becomes a mixed slurry with water. This slurry is mixed with water using Ca
By sufficiently removing the content, the rare earth-containing alloy powder of the present invention having a powder particle size of about 10 to 500 μm can be obtained. If it is less than 10 μm, the amount of oxygen in the alloy is large, and excellent magnet characteristics cannot be obtained. Further, if the thickness is 500 μm or more, the diffusion reaction at the time of reduction is often insufficient, and α-Fe phase and the like appear in the magnet, so that iHc decreases and the squareness of the demagnetization curve decreases. The preferable particle size of the present invention is 20 to 300 μm in view of workability and magnet characteristics in the subsequent magnetizing step. The obtained alloy powder R: 12.5 to 20 atomic% (of R R 1: 0.05 to 5 atomic%), B: 4 to 20 atomic%, Fe: forty-five to eighty-two atomic%, and Co: 35 atomic% or less (However, 0% is excluded) (Here, R 1 is one or more of the heavy rare earth elements Gd, Tb, Dy, Ho, Er, Tm, Yb, and R 2 is 80 atomic% or more of Nd and / or Pr. (~Ten
0%), the rest (20 to 0%) consists of at least one rare earth element containing Y other than R 1 and R = R 1 + R 2 (atomic%), and the main phase (80 vol% of the alloy) The above) is a tetragonal crystal with an oxygen content of 10,000 ppm or less, a carbon content of 1000 ppm or less, and a calcium content of 2000 ppm or less.

本発明における希土類合金粉末はR1−R2−Fe−Co−B磁
石合金を製造する際にそのまま微粉砕して、ひき続きプ
レス成形→焼結→時効処理という粉末治金的方法によっ
て永久磁石にすることができる。この微粉砕はアトライ
タ、ボールミル、ジェットミル等を用いて好ましくは1
〜20μm、より好ましくは2〜10μmにする。なお、異
方性磁石を製造するためには磁界中にて粒子を配向、成
形できる。本発明の希土類合金粉末を用いれば、希土類
金属塊、鉄およびボロンなどの原料塊を原料にして永久
磁石を製造する場合よりも合金溶解→鋳造→粗粉砕など
の磁石の製造工程の省略が可能となり、かつ安い出発原
料を用いるために製品磁石の価格が安価となるという利
点を有し、実用永久磁石材料を量産規模において容易に
作りうる点から経済的効果も大きい。
The rare earth alloy powder in the present invention is finely pulverized as it is during the production of the R 1 -R 2 -Fe-Co-B magnet alloy, and is subsequently subjected to press molding → sintering → aging treatment by a powder metallurgical method. Can be This fine pulverization is preferably carried out using an attritor, ball mill, jet mill, etc.
-20 μm, more preferably 2-10 μm. In order to manufacture an anisotropic magnet, particles can be oriented and shaped in a magnetic field. By using the rare earth alloy powder of the present invention, it is possible to omit the manufacturing process of the magnet such as alloy melting → casting → coarse crushing as compared with the case of manufacturing a permanent magnet from a raw material mass such as a rare earth metal mass, iron and boron. In addition, since the price of the product magnet is low because a cheap starting material is used, the practical permanent magnet material can be easily manufactured on a mass production scale, and thus the economical effect is large.

本発明の合金粉末に含まれる酸素は最も酸化しやすい希
土類元素と結合して希土類酸化物を形成し、酸素含有量
が10000ppmを越えると永久磁石中に酸化物(R2O3)とし
て4%以上残留することになり、磁石特性とくに保磁力
が10kOe以下になるので好ましくない。
Oxygen contained in the alloy powder of the present invention forms a rare earth oxide by combining with the rare earth element that is most easily oxidized, and when the oxygen content exceeds 10,000 ppm, 4% as an oxide (R 2 O 3 ) in the permanent magnet. This is not preferable, because the magnetic properties, especially the coercive force, are 10 kOe or less.

含有炭素量が1000ppmを越えると酸素の場合と同様炭化
物(RC2等)として永久磁石中に残留し減磁曲線の角形
性を低下させ保磁力が10kOe以下となる。含有炭素量は
好ましくは600ppm以下、さらに好ましくは400ppm以下と
する。
If the carbon content exceeds 1000 ppm, it will remain in the permanent magnet as carbides (RC 2 etc.) as in the case of oxygen, and the squareness of the demagnetization curve will be reduced, and the coercive force will be 10 kOe or less. The carbon content is preferably 600 ppm or less, more preferably 400 ppm or less.

またカルシウム含有量が2000ppmを越えると後続のこの
合金粉末を用いて磁石化する途中の焼結工程において還
元性の極めて高いCa蒸気を多量に発生し、熱処理炉をい
ちじるしく汚染することになって、場合によっては熱処
理炉の炉壁を損耗して工業的に安定な生産が不可能とな
る。また、でき上った永久磁石中に含まれるCa量も多く
なって磁石特性の劣化を生ずる。生成合金中のCa量は好
ましくは1000ppm以下とする。
Further, if the calcium content exceeds 2000 ppm, a large amount of extremely reducing Ca vapor is generated in the sintering process during the subsequent magnetization using this alloy powder, which will contaminate the heat treatment furnace. In some cases, the furnace wall of the heat treatment furnace is worn away, making industrially stable production impossible. In addition, the amount of Ca contained in the completed permanent magnet also increases, resulting in deterioration of magnet characteristics. The amount of Ca in the produced alloy is preferably 1000 ppm or less.

本願発明の希土類合金粉末の成分範囲の限定理由は以下
による。
The reason for limiting the component range of the rare earth alloy powder of the present invention is as follows.

R(Yを含む希土類元素のうち少なくとも1種)は、新
規なR1−R2−Fe−Co−B系永久磁石を製造する合金粉末
として必須元素であって、12.5原子%よりも少なくなる
と本系合金化合物中にα−Feが析出して保磁力が急激に
低下し、Rが20原子%を越えると保磁力は10kOe以上の
大きい値を示すが残留磁束密度Brが低下して(BH)max2
0MGOe以上に必要なBrが得られなくなる。したがって希
土類元素Rの量は、12.5原子%〜20原子%の範囲とす
る。R1の量は上述Rの一部を構成する。R1量は僅か0.05
原子%の存在でもHcが増加しており、さらに減磁曲線の
角形性も改善され(BH)maxが増加する。そこでR1量の
下限値はiHc増加の効果と(BH)max増大の効果を考慮し
て0.05原子%以上とする。R1量が増加するにつれてiHc
は上昇していき、(BH)maxは0.4原子%をピークとして
わずかずつ減少するが、例えば3原子%の含有でも(B
H)maxは30MGOe以上を示す。
R (at least one of rare earth elements including Y) is an essential element as an alloy powder for producing a new R 1 -R 2 -Fe-Co-B based permanent magnet, and if it is less than 12.5 atomic%. Α-Fe is precipitated in this alloy compound and the coercive force sharply decreases. When R exceeds 20 atomic%, the coercive force shows a large value of 10 kOe or more, but the residual magnetic flux density Br decreases (BH ) Max2
You will not be able to obtain the required Br above 0 MGOe. Therefore, the amount of the rare earth element R is set in the range of 12.5 atomic% to 20 atomic%. The amount of R 1 forms part of R above. R 1 amount is only 0.05
Even in the presence of atomic%, Hc increases, and the squareness of the demagnetization curve is also improved, and (BH) max increases. Therefore, the lower limit of the R 1 amount is set to 0.05 atom% or more in consideration of the effect of increasing iHc and the effect of increasing (BH) max. IHc as R 1 content increases
Increases, and (BH) max decreases gradually with a peak at 0.4 at%, but even if the content of (BH) max is 3 at%,
H) max indicates 30 MGOe or more.

安定性が特に要求される用途にはiHcが高いほど、すな
わちR1を多く含有する方が有利である。しかしR1を構成
する元素は希土類鉱石中にもわずかしか含まれておら
ず、その酸化物も大変高価である。従ってその上限は5
原子%とする。また、R1としてはDy,Tbが望ましい。R2
はNdとPrの合計がR2の80%以上で、残りがR1以外のYを
含む希土類元素の1種以上とする。但し、Sm,Laはでき
るだけ少ない方がよい。
For applications in which stability is particularly required, it is advantageous that the iHc is higher, that is, the content of R 1 is larger. However, the elements composing R 1 are contained only in rare earth ores, and their oxides are also very expensive. Therefore, the upper limit is 5
Atomic% Further, as R 1 is Dy, Tb is preferable. R 2
The total of Nd and Pr is 80% or more of R 2 , and the rest is one or more rare earth elements containing Y other than R 1 . However, Sm and La should be as small as possible.

B量は、4原子%以下になるとiHcが10kOe以下になる。
またB量の増加もR量の増加と同じくiHcを増加させる
が、Brが低下していく。(BH)max20MGOe以上であるた
めにはB20原子%以下が必要である。よって、B量は、
4原子%〜20原子%の範囲とする。
When the B content is 4 atomic% or less, iHc becomes 10 kOe or less.
In addition, increasing B content also increases iHc as does increasing R content, but Br decreases. To be (BH) max20MGOe or more, B20 atomic% or less is required. Therefore, the amount of B is
The range is from 4 atom% to 20 atom%.

Coの添加はこのR1−R2−Fe−Co−B系永久磁石のキュリ
ー温度(Tc)を増加させる効果がある(第1図)。キュ
リー温度はCoの添加量の増加に伴なって連続的に上昇し
ていく。従ってCoはわずかでも有効であり下限は特に限
定されないが好ましくは0.1原子%以上とする。また、C
o量が35原子%を越えると、永久磁石の飽和磁化及び保
磁力が低下して20MGOeより低くなる。FeBR系ではBrの温
度係数は約0.13%/℃(室温〜150℃)であるがCo5原子
%以上の含有により約0.1%/℃となる。なお、Co25原
子%以下で他の特性を実質上劣化させることなくキュリ
ー温度増大に寄与し、約20原子%(17〜23原子%)では
iHcも増大させる。Co量は5〜6原子%とするのが最も
好ましい。
The addition of Co has the effect of increasing the Curie temperature (Tc) of the R 1 -R 2 -Fe-Co-B system permanent magnet (Fig. 1). The Curie temperature continuously rises as the amount of Co added increases. Therefore, Co is effective even in a small amount, and the lower limit is not particularly limited, but is preferably 0.1 atom% or more. Also, C
When the amount exceeds 35 atom%, the saturation magnetization and coercive force of the permanent magnet decrease, and the value becomes lower than 20MGOe. In the FeBR system, the temperature coefficient of Br is about 0.13% / ° C (room temperature to 150 ° C), but it becomes about 0.1% / ° C when the content of Co is 5 atomic% or more. It should be noted that when Co is 25 at% or less, it contributes to the Curie temperature increase without substantially deteriorating other properties, and at about 20 at% (17 to 23 at%)
It also increases iHc. Most preferably, the amount of Co is 5 to 6 atomic%.

Fe量は、新規なR1−R2−Fe−Co−B系永久磁石を製造す
る合金粉末として、必須元素であるが、45原子%未満で
は残留磁束密度Brが低下し、82原子%を越えると、高い
保磁力が得られないので、Fe量は60原子%〜82原子%に
限定する。Fe量はさらに好ましくは45〜80原子%とす
る。さらに、FeとCoの合計量は60原子%以上とするのが
好ましく、最も好ましくはFe量は60原子%以上とする。
Fe content is an essential element as an alloy powder for producing a new R 1 -R 2 -Fe-Co-B system permanent magnet, but if it is less than 45 atomic%, the residual magnetic flux density Br decreases, and 82 atomic% If it exceeds, a high coercive force cannot be obtained, so the Fe content is limited to 60 atom% to 82 atom%. The Fe content is more preferably 45 to 80 atomic%. Further, the total amount of Fe and Co is preferably 60 atom% or more, and most preferably the Fe amount is 60 atom% or more.

また、この発明による合金粉末は、R,B,Fe,Coの他、工
業的生産上不可避的不純物の存在を許容できる。例え
ば、2原子%以下のP、2原子%のS、2原子%以下の
Cu、合計量で2原子%以下を含有してもなお実用的な磁
気特性を示し、磁石合金の製造性改善、低価格化が可能
である。但しこれらの元素は一般にBrを低下させるので
少ない方がよく(例えば0.5原子%以下、より好ましく
は0.1原子%未満)、Br9kG以上の範囲とする。さらに、
前記R・Fe・Co・B合金中のFeに部分的に代わり、 5.0原子%以下のAl, 3.0原子%以下のTi, 6.0原子%以下のNi, 5.5原子%以下のV, 4.5原子%以下のCr, 5.0原子%以下のMn, 5.0原子%以下のBi, 9.0原子%以下のNb, 7.0原子%以下のTa, 5.2原子%以下のMo, 5.0原子%以下のW, 1.0原子%以下のSb, 3.5原子%以下のGe, 1.5原子%以下のSn, 3.3原子%以下のZr, 3.3原子%以下のHf,及び 5.0原子%以下のSi のうち少なくとも1種を添加含有させることにより、永
久磁石合金の高保磁力化が可能になる。
Further, the alloy powder according to the present invention can tolerate the presence of impurities that are unavoidable in industrial production in addition to R, B, Fe and Co. For example, P of 2 atomic% or less, S of 2 atomic%, S of 2 atomic% or less
Even if the total amount of Cu is 2 atomic% or less, the magnetic properties are still practical, and it is possible to improve the manufacturability of magnet alloys and reduce the cost. However, since these elements generally lower Br, it is preferable that the amount thereof be small (for example, 0.5 atomic% or less, more preferably less than 0.1 atomic%), and Br 9 kG or more. further,
Partial substitution for Fe in the R, Fe, Co and B alloys, 5.0 atomic% or less Al, 3.0 atomic% or less Ti, 6.0 atomic% or less Ni, 5.5 atomic% or less V, 4.5 atomic% or less Cr, 5.0 atomic% or less Mn, 5.0 atomic% or less Bi, 9.0 atomic% or less Nb, 7.0 atomic% or less Ta, 5.2 atomic% or less Mo, 5.0 atomic% or less W, 1.0 atomic% or less Permanent addition of at least one of Sb, 3.5 atomic% or less Ge, 1.5 atomic% or less Sn, 3.3 atomic% or less Zr, 3.3 atomic% or less Hf, and 5.0 atomic% or less Si It is possible to increase the coercive force of the magnet alloy.

上述の添加元素は一般にiHcを増し、減磁曲線の角形性
を増す効果があるが、一方その添加量が増すに従い、Br
が低下していく。(BH)max20MGOe以上を有するにはBr9
kG以上が必要であり、そのためBi、Ni、Mnの場合を除き
添加量の各々(及び混合添加の場合)の上限は先述の値
以下と定められる。Biについてはその高い蒸気圧、Ni、
MnについてはiHcの観点からその上限を定める。また、S
iはキュリー温度を高める効果がある。2種以上の元素
を添加する場合には添加量の合計の上限は、実際に添加
された当該元素の各上限値のうち最大値を有するものの
値以下となる。例えばTi,Ni,Nbを添加した場合には、Nb
の9%以下となる。とくに添加元素のうち、V,Nb,Ta,M
o,W,Cr,Alが好ましい。添加元素の含有量は少量が好ま
しく、一般に3原子%以下が有効である(Alの場合0.1
〜3原子%特に0.2〜2原子%)。なおこれらの添加元
素は金属粉として、または、酸化物、或いは他の構成元
素との合金ないし混合酸化物として出発原料中に配合し
ておくこともできる。
The above-mentioned additional elements generally have the effect of increasing iHc and increasing the squareness of the demagnetization curve, but as the amount of addition increases, Br
Is decreasing. Br9 to have more than (BH) max20MGOe
Since kG or more is required, the upper limit of each addition amount (and in the case of mixed addition) is specified to be equal to or less than the above value, except for Bi, Ni, and Mn. For Bi, its high vapor pressure, Ni,
An upper limit is set for Mn from the viewpoint of iHc. Also, S
i has the effect of increasing the Curie temperature. In the case of adding two or more elements, the upper limit of the total addition amount is less than or equal to the maximum value among the upper limits of the elements actually added. For example, when Ti, Ni, Nb is added, Nb
Of 9% or less. Especially, among the additive elements, V, Nb, Ta, M
O, W, Cr and Al are preferred. The content of the additional element is preferably small, and generally 3 atom% or less is effective (0.1% for Al).
.About.3 atom%, especially 0.2 to 2 atom%). It should be noted that these additive elements may be mixed in the starting material as metal powder, or as an oxide, or an alloy or mixed oxide with other constituent elements.

結晶相は主相(合金の80容量%以上、好ましくは90容量
%以上、さらに好ましくは95容量%以上)は正方晶であ
ることが磁石として高い磁気特性を発現するのに不可欠
である。
It is indispensable that the main phase (80% by volume or more of the alloy, preferably 90% by volume or more, more preferably 95% by volume or more) of the crystal phase is a tetragonal crystal in order to exhibit high magnetic properties as a magnet.

この磁性相はFeCoBR正方晶化合物結晶で構成され、非磁
性相により粒界を囲まれている。非磁性相は主としてR
リッチ相(R金属)から成る。Bの多い場合Bリッチな
相も部分的に存在しうる。非磁性相粒界域の存在は高特
性に寄与するものと考えられ、本発明合金の重要な組織
上の特徴を成す。非磁性相はほんのわずかでも有効であ
り、例えば1vol%以上は十分な量である。正方晶結晶の
格子パラメータはa約8.8Å、c約12.2Åであり、その
中心組成はR2(Fe,Co)l4Bであると考えられる。この合
金粉末は一般に結晶性であり、典型的には粉末粒子を構
成する結晶の粒径が、約1μm以上である(但し、粉末
粒子径がこれ以上の場合に限る)。正方晶相の量は、X
線回折の強度やX線マイクロアナライザ等を用いて測定
できる。さらに、この合金粉末を用いた焼結永久磁石は
結晶質であり、R(Fe,Co)B正方晶相の平均結晶粒径
は、1〜40μm(さらに好ましくは3〜20μm)である
ことが優れた永久磁石特性のために望ましい。
This magnetic phase is composed of FeCoBR tetragonal compound crystals, and the grain boundaries are surrounded by the nonmagnetic phase. Non-magnetic phase is mainly R
It consists of a rich phase (R metal). When the amount of B is large, a B-rich phase may be partially present. The existence of the non-magnetic phase grain boundary region is considered to contribute to high properties, and constitutes an important structural feature of the alloy of the present invention. Even a small amount of the non-magnetic phase is effective, for example, 1 vol% or more is a sufficient amount. It is considered that the lattice parameters of the tetragonal crystal are a about 8.8Å and c about 12.2Å, and the central composition thereof is R 2 (Fe, Co) l 4 B. This alloy powder is generally crystalline, and the grain size of the crystal that constitutes the powder grain is typically about 1 μm or more (provided that the powder grain size is not less than this). The amount of tetragonal phase is X
It can be measured using the intensity of line diffraction or an X-ray microanalyzer. Further, the sintered permanent magnet using this alloy powder is crystalline, and the average crystal grain size of the R (Fe, Co) B tetragonal phase is 1 to 40 μm (more preferably 3 to 20 μm). Desirable for excellent permanent magnet properties.

以下本発明の態様及び効果について実施例に従って説明
する。但し本発明は実施例の記載に必ずしも制限されな
い。
Hereinafter, aspects and effects of the present invention will be described according to examples. However, the present invention is not necessarily limited to the description of the examples.

〔実施例〕〔Example〕

実施例1 Nd2O3粉末:54.8gr Dy2O3粉末: 5.6gr フェロボロン粉末(19.5wt%B−Fe合金粉末) : 6.5gr Fe粉 :42.6gr Co粉 :18.6gr 金属Ca :53.5gr (化学量論比の2.5倍) CaCl2 : 2.6gr (希土類酸化物原料の4.3wt%) の原料粉末合計184.2grを用い、30.0%Nd−3.6%Dy−4
7.7%Fe−17.5%Co−1.12%B(重量%) [14.0%Nd−1.5%Dy−57.5%Fe−20%Co−7.0%B(原
子%)]の組成合金を狙いにして、V型混合機を用いて
混合した。ついでこの混合原料の圧縮体をステンレス製
容器に充填し、マッフル炉中に装入後容器内をアルゴン
ガス気流中において昇温した。1150℃×3hrの恒温保持
後室温まで炉冷した。えられた還元反応生成物を8mesh
スルーに粗粉砕後10のイオン交換水中に投入し、反応
生成物中の酸化カルシウム(CaO),CaO・2CaCl2、未反
応の残留カルシウムを水酸化カルシウム(Ca(OH)
にして反応生成物を崩壊させスラリー状にした。1時間
攪拌した後、30分間静置して水酸化カルシウム懸濁液を
すて、再び注水し、攪拌・静置・懸濁液除去の工程を複
数回くり返した。このようにして分離・採取されたNd−
Dy−Fe−Co−B系合金粉末を真空中で乾燥し、20〜300
μmの本発明の磁石材料用希土類合金粉末84grをえた。
Example 1 Nd 2 O 3 powder: 54.8gr Dy 2 O 3 powder: 5.6gr Ferroboron powder (19.5wt% B-Fe alloy powder): 6.5gr Fe powder: 42.6gr Co powder: 18.6gr Metal Ca: 53.5gr ( 2.5 times the stoichiometric ratio) CaCl 2 : 2.6gr (4.3wt% of rare earth oxide raw material) 184.2gr in total, 30.0% Nd-3.6% Dy-4
Aiming at a composition alloy of 7.7% Fe-17.5% Co-1.12% B (weight%) [14.0% Nd-1.5% Dy-57.5% Fe-20% Co-7.0% B (atomic%)], V type Mix using a mixer. Then, the compressed body of the mixed raw material was filled in a stainless steel container, charged into a muffle furnace, and then heated in an argon gas stream in the container. After maintaining a constant temperature of 1150 ° C for 3 hours, the furnace was cooled to room temperature. 8mesh of the obtained reduction reaction product
After roughly crushing into a through, put into 10 ion-exchanged water to remove calcium oxide (CaO), CaO · 2CaCl 2 , and unreacted residual calcium in the reaction product calcium hydroxide (Ca (OH) 2 ).
The reaction product was disintegrated into a slurry. After stirring for 1 hour, the mixture was left standing for 30 minutes to drain the calcium hydroxide suspension, water was poured again, and the steps of stirring, standing, and suspension removal were repeated several times. Nd- separated and collected in this way
Dy-Fe-Co-B type alloy powder is dried in vacuum to 20 ~ 300
84 μm of the rare earth alloy powder for magnet materials of the present invention having a size of 84 μm was obtained.

成分分析の結果、下記の通り Nd:30.2wt% Dy: 3.3wt% Fe:48.2wt% Co:15.8wt% B : 1.1wt% Ca: 800ppm O2:4100ppm C : 670ppm の所望の合金粉末がえられた。X線回折の図形の測定に
より、a=8.76Å,c=12.15Åを有する正方晶系の金属
間化合物を95%以上の主相とする合金粉末であった。
As a result of the component analysis, as shown below, Nd: 30.2 wt% Dy: 3.3 wt% Fe: 48.2 wt% Co: 15.8 wt% B: 1.1 wt% Ca: 800 ppm O 2 : 4100 ppm C: 670 ppm of the desired alloy powder. Was given. According to the X-ray diffraction pattern measurement, the alloy powder was a tetragonal intermetallic compound having a = 8.76Å, c = 12.15Å as a main phase of 95% or more.

この粉末を微粉砕し、平均粒径2.50μmの粉末にして1.
5t/dcm2の圧力で10kOeに磁界中において圧縮成型体にし
た。その後1120℃−2時間のAr気流中焼結と600℃−1
時間の時効処理を行い、永久磁石試料を作製した。
This powder is pulverized to a powder with an average particle size of 2.50 μm. 1.
A compact was formed in a magnetic field of 10 kOe at a pressure of 5 t / dcm 2 . After that, sintering at 1120 ℃ -2 hours in Ar gas flow and 600 ℃ -1
Aging treatment for time was performed to prepare a permanent magnet sample.

Br=11.5kG iHc=16.3kOe (BH)max=31.7MGOe のすぐれた磁石特性がえられた。また、この合金磁石の
Brの温度係数α=0.075%/℃(室温−150℃)であっ
た。
Excellent magnet characteristics of Br = 11.5kG iHc = 16.3kOe (BH) max = 31.7MGOe were obtained. Also, of this alloy magnet
The Br temperature coefficient α was 0.075% / ° C. (room temperature −150 ° C.).

実施例2 Nd2O3粉末:47.0gr Dy2O3粉末: 1.6gr フェロボロン粉末(19.0wt%B−Fe合金粉末) : 6.4gr Fe粉 :61.2gr Co粉 : 4.4gr 金属Ca :43.3gr (化学量論比の2.5倍) CaCl2 : 2.5gr (希土類酸化物原料の5.0wt%) の原料粉末合計166.4grを用い、30.4%Nd−1.2%Dy−6
2.7%Fe−4.5%Co−1.2%B(重量%) [13.8Nd−0.5%Dy−73.5%Fe−5%Co−7.2%B(原子
%)] 組成合金を狙いにして、実施例1と同様にして1070℃−
3時間の還元処理をし、20〜500μmの本発明の磁石材
料用希土類合金粉末を79grをえた。
Example 2 Nd 2 O 3 powder: 47.0gr Dy 2 O 3 powder: 1.6gr Ferroboron powder (19.0wt% B-Fe alloy powder): 6.4gr Fe powder: 61.2gr Co powder: 4.4gr Metal Ca: 43.3gr ( 2.5 times the stoichiometric ratio) CaCl 2 : 2.5gr (5.0wt% of rare earth oxide material) 166.4gr in total, 30.4% Nd-1.2% Dy-6
2.7% Fe-4.5% Co-1.2% B (wt%) [13.8Nd-0.5% Dy-73.5% Fe-5% Co-7.2% B (atomic%)] Aiming at a composition alloy, as in Example 1 Similarly, at 1070 ℃-
After reduction treatment for 3 hours, 79 gr of the rare earth alloy powder for a magnet material of the present invention having a particle size of 20 to 500 μm was obtained.

成分分析の結果、下記の通り Nd:29.5wt% Dy: 1.1wt% Fe:61.3wt% Co: 4.1wt% B : 1.0wt% Ca: 490ppm O2:3300ppm C : 480ppm の所望の合金粉末がえられた。X線回折図形の測定によ
りa=8.79Å,c=12.18Åを有する正方晶系の金属間化
合物を93%以上の主相とする合金粉末であった。
Results of component analysis, as follows Nd: 29.5wt% Dy: 1.1wt% Fe: 61.3wt% Co: 4.1wt% B: 1.0wt% Ca: 490ppm O 2: 3300ppm C: desired alloy powder 480ppm replacement Was given. According to the X-ray diffraction pattern measurement, the alloy powder was a tetragonal intermetallic compound having a = 8.79Å, c = 12.18Å as a main phase of 93% or more.

実施例1と同様にして永久磁石材料を作成して Br=12.5kG iHc=12.1kOe (BH)max=37.4MGOe のすぐれた磁石特性がえられた。この磁石合金の温度特
性はα=0.09%℃であった。
A permanent magnet material was prepared in the same manner as in Example 1, and excellent magnet characteristics of Br = 12.5 kG iHc = 12.1 kOe (BH) max = 37.4 MGOe were obtained. The temperature characteristic of this magnet alloy was α = 0.09% ° C.

実施例3 Nd2O3粉末:36.3gr CeO2粉末 : 9.2gr Dy2O3粉末: 3.1gr Gd2O3粉末: 3.0gr Fe粉 :49.9gr Co粉 : 8.0gr フェロボロン粉(19.0wt%B−Fe合金粉) : 9.0gr 金属Ca :68.5gr (化学量論比の3.2倍) CaCl2 : 5.2gr (希土類酸化物原料の10wt%) の原料粉末合計192.2grを用い、24.4%Nd−4.3%Ce−2.
5%Dy−2.4%Gd−55.7%Fe−9.0%Co−1.7%B(重量
%) [11%Nd−2%Ce−1%Dy−1%Gd−65%Fe−10%Co−
10%B(原子%)]組成合金を狙いにして実施例1と同
様にして30〜500μmの粉末87grをえた。
Example 3 Nd 2 O 3 powder: 36.3gr CeO 2 powder: 9.2gr Dy 2 O 3 powder: 3.1gr Gd 2 O 3 powder: 3.0gr Fe powder: 49.9gr Co powder: 8.0gr Ferroboron powder (19.0wt% B -Fe alloy powder): 9.0gr Metal Ca: 68.5gr (3.2 times the stoichiometric ratio) CaCl 2 : 5.2gr (10wt% of rare earth oxide raw material) 192.2gr in total, 24.4% Nd-4.3 % Ce-2.
5% Dy-2.4% Gd-55.7% Fe-9.0% Co-1.7% B (wt%) [11% Nd-2% Ce-1% Dy-1% Gd-65% Fe-10% Co-
10% B (atomic%)] Aiming at a composition alloy, powder 87gr having a particle size of 30 to 500 μm was obtained in the same manner as in Example 1.

成分分析の結果、下記の通り Nd:24.1wt% Ce: 4.0wt% Dy: 2.3wt% Gd: 2.2wt% Fe:55.9wt% Co: 8.8wt% B : 1.6wt% Ca:1100ppm O2:5500ppm C : 600ppm の所望の合金粉末がえられた。X線回折図形の測定によ
りa=8.80Å,c=12.24Åを有する正方晶系の金属間化
合物を87%以上の主相とする合金粉末であった。
As a result of component analysis, as shown below, Nd: 24.1wt% Ce: 4.0wt% Dy: 2.3wt% Gd: 2.2wt% Fe: 55.9wt% Co: 8.8wt% B: 1.6wt% Ca: 1100ppm O 2 : 5500ppm C: 600 ppm of the desired alloy powder was obtained. According to the X-ray diffraction pattern measurement, it was an alloy powder having a tetragonal intermetallic compound having a = 8.80Å, c = 12.24Å as a main phase of 87% or more.

えられた粉末を微粉砕し、平均粒度3.5μmの粉末にし
て1.5t/cm2の圧力で10kOeの磁界中において圧縮成型体
にした。その後1100℃−2時間の焼結と600℃−1時間
の時効処理を行い永久磁石試料を作製した。
The obtained powder was finely pulverized to obtain a powder having an average particle size of 3.5 μm, and a compression molding was performed in a magnetic field of 10 kOe at a pressure of 1.5 t / cm 2 . After that, sintering was performed at 1100 ° C. for 2 hours and aging treatment was performed at 600 ° C. for 1 hour to prepare a permanent magnet sample.

Br =10.7kG iHc=10.4kOe (BH)max=25.2MGOe のすぐれた磁石特性がえられた。Excellent magnet characteristics of Br = 10.7kG iHc = 10.4kOe (BH) max = 25.2MGOe were obtained.

〔効果〕〔effect〕

詳述の通り、本発明によれば、R1−R2−Fe−Co−B系の
磁石を製造するための同様な組成の合金粉末が希土類酸
化物及び酸化ホウ素原料を出発原料として用いて安価に
得られ、その使用により、優れた特性のR1−R2−Fe−Co
−B系永久磁石が得られると共に磁石製造工程から希土
類金属の単離精製−合金の溶製−冷却(通例鋳造)−粉
砕という所定合金粉末の製造工程が省略でき、磁石製造
工程の短縮が実現する。この固定短縮は、好ましくない
成分ないし不純物(酸素等)の工程中における混入を避
ける上で極めて有用である。特に溶製から粉砕までの工
程において酸素等の混入を防止することは複雑な工程管
理を必要として困難であり、製造コストの増大の一因と
なるからである。
As described in detail, according to the present invention, an alloy powder having the same composition for producing an R 1 —R 2 —Fe—Co—B magnet is prepared by using a rare earth oxide and a boron oxide raw material as starting materials. R 1 -R 2 -Fe-Co with excellent properties obtained at low cost
-The B-type permanent magnet is obtained, and the isolation and purification of the rare earth metal from the magnet manufacturing process-The melting of the alloy-The cooling (usually casting) -The crushing of the predetermined alloy powder manufacturing process can be omitted, and the magnet manufacturing process can be shortened. To do. This shortening of fixation is extremely useful in avoiding contamination of undesirable components or impurities (oxygen etc.) during the process. This is because it is difficult to prevent oxygen and the like from being mixed in the processes from melting to crushing, which requires complicated process control, which is one of the causes of an increase in manufacturing cost.

さらに希土類酸化物として、夫々の希土類酸化物として
分離されたものを用いる必要は必ずしもなく、目標組成
に近い酸化物混合物あるいは、部分的に不足希土類酸化
物を加えて出発原料とすることにより、希土類酸化物の
分離工程自体においても、工程の短縮・コストダウンが
可能となる。さらにCoの添加によって、永久磁石のキュ
リー温度の上昇、減磁曲線の角形性の向上並びに耐酸化
性の向上、また製造工程上の還元反応生成物の崩壊時の
歩止まり向上、微粉末の耐酸化安定性などがもたらされ
る。
Furthermore, as the rare earth oxide, it is not always necessary to use those separated as the respective rare earth oxides, but it is not necessary to use an oxide mixture close to the target composition or a partial deficiency rare earth oxide as the starting material. Also in the oxide separation process itself, the process can be shortened and the cost can be reduced. Furthermore, the addition of Co raises the Curie temperature of the permanent magnet, improves the squareness of the demagnetization curve and oxidation resistance, improves the yield when the reduction reaction product collapses during the manufacturing process, and improves the acid resistance of the fine powder. It brings about chemical stability.

また本発明の合金は、直接還元法によって直接に、磁気
特性上必須の正方晶磁性相を主相とする合金として得ら
れる点で効果大であり、しかも粉末状として得られるこ
とも大きな利点である。希土類磁石を希土類酸化物を還
元した合金粉末から得る方法はSm・コバルト磁石で知ら
れている。しかしSm・コバルト磁石は1150〜1300℃の高
い還元温度を必要とするため粒成長を起こしたり、崩壊
時に粒度の揃った粉末を得にくく、また還元時に用いる
容器と反応のために著しく損傷させる。
Further, the alloy of the present invention is very effective in that it can be directly obtained by the direct reduction method as an alloy having a tetragonal magnetic phase essential for magnetic properties as a main phase, and it is also a great advantage that it can be obtained as a powder. is there. A method of obtaining a rare earth magnet from an alloy powder obtained by reducing a rare earth oxide is known as an Sm / cobalt magnet. However, the Sm / cobalt magnet requires a high reduction temperature of 1150 to 1300 ° C, which causes grain growth and makes it difficult to obtain a powder having a uniform grain size at the time of disintegration, and significantly damages it due to the reaction with the container used for reduction.

以上を総合して、本発明の効果は、顕著なものであると
認められる。
Based on the above, the effect of the present invention is recognized to be remarkable.

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

第1図は本発明の一実施例Fe−xCo−8B−13.8Nd−1.0Dy
の系におけるCo量とキュリー温度Tc(℃)の関係を示す
グラフである。
FIG. 1 shows an embodiment of the present invention Fe-xCo-8B-13.8Nd-1.0Dy.
3 is a graph showing the relationship between the amount of Co and the Curie temperature Tc (° C.) in the system of FIG.

───────────────────────────────────────────────────── フロントページの続き (51)Int.Cl.6 識別記号 庁内整理番号 FI 技術表示箇所 H01F 1/06 (72)発明者 藤村 節夫 大阪府三島郡島本町江川2丁目15―17 住 友特殊金属株式会社山崎製作所内 (56)参考文献 特開 昭59−64733(JP,A)─────────────────────────────────────────────────── ─── Continuation of the front page (51) Int.Cl. 6 Identification number Internal reference number FI Technical indication location H01F 1/06 (72) Inventor Setsuo Fujimura 2-15-17 Egawa, Shimamoto-cho, Mishima-gun, Osaka Sumitomo Yamazaki Seisakusho Co., Ltd. (56) References JP-A-59-64733 (JP, A)

Claims (2)

【特許請求の範囲】[Claims] 【請求項1】希土類Rの化合物を含む原料の還元剤とし
て用いられるカルシウムを微量含有して、希土類R、
B、Fe、及びCoを主成分とする下記組成のカルシウム還
元粉であって、 R :12.5〜20原子%(Rのうち R1:0.05〜5原子%)、 B :4〜20原子%、 Fe:45〜82原子%、及び Co:35原子%以下(但し0%を除く)、 (ここでR1は重希土類元素Gd、Tb、Dy、Ho、Er、Tm、Yb
の内の1種以上、R2はNd及び/又はPrが80原子%以上
で、残りがR1以外のYを含む希土類元素の少なくとも1
種とし、R=R1+R2(原子%)とする)からなる合金粉
末であって主相(合金の80vol%以上)、 酸素含有量10000ppm以下、 炭素含有量1000ppm以下、及び、 カルシウム含有量2000ppm以下とし、かつ、 主相(特定の相が80vol%以上)が正方晶であることを
特徴とする希土類含有合金粉末。
1. A rare earth R, containing a trace amount of calcium used as a reducing agent for a raw material containing a compound of the rare earth R,
A calcium reduced powder containing B, Fe, and Co as main components and having the following composition, wherein R: 12.5 to 20 atom% (R 1 : 0.05 to 5 atom% of R), B: 4 to 20 atom%, Fe: 45 to 82 atomic% and Co: 35 atomic% or less (excluding 0%), (where R 1 is a heavy rare earth element Gd, Tb, Dy, Ho, Er, Tm, Yb).
One or more of the, at R 2 is Nd and / or Pr is 80 atomic% or more, at least the remainder of rare earth elements including Y other than R 1 1
Seed, R = R 1 + R 2 (atomic%)), the main phase (80 vol% or more of the alloy), oxygen content 10000 ppm or less, carbon content 1000 ppm or less, and calcium content A rare earth-containing alloy powder characterized in that the content is 2000 ppm or less and the main phase (specific phase is 80 vol% or more) is tetragonal.
【請求項2】希土類Rの化合物を含む原料の還元剤とし
て用いられるカルシウムを微量含有して、希土類R、
B、Fe、及びCoを主成分とする下記組成のカルシウム還
元粉であって、 R :12.5〜20原子%(Rのうち R1:0.05〜5原子%)、 B :4〜20原子%、 Fe:45〜82原子%、及び Co:35原子%以下(但し0%を除く)、 (ここでR1は重希土類元素Gd、Tb、Dy、Ho、Er、Tm、Yb
の内の1種以上、R2はNd及び/又はPrが80原子%以上
で、残りがR1以外のYを含む希土類元素の少なくとも1
種とし、R=R1+R2(原子%)とする)からなる合金粉
末であって主相(合金の80vol%以上)、 酸素含有量10000ppm以下、 炭素含有量1000ppm以下、及び、 カルシウム含有量2000ppm以下とし、かつ、 主相(特定の相が80vol%以上)が正方晶であり、 前記Feに部分的に代わり、 5.0原子%以下のAl、 3.0原子%以下のTi、 5.5原子%以下のV、 6.0原子%以下のNi、 4.5原子%以下のCr、 5.0原子%以下のMn、 5.0原子%以下のBi、 9.0原子%以下のNb、 7.0原子%以下のTa、 5.2原子%以下のMo、 5.0原子%以下のW、 1.0原子%以下のSb、 3.5原子%以下のGe、 1.5原子%以下のSn、 3.3原子%以下のZr、 3.3原子%以下のHf、及び 5.0原子%以下のSiのうち少なくとも1種の添加含有さ
せることを特徴とする希土類含有合金粉末。
2. A rare earth R, containing a trace amount of calcium used as a reducing agent for a raw material containing a compound of the rare earth R,
A calcium reduced powder containing B, Fe, and Co as main components and having the following composition, wherein R: 12.5 to 20 atom% (R 1 : 0.05 to 5 atom% of R), B: 4 to 20 atom%, Fe: 45 to 82 atomic% and Co: 35 atomic% or less (excluding 0%), (where R 1 is a heavy rare earth element Gd, Tb, Dy, Ho, Er, Tm, Yb).
One or more of the, at R 2 is Nd and / or Pr is 80 atomic% or more, at least the remainder of rare earth elements including Y other than R 1 1
Seed, R = R 1 + R 2 (atomic%)), the main phase (80 vol% or more of the alloy), oxygen content 10000 ppm or less, carbon content 1000 ppm or less, and calcium content 2000ppm or less, and the main phase (specific phase is 80vol% or more) is a tetragonal crystal, partially replacing Fe, 5.0 atomic% or less Al, 3.0 atomic% or less Ti, 5.5 atomic% or less V, 6.0 atomic% or less Ni, 4.5 atomic% or less Cr, 5.0 atomic% or less Mn, 5.0 atomic% or less Bi, 9.0 atomic% or less Nb, 7.0 atomic% or less Ta, 5.2 atomic% or less Mo W of 5.0 atomic% or less, Sb of 1.0 atomic% or less, Ge of 3.5 atomic% or less, Sn of 1.5 atomic% or less, Zr of 3.3 atomic% or less, Hf of 3.3 atomic% or less, and Si of 5.0 atomic% or less. At least one of the above is added and contained in the rare earth-containing alloy powder.
JP60275875A 1984-12-10 1985-12-10 Rare earth containing alloy powder Expired - Lifetime JPH0791564B2 (en)

Applications Claiming Priority (2)

Application Number Priority Date Filing Date Title
JP59-260479 1984-12-10
JP26047984 1984-12-10

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JPH0791564B2 true JPH0791564B2 (en) 1995-10-04

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* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
JPH0735521B2 (en) * 1990-08-30 1995-04-19 住友特殊金属株式会社 Raw material powder for R-Fe-B permanent magnets

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* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
JPS5964733A (en) * 1982-09-27 1984-04-12 Sumitomo Special Metals Co Ltd Permanent magnet

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