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JPH0774820B2 - Magnetic field gradient measuring method using search coil and search coil - Google Patents
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JPH0774820B2 - Magnetic field gradient measuring method using search coil and search coil - Google Patents

Magnetic field gradient measuring method using search coil and search coil

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Publication number
JPH0774820B2
JPH0774820B2 JP19232688A JP19232688A JPH0774820B2 JP H0774820 B2 JPH0774820 B2 JP H0774820B2 JP 19232688 A JP19232688 A JP 19232688A JP 19232688 A JP19232688 A JP 19232688A JP H0774820 B2 JPH0774820 B2 JP H0774820B2
Authority
JP
Japan
Prior art keywords
magnetic field
search coil
component
error
field gradient
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 - Fee Related
Application number
JP19232688A
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Japanese (ja)
Other versions
JPH0240577A (en
Inventor
桂子 熊谷
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.)
Fuji Electric Co Ltd
Original Assignee
Fuji Electric Co Ltd
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Priority to JP19232688A priority Critical patent/JPH0774820B2/en
Publication of JPH0240577A publication Critical patent/JPH0240577A/en
Publication of JPH0774820B2 publication Critical patent/JPH0774820B2/en
Anticipated expiration legal-status Critical
Expired - Fee Related legal-status Critical Current

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  • Particle Accelerators (AREA)

Description

【発明の詳細な説明】 〔産業上の利用分野〕 本発明は、加速器や電子蓄積リングなどに用いられる4
極電磁石の磁場勾配を高精度に測定するためのサーチコ
イルによる磁場勾配測定方法およびサーチコイルに関す
る。
DETAILED DESCRIPTION OF THE INVENTION [Industrial field of application] The present invention is used in accelerators, electron storage rings, and the like.
The present invention relates to a magnetic field gradient measuring method using a search coil and a search coil for measuring a magnetic field gradient of a polar electromagnet with high accuracy.

〔従来の技術〕[Conventional technology]

加速器に用いられる主な電磁石として、荷電粒子偏向用
の2極電磁石と荷電粒子収束用の4極電磁石とがある。
4極電磁石は、中心軌道からずれた荷電粒子に対してず
れの大きさに比例した収束値からを与えて、荷電粒子を
中心軌道付近に収束させる機能を持つ。
Main electromagnets used in the accelerator include a two-pole electromagnet for deflecting charged particles and a four-pole electromagnet for converging charged particles.
The quadrupole electromagnet has a function of giving a charged value deviated from the central orbit from a convergence value proportional to the magnitude of the deviance to converge the charged particles near the central orbit.

第2図に4極電磁石の断面図を示す。ここで1は磁極、
2はコイル、3は4極電磁石の中心、4はボア半径を示
す。この4極電磁尺の中をz方向に進む電子は、x方向
には収束力を受けy方向には発散力を受ける。y方向の
収束は、この4極電磁石とは90゜磁極の位置が異なる次
段に配置された4極電磁石により行う。
FIG. 2 shows a sectional view of the quadrupole electromagnet. Where 1 is the magnetic pole,
2 is a coil, 3 is the center of a quadrupole electromagnet, and 4 is a bore radius. The electrons traveling in the z direction through the quadrupole electromagnetic scale receive a focusing force in the x direction and a diverging force in the y direction. Convergence in the y direction is performed by a quadrupole electromagnet arranged at the next stage having a 90 ° magnetic pole position different from that of the quadrupole electromagnet.

x軸上の座標(x,0)を通る電荷が−e,速度がvの電子
に働く収束力Fxは次式で与えられる。
The convergence force Fx that acts on the electron with the charge −e and the velocity v passing through the coordinate (x, 0) on the x-axis is given by the following equation.

Fx=−evBy(x,0) ここでBy(x,0)は、座標(x,0)における磁場のy方向
成分である。理想着な4極電磁石ではBy(x,0)はxに
比例する。即ち、磁場勾配B′y(x,0)は、 となる。従って収束力Fxは中心からのずれに比例する。
Fx = −evBy (x, 0) where By (x, 0) is the y-direction component of the magnetic field at coordinates (x, 0). In an ideally worn quadrupole electromagnet, By (x, 0) is proportional to x. That is, the magnetic field gradient B'y (x, 0) is Becomes Therefore, the convergence force Fx is proportional to the deviation from the center.

4極電磁石では、設計どおりの収束力を得るために、磁
場勾配B′y(x,0)のある所定の一定値からの誤差
が、決められたxの範囲内にわたってできるだけ小さい
ことが望ましい。そこで、4極電磁石を製作したとき、
その性能を評価するために、磁場勾配B′y(x,0)を
高精度に測定することが必要である。
In the case of a quadrupole electromagnet, it is desirable that the error from the predetermined constant value of the magnetic field gradient B′y (x, 0) be as small as possible within the determined range of x in order to obtain the convergent force as designed. So, when making a 4-pole electromagnet,
In order to evaluate its performance, it is necessary to measure the magnetic field gradient B'y (x, 0) with high accuracy.

磁場勾配B′y(x,0)を測定する方法として、サーチ
コイルを用いる方法がある。第3図に箱形レーストラッ
ク状のサーチコイルの例を示す。Dはサーチコイル5の
x方向の横巾、Lはy方向の高さ、Mはz方向の長さで
ある。図示のように、サーチコイル5は内部が空洞の枠
体にコイルを巻回し、空洞中を通る磁場の変化を測定す
るものである。即ち、4極電磁石を一定の電流値に励磁
した状態で、サーチコイルをx軸に沿って移動させて、
電磁誘導によって磁場の空間的変化,つまり磁場勾配
B′y(x,0)を測定する。第3図のサーチコイル5の
x−y平面での断面図を第4図に示す。図において3は
前記した4極電磁石の中心、6はサーチコイルの中心
x0、7はサーチコイルの巻線である。このサーチコイル
5をx方向に等速移動させたときのサーチコイル出力電
圧は、磁場のy方向成分Byの断面D×L内での積分値に
比例する。サーチコイルの位置をその中心座標x0で代表
させる時、位置x0の関数としてサーチコイル出力から導
出される磁場勾配′y(x,0)は、x0における磁場勾
配ではなくサーチコイルの中心がx0にあるときのサーチ
コイルの断面D×L内での平均の磁場勾配である。4極
磁場成分のみを有する理想的な4極電磁石においては、
この平均値はx0における値と一致する。これは、4極磁
場のy方向成分By(x,y)はxに比例しyに依存せず、
従ってサーチコイルの断面D×L内の平均磁場はその中
心座標であるx0における磁場に等しいからである。
As a method for measuring the magnetic field gradient B'y (x, 0), there is a method using a search coil. FIG. 3 shows an example of a box-shaped racetrack-shaped search coil. D is the width of the search coil 5 in the x direction, L is the height in the y direction, and M is the length in the z direction. As shown in the figure, the search coil 5 is one in which the coil is wound around a frame body having a hollow inside, and changes in the magnetic field passing through the hollow are measured. That is, with the quadrupole electromagnet excited to a constant current value, the search coil is moved along the x-axis,
The spatial variation of the magnetic field, that is, the magnetic field gradient B'y (x, 0) is measured by electromagnetic induction. FIG. 4 shows a sectional view of the search coil 5 of FIG. 3 in the xy plane. In the figure, 3 is the center of the quadrupole electromagnet, and 6 is the center of the search coil.
x 0 and 7 are windings of the search coil. The search coil output voltage when the search coil 5 is moved at a constant speed in the x direction is proportional to the integral value of the y direction component By of the magnetic field in the cross section D × L. When the position of the search coil is represented by its center coordinate x 0 , the magnetic field gradient ′ y (x, 0) derived from the search coil output as a function of the position x 0 is not the magnetic field gradient at x 0 but the center of the search coil. Is the average magnetic field gradient in the cross section D × L of the search coil when is at x 0 . In an ideal quadrupole electromagnet having only a quadrupole magnetic field component,
This average is in agreement with the value at x 0 . This is because the y-direction component By (x, y) of the quadrupole magnetic field is proportional to x and does not depend on y,
Therefore, the average magnetic field in the cross section D × L of the search coil is equal to the magnetic field at the center coordinate x 0 .

〔発明が解決しようとする課題〕[Problems to be Solved by the Invention]

従来のこの種のサーチコイルによる磁場測定方法および
サーチコイルにおける問題点は次のとおりである。
The problems with the conventional magnetic field measuring method and search coil using this type of search coil are as follows.

実際に使用される4極電磁石は、4極磁場成分以外によ
り高次の磁場成分,即ち12極,20極,28極成分などを有し
ており、これらの磁場成分はy座標依存性を持つととも
にx座標に対しても直線的ではない依存性を持つ。従っ
て、これらの高次の磁場成分を有する実際の4極電磁石
においては、サーチコイルの断面D×L内の磁場の平均
値はサーチコイルの中心位置での磁場の値とは一致しな
い。よってサーチコイル出力に基づく磁場勾配′y
(x0,0)は位置(x0,0)における真の磁場勾配B′y
(x0,0)とは異なる。
The quadrupole electromagnet actually used has higher-order magnetic field components other than the quadrupole magnetic field component, that is, 12 poles, 20 poles, 28 poles, etc., and these magnetic field components have y coordinate dependence. Also, it has a non-linear dependency on the x coordinate. Therefore, in an actual quadrupole electromagnet having these high-order magnetic field components, the average value of the magnetic field in the cross section D × L of the search coil does not match the value of the magnetic field at the center position of the search coil. Therefore, the magnetic field gradient'y based on the search coil output
(X 0 , 0) is the true magnetic field gradient B'y at the position (x 0 , 0)
Not the same as (x 0 , 0).

実際の4極電磁石における4極磁場成分以外の高次の磁
場成分は第2図のボア半径内では高々数%であること,
およびサーチコイルの寸法をある程度小さくすればサー
チコイルの断面D×L内における磁場の平均値とサーチ
コイルの中心位置での磁場の値との差が小さくなり10-3
オーダーの精度の測定では特に支障はないことから、こ
の相異は従来特に問題にされていなかった。
The high-order magnetic field components other than the quadrupole magnetic field component in the actual quadrupole electromagnet are several% at most within the bore radius of FIG.
And the difference between the value of the magnetic field at the center position of the average value of the magnetic field and search coil in a search coil of the cross-section D × in L if somewhat smaller size of the search coil is reduced 10 -3
Since there is no particular problem in measuring the order accuracy, this difference has not been a problem in the past.

しかしながら電子蓄積リングのように、荷電粒子を長時
間所定の軌道に保持せねばならない場合には、4極電磁
石も特に磁場精度が高いものが要求され、従ってその評
価のための磁場勾配測定も10-4オーダー程度の高精度が
要求される。しかし、4極磁場成分以外の高次の磁場成
分を考慮していない従来のサーチコイルでは、このよう
な高い精度で磁場勾配測定を行うことはできないという
問題があった。また、測定精度を上げるためにサーチコ
イルの断面D×Lを小さくすると、サーチコイル寸法の
製作精度を確保できなくなったり、出力信号が小さくな
りS/N比が悪くなるなどの問題があった。
However, when charged particles must be held in a predetermined orbit for a long time like an electron storage ring, a quadrupole electromagnet with a particularly high magnetic field accuracy is required. -High accuracy of about 4 orders is required. However, the conventional search coil that does not consider the higher-order magnetic field components other than the quadrupole magnetic field component has a problem that the magnetic field gradient measurement cannot be performed with such high accuracy. Further, if the cross section D × L of the search coil is made small in order to improve the measurement accuracy, there are problems that the manufacturing accuracy of the search coil dimensions cannot be ensured, the output signal becomes small, and the S / N ratio deteriorates.

この発明の目的は、上記従来の問題点を除去し、4極磁
場成分以外の高次の磁場成分を有す4極電磁石の磁場勾
配を高精度で測定できるサーチコイルによる磁場勾配測
定方法およびサーチコイルを提供することにある。
An object of the present invention is to eliminate the above-mentioned conventional problems and to measure a magnetic field gradient of a quadrupole electromagnet having a high-order magnetic field component other than the quadrupole magnetic field component with high accuracy and a magnetic field gradient measuring method using a search coil. To provide a coil.

〔課題を解決するための手段〕[Means for Solving the Problems]

上記目的を達成するために、この発明によれば、4極電
磁石の極内の対称軸であるx軸に沿って、これと直角方
向であるy方向の磁場Byの勾配B′yを測定するx方向
の横巾D,y方向の高さL,z方向の長さMを有する箱形レー
ストラック状のサーチコイルによる磁場勾配測定方法に
おいて、磁場Byを直交座標系x,yにおける4極成分およ
び各高次の成分の和で表し、それにより真の磁場とサー
チコイルにおける平均の磁場との誤差を、サーチコイル
の中心座標(x0,0)とx方向の横巾Dとy方向の高さL
との関数として求め、この誤差の大きさが測定範囲内の
x方向の最大座標の点で最小になるようなD/Lを有する
サーチコイルを用いて磁場勾配を測定することとなる。
To achieve the above object, according to the present invention, the gradient B′y of the magnetic field By in the y direction, which is the direction perpendicular to the x axis, which is the axis of symmetry in the pole of the quadrupole electromagnet, is measured. In a magnetic field gradient measuring method using a box-shaped racetrack-shaped search coil having a width D in the x direction, a height L in the y direction, and a length M in the z direction, the magnetic field By is defined as a quadrupole component in the Cartesian coordinate system x, y. And the sum of each higher-order component, whereby the error between the true magnetic field and the average magnetic field in the search coil is calculated by measuring the center coordinates (x 0 , 0) of the search coil, the horizontal width D in the x direction, and the y direction. Height L
And the magnetic field gradient is measured using a search coil having D / L such that the magnitude of this error is minimized at the point of maximum coordinate in the x direction within the measurement range.

また、サーチコイルの形状は、D/Lが略1なる形状のも
のが好適である。
The shape of the search coil is preferably such that D / L is approximately 1.

〔作用〕[Action]

このように、4極成分以外の高次の成分を含む磁場の磁
場勾配を有限な大きさを持つサーチコイルで測定すると
きに生じる誤差を正しく評価し、この誤差の大きさを測
定範囲内で最小あるいは所定の限界値以下になるように
サーチコイルの形状を決定し、そのサーチコイルを用い
て磁場勾配を測定することにより、高精度の磁場勾配の
測定が可能となる。以下に原理を説明する。
In this way, the error caused when measuring the magnetic field gradient of the magnetic field including higher-order components other than the 4-pole component with the search coil having a finite magnitude is correctly evaluated, and the magnitude of this error is measured within the measurement range. By determining the shape of the search coil so as to be the minimum or less than a predetermined limit value and measuring the magnetic field gradient using the search coil, it is possible to measure the magnetic field gradient with high accuracy. The principle will be described below.

磁場のスカラーポテンシャルV(x,y)を、各高次の磁
場成分の和で表すと次の(1)式となる。
If the scalar potential V (x, y) of the magnetic field is expressed by the sum of the higher-order magnetic field components, the following equation (1) is obtained.

これをyで偏微分した値,即ち磁場のy方向成分を次式
で表す。
The value obtained by partial differentiation with respect to y, that is, the y-direction component of the magnetic field is expressed by the following equation.

ここでμ0は透磁率である。従って測定を行いたいx軸
上の点x0における磁場のy方向成分は次の(3)式のよう
に表せる。
Here, μ 0 is the magnetic permeability. Therefore, the y-direction component of the magnetic field at the point x 0 on the x-axis to be measured can be expressed by the following equation (3).

また、点x0を中心とする横巾D,高さLのサーチコイルに
おける磁場のy方向成分は次の(4)となる。
Further, the y-direction component of the magnetic field in the search coil having the width D and the height L centered on the point x 0 is as follows (4).

よって、点x0を中心とし、上記の大きさを持つサーチコ
イルにおける平均の磁場と真の磁場との間には、次の
(5)式で表される誤差ε(n)(x0)を生じる。
Therefore, with the point x 0 as the center and between the average magnetic field and the true magnetic field in the search coil having the above size,
An error ε (n) (x 0 ) represented by the equation (5) is generated.

この式から、サーチコイルの形状,即ちD/Lと磁場勾配
を測定する点x0を与えたときの誤差の値を求めることが
できる。
From this equation, it is possible to obtain the error value when the shape of the search coil, that is, D / L and the point x 0 for measuring the magnetic field gradient are given.

高次の磁場成分は後述するようにxの絶対値が小さくな
ると急激に減衰するので、上記の誤差は、測定範囲の最
大のx座標xmで評価する。そして誤差ε(xm)が最小あ
るいは所定の限界値以下になるようにサーチコイルの形
状を決定する。
Since the high-order magnetic field component is rapidly attenuated as the absolute value of x becomes small as described later, the above error is evaluated at the maximum x coordinate x m of the measurement range. Then, the shape of the search coil is determined so that the error ε (x m ) is the minimum or less than a predetermined limit value.

数値計算結果によると、実際の4極電磁石の寸法範囲に
おけるD/Lの好適値は1.0〜2.0の範囲にあり、特に最も
一般的な4極電磁石の寸法に対してはD/L1という特
定の形状のサーチコイルで、十分に高精度の磁場勾配の
測定が可能である。
According to the numerical calculation results, the suitable value of D / L in the size range of the actual quadrupole electromagnet is in the range of 1.0 to 2.0, and in particular, for the most common size of the quadrupole electromagnet, D / L1 is specified. The shape of the search coil can measure the magnetic field gradient with sufficiently high accuracy.

〔実施例〕〔Example〕

(1)式の磁場のスカラーポテンシャルV(x,y)の4極,1
2極,20極,28極成分の和をx,yの直交座標系で表すと次式
(6)となる。
Four poles of the scalar potential V (x, y) of the magnetic field in Eq. (1), 1
When the sum of 2-pole, 20-pole and 28-pole components is expressed in the Cartesian coordinate system of x and y,
It becomes (6).

V(x,y)=2a2xy+a6(6xy5−20x3y3+6x5y) +a10(10xy9−120x3y7+252x5y5−120x7y3+10x9y) +a14(14xy13−364x3y11+2002x5y9−3432x7y7 +2002x9y5−364x11y3+14x3y) (6) ここでa2の項が4極磁場成分,a6の項が12極磁場成分,
a10の項が20極磁場成分,a14の項が28極磁場成分の項で
ある。(6)式より磁場のy方向成分By(x,y)は次の(7)
式となる。
V (x, y) = 2a 2 xy + a 6 (6xy 5 −20x 3 y 3 + 6x 5 y) + a 10 (10xy 9 −120x 3 y 7 + 252x 5 y 5 −120x 7 y 3 + 10x 9 y) + a 14 (14xy 13 −364x 3 y 11 + 2002x 5 y 9 −3432x 7 y 7 + 2002x 9 y 5 −364x 11 y 3 + 14x 3 y) (6) where the term a 2 is a 4-pole magnetic field component, and the term a 6 is 12 poles. Magnetic field component,
The term a 10 is the 20-pole magnetic field component, and the term a 14 is the 28-pole magnetic field component. From equation (6), the y-direction component of the magnetic field By (x, y) is
It becomes an expression.

By(x,y)=−μ0〔2a2x+a6(30xy4−60x3y2+6x5) +a10(90xy8−840x3y6+1260x5y4−360x7y2+10x9) +a14(182xy12−4004x3y10+18018x5y8−2402x7y6 +10010x9y4−1092x11y2+14x13)〕 (7) (7)式を用いて4極磁場成分について(5)式を計算すると
恒等的に零になる。即ち、4極磁場成分は前記のよう
に、有限の大きさのサーチコイルの場合でも誤差要因と
はならず、誤差要因は12極以上の高次の磁場成分であ
る。
By (x, y) = − μ 0 [2a 2 x + a 6 (30xy 4 −60x 3 y 2 + 6x 5 ) + a 10 (90xy 8 −840x 3 y 6 + 1260x 5 y 4 −360x 7 y 2 + 10x 9 ) + a 14 (182xy 12 −4004x 3 y 10 + 18018x 5 y 8 −2402x 7 y 6 + 10010x 9 y 4 −1092x 11 y 2 + 14x 13 )] (7) By using Eq. When calculated, it becomes equal to zero. That is, as described above, the quadrupole magnetic field component does not become an error factor even in the case of a search coil having a finite size, and the error factor is a high-order magnetic field component of 12 poles or more.

12極磁場成分であるn=6に関してε(n)(x0)を計算
すると、次式(8)となる。
When ε (n) (x 0 ) is calculated for n = 6 which is a 12-pole magnetic field component, the following equation (8) is obtained.

サーチコイルの位置をx0/Lで規格化し、ε(6)(x0)=
0とすれば、(8)式はD/Lについての代数方程式となり、
D/Lを求めることができる。即ち、12極磁場成分による
誤差を零にするサーチコイルのD/Lの値を、規格化した
測定位置x0/Lの関数として求めることができる。
The position of the search coil is standardized by x 0 / L, and ε (6) (x 0 ) =
If 0, then Eq. (8) becomes an algebraic equation for D / L,
D / L can be calculated. That is, the value of D / L of the search coil that makes the error due to the 12-pole magnetic field component zero can be obtained as a function of the standardized measurement position x 0 / L.

同様にして、20極磁場成分、28極磁場成分による誤差を
零にするD/Lとx0/Lとの関係も求めることができる。な
お、28極磁場成分よりもさらに高次の磁場成分は、4極
磁場成分に比べその存在比が非常に小さいので無視す
る。
Similarly, the relationship between D / L and x 0 / L that makes the error due to the 20-pole magnetic field component and the 28-pole magnetic field component zero can be obtained. It should be noted that magnetic field components higher than the 28-pole magnetic field component have a much smaller abundance ratio than the 4-pole magnetic field component, and are therefore ignored.

第1図に数値計算の結果を示す。図から明らかなよう
に、各磁場成分毎に、またx0/L軸上の位置毎に、誤差を
零とするD/Lの値は異なる。しかしx0/Lが大きい所では
誤差を零にするD/Lの値は1に収束する。
Figure 1 shows the result of numerical calculation. As is clear from the figure, the value of D / L at which the error is zero differs for each magnetic field component and for each position on the x 0 / L axis. However, when x 0 / L is large, the value of D / L that makes the error zero converges to 1.

一般的な4極電磁石における磁場勾配測定範囲は当然の
ことながら磁場使用範囲内であり、その範囲は第2図の
ボア半径4内に相当する。この中で磁場のスカラーポテ
ンシャルの各成分V(n)は(1)式に示すように4極電磁石
中心からの距離rのn乗で大きくなり、磁場の各成分By
(n)はrの(n−1)乗で変化する。4極電磁石の基本
成分である4極磁場成分はスカラーポテンシャルV(2)
がrの2条で、磁場By(2)がrの1乗で変化する。そし
て高次の磁場成分は4極磁場成分に対してrについて4
乗以上の大きさで4極電磁石中心に向って減衰する。従
って、磁場勾配測定における誤差を最小にするには、磁
場勾配測定範囲の最大のx座標xmで誤差が小さいサーチ
コイルを用いるのが適当である。一般にはxmはLの数倍
以上の値なので、第1図より、D/L=1のサーチコイル
を用いて磁場勾配を測定するのが好ましい。
The magnetic field gradient measurement range in a general quadrupole electromagnet is naturally within the magnetic field use range, and the range corresponds to the bore radius 4 in FIG. In this, each component V (n) of the scalar potential of the magnetic field increases with the n-th power of the distance r from the center of the quadrupole electromagnet as shown in equation (1), and each component of the magnetic field By
(n) changes with r to the (n-1) th power. The quadrupole magnetic field component, which is the basic component of the quadrupole electromagnet, is a scalar potential V (2)
Is the second line of r, and the magnetic field By (2) changes with the first power of r. And the higher-order magnetic field component is 4 for r with respect to the quadrupole magnetic field component.
If the size is equal to or larger than the power, it attenuates toward the center of the 4-pole electromagnet. Therefore, in order to minimize the error in the magnetic field gradient measurement, it is appropriate to use a search coil having a small error in the maximum x coordinate x m of the magnetic field gradient measurement range. In general, x m is a value which is several times or more of L, so that it is preferable to measure the magnetic field gradient using a search coil of D / L = 1 from FIG.

特別な場合として、測定範囲が狭く、かつその範囲を特
に高精度に測定する必要がある場合は、D/L>1の適当
な値を選ぶことになるが、その際は各磁場成分によって
誤差を最小にする最適なD/Lの値が異なるので、各磁場
成分の存在比を考慮して、誤差を最小にするD/Lの値を
決定し、そのD/Lの値を持つサーチコイルによる磁場勾
配の測定を行う。各高次の磁場成分の存在比は計算機シ
ミュレーションなどにより推定できる。平均的な4極電
磁石でのボア半径内における各高次の磁場成分の存在比
はそれぞれ数%以下である。存在比から各成分の係数an
を決定でき、(5)式から誤差ε(xm)を評価できる。よ
ってこの誤差ε(xm)が最小あるいは所望の精度内に収
まるようにD/Lの値を決定する。
As a special case, if the measurement range is narrow and it is necessary to measure the range with high accuracy, an appropriate value of D / L> 1 should be selected. Since the optimal D / L value that minimizes is different, the D / L value that minimizes the error is determined in consideration of the existence ratio of each magnetic field component, and the search coil with that D / L value is determined. To measure the magnetic field gradient. The abundance ratio of each high-order magnetic field component can be estimated by computer simulation or the like. The abundance ratio of each high-order magnetic field component within the bore radius of an average quadrupole electromagnet is several percent or less. From the abundance ratio, the coefficient of each component a n
And the error ε (x m ) can be evaluated from Eq. (5). Therefore, the value of D / L is determined so that this error ε (x m ) is within the minimum or desired accuracy.

一例として、x0/L=0.4付近の磁場勾配を磁場の28極成
分による誤差がほぼ零になるように測定したい場合は、
第1図より、D/Lを略1.6にすれば良いことがわかる。
As an example, if you want to measure the magnetic field gradient near x 0 / L = 0.4 so that the error due to the 28-pole component of the magnetic field becomes almost zero,
From Fig. 1, it can be seen that D / L should be approximately 1.6.

〔発明の効果〕〔The invention's effect〕

以上に述べたように、本発明によれば、4極電磁石の磁
場を、4極成分および各高次の成分の和で表し、それに
より真の磁場とサーチコイルにおける平均の磁場との誤
差を、サーチコイルの中心座標(x0,0)とx方向の横巾
Dとy方向の高さLとの関数として求め、この誤差の大
きさが測定範囲内のx方向の最大座標の点において最大
になることを利用して、この誤差の値を最小にするよう
なD/Lの値を持つサーチコイルによって磁場勾配を測定
するので、非常に高精度の測定が可能になる。また実際
的な測定範囲において、D/L1のサーチコイルを用い
れば、磁場の4極成分に対する各多極成分の存在比が未
知の場合でも、最も誤差の小さい高精度の磁場勾配測定
が可能になる。
As described above, according to the present invention, the magnetic field of the quadrupole electromagnet is represented by the sum of the quadrupole component and each higher-order component, whereby the error between the true magnetic field and the average magnetic field in the search coil is calculated. , As a function of the center coordinates (x 0 , 0) of the search coil, the lateral width D in the x direction and the height L in the y direction, and the magnitude of this error is at the point of the maximum coordinate in the x direction within the measurement range. By taking advantage of the maximum value, the magnetic field gradient is measured by the search coil having the D / L value that minimizes the value of this error, so that extremely high accuracy measurement is possible. Also, in the practical measurement range, using the D / L1 search coil enables highly accurate magnetic field gradient measurement with the smallest error even when the existence ratio of each multipole component to the quadrupole component of the magnetic field is unknown. Become.

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

第1図は規格化されたサーチコイルの中心位置x0/Lに対
する各高次の磁場成分毎の誤差を零にするサーチコイル
の横巾Dと高さLとの比の関係を表すもので、これによ
り本発明のサーチコイルによる磁場勾配測定方法に用い
られるサーチコイルの形状が決定される図、第2図は4
極電磁石の断面図、第3図はサーチコイルの斜視図、第
4図はサーチコイルの断面図である。 5:サーチコイル。
FIG. 1 shows the relationship between the width D of the search coil and the height L for zeroizing the error for each higher-order magnetic field component with respect to the standardized center position x 0 / L of the search coil. FIG. 4 shows the shape of the search coil used in the magnetic field gradient measuring method according to the present invention.
FIG. 3 is a perspective view of the search coil, and FIG. 4 is a cross-sectional view of the search coil. 5: Search coil.

Claims (2)

【特許請求の範囲】[Claims] 【請求項1】4極電磁石の極内の対称軸であるx軸に沿
って、これと直角方向であるy方向の磁場Byの勾配B′
yを測定するx方向の横巾D,y方向の高さL,z方向の長さ
Mを有する箱形レーストラック状のサーチコイルによる
磁場勾配測定方法において、磁場Byを直交座標系x,yに
おける4極成分および各高次の成分の和で表し、それに
より真の磁場とサーチコイルにおける平均の磁場との誤
差を、サーチコイルの中心座標(x0,0)と前記x方向の
横巾Dとy方向の高さLとの関数として求め、この誤差
の大きさが測定範囲内のx方向の最大座標の点で最小に
なるようなD/Lを有するサーチコイルを用いて磁場勾配
を測定することを特徴とするサーチコイルによる磁場勾
配測定方法。
1. A gradient B'of a magnetic field By in the y direction, which is a direction perpendicular to the x axis, which is the axis of symmetry in the pole of the quadrupole electromagnet.
In a magnetic field gradient measuring method using a box-shaped racetrack-shaped search coil having a width D in the x direction for measuring y, a height L in the y direction, and a length M in the z direction, the magnetic field By is set to the orthogonal coordinate system x, y. The error between the true magnetic field and the average magnetic field in the search coil is represented by the sum of the quadrupole component and each higher-order component in the search coil, and the center coordinate (x 0 , 0) of the search coil and the width in the x direction. The magnetic field gradient is obtained by using a search coil having D / L such that the magnitude of this error is minimized at the point of the maximum coordinate in the x direction within the measurement range, as a function of D and the height L in the y direction. A magnetic field gradient measuring method using a search coil, which comprises measuring.
【請求項2】4極電磁石の極内の対称軸であるx軸に沿
って、これと直角方向であるy方向の磁場Byの勾配B′
yを測定するx方向の横巾D,y方向の高さL,z方向の長さ
Mを有する箱形レーストラック状のサーチコイルにおい
て、D/Lが略1なる形状を有することを特徴とするサー
チコイル。
2. A gradient B'of a magnetic field By in the y direction, which is perpendicular to the x axis, which is the axis of symmetry within the pole of the quadrupole electromagnet.
A box-shaped racetrack-shaped search coil having a lateral width D in the x direction for measuring y, a height L in the y direction, and a length M in the z direction, characterized in that D / L is substantially 1 Search coil to do.
JP19232688A 1988-08-01 1988-08-01 Magnetic field gradient measuring method using search coil and search coil Expired - Fee Related JPH0774820B2 (en)

Priority Applications (1)

Application Number Priority Date Filing Date Title
JP19232688A JPH0774820B2 (en) 1988-08-01 1988-08-01 Magnetic field gradient measuring method using search coil and search coil

Applications Claiming Priority (1)

Application Number Priority Date Filing Date Title
JP19232688A JPH0774820B2 (en) 1988-08-01 1988-08-01 Magnetic field gradient measuring method using search coil and search coil

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JPH0240577A JPH0240577A (en) 1990-02-09
JPH0774820B2 true JPH0774820B2 (en) 1995-08-09

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* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
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