JP3687791B2 - Novel rare earth complexes with circularly polarized light emission - Google Patents
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本発明は、円偏光発光性を有する新規希土類錯体に関する。 The present invention relates to a novel rare earth complex having circularly polarized light emission.
希土類錯体は、色純度が高く、かつ励起に対して安定な発光体であるため、例えば、発光性インク(例えば、特許文献1参照。)や有機エレクトロルミネッセンス素子(例えば、特許文献2参照。)に好適に利用される。このうち、円偏光発光性を有する希土類錯体としては、例えば、トリス(3−トリフルオロアセチルカンフォラト)ユウロピウム等が知られている(例えば、非特許文献1参照。)。ここで、円偏光発光性とは、例えば紫外線の照射等により蛍光または燐光を発する化合物において、該化合物の発する蛍光または燐光の左右の円偏光の強度が異なるという性質を表す。すなわち、放射された蛍光または燐光の右円偏光成分の強度をIRとし、左円偏光成分の強度をILとし、次式 Since the rare earth complex is a light emitter that has high color purity and is stable with respect to excitation, for example, a luminescent ink (see, for example, Patent Document 1) and an organic electroluminescence element (see, for example, Patent Document 2). Is suitably used. Among these, as a rare earth complex having circularly polarized light emission property, for example, tris (3-trifluoroacetylcamphorato) europium is known (for example, see Non-Patent Document 1). Here, the circularly polarized light-emitting property represents a property that, for example, in a compound that emits fluorescence or phosphorescence by irradiation with ultraviolet rays or the like, the intensity of the circularly polarized light on the left and right of the fluorescence or phosphorescence emitted by the compound is different. That is, the intensity of the right circularly polarized component of the emitted fluorescence or phosphorescence and I R, the intensity of left-handed circularly polarized light component and I L, the following equation
このような円偏光発光性を有する化合物は、例えば、有機エレクトロルミネッセンス素子等に利用すると発光した光を有効に利用することができる(例えば、特許文献3参照。)。しかしながら、例えば、トリス(3−トリフルオロアセチルカンフォラト)ユウロピウム等公知の希土類錯体は発光強度が十分でなかった。 Such a circularly polarized light-emitting compound can effectively use emitted light when used in, for example, an organic electroluminescence device (see, for example, Patent Document 3). However, for example, known rare earth complexes such as tris (3-trifluoroacetylcamphorato) europium have insufficient luminescence intensity.
本発明は、発光強度が極めて大きく、かつ、円偏光発光性を有する希土類錯体を提供する。 The present invention provides a rare earth complex having extremely high emission intensity and circularly polarized light emission.
本発明者らは上記課題を解決すべく鋭意研究を重ねた結果、新規な希土類錯体を得、これが極めて大きい発光強度と円偏光発光性とを有することを見いだした。 As a result of intensive studies to solve the above-mentioned problems, the present inventors have obtained a novel rare earth complex, which has been found to have extremely high emission intensity and circularly polarized light emission.
すなわち本発明は、一般式(1) That is, the present invention relates to the general formula (1)
(式中、X1およびX2はそれぞれ独立に、水素原子、ハロゲン原子、炭素数1〜4のアルキル基、炭素数1〜4のアルコキシル基を表し、Y1、Y2、Y3およびY4はそれぞれ独立に水素原子、ハロゲン原子、炭素数1〜4のアルキル基を表し、R1は炭素数1〜8のアルキル基、炭素数1〜8のフッ素置換アルキル基、またはフェニル基を表し、R2は、
(a)シクロペンタジエニル基(基中に存在する1個のCH2基はまた、−O−または−S−により置き換えられていてもよい)、
(b)フェニル基(基中に存在する1個または2個のCH基はまた、Nにより置き換えられていてもよい)、
(c)ナフチル基(基中に存在する1個または2個のCH基はまた、Nにより置き換えられていてもよい)、
からなる群から選ばれる基を表し、上記(a)、(b)及び(c)の基はアルキル基またはハロゲン原子で置換されていてもよく、Lnは希土類金属原子を表す。)で表される光学活性希土類錯体を提供する。
(In the formula, X 1 and X 2 each independently represent a hydrogen atom, a halogen atom, an alkyl group having 1 to 4 carbon atoms, or an alkoxyl group having 1 to 4 carbon atoms; Y 1 , Y 2 , Y 3 and Y 4 each independently represents a hydrogen atom, a halogen atom, or an alkyl group having 1 to 4 carbon atoms, and R 1 represents an alkyl group having 1 to 8 carbon atoms, a fluorine-substituted alkyl group having 1 to 8 carbon atoms, or a phenyl group. , R 2 is
(A) a cyclopentadienyl group (one CH 2 group present in the group may also be replaced by —O— or —S—),
(B) a phenyl group (one or two CH groups present in the group may also be replaced by N),
(C) a naphthyl group (one or two CH groups present in the group may also be replaced by N),
The group (a), (b) and (c) above may be substituted with an alkyl group or a halogen atom, and Ln represents a rare earth metal atom. An optically active rare earth complex represented by
本発明によれば、従来の円偏光発光性を有する希土類錯体に比べて、発光強度の非常に大きい希土類錯体(1)を提供することができる。 According to the present invention, it is possible to provide a rare earth complex (1) having a very high emission intensity as compared with a conventional rare earth complex having circularly polarized light emission.
以下、本発明を詳細に説明する。
本発明の一般式(1)で表される化合物の光学純度は、90%以上であることが好ましい。また、一般式(1)のX1およびX2は水素原子であることが好ましく、Y1、Y2、Y3およびY4は水素原子であることが好ましく、LnはEuであることが好ましい。
また、R1がトリフルオロメチル基であって、かつ、R2がチエニル基であることが好ましい。
Hereinafter, the present invention will be described in detail.
The optical purity of the compound represented by the general formula (1) of the present invention is preferably 90% or more. Further, X 1 and X 2 in the general formula (1) are preferably hydrogen atoms, Y 1 , Y 2 , Y 3 and Y 4 are preferably hydrogen atoms, and Ln is preferably Eu. .
Moreover, it is preferable that R 1 is a trifluoromethyl group and R 2 is a thienyl group.
一般式(1)で表される光学活性希土類錯体(以下、希土類錯体(1)と言う。)としては、一般式(1−1) As the optically active rare earth complex represented by the general formula (1) (hereinafter referred to as the rare earth complex (1)), the general formula (1-1)
一般式(1−2)
General formula (1-2)
R−Δ構造とS−Λ構造は、互いに鏡像異性体の関係にある。
The R-Δ structure and the S-Λ structure are in an enantiomeric relationship with each other.
円偏光発光は、一般に、光学活性を持つ発光化合物によって引き起こされ、光学純度が高くなるとその偏光の度合いも大きくなる。円偏光発光とは、放射された蛍光または燐光の右円偏光成分の強度をIRとし、左円偏光成分の強度をILとし、次式 Circularly polarized light emission is generally caused by a light-emitting compound having optical activity, and the degree of polarization increases as the optical purity increases. The circularly polarized luminescence, the intensity of the right circularly polarized component of the emitted fluorescence or phosphorescence and I R, the intensity of left-handed circularly polarized light component and I L, the following equation
一般に、希土類錯体は正四角反柱型の配位構造をとるため、希土類金属原子周辺の絶対配置に関して2種の立体異性体が存在する。以下、この2種の異性体をΔとΛで区別する。したがって、希土類錯体に光学活性な配位子を導入したとしても、依然として、Δ、Λの2種の立体異性体が等量混在するため、光学純度の高い化合物が得られなかった。 Generally, since a rare earth complex has a regular tetragonal prismatic coordination structure, there are two types of stereoisomers with respect to the absolute configuration around the rare earth metal atom. Hereinafter, these two isomers are distinguished by Δ and Λ. Therefore, even if an optically active ligand is introduced into the rare earth complex, an equivalent amount of the two stereoisomers of Δ and Λ are still mixed, so that a compound with high optical purity cannot be obtained.
そこで、光学活性な配位子としてジアステレオ選択性を持つ配位子を導入することによって、光学純度の非常に高い希土類錯体を得ることができ、また、これが極めて大きい発光強度と円偏光発光性とを有することを見いだした。本発明においてジアステレオ選択性を持つ配位子とは、2種の鏡像異性体が存在する(以下、R、Sで表す)配位子で、一方の鏡像体(例えばR体の配位子)を用いて希土類と錯体を形成するとき、希土類錯体の一方の立体異性体(例えばΔ体の希土類錯体)が選択的に生成するという性質を持つ配位子のことを意味する。ジアステレオ選択性を持つ配位子は2種より多い立体異性体を持っていても良い。 Therefore, by introducing a diastereoselective ligand as an optically active ligand, it is possible to obtain a rare earth complex with very high optical purity. And found to have In the present invention, a ligand having diastereoselectivity is a ligand in which two kinds of enantiomers exist (hereinafter represented by R and S), and one of the enantiomers (for example, an R-form ligand). ) Means a ligand having a property that one stereoisomer of the rare earth complex (for example, a Δ rare earth complex) is selectively formed. Ligands with diastereoselectivity may have more than two stereoisomers.
ジアステレオ選択性を持つ配位子としては、例えば下記一般式(2) As a ligand having diastereoselectivity, for example, the following general formula (2)
(式中、X1、X2、Y1、Y2、Y3およびY4は一般式(1)においてと同じ意味を表す。)で表される配位子(以下、配位子(2)と言う。)を挙げることができる。配位子(2)はビナフチル基の部分に軸不斉を有するため、2種の光学異性体が存在する。以下、この2種の異性体をRとSで区別する。配位子(2)を用いると、例えば下記一般式(3) (Wherein, X 1 , X 2 , Y 1 , Y 2 , Y 3 and Y 4 have the same meaning as in general formula (1)) (hereinafter referred to as ligand (2 ))). Since the ligand (2) has axial asymmetry at the binaphthyl group, there are two optical isomers. Hereinafter, these two isomers are distinguished by R and S. When the ligand (2) is used, for example, the following general formula (3)
(式中、X1、X2、Y1、Y2、Y3およびY4は一般式(1)においてと同じ意味を表す。R3、R4はそれぞれ独立に、炭素数1〜20のアルキル基、炭素数1〜20のフッ素置換アルキル基、水酸基、ニトロ基、アミノ基、スルホニル基、シアノ基、シリル基、ホスホン酸基、ジアゾ基、メルカプト基、アリール基、ヘテロアリール基を表す)で表される光学活性希土類錯体(以下、希土類錯体(3)と言う)を得ることができる。このとき、配位子(2)としてR体を用いると、希土類錯体(3)はΔ体(以下、R―Δ希土類錯体(3)と言う。)が選択的に生成した。また、配位子(2)としてS体を用いると、希土類錯体(3)はΛ体(以下、S―Λ希土類錯体(3)と言う。)が選択的に生成した。 (In the formula, X 1 , X 2 , Y 1 , Y 2 , Y 3 and Y 4 represent the same meaning as in general formula (1). R 3 and R 4 each independently has 1 to 20 carbon atoms. An alkyl group, a C1-C20 fluorine-substituted alkyl group, a hydroxyl group, a nitro group, an amino group, a sulfonyl group, a cyano group, a silyl group, a phosphonic acid group, a diazo group, a mercapto group, an aryl group, or a heteroaryl group) An optically active rare earth complex represented by the following (hereinafter referred to as rare earth complex (3)) can be obtained. At this time, when the R form was used as the ligand (2), a rare earth complex (3) was selectively produced as a Δ form (hereinafter referred to as R-Δ rare earth complex (3)). Further, when the S form was used as the ligand (2), a Λ form (hereinafter referred to as S-Λ rare earth complex (3)) was selectively produced as the rare earth complex (3).
希土類錯体(3)は円偏光発光性を有するが、発光強度の点を考慮すると、このうち本発明の希土類錯体である下記一般式(1) The rare earth complex (3) has a circularly polarized light emission property, but considering the light emission intensity, the rare earth complex of the present invention is represented by the following general formula (1).
で表される化合物(希土類錯体(1))が好ましい。一般式(1)中、X1およびX2で示される置換基としては、それぞれ独立に、水素原子、フッ素原子、塩素原子等のハロゲン原子、メチル基、エチル基、iso−プロピル基等のアルキル基、及びメトキシ基、エトキシ基、tert−ブトキシ基等のアルコキシ基が挙げられるが、好ましくは水素原子である。
一般式(1)中、Y1、Y2、Y3およびY4で示される置換基としては、それぞれ独立に、水素原子、フッ素原子、塩素原子等のハロゲン原子、メチル基、エチル基、及びiso−プロピル基等のアルキル基が挙げられるが、好ましくは水素原子である。
The compound (rare earth complex (1)) represented by these is preferable. In general formula (1), the substituents represented by X 1 and X 2 are each independently a halogen atom such as a hydrogen atom, a fluorine atom or a chlorine atom, or an alkyl such as a methyl group, an ethyl group or an iso-propyl group. Group, and alkoxy groups such as a methoxy group, an ethoxy group, and a tert-butoxy group, and a hydrogen atom is preferable.
In the general formula (1), the substituents represented by Y 1 , Y 2 , Y 3 and Y 4 are each independently a halogen atom such as a hydrogen atom, a fluorine atom or a chlorine atom, a methyl group, an ethyl group, and An alkyl group such as an iso-propyl group is exemplified, and a hydrogen atom is preferred.
一般式(1)中、R1で示される置換基としては、メチル基、トリフルオロメチル基、ペンタフルオロエチル基、ヘキサフルオロ−iso−プロピル基、及びパーフルオロヘキシル基が挙げられるが、好ましくはトリフルオロメチル基である。
一般式(1)中、R2で示される置換基としては、フェニル基、トリル基、フルオロフェニル基、ペンタフルオロフェニル基、トリフルオロメチルフェニル基、クロロフェニル基、ナフチル基、フリル基、チエニル基、チアンスニル基、ピラニル基、イソベンゾフラニル基、ピラゾリル基、ピリジル基、及びピラジニル基を挙げることが出来る。更に上記の基のアルキル基置換体、アリール基置換体、アルコキシ基置換体、アリールオキシ基置換体、ハロゲン原子置換体、アルコキシカルボニル基置換体、ニトリル基置換体及びニトロ基置換体が挙げられるが、好ましくはフェニル基、トリル基、ナフチル基、フリル基、チエニル基で、更に好ましくはチエニル基である。
In the general formula (1), examples of the substituent represented by R 1 include a methyl group, a trifluoromethyl group, a pentafluoroethyl group, a hexafluoro-iso-propyl group, and a perfluorohexyl group. A trifluoromethyl group.
In the general formula (1), examples of the substituent represented by R 2 include a phenyl group, a tolyl group, a fluorophenyl group, a pentafluorophenyl group, a trifluoromethylphenyl group, a chlorophenyl group, a naphthyl group, a furyl group, a thienyl group, Mention may be made of thianthnyl, pyranyl, isobenzofuranyl, pyrazolyl, pyridyl and pyrazinyl. Furthermore, alkyl group-substituted products, aryl group-substituted products, alkoxy group-substituted products, aryloxy group-substituted products, halogen atom-substituted products, alkoxycarbonyl group-substituted products, nitrile group-substituted products, and nitro group-substituted products of the above groups may be mentioned. Preferably a phenyl group, a tolyl group, a naphthyl group, a furyl group, and a thienyl group, more preferably a thienyl group.
一般式(1)の化合物中、Lnで示される希土類金属としては、原子番号57から71の各原子が挙げられるが、好ましくはEuまたはYbである。 In the compound of the general formula (1), examples of the rare earth metal represented by Ln include each atom having an atomic number of 57 to 71, preferably Eu or Yb.
本発明の希土類錯体(1)の製造方法としては、例えば、アルコールやアセトン等の有機溶媒中、下記一般式(2) Examples of the method for producing the rare earth complex (1) of the present invention include the following general formula (2) in an organic solvent such as alcohol and acetone.
(式中、X1、X2、Y1、Y2、Y3およびY4は一般式(1)においてと同じ意味を表す。)で表される化合物と、下記一般式(4) (Wherein, X 1 , X 2 , Y 1 , Y 2 , Y 3 and Y 4 represent the same meaning as in general formula (1)), and the following general formula (4)
(式中、Ln、R1およびR2は一般式(1)においてと同じ意味を表す。)を−50〜80℃、好ましくは0〜40℃で1〜24時間攪拌して反応させる。一般式(2)の化合物は、例えば、Org.Synth.,Coll.Vol.8 57(1993)に記載の方法で製造することができる。また、一般式(4)の化合物は、例えば、特願2003−143292号に記載の方法で製造することができる。反応終了後、溶媒を留去して目的の希土類錯体(1)を得ることができる。必要に応じて、例えば再結晶等の精製を行ってもよい。 (Wherein, Ln, R 1 and R 2 have the same meaning as in formula (1)) are allowed to react with stirring at −50 to 80 ° C., preferably at 0 to 40 ° C. for 1 to 24 hours. The compound of the general formula (2) is, for example, Org. Synth. , Coll. Vol. 8 57 (1993). Moreover, the compound of General formula (4) can be manufactured by the method as described in Japanese Patent Application No. 2003-143292, for example. After completion of the reaction, the solvent is distilled off to obtain the desired rare earth complex (1). If necessary, purification such as recrystallization may be performed.
本発明の希土類錯体(1)を円偏光発光材料として使用するときはR−Δ希土類錯体(1)、及びS−Λ希土類錯体(1)の2種の光学異性体のうち、どちらか一方を過剰に含んだ状態で使用するとよいが、好ましくは、その光学純度が90%以上、さらに好ましくは95%以上で使用するとよい。 When the rare earth complex (1) of the present invention is used as a circularly polarized light emitting material, either one of the two optical isomers of the R-Δ rare earth complex (1) and the S-Λ rare earth complex (1) is used. Although it may be used in an excessively contained state, the optical purity is preferably 90% or more, more preferably 95% or more.
以下に、実施例にて本発明を更に詳細に説明するが、本発明は以下の例に限るものではない。また、以下で部は質量部を表す。 EXAMPLES Hereinafter, the present invention will be described in more detail with reference to examples, but the present invention is not limited to the following examples. Moreover, a part represents a mass part below.
(実施例1)
下記式(5)で表される(S)−BINAPO2.00部、下記式(6)で表されるユウロピウム−テノイルトリフルオロアセトナート錯体2.60部、メタノール75部を室温で2時間攪拌して反応させた。反応終了後、エバポレーターで溶媒を留去して、薄黄色粉末を得た。これをエタノールから再結晶して下記式(7)で表される希土類錯体(S−Λ体;以下S−Λ希土類錯体(7)と言う。)を2.91部得た。
(Example 1)
2.00 parts of (S) -BINAPO represented by the following formula (5), 2.60 parts of europium-thenoyltrifluoroacetonate complex represented by the following formula (6), and 75 parts of methanol were stirred at room temperature for 2 hours. And reacted. After completion of the reaction, the solvent was distilled off with an evaporator to obtain a light yellow powder. This was recrystallized from ethanol to obtain 2.91 parts of a rare earth complex represented by the following formula (7) (S-Λ body; hereinafter referred to as S-Λ rare earth complex (7)).
1H NMR(d6−Acetone) δ 5.12(s), 6.44(s), 6.71(t), 6.89(t), 7.18(q), 7.23(t), 7.30(t), 7.63(t), 7.76(t), 7.89(m), 8.05(m), 8.31(t)
31P NMR(d6−Acetone) δ −67.47(s)
元素分析 測定値 C57.19% H3.71% Eu10.4%
計算値 C55.55% H3.02% Eu10.3%
1 H NMR (d 6 -acetone) δ 5.12 (s), 6.44 (s), 6.71 (t), 6.89 (t), 7.18 (q), 7.23 (t ), 7.30 (t), 7.63 (t), 7.76 (t), 7.89 (m), 8.05 (m), 8.31 (t)
31 P NMR (d 6 -acetone) δ −67.47 (s)
Elemental analysis Measured value C57.19% H3.71% Eu10.4%
Calculated value C55.55% H3.02% Eu10.3%
(実施例2)
(S)−BINAPO1.98部、下記式(8)で示されるユウロピウム−ベンゾイルトリフルオロアセトナート錯体2.56部、メタノール70部を室温で2時間攪拌して反応させた。反応終了後、エバポレーターで溶媒を留去して、薄黄色粉末を得た。これをエタノールから再結晶して下記式(9)で示される希土類錯体(S−Λ体;以下S−Λ希土類錯体(9)と言う。)を2.12部得た。
(Example 2)
1.98 parts of (S) -BINAPO, 2.56 parts of europium-benzoyltrifluoroacetonate complex represented by the following formula (8), and 70 parts of methanol were reacted at room temperature for 2 hours with stirring. After completion of the reaction, the solvent was distilled off with an evaporator to obtain a light yellow powder. This was recrystallized from ethanol to obtain 2.12 parts of a rare earth complex represented by the following formula (9) (S-Λ form; hereinafter referred to as S-Λ rare earth complex (9)).
以下の方法で式(9)で表される希土類錯体が生成していることを確認した。
1H NMR(d6−Acetone) δ 5.56(s), 6.42(s), 6.91(t), 7.13(m), 7.25(d), 7.36(t), 7.64(s), 7.75(t), 7.93(m), 7.99−8.14(m)
31P NMR(d6−Acetone) δ −62.55(s)
元素分析 測定値 C60.92% H3.96% Eu10.3%
計算値 C61.21% H3.47% Eu10.5%
It confirmed that the rare earth complex represented by Formula (9) was producing | generating with the following method.
1 H NMR (d 6 -acetone) δ 5.56 (s), 6.42 (s), 6.91 (t), 7.13 (m), 7.25 (d), 7.36 (t ), 7.64 (s), 7.75 (t), 7.93 (m), 7.99-8.14 (m)
31 P NMR (d 6 -acetone) δ −62.55 (s)
Elemental analysis Measured value C60.92% H3.96% Eu10.3%
Calculated C61.21% H3.47% Eu10.5%
(実施例3)
(S)−BINAPO1.99部、下記式(10)で示されるユウロピウム−ナフトイルトリフルオロアセトナート錯体3.00部、アセトン70部を室温で2時間攪拌して反応させた。反応終了後、エバポレーターで溶媒を留去して、薄黄色粉末を得た。これをエタノールから再結晶して下記式(11)で示される希土類錯体(S−Λ体;以下S−Λ希土類錯体(11)と言う。)を2.12部得た。
(Example 3)
1.99 parts of (S) -BINAPO, 3.00 parts of europium-naphthoyltrifluoroacetonate complex represented by the following formula (10), and 70 parts of acetone were reacted by stirring at room temperature for 2 hours. After completion of the reaction, the solvent was distilled off with an evaporator to obtain a light yellow powder. This was recrystallized from ethanol to obtain 2.12 parts of a rare earth complex represented by the following formula (11) (S-Λ form; hereinafter referred to as S-Λ rare earth complex (11)).
以下の方法で式(11)で表される希土類錯体が生成していることを確認した。
1H NMR(d6−Acetone) δ 5.91(s), 6.44(s), 6.87(t), 7.07(m), 7.13−7.29(m), 7.42−7.47(m), 7.61(t), 7.76(t), 7.94(m), 8.01−8.22(m)
31P NMR(d6−Acetone) δ −64.25(s)
元素分析 測定値 C63.74% H3.51% Eu9.4%
計算値 C63.05% H3.69% Eu9.3%
It was confirmed that the rare earth complex represented by the formula (11) was generated by the following method.
1 H NMR (d 6 -acetone) δ 5.91 (s), 6.44 (s), 6.87 (t), 7.07 (m), 7.13-7.29 (m), 7 .42-7.47 (m), 7.61 (t), 7.76 (t), 7.94 (m), 8.01-8.22 (m)
31 P NMR (d 6 -acetone) δ −64.25 (s)
Elemental analysis Measured value C63.74% H3.51% Eu9.4%
Calculated C63.05% H3.69% Eu9.3%
(実施例4)
(S)−BINAPO2.00部、下記式(12)で表されるイッテルビウム−テノイルトリフルオロアセトナート錯体2.68部、アセトン50部を室温で2時間攪拌して反応させた。反応終了後、エバポレーターで溶媒を留去して、薄黄色粉末を得た。これをエタノールから再結晶して下記式(13)で示される希土類錯体(S−Λ体;以下S−Λ希土類錯体(13)と言う。)を1.27部得た。
(Example 4)
2.00 parts of (S) -BINAPO, 2.68 parts of ytterbium-thenoyltrifluoroacetonate complex represented by the following formula (12), and 50 parts of acetone were reacted by stirring at room temperature for 2 hours. After completion of the reaction, the solvent was distilled off with an evaporator to obtain a light yellow powder. This was recrystallized from ethanol to obtain 1.27 parts of a rare earth complex represented by the following formula (13) (S-Λ form; hereinafter referred to as S-Λ rare earth complex (13)).
以下の方法で式(11)で表される希土類錯体が生成していることを確認した。
元素分析 測定値 C53.01% H3.70% Yb11.4%
計算値 C53.48% H3.17% Yb11.3%
It was confirmed that the rare earth complex represented by the formula (11) was generated by the following method.
Elemental analysis Measured value C53.01% H3.70% Yb11.4%
Calculated C53.48% H3.17% Yb 11.3%
(実施例5)
実施例4において、式(12)で表される錯体に代えて、下記式(14)で表されるイッテルビウム−ベンゾイルトリフルオロアセトナート錯体を用いることで、下記式(15)で示される希土類錯体(S−Λ体;以下S−Λ希土類錯体(15)と言う。)を2.14部得た。
(Example 5)
In Example 4, the ytterbium-benzoyltrifluoroacetonate complex represented by the following formula (14) is used in place of the complex represented by the formula (12), whereby the rare earth complex represented by the following formula (15) is used. 2.14 parts of (S-Λ body; hereinafter referred to as S-Λ rare earth complex (15)) were obtained.
(実施例6)
実施例4において、式(12)で表される錯体に代えて、下記式(16)で表されるイッテルビウム−ナフトイルトリフルオロアセトナート錯体を用いることで、下記式(17)で示される希土類錯体(S−Λ体;以下S−Λ希土類錯体(17)と言う。)を1.88部得た。
(Example 6)
In Example 4, the ytterbium-naphthoyltrifluoroacetonate complex represented by the following formula (16) is used in place of the complex represented by the formula (12), whereby the rare earth represented by the following formula (17) is used. 1.88 parts of a complex (S-Λ form; hereinafter referred to as S-Λ rare earth complex (17)) was obtained.
(実施例7〜12)
実施例1〜6において(S)−BINAPOの代わりに(R)−BINAPOを用いることでそれぞれ、R−Δ希土類錯体(7)、(9)、(11)、(13)、(15)、(17)を得た。
(Examples 7 to 12)
In Examples 1 to 6, by using (R) -BINAPO instead of (S) -BINAPO, R-Δ rare earth complexes (7), (9), (11), (13), (15), (17) was obtained.
(比較例1)
特開2003−327590号公報に記載の方法に従って、(S)−BINAPOとイッテルビウム−ヘキサフルオロアセチルアセトナート錯体とから下記式(18)で表される希土類錯体(S−Λ体;以下S−Λ希土類錯体(18)と言う。)を得た。
(Comparative Example 1)
According to the method described in JP-A-2003-327590, a rare earth complex (S-Λ form; hereinafter referred to as S-Λ) represented by the following formula (18) from (S) -BINAPO and an ytterbium-hexafluoroacetylacetonate complex Rare earth complex (18) ”was obtained.
(評価例1)
(円偏光発光特性測定)
S−Λ希土類錯体(7)及びS−Λ希土類錯体(9)0.1部をアセトン1部に溶解し、日本分光(株)製CPL−200を用いて円偏光発光特性の測定を行った。g値は波長590nmの発光光でそれぞれ−0.04、−0.08であった。
(Evaluation example 1)
(Measurement of circularly polarized light emission characteristics)
0.1 parts of S-Λ rare earth complex (7) and S-Λ rare earth complex (9) were dissolved in 1 part of acetone, and circularly polarized light emission characteristics were measured using CPL-200 manufactured by JASCO Corporation. . The g values were -0.04 and -0.08 for emitted light having a wavelength of 590 nm, respectively.
(評価例2)
(発光評価)
本発明のS−Λ希土類錯体(7)とS−Λ希土類錯体(9)と比較化合物:トリス(3−トリフルオロアセチルカンフォラト)ユウロピウム(アルドリッチ社製)とを、それぞれ0.1部をアセトン5部に溶解した溶液を作製した。この溶液にブラックライトランプにより紫外光(約365nm)を照射した。本発明のS−Λ希土類錯体(7)及びS−Λ希土類錯体(9)の溶液については赤色に強く発光したが、トリス(3−トリフルオロアセチルカンフォラト)ユウロピウム溶液は非常に弱い発光しか観察されなかった。
(Evaluation example 2)
(Emission evaluation)
0.1 parts of each of S-Λ rare earth complex (7) and S-Λ rare earth complex (9) of the present invention and comparative compound: tris (3-trifluoroacetylcamphorato) europium (manufactured by Aldrich) A solution dissolved in 5 parts of acetone was prepared. This solution was irradiated with ultraviolet light (about 365 nm) by a black light lamp. The solution of the S-Λ rare earth complex (7) and the S-Λ rare earth complex (9) of the present invention emitted strong red light, whereas the tris (3-trifluoroacetylcamphorato) europium solution emitted very weak light. Not observed.
作製した溶液の蛍光発光強度を、日立製F−4000を用いて比較した。波長410nmで励起したときの発光強度を図1に示す。本発明の光学活性希土類錯体と比較化合物:トリス(3−トリフルオロアセチルカンフォラト)ユウロピウムとでは発光強度に大きな差が見られた。 The fluorescence emission intensities of the prepared solutions were compared using Hitachi F-4000. The emission intensity when excited at a wavelength of 410 nm is shown in FIG. There was a large difference in emission intensity between the optically active rare earth complex of the present invention and the comparative compound: tris (3-trifluoroacetylcamphorato) europium.
(評価例3)
評価例2と同様の方法で、本発明のS−Λ希土類錯体(13)と比較化合物:S−Λ希土類錯体(18)とを、それぞれ0.1部をアセトン5部に溶解した溶液を作製した。いずれも900nm以上の波長領域(赤外領域)で発光するため、該波長領域の測定に対応した、SPEX社 Fluorolog−3システムを用いて、前記溶液の蛍光発光強度を比較した。励起スペクトルが極大になる波長(本発明のS−Λ希土類錯体(13):405nm、S−Λ希土類錯体(18):366nm)で励起したときの発光強度を図2に示す。本発明の光学活性希土類錯体の方が、比較化合物:S−Λ希土類錯体(18)に比べて発光強度が大きかった。
(Evaluation example 3)
In the same manner as in Evaluation Example 2, a solution was prepared by dissolving 0.1 part of each of the S-Λ rare earth complex (13) of the present invention and the comparative compound: S-Λ rare earth complex (18) in 5 parts of acetone. did. Since both emitted light in a wavelength region of 900 nm or more (infrared region), the fluorescence emission intensities of the solutions were compared using a SPEX Fluorolog-3 system corresponding to the measurement of the wavelength region. FIG. 2 shows the emission intensity when excited with the wavelength at which the excitation spectrum becomes maximum (S-Λ rare earth complex (13) of the present invention: 405 nm, S-Λ rare earth complex (18): 366 nm). The optically active rare earth complex of the present invention had higher emission intensity than the comparative compound: S-Λ rare earth complex (18).
本発明の円偏光発光性を有する希土類錯体は、色純度が高く、発光強度が非常に大きく、発光した光を有効に利用できるため、発光性インクや有機エレクトロルミネッセンス素子に好適に利用される。 The rare earth complex having circularly polarized light emission property of the present invention has high color purity, very high emission intensity, and can effectively use emitted light, and thus is suitably used for light emitting inks and organic electroluminescence elements.
Claims (7)
(a)シクロペンタジエニル基(基中に存在する1個のCH2基はまた、−O−または−S−により置き換えられていてもよい)、
(b)フェニル基(基中に存在する1個または2個のCH基はまた、Nにより置き換えられていてもよい)、
(c)ナフチル基(基中に存在する1個または2個のCH基はまた、Nにより置き換えられていてもよい)、
からなる群から選ばれる基を表し、上記(a)、(b)及び(c)の基はアルキル基またはハロゲン原子で置換されていてもよく、Lnは希土類金属原子を表す。)で表される光学活性希土類錯体。 General formula (1)
(A) a cyclopentadienyl group (one CH 2 group present in the group may also be replaced by —O— or —S—),
(B) a phenyl group (one or two CH groups present in the group may also be replaced by N),
(C) a naphthyl group (one or two CH groups present in the group may also be replaced by N),
The group (a), (b) and (c) above may be substituted with an alkyl group or a halogen atom, and Ln represents a rare earth metal atom. An optically active rare earth complex represented by:
The optically active rare earth complex according to any one of claims 1 to 6, wherein the compound represented by the general formula (1) has an optical purity of 90% or more.
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