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Single crystals of disodium beryllodiborate have been obtained by spontaneous nucleation from a high-temperature melt. Na2[BeB2O5] adopts a new structure type and contains [BeB2O7]6− rings as building units that are made up from one BeO4 tetra­hedron and two BO3 triangles. These rings are further condensed and form {[BeB2O5]2−} two-dimensional layers extending parallel to the ab plane with the Na+ cations in a [6 + 1] coordination located between the layers. All atoms except Be and an O atom (both with site symmetry .2) are in general positions.

Supporting information

cif

Crystallographic Information File (CIF) https://doi.org/10.1107/S1600536807028942/wm2126sup1.cif
Contains datablocks global, I

hkl

Structure factor file (CIF format) https://doi.org/10.1107/S1600536807028942/wm2126Isup2.hkl
Contains datablock I

Key indicators

  • Single-crystal X-ray study
  • T = 293 K
  • Mean [sigma](O-B) = 0.001 Å
  • R factor = 0.022
  • wR factor = 0.059
  • Data-to-parameter ratio = 10.2

checkCIF/PLATON results

No syntax errors found



Alert level C PLAT062_ALERT_4_C Rescale T(min) & T(max) by ..................... 1.11
Alert level G ABSTM02_ALERT_3_G When printed, the submitted absorption T values will be replaced by the scaled T values. Since the ratio of scaled T's is identical to the ratio of reported T values, the scaling does not imply a change to the absorption corrections used in the study. Ratio of Tmax expected/reported 1.109 Tmax scaled 0.981 Tmin scaled 0.961 PLAT199_ALERT_1_G Check the Reported _cell_measurement_temperature 293 K PLAT200_ALERT_1_G Check the Reported _diffrn_ambient_temperature . 293 K
0 ALERT level A = In general: serious problem 0 ALERT level B = Potentially serious problem 1 ALERT level C = Check and explain 3 ALERT level G = General alerts; check 2 ALERT type 1 CIF construction/syntax error, inconsistent or missing data 0 ALERT type 2 Indicator that the structure model may be wrong or deficient 1 ALERT type 3 Indicator that the structure quality may be low 1 ALERT type 4 Improvement, methodology, query or suggestion 0 ALERT type 5 Informative message, check

Comment top

Borate crystals containing parallell aligned BO3 anions are predicted to have large nonlinear optical (NLO) coefficients, moderate birefringence and wide transparency in the UV region. Therefore they are considered to be good candidates for NLO applications (Chen et al., 1999). Based on a theoretical study, beryllium borates possess the largest energy gap among all alkaline and alkaline earth borates, and hence the shortest transmission cut-off wavelength (Li, 1989). Therefore, beryllium borates are studied intensively with the purpose of searching for new NLO materials in the UV region. The title compound, Na2[BeB2O5], (I), was found from the investigation of the pseudo-ternary system Na2O-BeO-B2O3.

A perspective view of the structure of (I) along the a direction is shown in Fig.1. The Be atoms are bonded to four O atoms to form slightly distorted BeO4 tetrahedra (site symmetry. 2). The Be—O bonds can be classified into two groups with different bond lengths of 1.6391 (14) Å for Be—O1 and 1.6584 (14) Å for Be—O2. The O—Be—O angles vary from 107.07 (12) to 111.37 (4)°, indicating a slight distortion from the ideal tetrahedron. The B atoms are coordinated to three O atoms to form planar BO3 triangles with a mean B—O bond length of 1.378 Å (Table 1) and O—B—O angles ranging from 116.70 (11) to 123.15 (11)°, which is in good agreement with the results of geometric studies for the triangular BO3 group (Zobetz, 1982). Two BO3 groups, slightly tilted against each other, share one O3 atom, and each of them also share a different O1 atom with a BeO4 tetrahedron to form a six-membered [BeB2O7]6- ring (Fig. 2). These [BeB2O7]6- rings are further condensed, resulting in a [BeB2O5]2- layer parallel to the ab plane. Between adjacent [BeB2O5]2- layers the Na+ cations are located in a [6 + 1] coordination, with one considerably longer Na—O bond of 2.8197 (10) Å (Table 1).

The conformation of the [BeB2O7]6- rings is similar to that of the [B3O7]5- units in LiB3O5 (LBO) (Chen et al., 2005), with the BO4 tetrahedron replaced by a BeO4 tetrahedron. From the study of LBO, it is known that the [B3O7]5- group can yield large NLO effects and short UV transmission cut-offs, but the spatial arrangement of the helical [B3O5] chains along the c axis is unfavorable for the generation of a large birefringence. Therefore, compounds with a [BeB2O5] layer structure may be good candidates for deep UV NLO applications. Unfortunately, in the case of (I), the direction of the [BeB2O7]6- groups in the two adjacent layers are completely opposite, and thus their contributions to the NLO effect are eliminated.

Related literature top

Nonlinear optical (NLO) applications of borate crystals with trigonal BO3 anions have been discussed by Chen et al. (1999). Among this group of compounds, beryllium borates are reported to exhibit the shortest transmission cut-off wavelength (Li, 1989). A review of the geometry of the BO3 group is given by Zobetz (1982), and a similar configuration of the [BeB2O7]6- unit is found in LiB3O5 (LBO) (Chen et al., 2005), where [B3O7]5- rings are present.

Experimental top

Single crystals of compound (I) were grown using a Na4B2O5 flux. The composition of the mixture for crystal growth was 2:1:3 of Na2CO3 (Hongguang Materials, 99.8%), BeO (Shuikoushan Materials, 99.8%), and H3BO3 (Jinghua Materials, 95%). This mixture was heated in a Pt crucible to 1073 K, held at this temperature for several hours, and then cooled at a rate of 3 K h-1 from 1073 to 873 K. The remaining solified flux attached to the crystals was readily dissolved in water. Crystals with an average size of 0.5 mm and mostly block-shaped habit were obtained.

Structure description top

Borate crystals containing parallell aligned BO3 anions are predicted to have large nonlinear optical (NLO) coefficients, moderate birefringence and wide transparency in the UV region. Therefore they are considered to be good candidates for NLO applications (Chen et al., 1999). Based on a theoretical study, beryllium borates possess the largest energy gap among all alkaline and alkaline earth borates, and hence the shortest transmission cut-off wavelength (Li, 1989). Therefore, beryllium borates are studied intensively with the purpose of searching for new NLO materials in the UV region. The title compound, Na2[BeB2O5], (I), was found from the investigation of the pseudo-ternary system Na2O-BeO-B2O3.

A perspective view of the structure of (I) along the a direction is shown in Fig.1. The Be atoms are bonded to four O atoms to form slightly distorted BeO4 tetrahedra (site symmetry. 2). The Be—O bonds can be classified into two groups with different bond lengths of 1.6391 (14) Å for Be—O1 and 1.6584 (14) Å for Be—O2. The O—Be—O angles vary from 107.07 (12) to 111.37 (4)°, indicating a slight distortion from the ideal tetrahedron. The B atoms are coordinated to three O atoms to form planar BO3 triangles with a mean B—O bond length of 1.378 Å (Table 1) and O—B—O angles ranging from 116.70 (11) to 123.15 (11)°, which is in good agreement with the results of geometric studies for the triangular BO3 group (Zobetz, 1982). Two BO3 groups, slightly tilted against each other, share one O3 atom, and each of them also share a different O1 atom with a BeO4 tetrahedron to form a six-membered [BeB2O7]6- ring (Fig. 2). These [BeB2O7]6- rings are further condensed, resulting in a [BeB2O5]2- layer parallel to the ab plane. Between adjacent [BeB2O5]2- layers the Na+ cations are located in a [6 + 1] coordination, with one considerably longer Na—O bond of 2.8197 (10) Å (Table 1).

The conformation of the [BeB2O7]6- rings is similar to that of the [B3O7]5- units in LiB3O5 (LBO) (Chen et al., 2005), with the BO4 tetrahedron replaced by a BeO4 tetrahedron. From the study of LBO, it is known that the [B3O7]5- group can yield large NLO effects and short UV transmission cut-offs, but the spatial arrangement of the helical [B3O5] chains along the c axis is unfavorable for the generation of a large birefringence. Therefore, compounds with a [BeB2O5] layer structure may be good candidates for deep UV NLO applications. Unfortunately, in the case of (I), the direction of the [BeB2O7]6- groups in the two adjacent layers are completely opposite, and thus their contributions to the NLO effect are eliminated.

Nonlinear optical (NLO) applications of borate crystals with trigonal BO3 anions have been discussed by Chen et al. (1999). Among this group of compounds, beryllium borates are reported to exhibit the shortest transmission cut-off wavelength (Li, 1989). A review of the geometry of the BO3 group is given by Zobetz (1982), and a similar configuration of the [BeB2O7]6- unit is found in LiB3O5 (LBO) (Chen et al., 2005), where [B3O7]5- rings are present.

Computing details top

Data collection: CrystalClear (Rigaku, 2000); cell refinement: CrystalClear; data reduction: CrystalClear; program(s) used to solve structure: SHELXS97 (Sheldrick, 1997); program(s) used to refine structure: SHELXL97 (Sheldrick, 1997); molecular graphics: DIAMOND (Brandenburg, 2004); software used to prepare material for publication: enCIFer (Allen et al., 2004).

Figures top
[Figure 1] Fig. 1. The structure of (I) in a projection approximately along the a axis with anisotropic displacement ellispoids drawn at the 60% probability level. Na—O bonds were omitted for clarity.
[Figure 2] Fig. 2. [BeB2O7](6-) building unit in compound (I).
disodium beryllodiborate top
Crystal data top
Na2[BeB2O5]F(000) = 304
Mr = 156.61Dx = 2.475 Mg m3
Monoclinic, C2/cMo Kα radiation, λ = 0.71073 Å
Hall symbol: -C 2ycCell parameters from 616 reflections
a = 5.8117 (5) Åθ = 2.3–27.5°
b = 8.1666 (7) ŵ = 0.39 mm1
c = 8.9830 (8) ÅT = 293 K
β = 99.665 (14)°Prism, colourless
V = 420.30 (7) Å30.12 × 0.10 × 0.05 mm
Z = 4
Data collection top
Rigaku Mercury CCD
diffractometer
489 independent reflections
Radiation source: Sealed Tube450 reflections with I > 2σ(I)
Graphite Monochromator monochromatorRint = 0.014
Detector resolution: 14.6306 pixels mm-1θmax = 27.5°, θmin = 4.4°
CCD_Profile_fitting scansh = 77
Absorption correction: multi-scan
(CrystalClear; Rigaku, 2000)
k = 910
Tmin = 0.866, Tmax = 0.884l = 1011
1621 measured reflections
Refinement top
Refinement on F20 restraints
Least-squares matrix: fullPrimary atom site location: structure-invariant direct methods
R[F2 > 2σ(F2)] = 0.022Secondary atom site location: difference Fourier map
wR(F2) = 0.059 w = 1/[σ2(Fo2) + (0.0287P)2 + 0.2765P]
where P = (Fo2 + 2Fc2)/3
S = 1.17(Δ/σ)max < 0.001
489 reflectionsΔρmax = 0.22 e Å3
48 parametersΔρmin = 0.18 e Å3
Crystal data top
Na2[BeB2O5]V = 420.30 (7) Å3
Mr = 156.61Z = 4
Monoclinic, C2/cMo Kα radiation
a = 5.8117 (5) ŵ = 0.39 mm1
b = 8.1666 (7) ÅT = 293 K
c = 8.9830 (8) Å0.12 × 0.10 × 0.05 mm
β = 99.665 (14)°
Data collection top
Rigaku Mercury CCD
diffractometer
489 independent reflections
Absorption correction: multi-scan
(CrystalClear; Rigaku, 2000)
450 reflections with I > 2σ(I)
Tmin = 0.866, Tmax = 0.884Rint = 0.014
1621 measured reflections
Refinement top
R[F2 > 2σ(F2)] = 0.02248 parameters
wR(F2) = 0.0590 restraints
S = 1.17Δρmax = 0.22 e Å3
489 reflectionsΔρmin = 0.18 e Å3
Special details top

Geometry. All e.s.d.'s (except the e.s.d. in the dihedral angle between two l.s. planes) are estimated using the full covariance matrix. The cell e.s.d.'s are taken into account individually in the estimation of e.s.d.'s in distances, angles and torsion angles; correlations between e.s.d.'s in cell parameters are only used when they are defined by crystal symmetry. An approximate (isotropic) treatment of cell e.s.d.'s is used for estimating e.s.d.'s involving l.s. planes.

Refinement. Refinement of F2 against ALL reflections. The weighted R-factor wR and goodness of fit S are based on F2, conventional R-factors R are based on F, with F set to zero for negative F2. The threshold expression of F2 > σ(F2) is used only for calculating R-factors(gt) etc. and is not relevant to the choice of reflections for refinement. R-factors based on F2 are statistically about twice as large as those based on F, and R- factors based on ALL data will be even larger.

Fractional atomic coordinates and isotropic or equivalent isotropic displacement parameters (Å2) top
xyzUiso*/Ueq
Na0.01389 (8)0.30641 (6)0.42612 (6)0.0142 (2)
O10.34432 (14)0.32884 (10)0.15850 (10)0.0113 (2)
O20.16865 (14)0.58926 (10)0.37065 (10)0.0108 (2)
O300.07376 (14)0.250.0140 (3)
B0.3344 (2)0.49318 (16)0.17748 (15)0.0087 (3)
Be0.50.2100 (2)0.250.0087 (4)
Atomic displacement parameters (Å2) top
U11U22U33U12U13U23
Na0.0145 (3)0.0145 (3)0.0150 (3)0.00079 (18)0.0065 (2)0.00110 (18)
O10.0127 (4)0.0078 (4)0.0154 (4)0.0005 (3)0.0082 (3)0.0002 (3)
O20.0109 (4)0.0099 (4)0.0124 (4)0.0028 (3)0.0046 (3)0.0008 (3)
O30.0135 (6)0.0073 (6)0.0243 (7)00.0120 (5)0
B0.0074 (6)0.0097 (6)0.0087 (6)0.0003 (4)0.0008 (5)0.0010 (5)
Be0.0090 (9)0.0064 (9)0.0115 (10)00.0043 (8)0
Geometric parameters (Å, º) top
Na—O2i2.3279 (10)O2—Nai2.3279 (10)
Na—O1ii2.3402 (9)O2—Naviii2.5473 (9)
Na—O1iii2.4203 (10)O3—Bv1.4123 (14)
Na—O32.4824 (10)O3—Bix1.4123 (14)
Na—O2iv2.5473 (9)O3—Naii2.4824 (10)
Na—O22.6243 (9)B—O11.3529 (15)
Na—Bv2.8128 (14)B—O2ii1.3675 (15)
Na—Bii2.8145 (14)B—O3x1.4123 (14)
Na—O12.8197 (10)B—Naxi2.8128 (14)
Na—Bevi2.9000 (6)B—Naii2.8145 (14)
Na—B3.0639 (13)Be—O1xii1.6391 (14)
Na—Be3.0991 (7)Be—O2v1.6584 (14)
O1—Be1.6391 (14)Be—O2iv1.6584 (14)
O1—Naii2.3402 (9)Be—Navi2.9000 (6)
O1—Navii2.4203 (10)Be—Navii2.9000 (6)
O2—Bii1.3675 (15)Be—Naxii3.0991 (7)
O2—Beviii1.6584 (14)
O2i—Na—O1ii135.07 (4)Be—O1—Na83.58 (4)
O2i—Na—O1iii69.25 (3)Naii—O1—Na75.89 (3)
O1ii—Na—O1iii93.45 (3)Navii—O1—Na145.70 (4)
O2i—Na—O3146.94 (3)Bii—O2—Beviii120.32 (8)
O1ii—Na—O374.16 (3)Bii—O2—Nai147.49 (8)
O1iii—Na—O398.53 (3)Beviii—O2—Nai91.79 (4)
O2i—Na—O2iv92.62 (3)Bii—O2—Naviii86.32 (7)
O1ii—Na—O2iv130.21 (3)Beviii—O2—Naviii92.48 (6)
O1iii—Na—O2iv91.58 (3)Nai—O2—Naviii87.38 (3)
O3—Na—O2iv56.11 (2)Bii—O2—Na83.32 (7)
O2i—Na—O292.78 (3)Beviii—O2—Na115.71 (6)
O1ii—Na—O257.28 (3)Nai—O2—Na87.22 (3)
O1iii—Na—O2116.52 (3)Naviii—O2—Na151.43 (4)
O3—Na—O2119.69 (3)Bv—O3—Bix124.46 (14)
O2iv—Na—O2151.43 (4)Bv—O3—Na88.00 (6)
O2i—Na—O1110.32 (3)Bix—O3—Na138.43 (6)
O1ii—Na—O1103.51 (3)Bv—O3—Naii138.43 (6)
O1iii—Na—O1152.30 (3)Bix—O3—Naii88.00 (6)
O3—Na—O166.22 (2)Na—O3—Naii80.12 (4)
O2iv—Na—O160.74 (3)O1—B—O2ii123.15 (11)
O2—Na—O191.15 (3)O1—B—O3x120.16 (11)
B—O1—Be122.68 (10)O2ii—B—O3x116.70 (11)
B—O1—Naii95.57 (7)O1—Be—O1xii107.35 (12)
Be—O1—Naii135.44 (7)O1—Be—O2v109.86 (4)
B—O1—Navii124.34 (7)O1xii—Be—O2v111.37 (4)
Be—O1—Navii89.03 (5)O1—Be—O2iv111.37 (4)
Naii—O1—Navii86.55 (3)O1xii—Be—O2iv109.86 (4)
B—O1—Na87.04 (7)O2v—Be—O2iv107.07 (12)
Symmetry codes: (i) x, y+1, z+1; (ii) x, y, z+1/2; (iii) x+1/2, y+1/2, z+1/2; (iv) x1/2, y1/2, z; (v) x1/2, y1/2, z+1/2; (vi) x1/2, y+1/2, z+1; (vii) x1/2, y+1/2, z1/2; (viii) x+1/2, y+1/2, z; (ix) x+1/2, y1/2, z; (x) x1/2, y+1/2, z; (xi) x1/2, y+1/2, z+1/2; (xii) x1, y, z+1/2.

Experimental details

Crystal data
Chemical formulaNa2[BeB2O5]
Mr156.61
Crystal system, space groupMonoclinic, C2/c
Temperature (K)293
a, b, c (Å)5.8117 (5), 8.1666 (7), 8.9830 (8)
β (°) 99.665 (14)
V3)420.30 (7)
Z4
Radiation typeMo Kα
µ (mm1)0.39
Crystal size (mm)0.12 × 0.10 × 0.05
Data collection
DiffractometerRigaku Mercury CCD
Absorption correctionMulti-scan
(CrystalClear; Rigaku, 2000)
Tmin, Tmax0.866, 0.884
No. of measured, independent and
observed [I > 2σ(I)] reflections
1621, 489, 450
Rint0.014
(sin θ/λ)max1)0.649
Refinement
R[F2 > 2σ(F2)], wR(F2), S 0.022, 0.059, 1.17
No. of reflections489
No. of parameters48
Δρmax, Δρmin (e Å3)0.22, 0.18

Computer programs: CrystalClear (Rigaku, 2000), CrystalClear, SHELXS97 (Sheldrick, 1997), SHELXL97 (Sheldrick, 1997), DIAMOND (Brandenburg, 2004), enCIFer (Allen et al., 2004).

Selected geometric parameters (Å, º) top
Na—O2i2.3279 (10)Na—O12.8197 (10)
Na—O1ii2.3402 (9)B—O11.3529 (15)
Na—O1iii2.4203 (10)B—O2ii1.3675 (15)
Na—O32.4824 (10)B—O3v1.4123 (14)
Na—O2iv2.5473 (9)Be—O1vi1.6391 (14)
Na—O22.6243 (9)Be—O2vii1.6584 (14)
O1—B—O2ii123.15 (11)O1—Be—O2vii109.86 (4)
O1—B—O3v120.16 (11)O1—Be—O2iv111.37 (4)
O2ii—B—O3v116.70 (11)O2vii—Be—O2iv107.07 (12)
O1—Be—O1vi107.35 (12)
Symmetry codes: (i) x, y+1, z+1; (ii) x, y, z+1/2; (iii) x+1/2, y+1/2, z+1/2; (iv) x1/2, y1/2, z; (v) x1/2, y+1/2, z; (vi) x1, y, z+1/2; (vii) x1/2, y1/2, z+1/2.
 

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