organic papers
o1972
Rolf Stomberget al. C20H22O6C4H8O2 DOI: 10.1107/S1600536803026114 Acta Cryst.(2003). E59, o1972±o1974 Acta Crystallographica Section EStructure Reports
Online ISSN 1600-5368
(+)-Pinoresinol±dioxane (1/1)
Rolf Stomberg,aWilson
Ibrahim,bVratislav Langerc* and
Knut Lundquistd
aDepartment of Chemistry, Division of Inorganic
Chemistry, GoÈteborg University, SE-412 96 GoÈteborg, Sweden,bDepartment of Organic Chemistry, Chalmers University of Technology, SE-412 96 GoÈteborg, Sweden,cDepartment of Environmental Inorganic Chemistry, Chalmers University of Technology, SE-412 96 GoÈteborg, Sweden, anddDepartment of Forest Products and Chemical Engineering, Chalmers University of Technology, SE-41296 GoÈteborg, Sweden
Correspondence e-mail: [email protected]
Key indicators
Single-crystal X-ray study T= 153 K
Mean(C±C) = 0.003 AÊ Rfactor = 0.041 wRfactor = 0.121
Data-to-parameter ratio = 11.2
For details of how these key indicators were automatically derived from the article, see http://journals.iucr.org/e.
#2003 International Union of Crystallography Printed in Great Britain ± all rights reserved
The crystal structure of a dioxane solvate of (+)-pinoresinol, C20H22O6C4H8O2, has been determined. The solvate is
stabilized by hydrogen bonding between the pinoresinol and dioxane molecules. The ®ve-membered rings in the central dioxabicyclooctane ring system of the pinoresinol molecules adopt envelope conformations, with the benzylic C atoms as ¯aps.
Comment
(+)-Pinoresinol, (Ia), was originally isolated from softwood species (Erdtman, 1955) but was later found to be a widely distributed constituent of plant extractives. Its absolute con®guration was determined by Freudenberg & Sidhu (1961). We have reported crystal structures of (Ia) (Lundquist & Stomberg, 1988) and the racemic form of pinoresinol (Stomberget al., 2001). A procedure for the isolation of (+)-pinoresinol from resinous exudates of softwood species has been described by Erdtman (1955). Gripenberg & Petrell (1960) found that crude (+)-pinoresinol obtained according to Erdtman (1955) could be conveniently puri®ed via the dioxane solvate. We report here the crystal structure of a dioxane solvate of (+)-pinoresinol, (I). The solvate crystallizes from solutions of (+)-pinoresinol in dioxane.
A perspective drawing of the molecules in (I) and the atomic numbering are shown in Fig. 1. There are OÐH O and CÐH O hydrogen bonds in the crystal structure of (I) (Table 1); the network of hydrogen bonds is shown in Fig. 2. On the ®rst-level graph-set (Bernsteinet al., 1995; Grellet al., 1999), the hydrogen bonds denoted as [a] and [c] (see Table 1) are intramolecular bonds of typeS(5). Hydrogen bonds [b], [d], [f] and [g] form interactions of type D(2) between the pinoresinol and dioxane molecules, and hydrogen bond [e] forms aC(8) chain. On the second-level graph-set, a number of hydrogen-bond patterns were recognized, the most impor-tant of which areC2
2(20) chains formed by hydrogen bonds [b]
and [d] in theacplane, andC2
2(18) chains formed by hydrogen
bonds [f] and [g] in theadirection. Two rings are also apparent
in Fig. 2,viz. oneR2
2(17) ring, formed by bonds of type [e], and
oneR3
3(10) ring, formed by bonds of types [e], [d] and [f]. The
assignment of graph-set descriptors was performed using
PLUTO, as described by Motherwellet al.(1999).
We have compared the conformation of the pinoresinol molecule in the crystal structure of pinoresinol±dioxane (1/1) with those of the pinoresinol molecules in the crystal struc-tures of (Ia) (Lundquist & Stomberg, 1988) and the racemic form of pinoresinol (Stomberget al., 2001). To describe the conformation of the ®ve-membered rings in the central
di-oxabicyclooctane ring system we have used the program
PLATON(Spek, 2002). In (I), the ®ve-membered rings in this
ring system adopt envelope conformations, with the benzylic C atoms as ¯aps (Fig. 1). The conformation of the pinoresinol molecules in the solvate is similar to that of the pinoresinol molecules in the racemate (Stomberget al., 2001). The mol-ecules in the crystal structure of (Ia) also adopt envelope conformations, but in this case, the O atoms constitute the ¯aps. Furthermore, the ¯aps point in the same direction in the solvate (Fig. 1) and the racemate, while they point in different directions in (Ia).
Experimental
(+)-Pinoresinol, (Ia), was obtained from a resinous exudate of spruce according to the procedure described by Gripenberg & Petrell (1960). Solutions of (Ia) in a small amount of dioxane gave crystals of the solvate (I) on standing at room temperature.
Crystal data
C20H22O6C4H8O2
Mr= 446.48
Monoclinic,P21
a= 9.8318 (16) AÊ
b= 6.066 (3) AÊ
c= 18.493 (2) AÊ
= 92.891 (13)
V= 1101.5 (6) AÊ3
Z= 2
Dx= 1.346 Mg mÿ3
MoKradiation Cell parameters from 25
re¯ections
= 23.4±24.9
= 0.10 mmÿ1
T= 153 (1) K Block, colourless 0.550.350.35 mm
Data collection
Rigaku AFC-6 diffractometer
!scans
3660 measured re¯ections 3479 independent re¯ections 2765 re¯ections withI> 2(I)
Rint= 0.013
max= 30.0
h= 0!13
k= 0!8
l=ÿ25!25 3 standard re¯ections
every 150 re¯ections intensity decay: none
Re®nement
Re®nement onF2
R[F2> 2(F2)] = 0.041
wR(F2) = 0.121
S= 1.04 3479 re¯ections 311 parameters
H-atom parameters constrained
w= 1/[2(F
o2) + (0.0679P)2
+ 0.1302P]
whereP= (Fo2+ 2Fc2)/3
(/)max< 0.001
max= 0.33 e AÊÿ3
min=ÿ0.22 e AÊÿ3
Table 1
Hydrogen-bonding geometry (AÊ,).
DÐH A DÐH H A D A DÐH A
[a] O2ÐH2A O1 0.82 2.24 2.671 (3) 113 [b] O2ÐH2A O8i 0.82 1.98 2.718 (2) 149 [c] O6ÐH6A O5 0.82 2.22 2.663 (3) 114 [d] O6ÐH6A O7 0.82 2.00 2.710 (2) 145 [e] C19ÐH19 O6ii 0.98 2.37 3.221 (3) 145 [f] C23ÐH23A O3ii 0.97 2.55 3.465 (3) 158 [g] C23ÐH23B O4iii 0.97 2.56 3.480 (3) 158
Symmetry codes: (i)xÿ1;y;1z; (ii) 2ÿx;1
2y;ÿz; (iii) 3ÿx;12y;ÿz.
H atoms were re®ned isotropically and were constrained to an ideal geometry using an appropriate riding model. For OH groups, the OÐH distances (0.82 AÊ) and CÐOÐH angles (109.5) were
®xed, while the torsion angles were allowed to re®ne, with the starting position based on the circular Fourier synthesis. For methyl groups, the CÐH distances (0.96 AÊ) and CÐCÐH angles (109.5) were kept
Acta Cryst.(2003). E59, o1972±o1974 Rolf Stomberget al. C20H22O6C4H8O2
o1973
organic papers
Figure 1
A perspective drawing of the title compound, showing the atom-numbering scheme. Displacement ellipsoids are shown at the 50% probability level.
Figure 2
organic papers
o1974
Rolf Stomberget al. C20H22O6C4H8O2 Acta Cryst.(2003). E59, o1972±o1974®xed, while the torsion angles were allowed to re®ne with the starting position based on a threefold averaged circular Fourier synthesis. For aromatic H atoms, the CÐH distance was ®xed at 0.93 AÊ and for tertiary H atoms at 0.98 AÊ. For secondary H atoms, the CÐH distance was ®xed to 0.97 AÊ, withUiso(H) = 1.2Ueq(C).
Data collection: TEXRAY (Molecular Structure Corporation, 1985); cell re®nement: TEXRAY; data reduction: TEXRAY; program(s) used to solve structure: SHELXTL (Bruker, 1997); program(s) used to re®ne structure:SHELXTL; molecular graphics: DIAMOND(Brandenburg, 2000); software used to prepare material for publication:SHELXTL.
References
Bernstein, J., Davis, R. E., Shimoni, L. & Chang, N.-L. (1995).Angew. Chem. Int. Ed. Engl.34, 1555±1573.
Brandenburg, K. (2000). DIAMOND. Version 2.1d. Crystal Impact GbR, Bonn, Germany.
Bruker (1997). SHELXTL. Version 5.10. Bruker AXS Inc., Madison, Wisconsin, USA.
Erdtman, H. (1955). Lignans, inModern Methods of Plant Analysis, edited by K. Paech & M. V. Tracey, Vol. III, pp. 428±449. Berlin±GoÈttingen± Heidelberg: Springer±Verlag.
Freudenberg, K. & Sidhu, G. S. (1961).Chem. Ber.94, 851±862. Grell, J., Bernstein, J. & Tinhofer, G. (1999).Acta Cryst.B55, 1030±1043. Gripenberg, J. & Petrell, I. (1960).Acta Chem. Scand.14, 226.
Lundquist, K. & Stomberg, R. (1988).Holzforschung,42, 375±384. Molecular Structure Corporation (1985). TEXSAN. TEXRAY Structure
Analysis Package.MSC, 3200 Research Forest Drive, The Woodlands, TX 77381, USA.
Motherwell, W. D. S., Shields, G. P. & Allen, F. H. (1999).Acta Cryst.B55, 1044±1056.
Spek, A. L.(2002).PLATON.Utrecht University, The Netherlands. Stomberg, R., Langer, V., Li, S. & Lundquist K. (2001).Acta Cryst.E57, o692±
supporting information
sup-1 Acta Cryst. (2003). E59, o1972–o1974
supporting information
Acta Cryst. (2003). E59, o1972–o1974 [https://doi.org/10.1107/S1600536803026114]
(+)-Pinoresinol
–
dioxane (1/1)
Rolf Stomberg, Wilson Ibrahim, Vratislav Langer and Knut Lundquist
(+)-pinoresinol–dioxane (1/1)
Crystal data
C20H22O6·C4H8O2
Mr = 446.48
Monoclinic, P21
Hall symbol: P 2yb
a = 9.8318 (16) Å
b = 6.066 (3) Å
c = 18.493 (2) Å
β = 92.891 (13)°
V = 1101.5 (6) Å3
Z = 2
F(000) = 476
Dx = 1.346 Mg m−3
Mo Kα radiation, λ = 0.71069 Å Cell parameters from 25 reflections
θ = 23.4–24.9°
µ = 0.10 mm−1
T = 153 K Plate, colourless 0.55 × 0.35 × 0.35 mm
Data collection
Rigaku AFC6 diffractometer
Radiation source: normal-focus rotating anode Graphite monochromator
ω scans
3660 measured reflections 3479 independent reflections 2765 reflections with I > 2σI
Rint = 0.013
θmax = 30.0°, θmin = 2.1°
h = 0→13
k = 0→8
l = −25→25
3 standard reflections every 150 reflections intensity decay: none
Refinement
Refinement on F2
Least-squares matrix: full
R[F2 > 2σ(F2)] = 0.041
wR(F2) = 0.121
S = 1.04 3479 reflections 311 parameters 1 restraint
Primary atom site location: structure-invariant direct methods
Secondary atom site location: difference Fourier map
Hydrogen site location: inferred from neighbouring sites
H-atom parameters constrained
w = 1/[σ2(F
o2) + (0.0679P)2 + 0.1302P]
where P = (Fo2 + 2Fc2)/3
(Δ/σ)max < 0.001
Δρmax = 0.33 e Å−3
Δρmin = −0.22 e Å−3
Special details
Experimental. Data were collected at low temperature using a Rigaku AFC6R diffractometer equiped with a low temperature device. The data were collected using ω-scan. Scans of (1.22 + 0.30tanθ) were made at a speed of 8.0ο/min. The weak reflections (I<10.0σI) were rescanned (maximum 3 rescans) and the counts were accumulated to assure good
supporting information
sup-2 Acta Cryst. (2003). E59, o1972–o1974
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)
x y z Uiso*/Ueq
C1 0.86723 (18) 0.7651 (4) 0.39457 (10) 0.0237 (4)
C2 0.78063 (19) 0.6263 (4) 0.43133 (10) 0.0248 (4)
H2 0.7484 0.4974 0.4093 0.042 (8)*
C3 0.74239 (18) 0.6788 (4) 0.50015 (10) 0.0228 (4)
C4 0.79078 (19) 0.8737 (4) 0.53375 (10) 0.0245 (4)
C5 0.8747 (2) 1.0127 (4) 0.49705 (11) 0.0273 (4)
H5 0.9060 1.1427 0.5188 0.043 (8)*
C6 0.91258 (19) 0.9590 (4) 0.42766 (11) 0.0262 (4)
H6 0.9688 1.0539 0.4033 0.042 (8)*
C7 0.5873 (2) 0.3774 (4) 0.50649 (13) 0.0316 (5)
H7A 0.5392 0.4286 0.4632 0.036 (7)*
H7B 0.5237 0.3164 0.5387 0.052 (9)*
H7C 0.6516 0.2661 0.4942 0.044 (8)*
C8 0.91926 (19) 0.6906 (4) 0.32359 (10) 0.0255 (4)
H8 0.9848 0.5711 0.3331 0.038 (7)*
C9 0.9850 (2) 0.8631 (4) 0.27647 (10) 0.0263 (4)
H9 0.9351 1.0029 0.2765 0.029 (7)*
C10 1.1386 (2) 0.8986 (5) 0.29093 (11) 0.0335 (5)
H10A 1.1580 1.0537 0.2991 0.040*
H10B 1.1708 0.8164 0.3334 0.040*
C11 1.15336 (18) 0.6312 (4) 0.11523 (10) 0.0254 (4)
C12 1.23149 (19) 0.7870 (4) 0.08078 (10) 0.0261 (4)
H12 1.2661 0.9084 0.1063 0.046 (8)*
C13 1.25762 (19) 0.7606 (4) 0.00794 (10) 0.0250 (4)
C14 1.20537 (19) 0.5794 (4) −0.03067 (10) 0.0276 (4)
C15 1.1261 (2) 0.4272 (4) 0.00362 (11) 0.0311 (5)
H15 1.0891 0.3081 −0.0222 0.039 (8)*
C16 1.1013 (2) 0.4517 (4) 0.07677 (11) 0.0293 (4)
H16 1.0495 0.3471 0.0998 0.034 (7)*
C17 1.4086 (2) 1.0689 (4) 0.00630 (13) 0.0339 (5)
H17A 1.3457 1.1710 0.0260 0.045 (8)*
H17B 1.4651 1.1451 −0.0264 0.051 (9)*
H17C 1.4646 1.0053 0.0449 0.048 (8)*
C18 1.11777 (19) 0.6620 (4) 0.19303 (10) 0.0262 (4)
H18 1.1279 0.5212 0.2187 0.039 (7)*
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sup-3 Acta Cryst. (2003). E59, o1972–o1974
H19 0.9491 0.8590 0.1635 0.033 (7)*
C20 0.8610 (2) 0.5794 (6) 0.20753 (11) 0.0430 (7)
H20A 0.7896 0.6026 0.1702 0.052*
H20B 0.8975 0.4321 0.2022 0.052*
C21 1.4511 (3) 0.5275 (5) −0.23373 (13) 0.0390 (6)
H21A 1.3798 0.4182 −0.2299 0.047*
H21B 1.5376 0.4575 −0.2206 0.047*
C22 1.4521 (3) 0.6092 (6) −0.30944 (13) 0.0560 (9)
H22A 1.4701 0.4875 −0.3416 0.067*
H22B 1.3633 0.6694 −0.3237 0.067*
C23 1.5316 (2) 0.9530 (5) −0.26788 (13) 0.0366 (5)
H23A 1.4453 1.0235 −0.2811 0.044*
H23B 1.6033 1.0617 −0.2715 0.044*
C24 1.5301 (3) 0.8708 (6) −0.19247 (13) 0.0517 (8)
H24A 1.6188 0.8103 −0.1782 0.062*
H24B 1.5124 0.9927 −0.1603 0.062*
O1 0.65778 (15) 0.5576 (3) 0.54108 (7) 0.0295 (3)
O2 0.75570 (17) 0.9280 (3) 0.60194 (8) 0.0353 (4)
H2A 0.6918 0.8507 0.6134 0.051 (9)*
O3 0.80826 (15) 0.6066 (4) 0.27825 (8) 0.0402 (5)
O4 1.20418 (14) 0.8221 (4) 0.22813 (7) 0.0348 (4)
O5 1.33514 (16) 0.8991 (3) −0.03163 (8) 0.0326 (4)
O6 1.23224 (18) 0.5481 (4) −0.10141 (8) 0.0416 (5)
H6A 1.2894 0.6379 −0.1133 0.060 (10)*
O7 1.42862 (19) 0.7052 (4) −0.18529 (9) 0.0434 (5)
O8 1.5538 (2) 0.7757 (4) −0.31618 (9) 0.0467 (5)
Atomic displacement parameters (Å2)
U11 U22 U33 U12 U13 U23
C1 0.0198 (7) 0.0274 (10) 0.0239 (8) −0.0003 (8) 0.0016 (6) −0.0013 (8)
C2 0.0229 (8) 0.0262 (10) 0.0253 (8) −0.0019 (8) 0.0010 (7) −0.0011 (8)
C3 0.0199 (8) 0.0233 (9) 0.0253 (8) −0.0033 (8) 0.0019 (6) 0.0011 (8)
C4 0.0225 (8) 0.0279 (10) 0.0230 (8) −0.0008 (8) 0.0005 (7) −0.0014 (8)
C5 0.0260 (9) 0.0268 (10) 0.0291 (9) −0.0053 (9) 0.0022 (7) −0.0030 (9)
C6 0.0218 (8) 0.0301 (11) 0.0269 (9) −0.0045 (8) 0.0034 (7) 0.0024 (8)
C7 0.0295 (10) 0.0225 (10) 0.0435 (12) −0.0056 (9) 0.0079 (9) −0.0025 (9)
C8 0.0216 (8) 0.0303 (10) 0.0247 (8) −0.0028 (8) 0.0025 (6) −0.0043 (8)
C9 0.0258 (9) 0.0314 (11) 0.0217 (8) −0.0006 (8) 0.0024 (7) 0.0001 (8)
C10 0.0300 (10) 0.0448 (14) 0.0260 (9) −0.0095 (10) 0.0048 (7) −0.0041 (10)
C11 0.0194 (8) 0.0326 (11) 0.0244 (8) 0.0010 (8) 0.0022 (6) 0.0006 (8)
C12 0.0231 (8) 0.0283 (10) 0.0270 (8) −0.0015 (8) 0.0017 (7) −0.0029 (9)
C13 0.0205 (8) 0.0285 (10) 0.0262 (8) −0.0014 (8) 0.0024 (6) 0.0012 (8)
C14 0.0232 (8) 0.0359 (12) 0.0241 (8) −0.0034 (9) 0.0035 (7) −0.0021 (9)
C15 0.0275 (9) 0.0345 (12) 0.0315 (10) −0.0094 (10) 0.0029 (8) −0.0066 (10)
C16 0.0256 (9) 0.0322 (11) 0.0305 (10) −0.0063 (9) 0.0058 (7) 0.0001 (9)
C17 0.0349 (10) 0.0250 (11) 0.0424 (11) −0.0069 (9) 0.0085 (9) −0.0043 (10)
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sup-4 Acta Cryst. (2003). E59, o1972–o1974
C19 0.0216 (8) 0.0416 (13) 0.0215 (8) 0.0014 (9) −0.0006 (6) −0.0002 (9)
C20 0.0276 (10) 0.072 (2) 0.0301 (10) −0.0145 (13) 0.0072 (8) −0.0175 (13)
C21 0.0431 (12) 0.0302 (12) 0.0450 (13) −0.0026 (11) 0.0132 (10) −0.0003 (11)
C22 0.086 (2) 0.0508 (18) 0.0323 (12) −0.0345 (18) 0.0166 (13) −0.0117 (13)
C23 0.0334 (11) 0.0323 (12) 0.0451 (12) −0.0046 (10) 0.0103 (9) −0.0004 (11)
C24 0.0679 (18) 0.0539 (19) 0.0340 (12) −0.0288 (16) 0.0099 (12) −0.0092 (13)
O1 0.0336 (7) 0.0288 (8) 0.0265 (7) −0.0088 (7) 0.0062 (5) 0.0006 (7)
O2 0.0397 (8) 0.0402 (10) 0.0267 (7) −0.0131 (8) 0.0092 (6) −0.0074 (7)
O3 0.0266 (7) 0.0652 (13) 0.0294 (7) −0.0172 (9) 0.0071 (6) −0.0143 (9)
O4 0.0235 (6) 0.0541 (11) 0.0270 (7) −0.0086 (8) 0.0037 (5) −0.0078 (8)
O5 0.0337 (7) 0.0341 (9) 0.0304 (7) −0.0121 (8) 0.0053 (6) −0.0010 (7)
O6 0.0446 (9) 0.0542 (12) 0.0272 (7) −0.0235 (10) 0.0113 (7) −0.0108 (8)
O7 0.0540 (10) 0.0442 (11) 0.0339 (8) −0.0168 (9) 0.0202 (7) −0.0077 (9)
O8 0.0623 (11) 0.0427 (11) 0.0375 (8) −0.0181 (11) 0.0263 (8) −0.0075 (9)
Geometric parameters (Å, º)
C1—C6 1.390 (3) C14—C15 1.383 (3)
C1—C2 1.398 (3) C15—C16 1.395 (3)
C1—C8 1.502 (3) C15—H15 0.9300
C2—C3 1.382 (3) C16—H16 0.9300
C2—H2 0.9300 C17—O5 1.423 (3)
C3—O1 1.367 (2) C17—H17A 0.9600
C3—C4 1.407 (3) C17—H17B 0.9600
C4—O2 1.364 (2) C17—H17C 0.9600
C4—C5 1.382 (3) C18—O4 1.425 (3)
C5—C6 1.393 (3) C18—C19 1.535 (3)
C5—H5 0.9300 C18—H18 0.9800
C6—H6 0.9300 C19—C20 1.528 (4)
C7—O1 1.428 (3) C19—H19 0.9800
C7—H7A 0.9600 C20—O3 1.441 (2)
C7—H7B 0.9600 C20—H20A 0.9700
C7—H7C 0.9600 C20—H20B 0.9700
C8—O3 1.436 (2) C21—O7 1.426 (3)
C8—C9 1.526 (3) C21—C22 1.486 (4)
C8—H8 0.9800 C21—H21A 0.9700
C9—C10 1.535 (3) C21—H21B 0.9700
C9—C19 1.542 (3) C22—O8 1.431 (3)
C9—H9 0.9800 C22—H22A 0.9700
C10—O4 1.434 (2) C22—H22B 0.9700
C10—H10A 0.9700 C23—O8 1.422 (3)
C10—H10B 0.9700 C23—C24 1.482 (4)
C11—C16 1.384 (3) C23—H23A 0.9700
C11—C12 1.392 (3) C23—H23B 0.9700
C11—C18 1.509 (3) C24—O7 1.427 (3)
C12—C13 1.393 (3) C24—H24A 0.9700
C12—H12 0.9300 C24—H24B 0.9700
supporting information
sup-5 Acta Cryst. (2003). E59, o1972–o1974
C13—C14 1.395 (3) O6—H6A 0.8200
C14—O6 1.361 (2)
C6—C1—C2 119.04 (18) C11—C16—H16 119.9
C6—C1—C8 121.58 (18) C15—C16—H16 119.9
C2—C1—C8 119.12 (19) O5—C17—H17A 109.5
C3—C2—C1 120.7 (2) O5—C17—H17B 109.5
C3—C2—H2 119.7 H17A—C17—H17B 109.5
C1—C2—H2 119.7 O5—C17—H17C 109.5
O1—C3—C2 126.0 (2) H17A—C17—H17C 109.5
O1—C3—C4 114.12 (17) H17B—C17—H17C 109.5
C2—C3—C4 119.89 (19) O4—C18—C11 110.93 (17)
O2—C4—C5 119.4 (2) O4—C18—C19 104.25 (18)
O2—C4—C3 121.02 (19) C11—C18—C19 113.65 (16)
C5—C4—C3 119.53 (18) O4—C18—H18 109.3
C4—C5—C6 120.3 (2) C11—C18—H18 109.3
C4—C5—H5 119.9 C19—C18—H18 109.3
C6—C5—H5 119.9 C20—C19—C18 116.3 (2)
C1—C6—C5 120.60 (19) C20—C19—C9 104.80 (16)
C1—C6—H6 119.7 C18—C19—C9 102.70 (15)
C5—C6—H6 119.7 C20—C19—H19 110.8
O1—C7—H7A 109.5 C18—C19—H19 110.8
O1—C7—H7B 109.5 C9—C19—H19 110.8
H7A—C7—H7B 109.5 O3—C20—C19 106.4 (2)
O1—C7—H7C 109.5 O3—C20—H20A 110.4
H7A—C7—H7C 109.5 C19—C20—H20A 110.4
H7B—C7—H7C 109.5 O3—C20—H20B 110.4
O3—C8—C1 109.55 (15) C19—C20—H20B 110.4
O3—C8—C9 103.96 (16) H20A—C20—H20B 108.6
C1—C8—C9 117.75 (19) O7—C21—C22 110.4 (2)
O3—C8—H8 108.4 O7—C21—H21A 109.6
C1—C8—H8 108.4 C22—C21—H21A 109.6
C9—C8—H8 108.4 O7—C21—H21B 109.6
C8—C9—C10 115.99 (18) C22—C21—H21B 109.6
C8—C9—C19 101.40 (18) H21A—C21—H21B 108.1
C10—C9—C19 104.24 (16) O8—C22—C21 110.8 (2)
C8—C9—H9 111.5 O8—C22—H22A 109.5
C10—C9—H9 111.5 C21—C22—H22A 109.5
C19—C9—H9 111.5 O8—C22—H22B 109.5
O4—C10—C9 106.99 (16) C21—C22—H22B 109.5
O4—C10—H10A 110.3 H22A—C22—H22B 108.1
C9—C10—H10A 110.3 O8—C23—C24 110.2 (3)
O4—C10—H10B 110.3 O8—C23—H23A 109.6
C9—C10—H10B 110.3 C24—C23—H23A 109.6
H10A—C10—H10B 108.6 O8—C23—H23B 109.6
C16—C11—C12 119.81 (18) C24—C23—H23B 109.6
C16—C11—C18 119.32 (19) H23A—C23—H23B 108.1
supporting information
sup-6 Acta Cryst. (2003). E59, o1972–o1974
C11—C12—C13 119.8 (2) O7—C24—H24A 109.4
C11—C12—H12 120.1 C23—C24—H24A 109.4
C13—C12—H12 120.1 O7—C24—H24B 109.4
O5—C13—C12 125.5 (2) C23—C24—H24B 109.4
O5—C13—C14 114.22 (17) H24A—C24—H24B 108.0
C12—C13—C14 120.29 (19) C3—O1—C7 117.29 (16)
O6—C14—C15 119.3 (2) C4—O2—H2A 109.5
O6—C14—C13 121.2 (2) C8—O3—C20 105.85 (15)
C15—C14—C13 119.55 (18) C18—O4—C10 107.89 (16)
C14—C15—C16 120.3 (2) C13—O5—C17 117.57 (17)
C14—C15—H15 119.9 C14—O6—H6A 109.5
C16—C15—H15 119.9 C24—O7—C21 110.02 (19)
C11—C16—C15 120.3 (2) C23—O8—C22 110.41 (18)
C6—C1—C2—C3 −1.2 (3) C12—C11—C16—C15 −0.4 (3)
C8—C1—C2—C3 173.12 (18) C18—C11—C16—C15 176.1 (2)
C1—C2—C3—O1 179.45 (19) C14—C15—C16—C11 1.4 (3)
C1—C2—C3—C4 0.0 (3) C16—C11—C18—O4 166.43 (19)
O1—C3—C4—O2 1.2 (3) C12—C11—C18—O4 −17.1 (3)
C2—C3—C4—O2 −179.30 (19) C16—C11—C18—C19 −76.5 (3)
O1—C3—C4—C5 −178.51 (19) C12—C11—C18—C19 100.0 (2)
C2—C3—C4—C5 1.0 (3) O4—C18—C19—C20 −148.36 (17)
O2—C4—C5—C6 179.4 (2) C11—C18—C19—C20 90.7 (2)
C3—C4—C5—C6 −0.8 (3) O4—C18—C19—C9 −34.6 (2)
C2—C1—C6—C5 1.3 (3) C11—C18—C19—C9 −155.47 (19)
C8—C1—C6—C5 −172.8 (2) C8—C9—C19—C20 20.3 (2)
C4—C5—C6—C1 −0.3 (3) C10—C9—C19—C20 141.1 (2)
C6—C1—C8—O3 −138.4 (2) C8—C9—C19—C18 −101.68 (19)
C2—C1—C8—O3 47.5 (3) C10—C9—C19—C18 19.1 (2)
C6—C1—C8—C9 −19.9 (3) C18—C19—C20—O3 116.6 (2)
C2—C1—C8—C9 165.94 (18) C9—C19—C20—O3 4.0 (3)
O3—C8—C9—C10 −150.31 (19) O7—C21—C22—O8 57.5 (3)
C1—C8—C9—C10 88.3 (2) O8—C23—C24—O7 −57.5 (3)
O3—C8—C9—C19 −38.1 (2) C2—C3—O1—C7 −9.3 (3)
C1—C8—C9—C19 −159.49 (16) C4—C3—O1—C7 170.11 (17)
C8—C9—C10—O4 112.8 (2) C1—C8—O3—C20 169.2 (2)
C19—C9—C10—O4 2.3 (3) C9—C8—O3—C20 42.5 (3)
C16—C11—C12—C13 −0.5 (3) C19—C20—O3—C8 −28.8 (3)
C18—C11—C12—C13 −176.90 (18) C11—C18—O4—C10 160.50 (19)
C11—C12—C13—O5 −178.5 (2) C19—C18—O4—C10 37.8 (2)
C11—C12—C13—C14 0.3 (3) C9—C10—O4—C18 −25.2 (3)
O5—C13—C14—O6 0.4 (3) C12—C13—O5—C17 8.0 (3)
C12—C13—C14—O6 −178.5 (2) C14—C13—O5—C17 −170.81 (18)
O5—C13—C14—C15 179.7 (2) C23—C24—O7—C21 57.4 (3)
C12—C13—C14—C15 0.7 (3) C22—C21—O7—C24 −57.0 (3)
O6—C14—C15—C16 177.7 (2) C24—C23—O8—C22 56.9 (3)
supporting information
sup-7 Acta Cryst. (2003). E59, o1972–o1974
Hydrogen-bond geometry (Å, º)
D—H···A D—H H···A D···A D—H···A
[a]O2—H2A···O1 0.82 2.24 2.671 (3) 113
[b]O2—H2A···O8i 0.82 1.98 2.718 (2) 149
[c]O6—H6A···O5 0.82 2.22 2.663 (3) 114
[d]O6—H6A···O7 0.82 2.00 2.710 (2) 145
[e]C19—H19···O6ii 0.98 2.37 3.221 (3) 145
[f]C23—H23A···O3ii 0.97 2.55 3.465 (3) 158
[g]C23—H23B···O4iii 0.97 2.56 3.480 (3) 158