organic compounds
Malonamide: an orthorhombic polymorph
aSchool of Natural Sciences (Chemistry), Bedson Building, University of Newcastle, Newcastle upon Tyne NE1 7RU, England
*Correspondence e-mail: w.clegg@ncl.ac.uk
An orthorhombic polymorph of malonamide, C3H6N2O2, is reported. The unit-cell dimensions, and some aspects of the molecular geometry are significantly different from those of the known monoclinic form [Chieh et al. (1970). J. Chem. Soc. A, pp. 179–184] and of the tetragonal form described in the previous paper [Nichol & Clegg (2005). Acta Cryst. E61, o3424–o3426]. A simple R42(8) motif links the molecules together and the symmetry of the molecule means that this extends into a three-dimensional network.
Comment
In the previous paper (Nichol & Clegg, 2005), we reported a tetragonal polymorph of malonamide, (I). By crystallizing a second sample from the original reaction solution we have obtained a further polymorph, this time in the orthorhombic The only previously known polymorph of malonamide (Chieh et al., 1970) was reported in the P21/c at room temperature, with two independent molecules in the and a final R = 0.05. After realizing that we had identified a second crystalline form of this compound, we wished to redetermine the at room temperature in order to establish whether this was a temperature-induced or a completely new polymorph stable under the same conditions. To do this we had to recrystallize the sample again and what we actually obtained was (I) as yet another, orthorhombic, polymorph.
The molecular structure of (I) is shown in Fig. 1. The consists of one half of the molecule, the complete molecule being generated by a twofold rotation axis which passes through C2. Bond lengths and angles are in good agreement with the mean values for the other polymorphs and the dihedral angle between the O/N/C1/C2 mean plane and its symmetry equivalent (Fig. 2), at 71.90 (4)°, is much closer to the values calculated from the report of Chieh et al. (1970) for their two independent molecules (84.8 and 85.3°) than is the case with the tetragonal polymorph [58.68 (4)°].
Fig. 3 shows a packing diagram viewed along the a axis. Both independent N—H bonds are involved in hydrogen bonding and each O atom is therefore a bifurcated acceptor. The hydrogen bonding consists of a simple R42(8) graph-set motif (Etter, 1990; Bernstein et al., 1995), illustrated in Fig. 4. The crystallographic rotation symmetry of the molecule means that this simple motif extends into a complex three-dimensional network.
of this compound, we have made numerous attempts to obtain again the tetragonal form. Despite carrying out the preparation and crystallization in different locations, we have always obtained the orthorhombic form (the third polymorph, described in this paper) and never one of the others, either monoclinic or tetragonal. We wonder whether this is an example of the phenomenon of `disappearing polymorphs' (Dunitz & Bernstein, 1995Experimental
Equimolar amounts of 4,6-dihydroxypyrimidine and Na2CO3 were dissolved in 20 ml of hot distilled water, forming a pale-yellow solution, from which crystals of the tetragonal polymorph were initially obtained after several days (Nichol & Clegg, 2005). The solution was stored in a sealed container for several months. Large plate crystals of (I) were subsequently grown by evaporation of the cold solution on a watch glass over a period of a few hours.
Crystal data
|
Refinement
|
|
All H atoms were located in a difference map and their coordinates were refined freely, with Uiso(H) = 1.2Ueq(N,C). The C—H bond length refined to 0.964 (13) Å and the two N—H bond lengths refined to 0.887 (16) and 0.846 (19) Å.
Data collection: COLLECT (Nonius, 1998); cell EVALCCD (Duisenberg et al., 2003); data reduction: EVALCCD; program(s) used to solve structure: SHELXTL (Sheldrick, 2001); program(s) used to refine structure: SHELXTL; molecular graphics: DIAMOND3 (Brandenburg & Putz, 2004) and MERCURY (Version 1.3; Bruno et al., 2002); software used to prepare material for publication: Bruker SHELXTL and local programs.
Supporting information
10.1107/S1600536805030540/bt6746sup1.cif
contains datablocks global, I. DOI:Structure factors: contains datablock Ip. DOI: 10.1107/S1600536805030540/bt6746Isup2.hkl
Equimolar amounts of 4,6-dihydroxypyrimidine and Na2CO3 were dissolved in 20 ml of hot distilled water, forming a pale-yellow solution, from which crystals of the tetragonal polymorph were initially obtained after several days (Nichol & Clegg, 2005). The solution was stored in a sealed container for several months. Large plate crystals of (I) were subsequently grown by evaporation of the cold solution on a watch glass over a period of a few hours.
All H atoms were located in a difference map and their coordinates were refined freely, with Uiso(H) = 1.2Ueq(N,C). The C—H bond length refined to 0.964 (13) Å and the two N—H bond lengths refined to 0.887 (16) and 0.846 (19) Å.
Data collection: COLLECT (Nonius, 1998); cell
EVALCCD (Duisenberg et al., 2003); data reduction: EVALCCD; program(s) used to solve structure: SHELXTL (Sheldrick, 2001); program(s) used to refine structure: SHELXTL; molecular graphics: DIAMOND3 (Brandenburg & Putz, 2004) and Mercury (Version 1.3; Bruno et al., 2002); software used to prepare material for publication: Bruker SHELXTL and local programs.C3H6N2O2 | F(000) = 216 |
Mr = 102.10 | Dx = 1.427 Mg m−3 |
Orthorhombic, Pbcn | Mo Kα radiation, λ = 0.71073 Å |
Hall symbol: -P 2n 2ab | Cell parameters from 6050 reflections |
a = 5.3602 (9) Å | θ = 2.5–27.5° |
b = 7.5178 (8) Å | µ = 0.12 mm−1 |
c = 11.791 (2) Å | T = 150 K |
V = 475.14 (12) Å3 | Block cut from large plate, colourless |
Z = 4 | 0.42 × 0.36 × 0.26 mm |
Nonius KappaCCD diffractometer | 539 independent reflections |
Radiation source: sealed tube | 490 reflections with I > 2σ(I) |
Graphite monochromator | Rint = 0.021 |
ϕ and ω scans | θmax = 27.5°, θmin = 4.7° |
Absorption correction: multi-scan (SADABS; Sheldrick, 2003) | h = −6→6 |
Tmin = 0.911, Tmax = 0.970 | k = −9→9 |
8872 measured reflections | l = −15→15 |
Refinement on F2 | Secondary atom site location: difference Fourier map |
Least-squares matrix: full | Hydrogen site location: difference Fourier map |
R[F2 > 2σ(F2)] = 0.031 | Only H-atom coordinates refined |
wR(F2) = 0.083 | w = 1/[σ2(Fo2) + (0.0412P)2 + 0.1866P] where P = (Fo2 + 2Fc2)/3 |
S = 1.11 | (Δ/σ)max < 0.001 |
539 reflections | Δρmax = 0.31 e Å−3 |
43 parameters | Δρmin = −0.20 e Å−3 |
0 restraints | Extinction correction: SHELXL97, Fc*=kFc[1+0.001xFc2λ3/sin(2θ)]-1/4 |
Primary atom site location: structure-invariant direct methods | Extinction coefficient: 0.077 (17) |
C3H6N2O2 | V = 475.14 (12) Å3 |
Mr = 102.10 | Z = 4 |
Orthorhombic, Pbcn | Mo Kα radiation |
a = 5.3602 (9) Å | µ = 0.12 mm−1 |
b = 7.5178 (8) Å | T = 150 K |
c = 11.791 (2) Å | 0.42 × 0.36 × 0.26 mm |
Nonius KappaCCD diffractometer | 539 independent reflections |
Absorption correction: multi-scan (SADABS; Sheldrick, 2003) | 490 reflections with I > 2σ(I) |
Tmin = 0.911, Tmax = 0.970 | Rint = 0.021 |
8872 measured reflections |
R[F2 > 2σ(F2)] = 0.031 | 0 restraints |
wR(F2) = 0.083 | Only H-atom coordinates refined |
S = 1.11 | Δρmax = 0.31 e Å−3 |
539 reflections | Δρmin = −0.20 e Å−3 |
43 parameters |
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. |
x | y | z | Uiso*/Ueq | ||
O | 0.06613 (15) | 0.25831 (10) | 0.37641 (7) | 0.0222 (3) | |
N | −0.2702 (2) | 0.08531 (14) | 0.40865 (9) | 0.0250 (3) | |
H1N | −0.313 (3) | 0.1499 (19) | 0.4686 (14) | 0.030* | |
H2N | −0.355 (3) | −0.005 (3) | 0.3895 (13) | 0.030* | |
C1 | −0.06739 (19) | 0.12942 (13) | 0.35078 (8) | 0.0161 (3) | |
C2 | 0.0000 | 0.01335 (19) | 0.2500 | 0.0161 (4) | |
H2 | 0.136 (3) | −0.0629 (16) | 0.2721 (11) | 0.019* |
U11 | U22 | U33 | U12 | U13 | U23 | |
O | 0.0269 (5) | 0.0211 (5) | 0.0187 (5) | −0.0057 (3) | 0.0001 (3) | −0.0038 (3) |
N | 0.0295 (6) | 0.0226 (5) | 0.0228 (5) | −0.0060 (4) | 0.0109 (4) | −0.0065 (4) |
C1 | 0.0200 (5) | 0.0152 (5) | 0.0131 (5) | 0.0013 (4) | −0.0008 (4) | 0.0014 (3) |
C2 | 0.0195 (7) | 0.0142 (7) | 0.0144 (6) | 0.000 | 0.0012 (5) | 0.000 |
O—C1 | 1.2420 (13) | N—C1 | 1.3257 (14) |
N—H1N | 0.887 (16) | C1—C2 | 1.5178 (13) |
N—H2N | 0.846 (19) | C2—H2 | 0.963 (13) |
H1N—N—H2N | 120.8 (15) | N—C1—C2 | 117.02 (9) |
H1N—N—C1 | 119.0 (10) | C1—C2—C1i | 109.82 (12) |
H2N—N—C1 | 120.1 (11) | C1—C2—H2 | 108.1 (8) |
O—C1—N | 122.85 (10) | C1i—C2—H2 | 112.0 (8) |
O—C1—C2 | 120.12 (9) | ||
O—C1—C2—C1i | −45.99 (8) | N—C1—C2—C1i | 134.54 (10) |
Symmetry code: (i) −x, y, −z+1/2. |
D—H···A | D—H | H···A | D···A | D—H···A |
N—H1N···Oii | 0.887 (16) | 2.058 (17) | 2.9282 (13) | 166.4 (13) |
N—H2N···Oiii | 0.846 (19) | 2.116 (19) | 2.9502 (14) | 168.7 (15) |
Symmetry codes: (ii) x−1/2, −y+1/2, −z+1; (iii) −x−1/2, y−1/2, z. |
Experimental details
Crystal data | |
Chemical formula | C3H6N2O2 |
Mr | 102.10 |
Crystal system, space group | Orthorhombic, Pbcn |
Temperature (K) | 150 |
a, b, c (Å) | 5.3602 (9), 7.5178 (8), 11.791 (2) |
V (Å3) | 475.14 (12) |
Z | 4 |
Radiation type | Mo Kα |
µ (mm−1) | 0.12 |
Crystal size (mm) | 0.42 × 0.36 × 0.26 |
Data collection | |
Diffractometer | Nonius KappaCCD diffractometer |
Absorption correction | Multi-scan (SADABS; Sheldrick, 2003) |
Tmin, Tmax | 0.911, 0.970 |
No. of measured, independent and observed [I > 2σ(I)] reflections | 8872, 539, 490 |
Rint | 0.021 |
(sin θ/λ)max (Å−1) | 0.650 |
Refinement | |
R[F2 > 2σ(F2)], wR(F2), S | 0.031, 0.083, 1.11 |
No. of reflections | 539 |
No. of parameters | 43 |
H-atom treatment | Only H-atom coordinates refined |
Δρmax, Δρmin (e Å−3) | 0.31, −0.20 |
Computer programs: COLLECT (Nonius, 1998), EVALCCD (Duisenberg et al., 2003), EVALCCD, SHELXTL (Sheldrick, 2001), DIAMOND3 (Brandenburg & Putz, 2004) and Mercury (Version 1.3; Bruno et al., 2002), Bruker SHELXTL and local programs.
O—C1 | 1.2420 (13) | C1—C2 | 1.5178 (13) |
N—C1 | 1.3257 (14) | ||
O—C1—C2—C1i | −45.99 (8) | N—C1—C2—C1i | 134.54 (10) |
Symmetry code: (i) −x, y, −z+1/2. |
D—H···A | D—H | H···A | D···A | D—H···A |
N—H1N···Oii | 0.887 (16) | 2.058 (17) | 2.9282 (13) | 166.4 (13) |
N—H2N···Oiii | 0.846 (19) | 2.116 (19) | 2.9502 (14) | 168.7 (15) |
Symmetry codes: (ii) x−1/2, −y+1/2, −z+1; (iii) −x−1/2, y−1/2, z. |
Acknowledgements
We thank the EPSRC for funding.
References
Bernstein, J., Davis, R. E., Shimoni, L. & Chang, N.-L. (1995). Angew. Chem. Int. Ed. Engl. 34, 1555–1573. CrossRef CAS Web of Science Google Scholar
Brandenburg, K. & Putz, H. (2004). DIAMOND3. University of Bonn, Germany. Google Scholar
Bruno, I. J., Cole, J. C., Edgington, P. R., Kessler, M., Macrae, C. F., McCabe, P., Pearson, J. & Taylor, R. (2002). Acta Cryst. B58, 389–397. Web of Science CrossRef CAS IUCr Journals Google Scholar
Chieh, P. C., Subramanian, E. & Trotter, J. (1970). J. Chem. Soc. A, pp. 179–184. CrossRef Google Scholar
Duisenberg, A. J. M., Kroon-Batenburg, L. M. J. & Schreurs, A. M. M. (2003). J. Appl. Cryst. 36, 220–229. Web of Science CrossRef CAS IUCr Journals Google Scholar
Dunitz, J. D. & Bernstein, J. (1995). Acc. Chem. Res. 28, 193–200. CrossRef CAS Web of Science Google Scholar
Etter, M. C. (1990). Acc. Chem. Res. 23, 120–126. CrossRef CAS Web of Science Google Scholar
Nichol, G. S. & Clegg, W. (2005). Acta Cryst. E61, o3424–o3426. Web of Science CSD CrossRef IUCr Journals Google Scholar
Nonius (1998). COLLECT. Nonius BV, Delft, The Netherlands. Google Scholar
Sheldrick, G. M. (2001). SHELXTL. Version 6. Bruker AXS Inc., Madison, Wisconsin, USA. Google Scholar
Sheldrick, G. M. (2003). SADABS. University of Göttingen, Germany. Google Scholar
© International Union of Crystallography. Prior permission is not required to reproduce short quotations, tables and figures from this article, provided the original authors and source are cited. For more information, click here.
In the previous paper (Nichol & Clegg, 2005), we reported a tetragonal polymorph of malonamide, (I). By crystallizing a second sample from the original reaction solution we have obtained a further polymorph, this time in the orthorhombic crystal system. The only previously known polymorph of malonamide (Chieh et al., 1970) was reported in the space group P21/c at room temperature, with two independent molecules in the asymmetric unit and a final R = 0.05. After realising that we had identified a second crystalline form of this compound, we wished to redetermine the unit cell at room temperature in order to establish whether this was a temperature-induced phase transition or a completely new polymorph stable under the same conditions. To do this we had to recrystallize the sample again and what we actually obtained was (I) as yet another, orthorhombic, polymorph.
The molecular structure of (I) is shown in Fig. 1. The asymmetric unit consists of one half of the molecule, the complete molecule being generated by a twofold rotation axis which passes through C2. Bond lengths and angles are in good agreement with the mean values for the other polymorphs and the dihedral angle between the O/N/C1/C2 mean plane and its symmetry equivalent (Fig. 2), at 71.90 (4)°, is much closer to the values calculated from the report of Chieh et al. (1970) for their two independent molecules (84.8 and 85.3°) than is the case with the tetragonal polymorph [58.68 (4)°].
Fig. 3 shows a packing diagram viewed along the a axis. Both independent N—H bonds are involved in hydrogen bonding and each O atom is therefore a bifurcated acceptor. The hydrogen bonding consists of a simple R42(8) graph-set motif (Etter, 1990; Bernstein et al., 1995), illustrated in Fig. 4. The crystallographic rotation symmetry of the molecule means that this simple motif extends into a complex three-dimensional network.
Intrigued by the newly discovered polymorphism of this compound, we have made numerous attempts to obtain again the tetragonal form. Despite carrying out the preparation and crystallization in different locations, we have always obtained the orthorhombic form (the third polymorph, described in this paper) and never one of the others, either monoclinic or tetragonal. We wonder whether this is an example of the phenomenon of `disappearing polymorphs' (Dunitz & Bernstein, 1995).