organic compounds
Isovaline monohydrate
aDepartment of Chemistry, Howard University, 525 College Street NW, Washington, DC 20059, USA, bDepartment of Chemistry, Catholic University of America, Washington, DC 20064, USA, cNASA Johnson Space Center, Astromaterial and Exploration Science Directorate, Houston, TX 77058, USA, and dSolar System Exploration Division, NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA
*Correspondence e-mail: rbutcher99@yahoo.com
The title compound, C5H11NO2·H2O, is an isomer of the α-amino acid valine that crystallizes from water in its zwitterion form as a monohydrate. It is not one of the 20 proteinogenic amino acids that are used in living systems and differs from the natural amino acids in that it has no α-H atom. The compound exhibits hydrogen bonding between the water molecule and the carboxylate O atoms and an amine H atom. In addition, there are intermolecular hydrogen-bonding interactions between the carboxylate O atoms and amine H atoms. In the crystal, these extensive N—H⋯O and O—H⋯O hydrogen bonds lead to the formation of a three-dimensional network.
CCDC reference: 897401
Related literature
The structure of the title compound or its salts have not been reported to the CCDC but there are reports of homoleptic coordination complexes of zinc(II) with isovaline, see: Strasdelt et al. (2001). For literature related to eighty amino acids that have been detected in meteorites or comets, see: Glavin & Dworkin (2009); Burton et al. (2012). For the role that crystallization plays in chiral separation, see: Blackmond & Klussmann (2007); Blackmond et al. (2008). For the role of the H atom on the α-C atom in enhancing the rate of see: Yamada et al. (1983). For the mechanism of of amino acids lacking an α-H atom, see: Pizzarello & Groy (2011). For the role that crystallization can play in the enrichment of L-isovaline, see: Glavin & Dworkin (2009); Bada (2009); Bonner et al. (1979). For normal bond lengths and angles, see: Orpen (1993).
Experimental
Crystal data
|
Data collection: CrysAlis PRO (Agilent, 2012); cell CrysAlis PRO; data reduction: CrysAlis PRO; program(s) used to solve structure: SHELXS97 (Sheldrick, 2008); program(s) used to refine structure: SHELXL97 (Sheldrick, 2008); molecular graphics: SHELXTL (Sheldrick, 2008); software used to prepare material for publication: SHELXTL.
Supporting information
CCDC reference: 897401
10.1107/S1600536813031620/jj2178sup1.cif
contains datablock I. DOI:Structure factors: contains datablock I. DOI: 10.1107/S1600536813031620/jj2178Isup2.hkl
Supporting information file. DOI: 10.1107/S1600536813031620/jj2178Isup3.cml
A sample of the title compound was obtained from Acros Organics. Crystals of the title compound were grown from the slow evaporation of a racemic solution of the amino acid in water.
H atoms were placed in geometrically idealized positions and constrained to ride on their parent atoms with a C—H distances of 0.98 and 0.99 Å and an N—H distance of 0.91 \%A Uiso(H) = 1.2Ueq(C) and 0.96 Å for NH3 [Uiso(H) = 1.5Ueq(C)]. The water H's were refined isotropically with O—H distances constrained to be 0.82 Å and the H—O—H angle close to 104.5°.
Data collection: CrysAlis PRO (Agilent, 2012); cell
CrysAlis PRO (Agilent, 2012); data reduction: CrysAlis PRO (Agilent, 2012); program(s) used to solve structure: SHELXS97 (Sheldrick, 2008); program(s) used to refine structure: SHELXL97 (Sheldrick, 2008); molecular graphics: SHELXTL (Sheldrick, 2008); software used to prepare material for publication: SHELXTL (Sheldrick, 2008).Fig. 1. Diagram of the title compound showing atom labeling. Atomic displacement parameters are at the 30% probablity level. Hydogen bonds are shown as dashed lines. | |
Fig. 2. Packing diagram of the title compound viewed along the a axis showing tthe extensive N—H···O and O—H···O hydrogen bonds as dashed lines. |
C5H11NO2·H2O | F(000) = 296 |
Mr = 135.16 | Dx = 1.220 Mg m−3 |
Orthorhombic, P212121 | Cu Kα radiation, λ = 1.54184 Å |
Hall symbol: P 2ac 2ab | Cell parameters from 679 reflections |
a = 5.9089 (5) Å | θ = 3.7–75.3° |
b = 10.4444 (10) Å | µ = 0.84 mm−1 |
c = 11.9274 (11) Å | T = 123 K |
V = 736.10 (12) Å3 | Needle, colorless |
Z = 4 | 0.48 × 0.08 × 0.06 mm |
Agilent Xcalibur (Ruby, Gemini) diffractometer | 1204 independent reflections |
Radiation source: Enhance (Cu) X-ray Source | 1072 reflections with I > 2σ(I) |
Graphite monochromator | Rint = 0.072 |
Detector resolution: 10.5081 pixels mm-1 | θmax = 75.4°, θmin = 5.6° |
ω scans | h = −7→4 |
Absorption correction: multi-scan (CrysAlis PRO; Agilent, 2012) | k = −12→8 |
Tmin = 0.383, Tmax = 1.000 | l = −14→14 |
1662 measured reflections |
Refinement on F2 | Primary atom site location: structure-invariant direct methods |
Least-squares matrix: full | Secondary atom site location: difference Fourier map |
R[F2 > 2σ(F2)] = 0.056 | Hydrogen site location: inferred from neighbouring sites |
wR(F2) = 0.162 | H atoms treated by a mixture of independent and constrained refinement |
S = 1.11 | w = 1/[σ2(Fo2) + (0.093P)2 + 0.2964P] where P = (Fo2 + 2Fc2)/3 |
1204 reflections | (Δ/σ)max < 0.001 |
91 parameters | Δρmax = 0.37 e Å−3 |
3 restraints | Δρmin = −0.27 e Å−3 |
C5H11NO2·H2O | V = 736.10 (12) Å3 |
Mr = 135.16 | Z = 4 |
Orthorhombic, P212121 | Cu Kα radiation |
a = 5.9089 (5) Å | µ = 0.84 mm−1 |
b = 10.4444 (10) Å | T = 123 K |
c = 11.9274 (11) Å | 0.48 × 0.08 × 0.06 mm |
Agilent Xcalibur (Ruby, Gemini) diffractometer | 1204 independent reflections |
Absorption correction: multi-scan (CrysAlis PRO; Agilent, 2012) | 1072 reflections with I > 2σ(I) |
Tmin = 0.383, Tmax = 1.000 | Rint = 0.072 |
1662 measured reflections |
R[F2 > 2σ(F2)] = 0.056 | 3 restraints |
wR(F2) = 0.162 | H atoms treated by a mixture of independent and constrained refinement |
S = 1.11 | Δρmax = 0.37 e Å−3 |
1204 reflections | Δρmin = −0.27 e Å−3 |
91 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. |
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. |
x | y | z | Uiso*/Ueq | ||
O1 | 0.0058 (4) | 0.37096 (19) | 0.50201 (18) | 0.0316 (5) | |
O2 | −0.1536 (4) | 0.4257 (3) | 0.33811 (19) | 0.0385 (6) | |
O1W | 0.6455 (4) | 0.4874 (3) | 0.6172 (2) | 0.0467 (7) | |
H1W1 | 0.776 (5) | 0.465 (5) | 0.601 (3) | 0.070* | |
H1W2 | 0.661 (8) | 0.517 (5) | 0.682 (2) | 0.070* | |
N1 | 0.4267 (4) | 0.3850 (2) | 0.4302 (2) | 0.0297 (6) | |
H1A | 0.5663 | 0.3957 | 0.3994 | 0.045* | |
H1B | 0.4074 | 0.3014 | 0.4493 | 0.045* | |
H1C | 0.4141 | 0.4348 | 0.4925 | 0.045* | |
C1 | 0.0133 (6) | 0.4049 (2) | 0.4006 (3) | 0.0302 (6) | |
C2 | 0.2504 (5) | 0.4229 (3) | 0.3472 (2) | 0.0294 (6) | |
C3 | 0.2766 (6) | 0.3382 (3) | 0.2440 (3) | 0.0367 (7) | |
H3A | 0.2503 | 0.2486 | 0.2648 | 0.055* | |
H3B | 0.4301 | 0.3474 | 0.2139 | 0.055* | |
H3C | 0.1664 | 0.3640 | 0.1869 | 0.055* | |
C4 | 0.2832 (6) | 0.5657 (3) | 0.3178 (3) | 0.0344 (7) | |
H4A | 0.4384 | 0.5779 | 0.2885 | 0.041* | |
H4B | 0.1762 | 0.5888 | 0.2572 | 0.041* | |
C5 | 0.2477 (7) | 0.6556 (3) | 0.4151 (3) | 0.0451 (9) | |
H5A | 0.2565 | 0.7442 | 0.3886 | 0.068* | |
H5B | 0.3650 | 0.6408 | 0.4716 | 0.068* | |
H5C | 0.0984 | 0.6401 | 0.4482 | 0.068* |
U11 | U22 | U33 | U12 | U13 | U23 | |
O1 | 0.0326 (11) | 0.0293 (9) | 0.0329 (10) | 0.0009 (8) | 0.0031 (9) | 0.0061 (9) |
O2 | 0.0268 (11) | 0.0510 (13) | 0.0376 (11) | 0.0010 (11) | 0.0007 (9) | 0.0110 (11) |
O1W | 0.0379 (13) | 0.0627 (17) | 0.0396 (13) | 0.0087 (13) | −0.0008 (11) | −0.0148 (12) |
N1 | 0.0268 (12) | 0.0270 (11) | 0.0352 (14) | −0.0004 (9) | 0.0016 (11) | 0.0015 (11) |
C1 | 0.0324 (15) | 0.0214 (12) | 0.0367 (15) | −0.0017 (11) | 0.0027 (12) | 0.0020 (11) |
C2 | 0.0279 (15) | 0.0275 (13) | 0.0328 (14) | −0.0009 (12) | 0.0009 (11) | 0.0051 (13) |
C3 | 0.0371 (18) | 0.0392 (16) | 0.0338 (16) | 0.0040 (15) | −0.0005 (13) | 0.0010 (14) |
C4 | 0.0320 (15) | 0.0317 (15) | 0.0394 (15) | −0.0038 (13) | −0.0001 (13) | 0.0085 (14) |
C5 | 0.055 (2) | 0.0260 (14) | 0.054 (2) | −0.0030 (14) | 0.0026 (18) | 0.0020 (15) |
O1—C1 | 1.261 (4) | C2—C4 | 1.545 (4) |
O2—C1 | 1.255 (4) | C3—H3A | 0.9800 |
O1W—H1W1 | 0.830 (19) | C3—H3B | 0.9800 |
O1W—H1W2 | 0.832 (19) | C3—H3C | 0.9800 |
N1—C2 | 1.490 (4) | C4—C5 | 1.507 (5) |
N1—H1A | 0.9100 | C4—H4A | 0.9900 |
N1—H1B | 0.9100 | C4—H4B | 0.9900 |
N1—H1C | 0.9100 | C5—H5A | 0.9800 |
C1—C2 | 1.550 (4) | C5—H5B | 0.9800 |
C2—C3 | 1.524 (4) | C5—H5C | 0.9800 |
H1W1—O1W—H1W2 | 102 (3) | C2—C3—H3B | 109.5 |
C2—N1—H1A | 109.5 | H3A—C3—H3B | 109.5 |
C2—N1—H1B | 109.5 | C2—C3—H3C | 109.5 |
H1A—N1—H1B | 109.5 | H3A—C3—H3C | 109.5 |
C2—N1—H1C | 109.5 | H3B—C3—H3C | 109.5 |
H1A—N1—H1C | 109.5 | C5—C4—C2 | 114.2 (3) |
H1B—N1—H1C | 109.5 | C5—C4—H4A | 108.7 |
O2—C1—O1 | 126.2 (3) | C2—C4—H4A | 108.7 |
O2—C1—C2 | 116.4 (3) | C5—C4—H4B | 108.7 |
O1—C1—C2 | 117.4 (3) | C2—C4—H4B | 108.7 |
N1—C2—C3 | 108.1 (3) | H4A—C4—H4B | 107.6 |
N1—C2—C4 | 108.6 (3) | C4—C5—H5A | 109.5 |
C3—C2—C4 | 111.3 (3) | C4—C5—H5B | 109.5 |
N1—C2—C1 | 109.1 (2) | H5A—C5—H5B | 109.5 |
C3—C2—C1 | 110.7 (3) | C4—C5—H5C | 109.5 |
C4—C2—C1 | 108.9 (2) | H5A—C5—H5C | 109.5 |
C2—C3—H3A | 109.5 | H5B—C5—H5C | 109.5 |
O2—C1—C2—N1 | −175.8 (3) | O1—C1—C2—C4 | −114.2 (3) |
O1—C1—C2—N1 | 4.2 (4) | N1—C2—C4—C5 | −64.0 (3) |
O2—C1—C2—C3 | −57.0 (3) | C3—C2—C4—C5 | 177.0 (3) |
O1—C1—C2—C3 | 123.0 (3) | C1—C2—C4—C5 | 54.7 (4) |
O2—C1—C2—C4 | 65.8 (3) |
D—H···A | D—H | H···A | D···A | D—H···A |
O1W—H1W1···O1i | 0.83 (2) | 2.05 (2) | 2.811 (3) | 152 (4) |
O1W—H1W2···O2ii | 0.83 (2) | 1.96 (2) | 2.787 (3) | 171 (5) |
N1—H1A···O2i | 0.91 | 1.84 | 2.745 (3) | 177 |
N1—H1C···O1W | 0.91 | 2.09 | 2.792 (4) | 133 |
N1—H1B···O1iii | 0.91 | 1.98 | 2.832 (3) | 156 |
Symmetry codes: (i) x+1, y, z; (ii) −x+1/2, −y+1, z+1/2; (iii) x+1/2, −y+1/2, −z+1. |
D—H···A | D—H | H···A | D···A | D—H···A |
O1W—H1W1···O1i | 0.830 (19) | 2.05 (2) | 2.811 (3) | 152 (4) |
O1W—H1W2···O2ii | 0.832 (19) | 1.962 (19) | 2.787 (3) | 171 (5) |
N1—H1A···O2i | 0.91 | 1.84 | 2.745 (3) | 177.3 |
N1—H1C···O1W | 0.91 | 2.09 | 2.792 (4) | 132.6 |
N1—H1B···O1iii | 0.91 | 1.98 | 2.832 (3) | 155.5 |
Symmetry codes: (i) x+1, y, z; (ii) −x+1/2, −y+1, z+1/2; (iii) x+1/2, −y+1/2, −z+1. |
Acknowledgements
RJB wishes to acknowledge the NSF–MRI program (grant CHE-0619278) for funds to purchase the diffractometer. GB wishes to acknowledge support of this work from NASA (NNX10AK71A)
References
Agilent (2012). CrysAlis PRO. Agilent Technologies UK Ltd, Yarnton, England. Google Scholar
Bada, J. L. (2009). Proc. Natl Acad. Sci. 106, E85. Web of Science CrossRef PubMed Google Scholar
Blackmond, D. G. & Klussmann, M. (2007). Chem. Commun. pp. 3990–3996. Web of Science CrossRef Google Scholar
Blackmond, D., Viedma, C., Ortiz, J., Torres, T. & Izuma, T. (2008). J. Am. Chem. Soc. 130, 15274–15275. Web of Science PubMed Google Scholar
Bonner, W. A., Blair, N. E., Lemmon, R. M., Flores, J. J. & Pollock, G. E. (1979). Geochim. Cosmochim. Acta, 43, 1841–1846. CrossRef CAS Web of Science Google Scholar
Burton, A. S., Stern, J. C., Elsila, J. E., Dworkin, J. P. & Glavin, D. P. (2012). Chem. Soc. Rev. 41, 5459–5472. Web of Science CrossRef CAS PubMed Google Scholar
Glavin, D. P. & Dworkin, J. P. (2009). Proc. Natl Acad. Sci. 106, 5487–5492. Web of Science CrossRef PubMed CAS Google Scholar
Orpen, G. A. (1993). Chem. Soc. Rev. 22, 191–197. CrossRef CAS Web of Science Google Scholar
Pizzarello, S. & Groy, T. L. (2011). Geochim. Cosmochim. Acta, 75, 645–656. Web of Science CSD CrossRef CAS Google Scholar
Sheldrick, G. M. (2008). Acta Cryst. A64, 112–122. Web of Science CrossRef CAS IUCr Journals Google Scholar
Strasdelt, H., Busching, I., Behrends, S., Saak, W. & Barklage, W. (2001). Chem. Eur. J. 7, 1133–1137. Web of Science PubMed Google Scholar
Yamada, S., Hongo, C., Yoshioka, R. & Chibata, I. (1983). J. Org. Chem. 48, 843–846. CrossRef CAS Web of Science Google Scholar
This is an open-access article distributed under the terms of the Creative Commons Attribution (CC-BY) Licence, which permits unrestricted use, distribution, and reproduction in any medium, provided the original authors and source are cited.
The alpha amino acids are essential for life as they are the building blocks of all proteins and enzymes. Nature uses almost exclusively the L form of the nineteen naturally occurring chiral amino acids. Glycine is achiral. However, it is known that there are over eighty amino acids that have been detected in meteorites or comets (Glavin & Dworkin 2009; Burton et al., 2012). One of these extraterrestrial non proteinogenic amino acids is isovaline. The majority of these amino acids show little or no enrichment of one enantiomer over the other. An intriguing question is the process that lead to the separation and enrichment of the L enantiomer over the D. There are several possible explanations for this including the role that crystallization plays (Blackmond & Klussmann, 2007). Only two of the twenty amino acids used biologically crystallize in a chiral space group, which allows for spontaneous separation of enantiomers, at the level of the crystal, from a racemic solution (Blackmond et al., 2008). Isovaline, a non proteinogenic amino acid also allows for this separation of enantiomers at the level of the crystal as it crystallizes in the chiral space group, P212121.
Another important aspect in the prebiotic chemistry of the amino acids is the role of racemization. All of the nineteen naturally occurring chiral amino acids have a hydrogen atom on the alpha carbon atom, which enhances the rate of racemization (Yamada et al., 1983). However, little is known about the mechanism of racemization of amino acids lacking an alpha hydrogen atom (Pizzarello & Groy, 2011). The structure of isovaline given here can be used to examine the role that crystallization can play in the enrichment of L isovaline (Glavin & Dworkin 2009; Bada, 2009), and as a starting point in mechanistic studies of racemization mechanisms of isovaline (Bonner et al., 1979).
In the structure of the title compound the amino acid is in the usual zwitterionic form. While the structure of the title compound or its salts have not been reported there are reports of homoleptic coordination complexes of isovaline with zinc(II) (Strasdelt et al. (2001). However, there are several important differences between these structures and the title compound. The metal complexes all crystallized in non-chiral space groups and, of course, when coordinated to a metal, the isovaline will not be in a zwitterionic form but, apart from the COO- group, all the the bond lengths and angles are in the normal range for such compounds (Orpen, 1993). There is extensive N—H···O and O—H···O hydrogen bonding linking the zwitterions into a 3-D array.