organic compounds
Piperizinium hydrogen phosphite monohydrate
aDepartment of Chemistry, University of Aberdeen, Meston Walk, Aberdeen AB24 3UE, Scotland
*Correspondence e-mail: w.harrison@abdn.ac.uk
The title compound, C6H12N22+·HPO32−·H2O, contains doubly protonated piperizinium cations, hydrogen phosphite anions and water molecules. The component species have normal geometrical parameters and interact by way of N—H⋯O and O—H⋯O hydrogen bonds, resulting in [010] chains of alternating [HPO3]2− and H2O species, crosslinked by the organic moieties. A possible C—H⋯O interaction is also present.
Comment
The crystal structures of (protonated) amine hydrogen phosphites containing [HPO3]2− or [H2PO3]− oxo-anions are of crystallochemical interest in terms of the interplay between the hydrogen bonds linking the cations, anions, and, if applicable, water molecules together (Averbuch-Pouchot, 1993a,b; Harrison, 2003a,b).
The ), consists of two half-molecule {C2H6N} fragments of (C4H12N2)2+ piperizinium cations, an [HPO3]2− hydrogen phosphite group and a water molecule. Inversion symmetry (Fig. 1) generates the two complete piperizinium cations, and the water O atom is disordered over two adjacent sites (see Experimental). The hydrogen phosphite group shows its usual (Harrison, 2003a) pseudo-pyramidal geometry [mean d(P—O) = 1.521 (2) Å; mean θ(O—P—O) = 112.48 (9)°] and the organic species adopt typical chair conformations.
of the title compound, (IAs well as electrostatic forces, the component species in (I) interact by means of O—H⋯O and N—H⋯O hydrogen bonds (Table 2), and possibly a C—H⋯O interaction (see below). Infinite chains of alternating [HPO3]2− and H2O moieties are formed (Fig. 2) along [010] as a result of the water-to-phosphite O—H⋯O hydrogen bonds, with the repeating units generated by translation symmetry. The resulting P1⋯P1ii (Fig. 2; see Table 2 for symmetry code) separation of 6.5706 (7) Å is naturally much larger than the typical P⋯P separations (4.7–4.9 Å) seen when [H2PO3]− dihydrogen phosphite units link together by way of P—O—H⋯O—P interactions without an intervening water molecule (Averbuch-Pouchot, 1993a, Harrison, 2003a).
The piperizinium cations crosslink the [010] [HPO3]2−–H2O chains by way of the N—H⋯O hydrogen bonds (Table 2), with all four bonds close to linear [mean θ(N—H⋯O) = 168°]. A short C1—H5⋯O4aiv (Table 2) interaction was identified in a PLATON (Spek, 2003) analysis of (I). If it is not merely a packing artefact, it may provide some additional coherence between the piperizinium cations and the water component of the [HPO3]2−–H2O [010] chains, although its role, if any, in the disordering of the water molecule O4 atom is not obvious.
Experimental
H3PO3 (0.82 g; 1 mmol) and piperizine hexahydrate (1.92 g; 0.01 mmol) were dissolved in 10 ml deionized water, resulting in a clear solution. Block-shaped crystals of (I) grew as the water evaporated over several days.
Crystal data
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Refinement
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The water O atom was modelled as being disordered over two adjacent sites with isotropic displacement factors [d(O4a⋯O4b) = 0.638 (5) Å; fractional site occupancies = 0.563 (14) and 0.437 (14) for O4a and O4b, respectively, with their sum constrained to unity]. The present data did not reveal H-atom sites that could be unambiguously associated with either O4a or O4b; instead, two distinct features in the difference map provided H-atom sites that were reasonable for both O4a and O4b (see Table 2). These O—H H atoms were refined by riding on O4a in their as-found positions. The N—H H atoms were found in difference maps and refined by riding in their idealized positions [d(N—H) = 0.90 Å]. The H atoms bonded to C and P were placed in calculated positions [d(C—H) = 0.97 Å; d(P—H) = 1.32 Å] and refined by riding. For all H atoms, the constraint Uiso(H) = 1.2Ueq(carrier atom) was applied.
Data collection: SMART (Bruker, 1999); cell SAINT (Bruker, 1999); data reduction: SAINT; program(s) used to solve structure: SHELXS97 (Sheldrick, 1997); program(s) used to refine structure: SHELXL97; molecular graphics: ORTEP-3 (Farrugia, 1997); software used to prepare material for publication: SHELXL97.
Supporting information
https://doi.org/10.1107/S1600536804020185/sj6000sup1.cif
contains datablocks global, I, wh411t. DOI:Structure factors: contains datablock I. DOI: https://doi.org/10.1107/S1600536804020185/sj6000Isup2.hkl
Data collection: SMART (Bruker, 1999); cell
SAINT (Bruker, 1999); data reduction: SAINT; program(s) used to solve structure: SHELXS97 (Sheldrick, 1997); program(s) used to refine structure: SHELXL97; molecular graphics: ORTEP-3 (Farrugia, 1997); software used to prepare material for publication: SHELXL97.(C6H12N2)2+·[HPO3]2−·H2O | F(000) = 400 |
Mr = 186.15 | Dx = 1.443 Mg m−3 |
Monoclinic, P21/c | Mo Kα radiation, λ = 0.71073 Å |
Hall symbol: -P 2ybc | Cell parameters from 2470 reflections |
a = 12.2476 (8) Å | θ = 3.3–29.8° |
b = 6.5706 (4) Å | µ = 0.30 mm−1 |
c = 10.6592 (8) Å | T = 293 K |
β = 92.744 (1)° | Block, colourless |
V = 856.8 (1) Å3 | 0.27 × 0.23 × 0.19 mm |
Z = 4 |
Bruker SMART1000 CCD diffractometer | 2468 independent reflections |
Radiation source: normal-focus sealed tube | 1930 reflections with I > 2σ(I) |
Graphite monochromator | Rint = 0.022 |
ω scans | θmax = 30.0°, θmin = 3.3° |
Absorption correction: multi-scan (SADABS; Bruker, 1999) | h = −17→16 |
Tmin = 0.925, Tmax = 0.949 | k = −8→9 |
6211 measured reflections | l = −14→12 |
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)] = 0.042 | Hydrogen site location: difmap (O-H and N-H) and geom (C-H and P-H) |
wR(F2) = 0.131 | H-atom parameters constrained |
S = 1.02 | w = 1/[σ2(Fo2) + (0.0845P)2] where P = (Fo2 + 2Fc2)/3 |
2468 reflections | (Δ/σ)max < 0.001 |
100 parameters | Δρmax = 0.78 e Å−3 |
0 restraints | Δρmin = −0.44 e Å−3 |
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 | Occ. (<1) | |
P1 | 0.23916 (3) | −0.02316 (6) | 0.23270 (4) | 0.02544 (15) | |
H1 | 0.2609 | 0.0944 | 0.1366 | 0.031* | |
O1 | 0.27883 (11) | 0.0919 (2) | 0.35030 (14) | 0.0398 (3) | |
O2 | 0.11571 (10) | −0.0529 (2) | 0.22692 (13) | 0.0335 (3) | |
O3 | 0.30154 (11) | −0.2194 (2) | 0.21505 (14) | 0.0420 (4) | |
N1 | 0.01729 (11) | 0.6267 (2) | 0.10922 (13) | 0.0272 (3) | |
H2 | −0.0364 | 0.5840 | 0.1576 | 0.033* | |
H3 | 0.0549 | 0.7250 | 0.1512 | 0.033* | |
C1 | −0.03148 (15) | 0.7113 (3) | −0.01021 (17) | 0.0318 (4) | |
H4 | 0.0258 | 0.7674 | −0.0596 | 0.038* | |
H5 | −0.0817 | 0.8203 | 0.0082 | 0.038* | |
C2 | 0.09189 (15) | 0.4532 (3) | 0.08474 (18) | 0.0321 (4) | |
H6 | 0.1205 | 0.3975 | 0.1639 | 0.039* | |
H7 | 0.1530 | 0.5012 | 0.0383 | 0.039* | |
N2 | 0.39969 (11) | 0.5910 (2) | 0.03315 (15) | 0.0339 (4) | |
H8 | 0.3613 | 0.6719 | 0.0831 | 0.041* | |
H9 | 0.3531 | 0.5391 | −0.0264 | 0.041* | |
C3 | 0.48414 (15) | 0.7131 (3) | −0.0271 (2) | 0.0377 (4) | |
H10 | 0.5317 | 0.7769 | 0.0368 | 0.045* | |
H11 | 0.4496 | 0.8195 | −0.0780 | 0.045* | |
C4 | 0.44956 (15) | 0.4235 (3) | 0.10849 (19) | 0.0372 (4) | |
H12 | 0.3926 | 0.3446 | 0.1458 | 0.045* | |
H13 | 0.4964 | 0.4794 | 0.1759 | 0.045* | |
O4A | 0.2172 (5) | 0.5036 (5) | 0.3865 (3) | 0.0557 (14)* | 0.563 (14) |
H14 | 0.2488 | 0.3733 | 0.3721 | 0.067* | |
H15 | 0.2536 | 0.5828 | 0.3296 | 0.067* | |
O4B | 0.2678 (6) | 0.5011 (6) | 0.4032 (4) | 0.0507 (17)* | 0.437 (14) |
U11 | U22 | U33 | U12 | U13 | U23 | |
P1 | 0.0236 (2) | 0.0260 (2) | 0.0267 (2) | 0.00143 (15) | 0.00188 (16) | 0.00038 (16) |
O1 | 0.0408 (7) | 0.0355 (7) | 0.0416 (8) | 0.0016 (6) | −0.0139 (6) | −0.0054 (6) |
O2 | 0.0250 (6) | 0.0369 (7) | 0.0388 (7) | −0.0022 (5) | 0.0023 (5) | −0.0088 (5) |
O3 | 0.0453 (8) | 0.0385 (8) | 0.0431 (8) | 0.0168 (6) | 0.0109 (6) | −0.0020 (6) |
N1 | 0.0276 (7) | 0.0276 (7) | 0.0264 (7) | −0.0051 (5) | 0.0022 (5) | −0.0039 (5) |
C1 | 0.0364 (8) | 0.0248 (8) | 0.0339 (9) | 0.0031 (7) | −0.0010 (7) | 0.0004 (7) |
C2 | 0.0282 (8) | 0.0357 (9) | 0.0319 (9) | 0.0025 (7) | −0.0033 (7) | −0.0021 (7) |
N2 | 0.0235 (7) | 0.0417 (9) | 0.0365 (8) | 0.0052 (6) | 0.0004 (6) | −0.0117 (7) |
C3 | 0.0351 (9) | 0.0280 (9) | 0.0496 (11) | 0.0007 (7) | −0.0025 (8) | −0.0020 (8) |
C4 | 0.0293 (8) | 0.0467 (11) | 0.0357 (10) | −0.0037 (7) | 0.0035 (7) | 0.0015 (8) |
P1—O3 | 1.5151 (13) | N2—C3 | 1.479 (2) |
P1—O2 | 1.5230 (12) | N2—H8 | 0.9000 |
P1—O1 | 1.5234 (14) | N2—H9 | 0.9000 |
P1—H1 | 1.3200 | C3—C4ii | 1.512 (3) |
N1—C1 | 1.488 (2) | C3—H10 | 0.9700 |
N1—C2 | 1.492 (2) | C3—H11 | 0.9700 |
N1—H2 | 0.9000 | C4—C3ii | 1.512 (3) |
N1—H3 | 0.9000 | C4—H12 | 0.9700 |
C1—C2i | 1.513 (2) | C4—H13 | 0.9700 |
C1—H4 | 0.9700 | O4A—O4B | 0.638 (5) |
C1—H5 | 0.9700 | O4A—H14 | 0.9549 |
C2—C1i | 1.513 (2) | O4A—H15 | 0.9296 |
C2—H6 | 0.9700 | O4B—H14 | 0.9285 |
C2—H7 | 0.9700 | O4B—H15 | 0.9594 |
N2—C4 | 1.477 (3) | ||
O3—P1—O2 | 113.03 (8) | C4—N2—C3 | 111.13 (14) |
O3—P1—O1 | 112.44 (8) | C4—N2—H8 | 109.4 |
O2—P1—O1 | 111.96 (8) | C3—N2—H8 | 109.4 |
O3—P1—H1 | 106.3 | C4—N2—H9 | 109.4 |
O2—P1—H1 | 106.3 | C3—N2—H9 | 109.4 |
O1—P1—H1 | 106.3 | H8—N2—H9 | 108.0 |
C1—N1—C2 | 111.10 (13) | N2—C3—C4ii | 109.44 (15) |
C1—N1—H2 | 109.4 | N2—C3—H10 | 109.8 |
C2—N1—H2 | 109.4 | C4ii—C3—H10 | 109.8 |
C1—N1—H3 | 109.4 | N2—C3—H11 | 109.8 |
C2—N1—H3 | 109.4 | C4ii—C3—H11 | 109.8 |
H2—N1—H3 | 108.0 | H10—C3—H11 | 108.2 |
N1—C1—C2i | 110.40 (14) | N2—C4—C3ii | 110.48 (16) |
N1—C1—H4 | 109.6 | N2—C4—H12 | 109.6 |
C2i—C1—H4 | 109.6 | C3ii—C4—H12 | 109.6 |
N1—C1—H5 | 109.6 | N2—C4—H13 | 109.6 |
C2i—C1—H5 | 109.6 | C3ii—C4—H13 | 109.6 |
H4—C1—H5 | 108.1 | H12—C4—H13 | 108.1 |
N1—C2—C1i | 110.45 (14) | O4B—O4A—H14 | 68.0 |
N1—C2—H6 | 109.6 | O4B—O4A—H15 | 72.8 |
C1i—C2—H6 | 109.6 | H14—O4A—H15 | 100.7 |
N1—C2—H7 | 109.6 | O4A—O4B—H14 | 72.5 |
C1i—C2—H7 | 109.6 | O4A—O4B—H15 | 67.8 |
H6—C2—H7 | 108.1 | H14—O4B—H15 | 100.5 |
Symmetry codes: (i) −x, −y+1, −z; (ii) −x+1, −y+1, −z. |
D—H···A | D—H | H···A | D···A | D—H···A |
N1—H2···O2iii | 0.90 | 1.84 | 2.7147 (19) | 164 |
N1—H3···O2iv | 0.90 | 1.81 | 2.7043 (19) | 172 |
N2—H8···O3iv | 0.90 | 1.77 | 2.642 (2) | 163 |
N2—H9···O1v | 0.90 | 1.78 | 2.676 (2) | 171 |
O4A—H14···O1 | 0.95 | 1.90 | 2.840 (4) | 167 |
O4A—H15···O3iv | 0.93 | 1.90 | 2.811 (4) | 168 |
O4B—H14···O1 | 0.93 | 1.90 | 2.752 (4) | 151 |
O4B—H15···O3iv | 0.96 | 1.90 | 2.765 (4) | 149 |
C1—H5···O4Aiii | 0.97 | 2.38 | 3.300 (5) | 159 |
Symmetry codes: (iii) −x, y+1/2, −z+1/2; (iv) x, y+1, z; (v) x, −y+1/2, z−1/2. |
References
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