Supporting information
Crystallographic Information File (CIF) https://doi.org/10.1107/S0108270107048111/hj3053sup1.cif | |
Structure factor file (CIF format) https://doi.org/10.1107/S0108270107048111/hj3053Isup2.hkl |
CCDC reference: 669170
For related literature, see: Ayi et al. (2001); Brese & O'Keeffe (1991); Cheetham et al. (1999); Chidambaram et al. (1999); Chippindale et al. (1998, 2001); Choudhury et al. (2000); Cowley & Chippindale (1999); Escobal et al. (1999, 2000); Gerault et al. (1987); Kongshaug et al. (2001); Lightfoot & Cheetham (1989); Lightfoot et al. (1987); Maspoch et al. (2007); Natarajan (2002); Neeraj et al. (2002); Riou et al. (1987); Rojo et al. (2002); Ruszala et al. (1977); Thoma et al. (2004); Tong et al. (2002); Wang et al. (2003).
Single crystals of [Mn(PO4)2][NH3(CH2)2NH3]2 were prepared under solvothermal conditions. [Mn2(HPO4)3][NH3(CH2)2NH3]3/2·H2PO4 (0.15 g; Chippindale et al., 2001) was stirred with ethane-1,2-diamine (6.00 ml) at room temperature until homogeneous, sealed in a Teflon-lined autoclave, and heated at 433 K for 3 d. The solid product was collected by filtration, washed with methanol and dried in air at room temperature. It consisted of a cream–white powder containing colourless rectangular plates of the title compound suitable for single-crystal X-ray analysis. The powder X-ray diffraction pattern of the bulk product could be indexed on the basis of the orthorhombic unit cell determined from the single-crystal determination with refined lattice parameters a = 8.5667 (13) Å, b = 8.8633 (16) Å and c = 17.207 (3) Å, confirming that the sample is monophasic. An IR spectrum of the product showed features consistent with the presence of ethane-1,2-diammonium cations. A series of strong broad bands occurred in the region 3500–2400 cm−1 corresponding to –N—H and –CH2– stretching modes. The two medium intensity sharp bands observed at 1645 and 1540 cm−1 are due to NH3+ bending modes (antisymmetric and symmetric, respectively). A number of strong sharp bands appearing below 1400 cm−1 correspond to –CH2– group bending modes with P—O and Mn—O stretching and bending modes. Unambiguous individual assignments of these bands are not possible. Thermogravimetric analysis under flowing N2 showed weight losses of ca 15.8% over the range 443–521 K and ca 17% over the range 521–823 K. These correspond to the loss of two moles of ethylenediamine from [Mn(PO4)2][NH3(CH2)2NH3]2 (the calculated value for the loss of one mole of ethane-1,2-diamine is 16.27%). Collapse of the framework occurred above 823 K to give an amorphous residue.
All H atoms were located in difference Fourier maps. The fractional coordinates and isotropic displacement parameters of the H atoms bonded to N were refined, whilst the remaining H atoms were placed geometrically and constrained to ride on their parent C atoms [C—H = 0.95 Å and Uiso(H) = 1.2Ueq(C)].
Data collection: COLLECT (Nonius, 2001); cell refinement: DENZO/SCALEPACK (Otwinowski & Minor, 1997); data reduction: DENZO/SCALEPACK (Otwinowski & Minor, 1997); program(s) used to solve structure: SIR92 (Altomare et al., 1994); program(s) used to refine structure: CRYSTALS (Betteridge et al., 2003); molecular graphics: CAMERON (Watkin et al., 1996); software used to prepare material for publication: CRYSTALS (Betteridge et al., 2003).
(C2H10N2)2[Mn(PO4)2] | F(000) = 764.000 |
Mr = 369.12 | Dx = 1.871 Mg m−3 |
Orthorhombic, Pccn | Mo Kα radiation, λ = 0.71073 Å |
Hall symbol: -P 2ab 2ac | Cell parameters from 1717 reflections |
a = 17.2363 (5) Å | θ = 0–27.4° |
b = 8.5726 (2) Å | µ = 1.29 mm−1 |
c = 8.8689 (2) Å | T = 293 K |
V = 1310.47 (6) Å3 | Plate, colourless |
Z = 4 | 0.19 × 0.07 × 0.03 mm |
Enraf–Nonius KappaCCD diffractometer | 1167 reflections with I > 3σ(I) |
Graphite monochromator | Rint = 0.051 |
ω scans | θmax = 27.4°, θmin = 5.2° |
Absorption correction: multi-scan DENZO/SCALEPACK (Otwinowski & Minor, 1997) | h = 0→22 |
Tmin = 0.90, Tmax = 0.96 | k = 0→11 |
1724 measured reflections | l = 0→11 |
1477 independent reflections |
Refinement on F | Primary atom site location: structure-invariant direct methods |
Least-squares matrix: full | Hydrogen site location: difference Fourier map |
R[F2 > 2σ(F2)] = 0.026 | H atoms treated by a mixture of independent and constrained refinement |
wR(F2) = 0.026 | Method = Prince modified Chebychev polynomial, (Watkin, 1994)
W = [weight] * [1-(deltaF/6*sigmaF)2]2 1.64 -0.625 1.22 |
S = 1.09 | (Δ/σ)max = 0.001 |
1167 reflections | Δρmax = 0.33 e Å−3 |
111 parameters | Δρmin = −0.35 e Å−3 |
(C2H10N2)2[Mn(PO4)2] | V = 1310.47 (6) Å3 |
Mr = 369.12 | Z = 4 |
Orthorhombic, Pccn | Mo Kα radiation |
a = 17.2363 (5) Å | µ = 1.29 mm−1 |
b = 8.5726 (2) Å | T = 293 K |
c = 8.8689 (2) Å | 0.19 × 0.07 × 0.03 mm |
Enraf–Nonius KappaCCD diffractometer | 1477 independent reflections |
Absorption correction: multi-scan DENZO/SCALEPACK (Otwinowski & Minor, 1997) | 1167 reflections with I > 3σ(I) |
Tmin = 0.90, Tmax = 0.96 | Rint = 0.051 |
1724 measured reflections |
R[F2 > 2σ(F2)] = 0.026 | 111 parameters |
wR(F2) = 0.026 | H atoms treated by a mixture of independent and constrained refinement |
S = 1.09 | Δρmax = 0.33 e Å−3 |
1167 reflections | Δρmin = −0.35 e Å−3 |
x | y | z | Uiso*/Ueq | ||
Mn1 | 0.2500 | 0.2500 | 0.46773 (4) | 0.0118 | |
P1 | 0.14663 (3) | 0.44520 (5) | 0.20374 (5) | 0.0108 | |
O1 | 0.07354 (8) | 0.37075 (18) | 0.13553 (16) | 0.0235 | |
O2 | 0.21401 (8) | 0.43996 (16) | 0.08917 (16) | 0.0202 | |
O3 | 0.16721 (8) | 0.35338 (16) | 0.34582 (16) | 0.0194 | |
O4 | 0.1301 (1) | 0.61600 (15) | 0.24409 (16) | 0.0255 | |
N1 | 0.15588 (11) | 0.6357 (2) | 0.55651 (19) | 0.0187 | |
N2 | 0.0462 (1) | 0.3898 (2) | 0.8330 (2) | 0.0182 | |
C1 | 0.09070 (11) | 0.5403 (2) | 0.6143 (2) | 0.0197 | |
C2 | 0.10116 (13) | 0.5101 (2) | 0.7810 (2) | 0.0233 | |
H11 | 0.1999 (19) | 0.578 (4) | 0.573 (4) | 0.046 (9)* | |
H12 | 0.1502 (15) | 0.643 (3) | 0.463 (3) | 0.027 (7)* | |
H13 | 0.1534 (15) | 0.726 (4) | 0.605 (4) | 0.037 (7)* | |
H21 | 0.0536 (16) | 0.307 (4) | 0.780 (3) | 0.033 (7)* | |
H22 | 0.0556 (16) | 0.371 (3) | 0.934 (3) | 0.026 (6)* | |
H23 | 0.0032 (17) | 0.426 (3) | 0.826 (3) | 0.022 (6)* | |
H111 | 0.0894 | 0.4436 | 0.5620 | 0.0237* | |
H112 | 0.0433 | 0.5944 | 0.5984 | 0.0237* | |
H211 | 0.1527 | 0.4754 | 0.7991 | 0.0280* | |
H212 | 0.0921 | 0.6040 | 0.8352 | 0.0280* |
U11 | U22 | U33 | U12 | U13 | U23 | |
Mn1 | 0.01248 (17) | 0.01190 (17) | 0.01103 (16) | 0.00225 (16) | 0.0000 | 0.0000 |
P1 | 0.0123 (2) | 0.0107 (2) | 0.00932 (19) | 0.00247 (15) | 0.00069 (16) | 0.00052 (16) |
O1 | 0.0154 (6) | 0.0378 (8) | 0.0172 (7) | −0.0061 (6) | −0.0053 (5) | 0.0051 (6) |
O2 | 0.0203 (7) | 0.0185 (6) | 0.0219 (7) | −0.0020 (6) | 0.0094 (6) | −0.0057 (6) |
O3 | 0.0230 (7) | 0.0195 (6) | 0.0157 (6) | 0.0040 (6) | −0.0056 (5) | 0.0047 (5) |
O4 | 0.0446 (9) | 0.0123 (6) | 0.0197 (7) | 0.0100 (6) | 0.0094 (6) | 0.0021 (5) |
N1 | 0.0264 (9) | 0.0155 (7) | 0.0141 (8) | 0.0028 (7) | 0.0018 (6) | −0.0023 (6) |
N2 | 0.0167 (8) | 0.0206 (9) | 0.0173 (8) | 0.0070 (7) | 0.0002 (6) | 0.0005 (6) |
C1 | 0.0229 (9) | 0.0199 (9) | 0.0163 (8) | 0.0022 (8) | −0.0013 (7) | −0.0022 (7) |
C2 | 0.0319 (11) | 0.0206 (9) | 0.0176 (9) | −0.0041 (8) | −0.0059 (8) | 0.0021 (8) |
Mn1—O2i | 2.0486 (13) | N1—H13 | 0.89 (3) |
Mn1—O2ii | 2.0486 (13) | N2—C2 | 1.474 (3) |
Mn1—O3 | 1.9976 (13) | N2—H21 | 0.86 (3) |
Mn1—O3iii | 1.9976 (13) | N2—H22 | 0.93 (3) |
P1—O1 | 1.5363 (14) | N2—H23 | 0.80 (3) |
P1—O2 | 1.5437 (13) | C1—C2 | 1.512 (3) |
P1—O3 | 1.5275 (13) | C1—H111 | 0.950 |
P1—O4 | 1.5339 (13) | C1—H112 | 0.950 |
N1—C1 | 1.482 (3) | C2—H211 | 0.950 |
N1—H11 | 0.92 (3) | C2—H212 | 0.950 |
N1—H12 | 0.84 (3) | ||
O2i—Mn1—O2ii | 116.56 (8) | H12—N1—H13 | 114 (3) |
O2i—Mn1—O3 | 98.52 (5) | C2—N2—H21 | 108.0 (18) |
O2ii—Mn1—O3 | 114.89 (6) | C2—N2—H22 | 108.1 (16) |
O2i—Mn1—O3iii | 114.89 (6) | H21—N2—H22 | 111 (2) |
O2ii—Mn1—O3iii | 98.52 (5) | C2—N2—H23 | 107.5 (19) |
O3—Mn1—O3iii | 114.47 (8) | H21—N2—H23 | 114 (3) |
O1—P1—O2 | 110.22 (8) | H22—N2—H23 | 107 (3) |
O1—P1—O3 | 107.53 (8) | N1—C1—C2 | 110.02 (16) |
O2—P1—O3 | 110.69 (8) | N1—C1—H111 | 109.336 |
O1—P1—O4 | 109.66 (9) | C2—C1—H111 | 109.336 |
O2—P1—O4 | 108.71 (8) | N1—C1—H112 | 109.336 |
O3—P1—O4 | 110.03 (8) | C2—C1—H112 | 109.336 |
Mn1iv—O2—P1 | 126.65 (8) | H111—C1—H112 | 109.467 |
Mn1—O3—P1 | 147.24 (9) | N2—C2—C1 | 110.41 (16) |
C1—N1—H11 | 106 (2) | N2—C2—H211 | 109.239 |
C1—N1—H12 | 107.2 (18) | C1—C2—H211 | 109.238 |
H11—N1—H12 | 107 (3) | N2—C2—H212 | 109.238 |
C1—N1—H13 | 106.4 (18) | C1—C2—H212 | 109.238 |
H11—N1—H13 | 116 (3) | H211—C2—H212 | 109.467 |
Symmetry codes: (i) −x+1/2, y, z+1/2; (ii) x, −y+1/2, z+1/2; (iii) −x+1/2, −y+1/2, z; (iv) −x+1/2, y, z−1/2. |
D—H···A | D—H | H···A | D···A | D—H···A |
N1—H11···O2i | 0.92 (3) | 1.91 (4) | 2.816 (2) | 173 (3) |
N1—H12···O4 | 0.84 (3) | 1.99 (3) | 2.811 (2) | 168 (3) |
N1—H13···O4v | 0.89 (3) | 1.88 (3) | 2.737 (2) | 163 (3) |
N2—H21···O1ii | 0.86 (3) | 2.02 (3) | 2.877 (2) | 174 (3) |
N2—H22···O1vi | 0.93 (3) | 1.81 (3) | 2.729 (2) | 170 (2) |
N2—H23···O1vii | 0.80 (3) | 2.21 (3) | 2.924 (3) | 147 (4) |
N2—H23···O4vii | 0.80 (3) | 2.41 (3) | 3.116 (3) | 147 (4) |
Symmetry codes: (i) −x+1/2, y, z+1/2; (ii) x, −y+1/2, z+1/2; (v) x, −y+3/2, z+1/2; (vi) x, y, z+1; (vii) −x, −y+1, −z+1. |
Experimental details
Crystal data | |
Chemical formula | (C2H10N2)2[Mn(PO4)2] |
Mr | 369.12 |
Crystal system, space group | Orthorhombic, Pccn |
Temperature (K) | 293 |
a, b, c (Å) | 17.2363 (5), 8.5726 (2), 8.8689 (2) |
V (Å3) | 1310.47 (6) |
Z | 4 |
Radiation type | Mo Kα |
µ (mm−1) | 1.29 |
Crystal size (mm) | 0.19 × 0.07 × 0.03 |
Data collection | |
Diffractometer | Enraf–Nonius KappaCCD diffractometer |
Absorption correction | Multi-scan DENZO/SCALEPACK (Otwinowski & Minor, 1997) |
Tmin, Tmax | 0.90, 0.96 |
No. of measured, independent and observed [I > 3σ(I)] reflections | 1724, 1477, 1167 |
Rint | 0.051 |
(sin θ/λ)max (Å−1) | 0.648 |
Refinement | |
R[F2 > 2σ(F2)], wR(F2), S | 0.026, 0.026, 1.09 |
No. of reflections | 1167 |
No. of parameters | 111 |
No. of restraints | ? |
H-atom treatment | H atoms treated by a mixture of independent and constrained refinement |
Δρmax, Δρmin (e Å−3) | 0.33, −0.35 |
Computer programs: COLLECT (Nonius, 2001), DENZO/SCALEPACK (Otwinowski & Minor, 1997), SIR92 (Altomare et al., 1994), CRYSTALS (Betteridge et al., 2003), CAMERON (Watkin et al., 1996).
Mn1—O2i | 2.0486 (13) | P1—O3 | 1.5275 (13) |
Mn1—O2ii | 2.0486 (13) | P1—O4 | 1.5339 (13) |
Mn1—O3 | 1.9976 (13) | N1—C1 | 1.482 (3) |
Mn1—O3iii | 1.9976 (13) | N2—C2 | 1.474 (3) |
P1—O1 | 1.5363 (14) | C1—C2 | 1.512 (3) |
P1—O2 | 1.5437 (13) | ||
O2i—Mn1—O2ii | 116.56 (8) | O2—P1—O3 | 110.69 (8) |
O2i—Mn1—O3 | 98.52 (5) | O1—P1—O4 | 109.66 (9) |
O2ii—Mn1—O3 | 114.89 (6) | O2—P1—O4 | 108.71 (8) |
O2i—Mn1—O3iii | 114.89 (6) | O3—P1—O4 | 110.03 (8) |
O2ii—Mn1—O3iii | 98.52 (5) | Mn1iv—O2—P1 | 126.65 (8) |
O3—Mn1—O3iii | 114.47 (8) | Mn1—O3—P1 | 147.24 (9) |
O1—P1—O2 | 110.22 (8) | N1—C1—C2 | 110.02 (16) |
O1—P1—O3 | 107.53 (8) | N2—C2—C1 | 110.41 (16) |
Symmetry codes: (i) −x+1/2, y, z+1/2; (ii) x, −y+1/2, z+1/2; (iii) −x+1/2, −y+1/2, z; (iv) −x+1/2, y, z−1/2. |
D—H···A | D—H | H···A | D···A | D—H···A |
N1—H11···O2i | 0.92 (3) | 1.91 (4) | 2.816 (2) | 173 (3) |
N1—H12···O4 | 0.84 (3) | 1.99 (3) | 2.811 (2) | 168 (3) |
N1—H13···O4v | 0.89 (3) | 1.88 (3) | 2.737 (2) | 163 (3) |
N2—H21···O1ii | 0.86 (3) | 2.02 (3) | 2.877 (2) | 174 (3) |
N2—H22···O1vi | 0.93 (3) | 1.81 (3) | 2.729 (2) | 170 (2) |
N2—H23···O1vii | 0.80 (3) | 2.21 (3) | 2.924 (3) | 147 (4) |
N2—H23···O4vii | 0.80 (3) | 2.41 (3) | 3.116 (3) | 147 (4) |
Symmetry codes: (i) −x+1/2, y, z+1/2; (ii) x, −y+1/2, z+1/2; (v) x, −y+3/2, z+1/2; (vi) x, y, z+1; (vii) −x, −y+1, −z+1. |
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Crystallization under solvothermal conditions has proved very successful for the synthesis of a wide range of metal–phosphate frameworks (Cheetham et al., 1999; Maspoch et al., 2007). Much of this work has focused on aluminium and gallium phosphates and their hetero-metal-substituted analogues, and many new materials with zeolite-like properties have been produced. The solvothermal method has also been used for the preparation of a range of transition-metal phosphates, including manganese(II) and manganese(III) compounds. Examples include Mn7(HPO4)4(PO4)2 (Riou et al., 1987; Rojo et al., 2002), Mn6(PO4)4·H2O (Stock, 2002) and MnPO4·H2O (Lightfoot et al., 1987) and synthetic minerals, such as hureaulite, Mn5(HPO4)2(PO4)2·4H2O (Gerault et al., 1987), and gatehouseite, Mn5(PO4)2(OH)4 (Ruszala et al., 1977), as well as open-framework materials in which inorganic or organic cations are accommodated in pores or interlayer spaces in the metal–phosphate frameworks. Of these materials, which are rather few in number compared with the phosphates of other transition metals, such as iron, cobalt or zinc, only one example, NH4Mn4(PO4)3 (Neeraj et al., 2002), has a three-dimensional manganese–phosphate framework. The remainder, NH4Mn2O(PO4)(HPO4)·H2O (Lightfoot & Cheetham, 1989), Na2Mn2O(PO4)2·H2O (Tong et al., 2002), Ba(MnPO4)2·H2O (Escobal et al., 1999), [Mn6(H2O)2(HPO4)4(PO4)2](pipH2)·H2O (pip is piperazine; Kongshaug et al., 2001), [Mn2(PO4)2](NH3(CH2)2NH3)·(H2O)2 (Song et al., 2003), [Mn2(PO4)3](NH3(CH2)2NH3)·(H2O)x [x = 1 (Escobal et al., 2000) and x = 1/5 (Chippindale et al., 2001)], [Mn2(PO4)3](NH3(CH2)2NH3)3/2·H2PO4 (Chippindale et al., 2001) and [Mn3(PO4)4](trenH3)2·(H2O)6 [tren is tris(2-aminoethyl)amine; Thoma et al., 2004], all have two-dimensional manganese–phosphate frameworks. We describe here the synthesis and characterization of [Mn(PO4)2][NH3(CH2)2NH3]2, the first example of an organically templated manganese phosphate with a one-dimensional chain-like structure.
The structure of [Mn(PO4)2][NH3(CH2)2NH3]2 consists of inorganic chains of formula [Mn(PO4)2]4− separated by ethylenediammonium cations. Atom Mn1 occupies a special position (4c), and is tetrahedrally coordinated to two O2 and two O3 atoms with an average Mn1—O distance of 2.024 Å (Table 1). The bond-valence summation around Mn1 is 2.14 (Brese & O'Keeffe, 1991), confirming that manganese is present in the compound in the +2 oxidation state. The Mn—O bond lengths are in close agreement with those found in other compounds in which Mn2+ is in a tetrahedral MnO4 unit, for example in [Mn3(PO4)4](trenH3)2·(H2O)6 (Thoma et al., 2004). Atom Mn1 is connected via Mn—O—P linkages through O2 and O3 atoms to an independent P atom, P1, which lies on a general position. In addition to the P1—O2 and P1—O3 bonds involved in bridging to atom Mn1, two terminal P1—O bonds, to atoms O1 and O4, complete the tetrahedral coordination around atom P1 (Fig. 1). The O—P—O angles lie in the range 107.5 (1)–110.2 (1)°. The P1—O1 and P1—O4 distances, at 1.536 (1) and 1.534 (1) Å, are somewhat longer than expected for terminal P═O bonds. Their elongation arises as a result of strong hydrogen-bonding interactions with the ethane-1,2-diammonium cations (see below).
The Mn1O4 and P1O4 tetrahedra are linked in strict alternation through their vertices to generate infinite square-twisted chains of formula [Mn(PO4)2]4− containing four-membered Mn2P2 rings of alternating Mn- and P-based units [described as single 4-rings (S4R) in zeolite notation]. The Mn2+ cations are well separated from each other within the chains [Mn1··· Mn1viii = 4.434 (1) Å]. The chains run parallel to the c axis (Fig. 2) and lie in layers in the bc plane. These layers are then stacked in an ABAB fashion along the a axis (Fig. 3), with the chains in layer A lying antiparallel to those in layer B.
In order to balance the negative charge of the manganese-phosphate chains, the ethane-1,2-diamine molecules located in the interlayer space must be diprotonated, and this is confirmed by the location of all H atoms in a difference Fourier map. A network of hydrogen bonds between the two NH3 groups of the ethane-1,2-diammonium cations and the O atoms of the phosphate groups serves to link the chains together to generate a three-dimensional assembly (Table 2). Hydrogen bonds involving atom N1 link the manganese–phosphate chains into layers in the bc plane. Atom N1 is within ca 3.1 Å of four O atoms, three of which are within the same chain [N1···O2i = 2.816 (2) Å, N1···O3 = 3.064 (2) Å and N1···O4 = 2.811 (2) Å; symmetry codes as in Table 2] with the fourth in a neighbouring chain [N1···O4v = 2.737 (2) Å]. Adjacent layers are then linked together by hydrogen bonds via atom N2, which is within ca 3.1 Å of five O atoms. Three of these O atoms are within the same chain (N2···O1ii = 2.877 (2) Å, N2···O1vi = 2.729 (2) Å and N2···O3ii = 2.951 (2) Å] and the remaining two are in a chain in an adjacent layer [N2···O1vii = 2.924 (2) and N2···O4vii = 3.116 (3) Å].
Curiously, to date the title compound has only been synthesized by heating a mixture of pre-formed [Mn2(HPO4)3][NH3(CH2)2NH3]3/2·H2PO4 and ethane-1,2-diamine in an autoclave at 433 K. Attempts to prepare it directly from a manganese(II) salt, phosphoric acid and ethane-1,2-diamine in a conventional solvothermal reaction have not so far been successful. In [Mn2(HPO4)3][NH3(CH2)2NH3]3/2·H2PO4, MnII is present in MnO6 units with octahedral geometry and in MnO5 units with a geometry intermediate between square pyramidal and trigonal bipyramidal. These units are linked through HPO4 tetrahedra to generate a layered structure with ethane-1,2-diammonium cations and hydrogen phosphate anions residing within the interlayer space. By contrast, the title compound contains Mn2+ in tetrahedral MnO4 units. The change in the coordination geometry of manganese on heating [Mn2(HPO4)3][NH3(CH2)2NH3]3/2·H2PO4 in ethane-1,2-diamine probably proceeds via a dissolution process, although the mechanism is not yet known. Tetrahedral MnO4 coordination geometry is still rather rare in manganese(II) phosphates and is most commonly found in mixed-metal phosphates, such as MnAlPOs and MnGaPOs, which have zeolite-like frameworks. With the exception of [Mn3(PO4)4](trenH3)2·(H2O)6 (Thoma et al., 2004), all the compounds listed in the introduction contain manganese coordinated to five, six or seven O atoms.
A number of amine-templated metal phosphates with chain structures based on MO4 and PO4 units have been reported. Two chain structure types have been identified. The first, more common type, contains edge-sharing M2P2 four-membered rings forming ladder-like structures with additional pendant phosphate groups. Examples include [Al(PO4)(HPO4)][NH3(CH2)2NH3] (Wang et al., 2003) and [M(HPO4)2][NH3(CH2)2NH3] [M = Co (Cowley & Chippindale, 1999) and M = Zn (Chidambaram et al., 1999)]. The second chain type contains corner-sharing M2P2 rings of the sort described here, for example [Al(PO4)2](NH4)[NH3CH2CH(NH3)CH3] (Ayi et al., 2001), [Ga(PO4)(HPO4)][NH3(CH2)4NH3] (Chippindale et al., 1998), [Co(HPO4)2](dmpH2) (dmp is N,N'-dimethylpiperazine; Choudhury et al., 2000)) and [Zn(HPO4)2](pipH2) (Natarajan, 2002).
In all cases, the packing together of the chains is driven by hydrogen-bonding interactions. Where the chains contain hydrogen phosphate groups, e.g. PO(OH) and PO(OH)2 groups, the possibility exists for interchain hydrogen-bonding interactions in addition to chain–amine interactions, as is observed, for example in [Co(HPO4)2][NH3(CH2)2NH3] (Cowley & Chippindale, 1999). In the title compound {and [Al(PO4)2](NH4)[NH3CH2CH(NH3)CH3]; Ayi et al., 2001}, no interchain interactions are possible and the metal–phosphate chains are well separated. Hydrogen-bonding networks in these cases therefore involve only chain–amine interactions.