research communications
Structure 4)3Al2(PO4)3 prepared by ionothermal synthesis in phosphonium based ionic liquids – a redetermination
of (NHaExploratory Materials and Catalysis Research, Honeywell UOP, Des Plaines IL 60201, USA, and bAdvanced Characterization, Honeywell UOP, Des Plaines IL 60201, USA
*Correspondence e-mail: christopher.nicholas@uop.com
After crystallization during ionothermal syntheses in phosphonium-containing ionic liquids, the structure of (NH4)3Al2(PO4)3 [triammonium dialuminum tris(phosphate)] was refined on the basis of powder X-ray diffraction data from a synchrotron source. (NH4)3Al2(PO4)3 is a member of the structural family with formula A3Al2(PO4)3, where A is a group 1 element, and of which the NH4, K, and Rb forms were previously known. The NH4 form is isostructural with the K form, and was previously solved from single-crystal X-ray data when the material (SIZ-2) crystallized from a choline-containing eutectic mixture [Cooper et al. (2004). Nature, 430, 1012–1017]. Our independent incorporates NH4 groups and shows that these NH4 groups are hydrogen bonded to framework O atoms present in rings containing 12 T sites in a channel along the c-axis direction. We describe structural details of (NH4)3Al2(PO4)3 and discuss differences with respect to isostructural forms.
1. Chemical context
Following the discovery of the microporous AlPO4-n series of materials (Wilson et al., 1982), many efforts have been directed toward the synthesis of novel phases utilizing traditional hydrothermal (Wilson, 2007; Yu & Xu, 2006) and solvothermal syntheses (Das et al., 2012). Recently, ionothermal synthesis has been added to the stable of synthetic methods. Ionothermal synthesis is an extension of the solvothermal method of synthesis using an ionic liquid as the solvent (replacing, for example, water or ethylene glycol) where a portion of the organic structure-directing agent from a typical zeolite synthesis is derived from the ionic liquid (Morris, 2009). Many new materials have been synthesized by ionothermal synthesis, with new aluminophosphate materials among the most common (Parnham & Morris, 2007; Xing et al., 2008, 2010).
An important issue in ionothermal synthesis is control of water (Ma et al., 2008). Excess water often leads to synthesis of dense AlPO4 phases such as the one with a tridymite-type of structure, which we observed as well during syntheses utilizing 85%wt H3PO4. To control the level of water in the synthesis, thereby allowing easy recycling of the ionic liquid solvent and to intentionally prepare ammonium aluminophosphates, we used (NH4)2HPO4 as the phosphorous source in the synthesis. Ammonium is a good structure-directing agent for aluminophosphate frameworks; multiple ammonium aluminum phosphates are known (Byrne et al., 2009; Vaughan et al., 2012). In the current phosphonium-based ionothermal synthesis, the presence of an ammonium cation in the relative absence of water provokes the formation of a 2/3 Al/P framework with the formula (NH4)3Al2(PO4)3. A structurally unrelated compound with the formula (NH4)3Al2(PO4)3 has previously been synthesized via a solvothermal approach (Medina et al., 2004).
The aluminophosphate database at Jilin (Li et al., 2019) currently lists 21 framework structures with a 2:3 ratio of Al:P. A framework with sub-stoichiometric Al content is by necessity anionically charged and must be cation-balanced, so most of the known frameworks, such as UT-3, UT-4 and UT-5 (Oliver et al., 1996) are charge-balanced by organoammonium cations. Low-water-content syntheses clearly favor 2:3 compounds as most of the known materials are synthesized from low-water-content preparations.
2. Structural commentary and survey of related compounds
The (NH4)3Al2(PO4)3 phase synthesized here is related to the series of A3Al2(PO4)3 materials synthesized via high-temperature solid-state methods (Devi & Vidyasagar, 2000) with varying monocations on the A site. Additionally, an independent synthesis previously yielded a (NH4)3Al2(PO4)3 material called SIZ-2 whose structure was solved and refined from single-crystal data (Cooper et al., 2004) and possesses nearly the same structure as refined from the current powder data of (NH4)3Al2(PO4)3. A polyhedral representation of the of (NH4)3Al2(PO4)3 is shown in Fig. 1. SIZ-2 crystallized from a choline chloride/urea eutectic mixture where decomposition of urea was proposed to be the source of ammonium in the structure. The of Cooper et al. (2004) included the ammonium N atoms, but made no attempt to find or model the corresponding H atoms.
Devi & Vidyasagar (2000) utilized Li, Na, K, Rb, Cs, and Tl as the A cation and succeeded in crystallizing compounds with A = Na, K, Rb, Tl. The thallium derivative yielded a completely different structure with trigonal–bipyramidal coordination of Al. The A = Na structure was not solved, but apparently crystallizes in an unrelated orthorhombic space-group type from that observed for A = K, Rb in their work, and for A = NH4 here. Devi & Vidyasagar (2000) utilized (NH4)2HPO4 as the phosphate source in their high-temperature preparations of A3Al2(PO4)3, but did not obtain (NH4)3Al2(PO4)3, likely due to the volatility of NH3 at high temperatures.
As in the K and Rb forms of the A3Al2(PO4)3 series, aluminum and phosphorus are both tetrahedrally coordinated and connected through corners throughout the (NH4)3Al2(PO4)3 structure. The NH4+ cations reside in a channel along the c-axis direction made from a 12 T-site ring of alternating AlO4 and PO4 tetrahedra (Fig. 2). The NH4+ groups occupy the available space and none of the ionic liquid solvent is present within the pores of the (NH4)3Al2(PO4)3 framework. Without the NH4+ groups, the structure would have 24% void volume. The framework is triply negatively charged and charge-balanced by the ammonium cations. Three of the six phosphate groups in the ring protrude inward such that the closest contact distance between the H atom of an ammonium group and the O atom of the nearest phosphate is between 1.83 and 1.87 Å, indicating significant hydrogen-bonding interactions. The full range of H⋯O hydrogen-bond lengths is between 1.83 and 1.97 Å (Table 1).
Crystallizing in space-group type Pna21, (NH4)3Al2(PO4)3 is isostructural to, but with a slightly larger than the K form synthesized by Devi & Vidyasagar (2000). Lattice expansion of ∼0.1–0.2 Å occurs along each of the three axes, leading to an overall 6.6% increase in cell volume from 1245 to 1327 Å3. A lattice expansion is no surprise as the ionic radius of NH4+ is between 1.4 and 1.67 Å depending on the (Sidey, 2016). This is slightly larger than the reported 1.37 to 1.55 Å range for K+ (Shannon, 1976). Much of the relative lattice expansion for (NH4)3Al2(PO4)3 occurs along the a and c axes. Tilting of tetrahedra accounts for a significantly smaller expansion of the long b axis. In addition, an isostructural K/As form is also known where two-thirds of the phosphate groups have been replaced by arsenate (Boughzala et al., 1997). Arsenate included on the phosphate sites increases the cell volume to 1307 Å3, just smaller than that recorded here for (NH4)3Al2(PO4)3. The pure arsenate form K3Al2(AsO4)3 was reported by Stöger & Weil (2012), which has a cell volume of 1328 Å3, essentially equivalent to that here.
An overlay plot of atomic positions of (NH4)3Al2(PO4)3 (red) versus SIZ-2 (blue) shows that although the independent refinements of the two (NH4)3Al2(PO4)3 materials were performed via different methods at different temperatures, most atom positions are similar, with no more than about 0.004 fractional position differences along the a or c axes (for these axes, about 0.03–0.04 Å, Fig. 3). One area stands out in the A3Al2(PO4)3 series. Fig. 4 shows the key area surrounding O11 where the largest position movement is observed in the two independent refinements of (NH4)3Al2(PO4)3.
The P3—O11 bond is always among the shortest P—O bonds found in the ; Wei et al., 2012). Each of the O atoms protruding into the pore possess short P—O bonds and hydrogen bonds to two ammonium ions (Table 1). In particular, N2, N3, O11, and P3 are effectively in a plane so that with the hydrogen bonding present in our refined model from N3 and N2 through the attached H atoms to O11, O11 moves closer to P3 while N2 and N3 move slightly further away versus the positions in the SIZ-2 Table 2 shows respective O—A and P—O distances for the four isostructural A3Al2(PO4)3 compounds. Other bond lengths and angles are otherwise relatively unremarkable versus other members of the structural class although we note that As/P—O distances are longer than P—O as expected.
here at 1.487 (5) Å. Two clusters of P—O bond lengths occur; one at about 1.49 Å and another at 1.55 Å. These distances are relatively typical for aluminophosphates (Richardson & Vogt, 1992
|
Rb3Al2(PO4)3 is structurally related to the NH4 and K forms, but crystallizes in a higher symmetry space-group type (Cmc21), accompanied with higher overall coordination numbers around Rb+ and a mirror plane perpendicular to a. The ionic radius of Rb+ is similar to that of NH4+, reported as 1.52–1.63 Å (Shannon, 1976). Lithium and cesium forms of the series have not yet been synthesized, likely because of the relatively small and large, respectively, ionic radii versus those of the fitting A cations. Our initial attempts at ion-exchange of (NH4)3Al2(PO4)3 with LiNO3 or CsNO3 in aqueous solution to form the Li or Cs form failed, with partial structural degradation and no ion-exchange observed.
3. Synthesis and crystallization
In a typical preparation, 1.65 g (NH4)2HPO4 was added to a 125 ml polytetrafluoroethene (PTFE) lined autoclave containing 24.02 g of ethyl tri(butyl)phosphonium diethyl phosphate. The mixture was stirred at room temperature for 2 min. To this mixture were added 0.49 g of Al(OH)3, and the contents were stirred at room temperature for 2 min. The contents of the autoclave were digested at 423 K for 24 h prior to isolating the product by filtration. Analytical results show this material has a molar ratio Al:P of 0.725. The X-ray diffraction pattern is shown in Fig. 5. (SEM) revealed agglomerated stacks of irregularly shaped blocky crystals of from 500 nm to 2–4 µm in length (Fig. 6). of (NH4)3Al2(PO4)3 at temperatures of 773 K or higher causes the formation of an AlPO4 phase with a tridymite-type structure. Ethyl tributyl phosphonium diethyl phosphate (Cyphos 169) was acquired from Cytec; aluminum hydroxide was acquired from Pfaltz and Bauer.
4. Refinement
Crystal data, data collection and structure . Following initial survey scans on in-house Cu source powder XRD instruments, final data were acquired from samples packed in thin glass capillaries on 11-BM at the Advanced Photon Source at Argonne National Laboratory. Starting atomic positions for the were adapted from the literature examples. Starting positions for the ammonium cations were located in a difference-Fourier map and subsequently refined using GSAS (Larson & Von Dreele, 2000) as tetrahedral rigid bodies with N—H bond lengths held at 0.9526 Å and tetrahedrality enforced, leading to H⋯H distances of 1.5556 Å. No soft constraints were applied to the framework positions. All atoms in the structure were refined with a common Uiso parameter. Two low-intensity reflections in the region 4.00–4.22°/2θ were excluded from the as belonging to an impurity phase after assessment of multiple (NH4)3Al2(PO4)3 batches. trials with a higher symmetry model (space-group type Cmc21) were attempted but showed poor agreement with the experimental data, with Rwp > 0.16.
details are summarized in Table 3
|
Supporting information
Data collection: local program at 11BM; data reduction: GSAS (Larson & Von Dreele, 2000); program(s) used to solve structure: coordinates from an isotypic structure; program(s) used to refine structure: GSAS (Larson & Von Dreele, 2000); molecular graphics: CrystalMaker (Palmer, 2005); software used to prepare material for publication: publCIF (Westrip, 2010).
(NH4)3Al2(PO4)3 | V = 1327.11 (2) Å3 |
Mr = 392.99 | Z = 4 |
Orthorhombic, Pna21 | Synchrotron radiation, λ = 0.373811 Å |
Hall symbol: P 2c -2n | µ = 0.12 mm−1 |
a = 8.98884 (6) Å | T = 100 K |
b = 17.01605 (10) Å | white |
c = 8.67653 (5) Å | cylinder, 0.70 × 0.70 mm |
11BM_synchrotron diffractometer | Scan method: continuous |
Specimen mounting: capillary | 2θmin = 2.45°, 2θmax = 20°, 2θstep = 0.001° |
Data collection mode: transmission |
Least-squares matrix: full | Profile function: CW Profile function number 4 with 18 terms Pseudovoigt profile coefficients as parameterized in P. Thompson, D.E. Cox & J.B. Hastings (1987). J. Appl. Cryst.,20,79-83. Asymmetry correction of L.W. Finger, D.E. Cox & A. P. Jephcoat (1994). J. Appl. Cryst.,27,892-900. Microstrain broadening by P.W. Stephens, (1999). J. Appl. Cryst.,32,281-289. #1(GU) = 1.163 #2(GV) = -0.126 #3(GW) = 0.063 #4(GP) = 0.000 #5(LX) = 0.143 #6(ptec) = -0.01 #7(trns) = 0.00 #8(shft) = 0.0000 #9(sfec) = 0.00 #10(S/L) = 0.0011 #11(H/L) = 0.0011 #12(eta) = 0.7694 #13(S400 ) = 1.1E-01 #14(S040 ) = 2.8E-03 #15(S004 ) = 1.0E-01 #16(S220 ) = 1.3E-02 #17(S202 ) = -9.0E-03 #18(S022 ) = 6.9E-03 Peak tails are ignored where the intensity is below 0.0010 times the peak Aniso. broadening axis 1.0 0.0 0.0 |
Rp = 0.082 | 95 parameters |
Rwp = 0.101 | 20 restraints |
Rexp = 0.060 | H atoms treated by a mixture of independent and constrained refinement |
R(F2) = 0.03552 | (Δ/σ)max = 0.17 |
49495 data points | Background function: GSAS Background function number 1 with 11 terms. Shifted Chebyshev function of 1st kind 1: 111.086 2: -42.2923 3: 17.4011 4: -1.76183 5: -7.25556 6: 2.97020 7: 2.60010 8: -3.84672 9: 5.91765 10: -3.48127 11: 1.19076 |
x | y | z | Uiso*/Ueq | ||
P1 | 0.1689 (3) | 0.21458 (16) | −0.0138 (5) | 0.0086 (3)* | |
P2 | 0.3100 (3) | 0.29952 (16) | 0.4927 (5) | 0.0086 (3)* | |
P3 | 0.2594 (3) | 0.5033 (2) | 0.0861 | 0.0086 (3)* | |
Al1 | 0.3631 (4) | 0.33375 (18) | 0.1361 (5) | 0.0086 (3)* | |
Al2 | 0.1295 (4) | 0.17048 (19) | 0.6462 (5) | 0.0086 (3)* | |
O1 | 0.2886 (7) | 0.1552 (3) | 0.0117 (8) | 0.0086 (3)* | |
O2 | 0.0384 (8) | 0.2046 (3) | 0.1014 (8) | 0.0086 (3)* | |
O3 | 0.2289 (7) | 0.3006 (3) | 0.0100 (8) | 0.0086 (3)* | |
O4 | 0.1017 (7) | 0.2138 (4) | 0.8252 (8) | 0.0086 (3)* | |
O5 | 0.1953 (7) | 0.3602 (3) | 0.5464 (8) | 0.0086 (3)* | |
O6 | 0.4625 (7) | 0.3234 (3) | 0.5425 (8) | 0.0086 (3)* | |
O7 | 0.2776 (8) | 0.2165 (3) | 0.5518 (7) | 0.0086 (3)* | |
O8 | 0.3087 (7) | 0.2962 (4) | 0.3126 (8) | 0.0086 (3)* | |
O9 | 0.1072 (5) | 0.4838 (3) | 0.1404 (8) | 0.0086 (3)* | |
O10 | 0.3228 (7) | 0.5700 (4) | 0.1747 (7) | 0.0086 (3)* | |
O11 | 0.2604 (6) | 0.5218 (3) | 0.9186 (6) | 0.0086 (3)* | |
O12 | 0.3716 (7) | 0.4348 (3) | 0.1188 (9) | 0.0086 (3)* | |
N1 | 0.0164 (8) | 0.3978 (4) | 0.8194 (9) | 0.0086 (3)* | |
H11 | 0.076 (5) | 0.425 (3) | 0.893 (4) | 0.0086 (3)* | |
H12 | −0.058 (4) | 0.368 (3) | 0.871 (5) | 0.0086 (3)* | |
H13 | 0.077 (5) | 0.364 (2) | 0.760 (5) | 0.0086 (3)* | |
H14 | −0.030 (5) | 0.435 (2) | 0.753 (5) | 0.0086 (3)* | |
N2 | 0.9630 (8) | 0.3743 (4) | 0.3168 (9) | 0.0086 (3)* | |
H21 | 1.036 (4) | 0.363 (3) | 0.393 (5) | 0.0086 (3)* | |
H22 | 0.915 (6) | 0.3268 (16) | 0.287 (6) | 0.0086 (3)* | |
H23 | 1.009 (5) | 0.397 (3) | 0.229 (4) | 0.0086 (3)* | |
H24 | 0.891 (5) | 0.410 (3) | 0.358 (6) | 0.0086 (3)* | |
N3 | 0.6786 (6) | 0.4917 (4) | 0.1118 (7) | 0.0086 (3)* | |
H31 | 0.755 (4) | 0.530 (2) | 0.095 (6) | 0.0086 (3)* | |
H32 | 0.668 (5) | 0.483 (3) | 0.2196 (14) | 0.0086 (3)* | |
H33 | 0.704 (5) | 0.4438 (18) | 0.062 (5) | 0.0086 (3)* | |
H34 | 0.587 (3) | 0.511 (3) | 0.071 (5) | 0.0086 (3)* |
P1—Al1 | 2.975 (5) | O3—P1 | 1.573 (6) |
P1—Al2i | 3.064 (5) | O3—Al1 | 1.724 (7) |
P1—O1 | 1.493 (6) | O4—P1iv | 1.522 (7) |
P1—O2 | 1.550 (7) | O4—Al2 | 1.737 (7) |
P1—O3 | 1.573 (6) | O5—P2 | 1.532 (6) |
P1—O4i | 1.522 (7) | O5—H21viii | 1.953 (13) |
P2—Al2 | 3.038 (4) | O5—H31ix | 1.97 (3) |
P2—O5 | 1.532 (6) | O6—P2 | 1.493 (7) |
P2—O6 | 1.493 (7) | O6—Al2iii | 1.753 (7) |
P2—O7 | 1.532 (6) | O7—P2 | 1.532 (6) |
P2—O8 | 1.563 (6) | O7—Al2 | 1.748 (7) |
P3—Al1 | 3.062 (5) | O8—P2 | 1.563 (6) |
P3—Al2ii | 3.060 (5) | O8—Al1 | 1.730 (7) |
P3—O9 | 1.484 (5) | O9—P3 | 1.484 (5) |
P3—O10 | 1.485 (6) | O9—H14x | 1.828 (10) |
P3—O11i | 1.487 (5) | O9—H23viii | 1.88 (3) |
P3—O12 | 1.567 (6) | O10—P3 | 1.485 (6) |
Al1—P1 | 2.975 (5) | O10—Al2ii | 1.780 (7) |
Al1—P3 | 3.062 (5) | O11—P3iv | 1.487 (5) |
Al1—O2iii | 1.732 (7) | O11—H24ix | 1.868 (10) |
Al1—O3 | 1.724 (7) | O11—H32ix | 1.84 (2) |
Al1—O8 | 1.730 (7) | O12—P3 | 1.567 (6) |
Al1—O12 | 1.727 (6) | O12—Al1 | 1.727 (6) |
Al2—P1iv | 3.064 (5) | N1—H11 | 0.9526 (1) |
Al2—P2 | 3.038 (4) | N1—H12 | 0.9526 (1) |
Al2—P3v | 3.060 (5) | N1—H13 | 0.9526 (1) |
Al2—O4 | 1.737 (7) | N1—H14 | 0.9526 |
Al2—O6vi | 1.753 (7) | N2—H21 | 0.9526 (1) |
Al2—O7 | 1.748 (7) | N2—H22 | 0.9526 (1) |
Al2—O10v | 1.780 (7) | N2—H23 | 0.9526 (1) |
O1—P1 | 1.493 (6) | N2—H24 | 0.9526 (1) |
O1—H12vii | 1.88 (2) | N3—H31 | 0.9526 (1) |
O1—H33vi | 1.897 (15) | N3—H32 | 0.9526 (1) |
O2—P1 | 1.550 (7) | N3—H33 | 0.9526 (1) |
O2—Al1vi | 1.732 (7) | N3—H34 | 0.9526 (1) |
O1—P1—O2 | 112.1 (4) | O6vi—Al2—O10v | 109.6 (3) |
O1—P1—O3 | 111.3 (4) | O7—Al2—O10v | 108.1 (3) |
O1—P1—O4i | 114.6 (4) | P1—O2—Al1vi | 147.3 (5) |
O2—P1—O3 | 106.1 (4) | P1—O3—Al1 | 128.9 (4) |
O2—P1—O4i | 106.9 (4) | P1iv—O4—Al2 | 140.1 (4) |
O3—P1—O4i | 105.4 (4) | P2—O6—Al2iii | 161.9 (5) |
O5—P2—O6 | 110.3 (4) | P2—O7—Al2 | 135.6 (5) |
O5—P2—O7 | 113.1 (4) | P2—O8—Al1 | 150.4 (4) |
O5—P2—O8 | 108.9 (4) | P3—O10—Al2ii | 139.0 (5) |
O6—P2—O7 | 109.2 (4) | P3—O12—Al1 | 136.7 (5) |
O6—P2—O8 | 107.8 (4) | H11—N1—H12 | 109.4713 (9) |
O7—P2—O8 | 107.4 (4) | H11—N1—H13 | 109.4719 (6) |
O9—P3—O10 | 111.1 (4) | H11—N1—H14 | 109.4706 |
O9—P3—O11i | 111.3 (4) | H12—N1—H13 | 109.4715 (1) |
O9—P3—O12 | 111.7 (4) | H12—N1—H14 | 109.4704 |
O10—P3—O11i | 110.0 (4) | H13—N1—H14 | 109.4715 (5) |
O10—P3—O12 | 103.2 (3) | H21—N2—H22 | 109.4716 (7) |
O11i—P3—O12 | 109.3 (4) | H21—N2—H23 | 109.4710 (4) |
O2iii—Al1—O3 | 113.8 (4) | H21—N2—H24 | 109.4716 (4) |
O2iii—Al1—O8 | 105.8 (4) | H22—N2—H23 | 109.4707 |
O2iii—Al1—O12 | 108.6 (4) | H22—N2—H24 | 109.4717 (8) |
O3—Al1—O8 | 104.1 (3) | H23—N2—H24 | 109.4706 (7) |
O3—Al1—O12 | 107.6 (4) | H31—N3—H32 | 109.4709 |
O8—Al1—O12 | 117.2 (4) | H31—N3—H33 | 109.4710 (5) |
O4—Al2—O6vi | 108.1 (3) | H31—N3—H34 | 109.4709 (1) |
O4—Al2—O7 | 109.8 (3) | H32—N3—H33 | 109.4717 |
O4—Al2—O10v | 108.5 (4) | H32—N3—H34 | 109.472 |
O6vi—Al2—O7 | 112.6 (4) | H33—N3—H34 | 109.4709 |
Symmetry codes: (i) x, y, z−1; (ii) −x+1/2, y+1/2, z−1/2; (iii) x+1/2, −y+1/2, z; (iv) x, y, z+1; (v) −x+1/2, y−1/2, z+1/2; (vi) x−1/2, −y+1/2, z; (vii) x+1/2, −y+1/2, z−1; (viii) x−1, y, z; (ix) −x+1, −y+1, z+1/2; (x) −x, −y+1, z−1/2. |
D—H···A | D—H | H···A | D···A | D—H···A |
N1—H11···O9iv | 0.95 (4) | 2.39 (4) | 3.250 (10) | 151 (3) |
N1—H11···O11 | 0.95 (4) | 2.35 (5) | 3.163 (8) | 143 (3) |
N1—H12···O1xi | 0.95 (4) | 1.88 (4) | 2.791 (10) | 159 (3) |
N1—H13···O5 | 0.95 (4) | 2.14 (4) | 2.934 (10) | 141 (3) |
N1—H14···O9xii | 0.95 (4) | 1.83 (4) | 2.776 (9) | 173 (3) |
N2—H21···O5xiii | 0.95 (4) | 1.96 (4) | 2.896 (10) | 170 (4) |
N2—H22···O8iii | 0.95 (4) | 2.31 (3) | 3.216 (10) | 158 (4) |
N2—H23···O9xiii | 0.95 (4) | 1.89 (5) | 2.738 (9) | 148 (4) |
N2—H24···O11xiv | 0.96 (4) | 1.86 (4) | 2.818 (9) | 174 (5) |
N3—H31···O5xiv | 0.96 (4) | 1.97 (4) | 2.821 (9) | 147 (3) |
N3—H32···O11xiv | 0.952 (15) | 1.85 (2) | 2.728 (8) | 153 (4) |
N3—H33···O1iii | 0.95 (3) | 1.90 (3) | 2.823 (9) | 164 (4) |
N3—H34···O12 | 0.96 (3) | 2.37 (4) | 2.925 (8) | 117 (4) |
Symmetry codes: (iii) x+1/2, −y+1/2, z; (iv) x, y, z+1; (xi) x−1/2, −y+1/2, z+1; (xii) −x, −y+1, z+1/2; (xiii) x+1, y, z; (xiv) −x+1, −y+1, z−1/2. |
Compound | O11—A1 | O11—A2 | O11—A3 | O11—P3 | Reference |
(NH4)3Al2(PO4)3 | 3.162 | 2.818 | 2.727 | 1.487 | This work |
SIZ-2 (A = NH4) | 3.090 | 2.834 | 2.688 | 1.496 | Cooper et al. (2004) |
K3Al2(PO4)3 | 2.754 | 2.824 | 2.722 | 1.487 | Devi & Vidyasagar (2000) |
K3Al2(AsO4)2(PO4) | 3.025 | 2.743 | 2.621 | 1.673 | Boughzala et al. (1997) |
For each of the compounds, the atomic numbering scheme of the current (NH4)3Al2(PO4)3 refinement has been utilized. For the first two compounds, A = NH4, while for the second two, A = K. For the As-containing compound, the P3 site is reported to have the highest occupancy of As at 0.86. |
Acknowledgements
We thank UOP for funding and allowing this publication. Use of the Advanced Photon Source at Argonne National Laboratory was supported by the US Department of Energy, Office of Science, Office of Basic Energy Sciences, under Contract No. DE-AC02–06CH11357. We acknowledge E. Fulmer, C. L. Nicholas and S. T. Wilson for helpful discussions and J. F. Kotek and A. Stolarski for the ICP and SEM results.
Funding information
Funding for this research was provided by: UOP LLC.
References
Boughzala, H., Driss, A. & Jouini, T. (1997). Acta Cryst. C53, 3–5. CrossRef ICSD CAS Web of Science IUCr Journals Google Scholar
Byrne, P. J., Warren, J. E., Morris, R. E. & Ashbrook, S. E. (2009). Solid State Sci. 11, 1001–1006. CrossRef CAS Google Scholar
Cooper, E. R., Andrews, C. D., Wheatley, P. S., Webb, P. B., Wormald, P. & Morris, R. E. (2004). Nature, 430, 1012–1016. Web of Science CSD CrossRef ICSD PubMed CAS Google Scholar
Das, S. K., Bhunia, M. K. & Bhaumik, A. (2012). Microporous Mesoporous Mater. 155, 258–264. CrossRef CAS Google Scholar
Devi, R. N. & Vidyasagar, K. (2000). Inorg. Chem. 39, 2391–2396. CrossRef ICSD PubMed CAS Google Scholar
Larson, A. C. & Von Dreele, R. B. (2000). General Structure Analysis System (GSAS). Report LAUR, 86–748 Los Alamos National Laboratory, New Mexico, USA. Google Scholar
Li, Y., Yu, J. & Xu, R. (2019). URL of AlPO database (freely accessible): https://mezeopor.jlu.edu.cn/alpo/alpo.jsp Google Scholar
Ma, H., Tian, Z., Xu, R., Wang, B., Wei, Y., Wang, L., Xu, Y., Zhang, W. & Lin, L. (2008). J. Am. Chem. Soc. 130, 8120–8121. CrossRef PubMed CAS Google Scholar
Medina, M. E., Iglesias, M., Gutiérrez-Puebla, E. & Monge, M. A. (2004). J. Mater. Chem. 14, 845–850. CrossRef CAS Google Scholar
Morris, R. E. (2009). Chem. Commun. pp. 2990–2998. Web of Science CrossRef Google Scholar
Oliver, S., Kuperman, A., Lough, A. & Ozin, G. A. (1996). Chem. Commun. pp. 1761–1762. CSD CrossRef Google Scholar
Palmer, D. (2005). CrystalMaker. CrystalMaker Software Ltd, Yarnton, England. Google Scholar
Parnham, E. & Morris, R. E. (2007). Acc. Chem. Res. 40, 1005–1013. CrossRef PubMed CAS Google Scholar
Richardson, J. W. & Vogt, E. T. C. (1992). Zeolites, 12, 13–19. CrossRef ICSD CAS Google Scholar
Shannon, R. D. (1976). Acta Cryst. A32, 751–767. CrossRef CAS IUCr Journals Web of Science Google Scholar
Sidey, V. (2016). Acta Cryst. B72, 626–633. Web of Science CrossRef IUCr Journals Google Scholar
Stöger, B. & Weil, M. (2012). Acta Cryst. E68, i15. CrossRef ICSD IUCr Journals Google Scholar
Vaughan, D. E. W., Yennawar, H. P. & Perrotta, A. J. (2012). Microporous Mesoporous Mater. 153, 18–23. CrossRef ICSD CAS Google Scholar
Wei, Y., Marler, B., Zhang, L., Tian, Z., Graetsch, H. & Gies, H. (2012). Dalton Trans. 41, 12408–12415. CSD CrossRef CAS PubMed Google Scholar
Westrip, S. P. (2010). J. Appl. Cryst. 43, 920–925. Web of Science CrossRef CAS IUCr Journals Google Scholar
Wilson, S. T. (2007). Introduction to Zeolite Science and Practice, 3rd ed, edited by J. Čejka, H. van Bekkum, A. Corma, & F. Schüth, ch. 4, pp. 105–135. Amsterdam: Elsevier. Google Scholar
Wilson, S. T., Lok, B. M., Messina, C. A., Cannan, T. R. & Flanigen, E. M. (1982). J. Am. Chem. Soc. 104, 1146–1147. CrossRef CAS Web of Science Google Scholar
Xing, H., Li, J., Yan, W., Chen, P., Jin, Z., Yu, J., Dai, S. & Xu, R. (2008). Chem. Mater. 20, 4179–4181. CSD CrossRef CAS Google Scholar
Xing, H., Li, Y., Su, T., Xu, J., Yang, W., Zhu, E., Yu, J. & Xu, R. (2010). Dalton Trans. 39, 1713–1715. CrossRef ICSD CAS PubMed Google Scholar
Yu, J. & Xu, R. (2006). Chem. Soc. Rev. 35, 593–604. Web of Science CrossRef PubMed CAS 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.