Reports: G10
47601-G10 DNA-Derived Building Blocks for the Construction of Porous Metal-Organic Framework Materials
Bio-MOF Construction
For CO2 capture, we have focused on using adenine as a linking biomolecule because it has an amino group and pyrimidine nitrogens. We note that alkylamine-containing liquids are currently used as chemisorbents for CO2 and therefore Lewis-basic amine sites within MOFs are expected to improve selectivity toward adsorption of CO2. In addition, adenine is rigid, which should facilitate formation of permanently porous frameworks, and it has multiple coordination modes. We have begun exploring the coordination chemistry of adenine in the context of forming bio-MOFs and have successfully produced a number of new bio-MOF materials and other solid-state structures which are permanently porous and have interesting inclusion and adsorption properties. These materials and their CO2 adsorption properties are detailed below.
Zn6(adeninate)6(pyridine)6(dimethylcarbamate)6
This
material consists of macrocycles that self-assemble into a porous 3-D
structure. Single crystal X-ray
diffraction data revealed that six Zn2+ occupy the vertices of the
macrocycle and adeninates bridge the Zn2+ through their imidazolate
nitrogens. Each Zn2+ binds in a tetrahedral fashion to two adeninates,
one pyridine molecule, and one dimethylcarbamate anion (formed in situ). Since
only the imidazolate nitrogens of the adeninate coordinate the Zn2+,
N1 and the amino group remain available for hydrogen bonding. The macrocycles self-assemble into an extended
structure via cooperative adeninate-adeninate hydrogen bonding interactions.
This stucture consists of alternating layers of macrocycles that stack in an
a-b-c fashion. Each macrocycle forms a total of 12 hydrogen bonds (two per
adeninate) with its six nearest-neighbor macrocycles within the structure. This
packing motif results in the formation of cylindrical cavities (~ 5 × 20 Å)
arranged peridically throughout the 3-D structure. The confines of each cavity
are defined by one central macrocycle and fragments of the six nearest-neighbor
macrocycles. Inspection of the structure reveals that three pyridine rings
occlude the entrance to each cavity, resulting in an aperture measuring only
~1.2 Å. In order to access the cavities, we heated the material to remove a
portion of the pyridine molecules to increase the pore aperture and allow
diffusion of guest molecules within the structure. Remarkably, the powder X-ray
diffraction pattern of the heated sample matches that of the as-synthesized
material, indicating that the material maintains its structural integrity. After removing the coordinated pyridine via
heating, we found that the material can selectively adsorb CO2 over
N2 and that we could tune the selectivity by carefully controlling
the amount of pyridine stripped from the material. More details can be found in a recent paper. ADDIN EN.CITE
Bio-MOF-1
Unlike traditional MOFs, bio-MOF-1 consists of rigid metal-adeninate columnar building units which are connected together by biphenyldicarboxylate linking molecules to generate a 3-D MOF with 1-D pores. Other structural details are included in a recent publication. 2 Bio-MOF-1 is anionic; therefore, small cations are distributed within the channels to balance the charge. The cations are mobile and can be removed and replaced with a variety of other cationic molecules via simple cation exchange experiments. This aspect enables facile tuning of the pore size, shape, and functionality. Therefore, bio-MOF-1 can be used as a universal scaffold' to produce a variety of functionally unique materials simply by changing the identity of the guest cation species (vide infra). Powder diffraction experiments reveal that bio-MOF-1 is stable in a number of organic solvents, water, and biological buffers, indicating that it can be used in a variety of environments. It is also permanently porous with a BET surface are of approximately 1700 m2/g, as evidenced by gas sorption measurements performed on the evacuated material. These initial studies on bio-MOF-1 reveal several encouraging details regarding bio-MOFs: 1) they can exhibit high permanent porosity; 2) they can be exceptionally stable under a wide variety of conditions, including biological and environmental media; and 3) the functionality of their pores can be varied by performing facile cation-exchange experiments.
Anionic bio-MOF-1 and other anionic bio-MOFs present the opportunity to systematically study the influence of the counter-cation on the adsorption and recognition properties of the material. Instead of preparing a new MOF for every target application, we can simply substitute new cations into the pores of bio-MOF-1 to endow the pores with the requisite dimensions and functionality needed for particular applications. For example, we can introduce chiral cations to generate pores with chiral recognition capabilities, or we can introduce certain receptor molecules that endow the framework with sequestration capacity for specific target species. All of the cation-exchanged varieties of bio-MOF-1 exhibit the structural rigidity and stability of the parent material.
We have found that the identity of the adsorbed cation can significantly impact CO2 uptake capacity in a somewhat unusual fashion. Specifically, we studied the CO2 adsorption properties of bio-MOF-1 as a function of the size of the organic cation. The organic cations we chose were dimethylammonium (H2NMe2), tetramethylammonium (NMe4), and tetraethylammonium (NEt4). As the size of the organic cation increases, the BET surface area decreases, as expected. However, the capacity for CO2 uptake scales neither with the size of the organic cation nor the BET surface area. In fact, we found that the NMe4-exchanged material has the highest CO2 capacity, followed by NEt4. The as-synthesized material, which has the smallest cation, adsorbs the least amount of CO2. This result suggests that there may be an optimal pore size for CO2 adsorption.