The Defect Structure of Kaolinite
{'Code': '06030107', 'Directorate': {'Abbreviation': 'GEO', 'LongName': 'Directorate For Geosciences'}, 'Division': {'Abbreviation': 'EAR', 'LongName': 'Division Of Earth Sciences'}}
{'SignBlockName': 'Felicia Fauntleroy', 'PO_EMAI': None, 'PO_PHON': None}
Several aspects of kaolinites (clays) will be investigated: 1)                  what possible defects are present in kaolinites, 2) do kaolinites               from different geologic origins have different defect structures,                                                                                               3) for those samples which appear to be mixtures of two                         kaolinites, can the two constituents be separated (if so, how do                they differ crystallographically and chemically), 4) in kaolinite                                                                                               samples which show different crystal morphologies, are                          themorphologies related to different defect structures, 5) is                   there                                                                           a relation between the  defect structure of a kaolinite and its                 chemical composition, 6) is there a relation between the defect                 structure of a kaolinite and its ability to intercalate organic                 compounds?  In addition to their scientific interest, clays are                 extremely important industrial and agricultural materials and                   their properties are critical to industrial and agricultural                    processes.
{'FirstName': 'Rossman', 'LastName': 'Giese', 'PI_MID_INIT': 'F', 'PI_SUFX_NAME': 'Jr.', 'PI_FULL_NAME': 'Rossman F Giese', 'EmailAddress': None, 'NSF_ID': '000186136', 'StartDate': '02/15/1989', 'EndDate': None, 'RoleCode': 'Principal Investigator'}
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{'Code': '1573', 'Text': 'Petrology and Geochemistry'}
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