Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

Experimental determination of smectite hydration states under diagenetic conditions

Conference · · Am. Assoc. Pet. Geol., Bull.; (United States)
OSTI ID:6641981
Knowledge of the hydration state of smectite under burial diagenetic conditions is necessary for the interpretation of the smectite to illite transformation, abnormal fluid pressure development, and reservoir properties. Simple changes in fluid composition, pressure, or temperature have been thought to affect the nu calculated for 80 cases of kerogen maturation at maximum temperature show a strong linear relationship (r = 0.77). The pseudo Eanges, suggest this occurs in 10/sup 6/-10/sup 7/ years. When plotted on an Arrhenius diagram (ln k versus l/T), reaction rate constantstion (to the 99% level). Geologic field data, and kerogen maturation experiments extrapolated to geologic time and temperature rer, (high E/sub a/) reactions geologically significant. Thus, the functional reaction to essentially complete hydrocarbon generaCheto montmorillonite in 1 molal NaCl solution under 15.1 MPa (2200 psi) pressure, to at least 175/sup 0/C, and in the same solution under 3.4 MPa (500 psi) to 125/sup 0/C. Two layers of water are also retained by Cheto montmorillonite in 5 molal NaCl solution 200/sup 0/C under pressures of 4.83 MPa (700 psi) and 46.2 MPa (6700 psi). This experimental evidence contradicts the previously suggested mechanism for generating fluid overpressuring in shales by simple thermal dehydration of smectite under burial conditions. Experiments done with dilute NaCl solutions demonstrate the effect of concentration on the swelling of smectite at depth, while experiments with KCl solutions illustrate the effect of the interlayer cation on the hydration state of the clay.
Research Organization:
Univ. of Illinois, Urbana
OSTI ID:
6641981
Report Number(s):
CONF-8405216-
Conference Information:
Journal Name: Am. Assoc. Pet. Geol., Bull.; (United States) Journal Volume: 68:4
Country of Publication:
United States
Language:
English