Interactions between organic acids anions in formation waters and reservoir mineral phases
暂无分享,去创建一个
[1] S. Ehrenberg. Kaolinized, potassium-leached zones at the contacts of the Garn Formation, Haltenbanken, mid-Norwegian continental shelf , 1991 .
[2] T. Barth. Organic acids and inorganic ions in waters from petroleum reservoirs, Norwegian continental shelf: a multivariate statistical analysis and comparison with American reservoir formation waters , 1991 .
[3] D. Manning,et al. An exploratory study of acetate decomposition and dissolution of quartz and Pb-rich potassium feldspar at 150°C, 50 MPa (500 bars) , 1991, Mineralogical Magazine.
[4] E. Pittman,et al. Secondary porosity revisited; the chemistry of feldspar dissolution by carboxylic acids and anions , 1990 .
[5] R. Ewing,et al. The effect of carboxylic acid anions on the stability of framework mineral grains in petroleum reservoirs , 1990 .
[6] J. Fisher,et al. Water-rock interaction in tertiary sandstones, San Joaquin basin, California, U.S.A. : diagenetic controls on water composition , 1990 .
[7] S. Ehrenberg,et al. Correlation of carbon dioxide abundance with temperature in clastic hydrocarbon reservoirs: relationship to inorganic chemical equilibrium , 1989 .
[8] L. Land,et al. Carbonate equilibria and pH buffering by organic acids — Response to changes in pCO2 , 1989 .
[9] H. Heasler,et al. Organic-Inorganic Interactions and Sandstone Diagenesis , 1989 .
[10] D. Savage,et al. The effect of organic acids on the dissolution of K-feldspar under conditions relevant to burial diagenesis , 1989, Mineralogical Magazine.
[11] E. Shock. Organic acid metastability in sedimentary basins , 1988 .
[12] Leif A. Hoyland,et al. Statfjord field: development strategy and reservoir management , 1988 .
[13] P. Bennett,et al. The dissolution of quartz in dilute aqueous solutions of organic acids at 25°C , 1988 .
[14] R. Surdam,et al. Difunctional carboxylic acid anions in oilfield waters , 1988 .
[15] T. Barth. Quantitative determination of volatile carboxylic acids in formation waters by isotachophoresis , 1987 .
[16] R. Surdam,et al. Oilfield waters and sandstone diagenesis , 1987 .
[17] J. Fisher. Distribution and occurrence of aliphatic acid anions in deep subsurface waters , 1987 .
[18] J. Drever,et al. The effect of oxalate on the dissolution rates of oligoclase and tremolite , 1987 .
[19] R. Morton,et al. Regional Variations in Formation Water Chemistry, Frio Formation (Oligocene), Texas Gulf Coast , 1987 .
[20] N. Hubbard,et al. Short-chain aliphatic acid anions in deep subsurface brines: A review of their origin, occurrence, properties, and importance and new data on their distribution and geochemical implications in the Palo Duro Basin, Texas , 1987 .
[21] P. Bennett,et al. Increased solubility of quartz in water due to complexing by organic compounds , 1987, Nature.
[22] Y. Kharaka,et al. Role of Organic Species Dissolved in Formation Waters from Sedimentary Basins in Mineral Diagenesis , 1986 .
[23] J. Hanor,et al. Distribution of dissolved volatile fatty acids in some Louisiana oil field brines , 1986 .
[24] Y. Kharaka,et al. Aliphatic Acid Anions in Oil-Field Waters--Implications for Origin of Natural Gas , 1978 .
[25] A. Wilson,et al. The absorptiometric determination of aluminium in water. A comparison of some chromogenic reagents and the development of an improved method. , 1974, The Analyst.