Abstract:
Embodiments of the present invention relate to heater patterns and related methods of producing hydrocarbon fluids from a subsurface hydrocarbon-containing formation (for example, an oil shale formation) where a heater cell may be divided into nested inner and outer zones. Production wells may be located within one or both zones. In the smaller inner zone, heaters may be arranged at a relatively high spatial density while in the larger surrounding outer zone, a heater spatial density may be significantly lower. Due to the higher heater density, a rate of temperature increase in the smaller inner zone of the subsurface exceeds that of the larger outer zone, and a rate of hydrocarbon fluid production ramps up faster in the inner zone than in the outer zone. In some embodiments, a ratio between a half-maximum sustained production time and a half-maximum rise time of a hydrocarbon fluid production function is relatively large.
Abstract:
Some embodiments relate to a method for producing, from sulfur-rich type IIs kerogen, a sweetened synthetic crude having a sulfur concentration of at most 1% wt/wt, a nitrogen concentration of at most 0.2% wt/wt and an API gravity of at least 30°. Hydrotreating is performed under only low-severity conditions of at most about 350 degrees Celsius and a maximum pressure of at most 120 atmospheres. In some embodiments, the feedstock to the hydrotreater comprises hydrocarbon pyrolysis liquids generated primarily by low temperature pyrolysis of the sulfur-rich type IIs kerogen. For example, the feedstock may be rich in easier-to-hydrotreat heterocyclic species. In some embodiments, it is possible to optimize the pyrolysis process by monitoring relative concentrations of the easier-to- hydrotreat heterocyclics and the harder-to-treat heterocyclics.
Abstract:
Embodiments of the present invention relate to heater patterns and related methods of producing hydrocarbon fluids from a subsurface hydrocarbon-containing formation (for example, an oil shale formation) where a heater cell may be divided into nested inner and outer zones. Production wells may be located within one or both zones. In the smaller inner zone, heaters may be arranged at a relatively high spatial density while in the larger surrounding outer zone, a heater spatial density may be significantly lower. Due to the higher heater density, a rate of temperature increase in the smaller inner zone of the subsurface exceeds that of the larger outer zone, and a rate of hydrocarbon fluid production ramps up faster in the inner zone than in the outer zone. In some embodiments, a ratio between a half-maximum sustained production time and a half-maximum rise time of a hydrocarbon fluid production function is relatively large.
Abstract:
Some embodiments of the present invention relate to the use of wind-electricity to produce unconventional oil from a kerogen-containing or bitumen-containing subsurface formation. A heater cell may be divided into nested inner and outer zones. In the smaller inner zone, heaters may be arranged at a relatively high spatial density while in the larger surrounding outer zone, a heater spatial density may be significantly lower. Due to the higher heater density, a rate of temperature increase in the smaller inner zone of the subsurface exceeds that of the larger outer zone, and a rate of hydrocarbon fluid production ramps up faster in the inner zone than in the outer zone. In some embodiments, at least a majority of the heaters in the inner zone are powered primarily by fuel combustion and at least a majority of heaters in the outer zone are powered primarily by electricity generated by wind. Alternatively, in other embodiments, at least a majority of the heaters in the inner zone are powered primarily by electricity generated by wind and at least a majority of heaters in the outer zone are powered primarily by fuel combustion.
Abstract:
A hydrocarbon strategic reserve method comprises operating production wells deployed in a post-pyrolysis oil shale formation at significantly elevated wellhead pressures for an extended period of time so as to store hot hydrocarbon fluids within pore space thereof. In some embodiments, the hydrocarbon fluids are stored at a depth of at least 100 meters or at least 200 meters or at least 300 meters. In some embodiments, the hydrocarbon fluids are stored substantially at or above bubble point curve thereof.
Abstract:
Embodiments of the present invention relate to a method and system for pyrolyzing kerogen or mobilizing bitumen using thermal energy of a carbonate molten salt mixture having a melting point of at most 395 degrees Celsius or at most 390 degrees Celsius or at most 385 degrees Celsius. The carbonate molten salt may include lithium cations (e.g. at a cationic molar concentration of at least 0.2) and/or relatively small quantities of nitrates (e.g. at an anionic molar concentration of at least 0.01 and at most 0.1). Preferably, the molten salt mixture is non-oxidizing or non-explosive when brought into contact with crude oil.
Abstract:
A method is disclosed for generating an areal map of a pre-determined hydrocarbon liquid property of a subsurface kerogen-containing source rock from an electromagnetic resistivity profile. Preferably, the profile is generated by a transient EM method such as a long-offset transient electromagnetic (LOTEM) method. In some embodiments, the areal map is generated by employing resistivity-hydrocarbon liquid-quality relationship data describing a relationship between (i) a property of hydrocarbon liquid generated within the source rock pore space to (ii) an electrical resistivity of the source rock. In some embodiments, it is possible to acquire such data even in the absence of source rock samples where the hydrocarbon liquids within the samples has been preserved. The areal map is useful for determining a target location and/or depth in the source rock to drill for oil. The presently-disclosed techniques are particularly relevant to tight oil formations.
Abstract:
An L-shaped or U-shaped subsurface heater assembly (e.g. a molten salt heater) having a catenary trajectory is disclosed herein. In some embodiments, the heater is configured to operate at an operating temperature T OPERATE of at least 450 degrees Celsius, or at least 500 degrees Celsius, or at least 550 degrees Celsius, or at least 600 degrees Celsius. In some embodiments, at least a heel section follows a catenary trajectory characterized by a catenary coefficient a having a value of at least 200 or at least 300 or at least 400. In some embodiments, at least the heel section of the heater is constructed of a nickel-free and/or chromium steel alloy, such as P91 steel. Although the creep rupture strength of this steel alloy is significantly less than those of more expensive austenitic stainless steels, the subsurface heater has high-temperature stability against creep rupture due to the catenary trajectory. Methods of operating the presently disclosed subsurface heater assembly to produce and/or mobilize hydrocarbon fluids are disclosed herein.
Abstract:
Embodiments of the present invention relate to heat transfer fluids (e.g. molten-salt) as a thermal buffer for heating, by thermal energy derived from wind-generated electricity, at least one of (i) a subsurface hydrocarbon-containing formation or (ii) a bed of hydrocarbon-containing rocks. During times when 5 wind is plentiful, wind electricity is used to heat the heat transfer fluid - e.g. by means of an electrically resistive heater immersed in the heat transfer fluid. At any time, thermal energy from the wind electricity may be transferred to the hydrocarbon-containing rocks or subsurface formation by the heat transfer fluid. In some embodiments, the fluid is 10 heated both by wind-generated electricity and by solar radiation. Some embodiments relate to a subsurface molten salt heater (e.g. powered by wind-generated electricity) having a non-thermally insulation portion through which molten salt flows. The heater is configured to maintain a temperature of the circulating molten salt, throughout the substantially non-thermally-insulated portion, at a temperature significantly above a 15 melt temperature of the molten salt.
Abstract:
In some embodiments, a pyrolysis method comprises: a. heating kerogen or bitumen to initiate pyrolysis so that a stream of pyrolysis formation gases is recovered via production wells or production conduits; b. monitoring or estimating a concentration of acid gas within the gas stream; c. contingent upon an acid gas concentration being below a threshold value, subjecting pyrolysis gases of the stream to sequestration; and d. responding to an estimated or monitored increase in acid gas concentration of the gas stream by performing at least one of: i. subjecting a greater fraction of the stream to an acid gas separation process and/or acid gas elimination process; and ii. subjecting a lesser fraction of the stream to a sequestration. The presently disclosed teachings are applicable both to in situ pyrolysis and to pyrolysis performed within an enclosure such as a pit.