Methods and systems for stimulating light tight shale oil formations to recover hydrocarbons from the formations. One embodiment includes positioning a downhole burner in a first well, supplying a fuel, oxidizer, and water to the burner to form steam, injecting the steam and surplus oxygen into the shale reservoir to form a heated zone within the shale reservoir, wherein the surplus oxygen reacts with hydrocarbons in the reservoir to generate heat; wherein the heat from the reactions with the hydrocarbons and the steam increases permeability in a kerogen-rich portion of the shale reservoir, and producing hydrocarbons from the shale reservoir.

Microfluidic structures and methods for manipulating fluids, fluid components, and reactions are provided. In one aspect, such structures and methods can allow production of droplets of a precise volume, which can be stored/maintained at precise regions of the device. In another aspect, microfluidic structures and methods described herein are designed for containing and positioning components in an arrangement such that the components can be manipulated and then tracked even after manipulation. For example, cells may be constrained in an arrangement in microfluidic structures described herein to facilitate tracking during their growth and/or after they multiply.

A geothermal reservoir induces gasification and water gas shift reactions to generate hydrogen. The hydrogen or protons are produced to surface by using hydrogen-only or proton-only membranes in production wells. Energy from the reservoir is produced to surface as protons or hydrogen.

A hydrocarbon reservoir is treated with heat to induce gasification, water-gas shift, and/or aquathermolysis reactions to generate gases including hydrogen. The hydrogen alone is produced to the surface by using hydrogen-only membranes in the production wells.

A hydrocarbon reservoir is treated with heat to induce gasification, water-gas shift, and/or aquathermolysis reactions to generate gases including hydrogen. The hydrogen alone is produced to the surface by using hydrogen-only membranes in the production wells.

The application discloses an integrated method and structure for in-situ hydrogen production from coal seams and coalbed methane exploitation, belonging to the technical field of energy exploitation. The method comprises: injecting gasification agent through an injection well, exploiting coalbed methane and gasification gas through a production well. The injection well is a stepped horizontal well, the injection well is provided with at least one, and the projections of the horizontal sections of any two injection wells in the vertical direction do not overlap. At least one horizontal section of the stepped horizontal well is arranged in any coal seam to be mined. The method of the present application avoids the large-area continuous gasification of a single coal seam and the repeated position gasification of overlapping multiple coal seams, reduces the change range and degree of formation stress, disperses the underground void volume, reduces the risk of formation or ground collapse.

Methods and systems for gasifying coal are disclosed herein. In some embodiments, a representative coal gasification system can comprise (i) an injection well extending from a ground surface to an underground coal gasification (UCG) reaction region of a coal seam; (ii) a production well spaced apart from the injection well and extending from the ground surface to the UCG reaction region, and (iii) conduits each extending from the ground surface to areas of the coal seam. End portions of the conduits within the coal can be laterally peripheral to the UCG reaction region. The conduits are configured to deliver a primary fluid from the ground surface to the primary region, the injection well is configured to deliver an oxidant gas to the UCG reaction region, and the production well is configured to deliver the product gas from the UCG reaction region to the ground surface.

A system for removing methane from subterranean clathrates includes an oxidant source, a feed pipe, a recovery pipe, and an ignition source. The feed pipe includes an inlet end in fluid communication with the oxidant source and an outlet end configured to be disposed within a subterranean deposit that includes a stored methane gas disposed within a clathrate hydrate. The recovery pipe includes a first end disposed within the subterranean deposit and a second end opposite the first end configured to engage a storage device. The ignition source is configured to trigger a combustion reaction to melt the clathrate hydrate to produce a released methane gas. A first portion of the released methane gas travels along a recovery flow path through the recovery pipe and a second portion of the released methane gas combusts with the oxidant in-situ to perpetuate the combustion reaction.

A system for removing methane from subterranean clathrates includes an oxidant source, a feed pipe, a recovery pipe, and an ignition source. The feed pipe includes an inlet end in fluid communication with the oxidant source and an outlet end configured to be disposed within a subterranean deposit that includes a stored methane gas disposed within a clathrate hydrate. The recovery pipe includes a first end disposed within the subterranean deposit and a second end opposite the first end configured to engage a storage device. The ignition source is configured to trigger a combustion reaction to melt the clathrate hydrate to produce a released methane gas. A first portion of the released methane gas travels along a recovery flow path through the recovery pipe and a second portion of the released methane gas combusts with the oxidant in-situ to perpetuate the combustion reaction.

The present invention is a process for the thermobaric production of hydrocarbons from natural reservoirs through conventional wells. The hydrocarbons are converted into corresponding vapor phase fractions in the downhole. Such conversion is accomplished through the use of a combination of gasifying agents, heated atmospheric air, and steam—all pumped into the downhole. Temperature and pressure gradients that develop in the reservoir lead to disintegration of low-porosity rock and decompaction of impermeable rock. The vapor phase fractions are recovered at the well head and condensed on-site into high quality liquid and gaseous products.