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Suzhou Grand Energy Technology Co., Ltd. was founded under the leadership of a national innovation talent team. It is a technology innovation oriented enterprise supported by the Suzhou Municipal Government, integrating instrument research and development, sales, and technical services. Adhering to independent innovation
Relying on the self-developed portable rock moisture collector, we carry out the determination of water content of fresh core samples from the well site, avoiding the error caused by the change of temperature conditions during the transportation and cutting of the samples.In conjunction with porosit
(1) Carbonate Cluster IsotopesCarbonate cluster isotopes (Δ47) are measured using a MAT253 mass spectrometer. Carbonate minerals are converted to pure CO2 gas, which is carried by helium into the ion source, where it is transformed into charged ions under the action of electron bombardment, and the
The gold tube hydrocarbon generation simulation is the most commonly used experimental system in the simulation of oil and gas generation from closed systems, hydrocarbon generation kinetics, and carbon isotope kinetics research. Utilizing the chemical reaction inertness and plasticity of gold, a cl
Taking the seepage mechanics of porous nano media as the theoretical basis, combining with the experimental data of shale gas desorption in the present field, and considering the initial pore pressure and mud density and other parameters, we use the self-developed shale core gas content calculation
Methane isothermal adsorption experiment is the main means of evaluating the adsorption capacity of shale, and according to the national standard GB/T 35210.1-2017 Method for Determination of Isothermal Adsorption of Methane from Shale Part 1: Volumetric Method, a high-pressure isothermal adsorption
The co-development of shale matrix laminations and nanopores leads to obvious anisotropy and pressure sensitivity of gas permeability, which has a large impact on gas reservoir simulation. The change curves of gas permeability and pressure in different directions of the test cube rock samples are ca