A method and device for in-situ determination of formation thermal parameters, a terminal and a storage medium

CN121827802BActive Publication Date: 2026-08-28CHINA UNIV OF GEOSCIENCES (BEIJING)
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Patent Information

Application Number
CN202512018795.X
Authority / Receiving Office
CN · China
Patent Type
Patents(China)
Current Assignee / Owner
Filing Date
2025-12-30
Publication Date
2026-08-28
Estimated Expiration
2045-12-30

AI Technical Summary

Technical Problem

[0003]本发明的目的在于提供一种地层热物性参数的原位测定方法、装置、终端及储存介质,旨在解决现有技术中难以实现快速获取地层温度梯度,精确评价地热资源量的技术问题

Benefits of technology

[0011]本发明提供的地层热物性参数的原位测定方法的有益效果在于:与现有技术相比,本发明通过使井壁取心仪下放到待测地层深度,弹出支撑装置,使支撑装置支撑井壁取心仪并使其稳定停留在待测地层,使用井壁取心仪钻取待测岩心;启动热参数测定装置并测定待测岩心温度变化导致的所述电阻丝电阻变化值;根据所述电阻丝基本物理参数、温度变化与电阻变化的关系、各热物性参数之间数学关系,计算各个测试点的岩心热物性参数;根据各个测试点的岩心热物性参数,计算全井段地层温度梯度,具有能够测定地层热物性参数,计算全井段地层温度梯度,实现快速获取地温梯度,精确评价地热资源量的技术效果。

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Abstract

The application provides a formation thermal parameter in-situ measurement method, device, terminal and storage medium, belongs to the technical field of full well section formation thermal parameter measurement, and the measurement method comprises the following steps: starting a drilling rig lifting device, lowering a sidewall coring instrument to a formation depth to be measured, and drilling a core to be measured by using the sidewall coring instrument; starting a thermal parameter measurement device, heating a resistance wire at a constant power, and measuring a resistance change value of the resistance wire caused by temperature change of the core to be measured; according to a basic physical parameter of the resistance wire, a relationship between temperature change and resistance change, and a mathematical relationship between thermal parameters, core thermal parameters of each test point are calculated, and a formation temperature gradient of a full well section is calculated. The application provides the formation thermal parameter in-situ measurement method, device, terminal and storage medium, which has the technical effects that formation thermal parameters can be measured, a formation temperature gradient of a full well section can be calculated, a formation temperature gradient can be quickly obtained, and a geothermal resource amount can be accurately evaluated.
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Citation Information

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