干热岩,水力裂缝扩展,天然裂缝,采热,流-固-热耦合,非连续离散裂缝模型,换热,青海共和盆地


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,"/> <span>干热岩储层裂缝扩展及采热一体化数值模型</span>

吉林大学学报(地球科学版) ›› 2025, Vol. 55 ›› Issue (2): 575-586.doi: 10.13278/j.cnki.jjuese.20230138

• 地质工程与环境工程 • 上一篇    下一篇

干热岩储层裂缝扩展及采热一体化数值模型

考佳玮1, 杨康2, 谭鹏3, 陈作1   

  1. 1.中石化石油工程技术研究院有限公司,北京102206

    2.中国石油化工股份有限公司西北油田分公司石油工程监督中心,新疆轮台841600

    3.中国石油集团工程技术研究院有限公司,北京102206

  • 出版日期:2025-03-26 发布日期:2025-05-10
  • 基金资助:

    基金项目:国家自然科学基金项目(52192621)


Integrated Numerical Model of Fracture Propagation and Production in Dry Hot Rock Reservoir

Kao Jiawei1, Yang Kang2, Tan Peng3, Chen Zuo1   

  1. 1. SINOPEC Research Institute of Petroleum Engineering Co., Ltd., Beijing 102206, China

    2. Petroleum Engineering Supervision Center, Northwest Oilfield Branch Company, SINOPEC, Luntai 841600, Xinjiang, China

    3. CNPC Engineering Technology R&D Company Limited, Beijing 102206, China

  • Online:2025-03-26 Published:2025-05-10
  • Supported by:
    Supported by the National Natural Science Foundation of China (52192621)

摘要: 为准确评价干热岩储层压裂及其注采热效果,本文建立了一种流--热耦合的干热岩水力裂缝扩展数值模型,可以模拟干热岩复杂压裂裂缝形态,并进行注采热分析。以青海省共和盆地干热岩为研究对象,基于其地质力学参数特征建立了2个算例,并开展了干热岩多井压裂及采热过程模拟。结果表明:干热岩起裂裂缝受非均匀应力场扰动呈体积裂缝特征,水力裂缝遇天然裂缝可激活并形成复杂裂缝形态;多井间压裂裂缝可通过天然裂缝连通,为注采热提供超过95%的流动换热通道;注采热时,流体主要沿着贯通裂缝流动,形成换热优势通道,导致注采热初期出口温度降幅较大,在前3 a,出口水温下降幅度达30~50 ℃,后期降速趋于平缓;提升压裂裂缝复杂性可增大有效换热面积,配合以合理的井位及注采参数提升换热效果,实现干热岩的高效开采。

关键词: 干热岩')">

干热岩, 水力裂缝扩展, 天然裂缝, 采热, 流-固-热耦合, 非连续离散裂缝模型, 换热,
')">青海共和盆地


Abstract:

To simulate hydraulic fracturing and heat injection and extraction effect in hot dry rock reservoir, we established a  thermo-hydro-mechanical  coupling hydraulic fracture propagation and heat transfer model for simulating the complex fracturing fracture morphology of dry hot rock and conducting injection-production thermal analysis. Taking the hot dry rock(HDR) in Qinghai Gonghe basin as a reference, we constructed two case considered the geo-mechanical parameter characteristics and simulated the multi-well fracturing and heat recovery process, the numerical results of fracturing and heat injection and recovery show that: In HDR, the fracture initiation is influenced by the non-uniform stress field, exhibiting volumetric fracture characteristics. Fractures created through multi-well fracturing connect via natural fractures, providing over 95% of the heat exchange flow channels for heat injection and production. During heat injection and production, fluid mainly flows along the connected fractures, forming dominant heat exchange channels. This leads to a significant decrease in outlet temperature during the initial stage of heat injection and production, with the outlet water temperature dropping by 30-50 ℃ within the first three years, followed by a gradual slowdown in the later stages. Enhanced fracture complexity can increase effective heat transfer area, while optimized well placement and injection-production parameters improve thermal efficiency, enabling sustainable geothermal energy exploitation.

Key words: hot dry rock, hydraulic fracture propagation, natural fracture, heat recovery, thermo-hydro-mechanical coupling, discontinuous discrete fracture model, heat transfer, Qinghai Gonghe basin

中图分类号: 

  • P314
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