用混合量子神经网络做地震反演,提升地下成像精度。
Seismic inversion using hybrid quantum neural networks
- 设计混合量子神经网络架构,结合地质物理约束
- 在合成数据和斯莱普纳油田真实数据上实现高精度反演
- 适合对量子计算与地球物理交叉研究感兴趣的读者
地震反演(包括叠后、叠前及全波形反演)计算和内存消耗巨大。近年来,物理信息机器学习等方法被提出以缓解部分瓶颈。受量子计算潜力的启发,本文尝试将经典物理信息算法映射至量子框架,探索其技术挑战——因量子计算原理与经典计算根本不同。量子计算机利用量子比特的叠加与纠缠,有望解决经典方法无法处理的问题。尽管当前硬件受限,但混合量子-经典算法(尤其在量子机器学习中)已展现近中期应用前景,且可高效模拟。本文开发了一种用于叠后与叠前地震反演的混合量子物理信息神经网络(HQ-PINN),采用编码器-解码器结构:混合量子神经网络编码器从地震数据估计P波与S波阻抗,解码器则基于地球物理关系重建地震响应。训练通过最小化输入与重建地震记录间的残差完成。系统评估了量子层设计、梯度策略与仿真后端对反演性能的影响。结果表明,该框架在合成数据与斯莱普纳油田实测数据上均能稳定生成准确结果,验证了量子计算在地球科学中的潜力,为未来量子增强型地球物理工作流铺平道路。
原文摘要 · Abstract (English)
Seismic inversion-including post-stack, pre-stack, and full waveform inversion is compute and memory-intensive. Recently, several approaches, including physics-informed machine learning, have been developed to address some of these limitations. Motivated by the potential of quantum computing, we report on our attempt to map one such classical physics-informed algorithm to a quantum framework. The primary goal is to investigate the technical challenges of this mapping, given that quantum algorithms rely on computing principles fundamentally different from those in classical computing. Quantum computers operate using qubits, which exploit superposition and entanglement, offering the potential to solve classically intractable problems. While current quantum hardware is limited, hybrid quantum-classical algorithms-particularly in quantum machine learning (QML)-demonstrate potential for near-term applications and can be readily simulated. We apply QML to subsurface imaging through the development of a hybrid quantum physics-informed neural network (HQ-PINN) for post-stack and pre-stack seismic inversion. The HQ-PINN architecture adopts an encoder-decoder structure: a hybrid quantum neural network encoder estimates P- and S-impedances from seismic data, while the decoder reconstructs seismic responses using geophysical relationships. Training is guided by minimizing the misfit between the input and reconstructed seismic traces. We systematically assess the impact of quantum layer design, differentiation strategies, and simulator backends on inversion performance. We demonstrate the efficacy of our approach through the inversion of both synthetic and the Sleipner field datasets. The HQ-PINN framework consistently yields accurate results, showcasing quantum computing's promise for geosciences and paving the way for future quantum-enhanced geophysical workflows.
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