论文标题

地质裂缝网络的量子算法

Quantum Algorithms for Geologic Fracture Networks

论文作者

Henderson, Jessie M., Podzorova, Marianna, Cerezo, M., Golden, John K., Gleyzer, Leonard, Viswanathan, Hari S., O'Malley, Daniel

论文摘要

解决大型方程式是建模自然现象的挑战,例如模拟地下流。为了避免在当前计算机上棘手的系统,通常有必要以小尺度(一种称为粗粒的方法)忽略信息。对于许多实际应用,例如多孔,同质材料中的流量,粗粒胶化提供了足够准确的溶液近似值。不幸的是,由于最小的量表存在关键网络拓扑,包括可以将网络推向渗透阈值的拓扑,包括关键的网络拓扑,包括关键网络拓扑,无法准确地粗粒。因此,对于准确对重要断裂系统进行建模是必要的新技术。用于求解线性系统的量子算法对其经典对应物提供了一种指数的改进,在这项工作中,我们引入了两种用于断裂流的量子算法。第一种算法是为未来量子计算机而设计的,该算法没有错误的潜力,但我们证明当前的硬件太嘈杂,无法进行足够的性能。第二种算法旨在具有噪声弹性,对于中小型的问题(订单10至1000个节点)已经表现良好,我们在实验中证明并在理论上进行解释。我们希望通过利用量子误差和预处理来进一步改善。

Solving large systems of equations is a challenge for modeling natural phenomena, such as simulating subsurface flow. To avoid systems that are intractable on current computers, it is often necessary to neglect information at small scales, an approach known as coarse-graining. For many practical applications, such as flow in porous, homogenous materials, coarse-graining offers a sufficiently-accurate approximation of the solution. Unfortunately, fractured systems cannot be accurately coarse-grained, as critical network topology exists at the smallest scales, including topology that can push the network across a percolation threshold. Therefore, new techniques are necessary to accurately model important fracture systems. Quantum algorithms for solving linear systems offer a theoretically-exponential improvement over their classical counterparts, and in this work we introduce two quantum algorithms for fractured flow. The first algorithm, designed for future quantum computers which operate without error, has enormous potential, but we demonstrate that current hardware is too noisy for adequate performance. The second algorithm, designed to be noise resilient, already performs well for problems of small to medium size (order 10 to 1000 nodes), which we demonstrate experimentally and explain theoretically. We expect further improvements by leveraging quantum error mitigation and preconditioning.

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