APS层析成像数据的流式采集与实时分析

Q3 Physics and Astronomy Synchrotron Radiation News Pub Date : 2023-07-04 DOI:10.1080/08940886.2023.2245693
Viktor Nikitin,, Pavel Shevchenko,, Alexey Deriy, Alan Kastengren,, Francesco De Carlo
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引用次数: 0

摘要

简介Brilliant同步加速器光源能够以超过7.7 GB/s的速率[1,2]进行连续断层摄影数据采集,在很短的时间内生成TB的数据,为以前所未有的高时间分辨率研究非常快速的过程打开了可能性。例如PSI TOMCAT光束线的科学家和他们的合作者最近创造了一项新的世界纪录,他们使用新型高速相机和高数值孔径宏观镜展示了每秒1000张断层图像(每毫秒40次投影的3D图像)的采集速度仅通过投影数据跟踪样本演变。在许多情况下,这种半盲的传统技术错过了动态现象,因为它的起源位置和时间并不事先知道。研究快速过程的另一个挑战是确定扫描的代表性感兴趣区域,即动态过程开始并随时间演变的区域。大多数情况下,动态现象会被忽略,因为它发生在不受观测的位置,进化速度比预测的要快,或者需要与仪器设置的空间或时间分辨率不同的分辨率。理想的环境控制系统参数是对不断进化的样本进行现场研究的另一个挑战。如果没有实时3D成像输入,实际上不可能确定适当的环境参数,例如冷却/加热速率、压力或加载力。有许多研究将极大地受益于通过使用实时图像重建进行反馈和控制而优化的快速3D成像。在材料工程和地质力学中,了解失效产生的机制是很重要的[3]。这些过程对3D成像来说非常具有挑战性,因为裂纹可能在样品的不同部分开始。作者在[2]中对铸造合金凝固过程中枝晶的超快形成或液态金属泡沫中气泡的生长和聚结进行了3D成像实验。这种基于铝合金的金属泡沫正被研究作为轻质材料,例如用于电动汽车的构造。地球科学中的一个重要主题是研究快速非平衡孔隙尺度过程,包括润湿、稀释、混合和反应现象,而不显著牺牲空间分辨率,例如在快速孔隙尺度流体动力学中——一种被称为海恩斯跳跃的增量毛细管水运动[4]。在[5]中,作者使用动态原位成像来研究多孔样品中甲烷水合物的形成过程。除了甲烷水合物解离过程非常快之外,它也发生在不同的样品区域,这使得具有代表性的动态3D更加具有挑战性。用于断层摄影实验中的数据采集的传统方法是基于从检测器流式传输的2D投影的实时可视化。这些投影通常用于在旋转台上对准样品并调整检测器曝光时间。飞行扫描模式下的进一步断层扫描包括在样品连续旋转的同时保存一系列投影。扫描后,采集的数据从探测器计算机传输到处理和可视化工作站,在那里执行重建过程和3D渲染。数据采集/传输和重建变得耗时,尤其是在动态层析成像实验的情况下。在这里,我们建议彻底改变做断层扫描的方法,见图1。我们采用流式方法进行实时重建,而不是处理来自探测器的2D投影。流式方法允许更快地调整采集参数,更方便地对齐,更容易地选择感兴趣的区域,节省数据减少,更好地控制动态实验等等。在下文中,我们将简要讨论所提出的流式采集模型的大部分细节,并演示我们如何在高级光子源的2-BM扇区使用它。有关该模型的更多详细信息,请参阅[6]。
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Streaming Collection and Real-Time Analysis of Tomographic Data at the APS
Introduction Brilliant synchrotron light sources are able to perform continuous tomographic data acquisition at more than 7.7 GB/s rate [1, 2] generating terabytes of data in a very short time, opening the possibility of studying very fast processes at unprecedented high temporal resolution. For example, scientists at the TOMCAT beamline of the PSI and their collaborators have recently set a new world record by demonstrating 1000 tomograms per second (3D image from 40 projections per millisecond) acquisition speed using a new high-speed camera and highnumerical-aperture macroscope.1 The majority of today’s high-speed tomographic equipment captures events in a predefined area of the sample and track sample evolution only through projection data. In many circumstances, this semi-blind traditional technique misses the dynamic phenomena since the location and timing of its origination are not known in advance. Another challenge in studying rapid processes is determining a representative region of interest for scanning, i.e., the region where the dynamic process begins and evolves over time. Most of the time, the dynamic phenomenon is missed because it happens in a location not under observation, evolves quicker than predicted, or demands a different spatial or temporal resolution than the instrument is set to. The ideal environmental control system parameters are another challenge for in-situ research of constantly evolving samples. Without real-time 3D imaging input, it is practically impossible to determine appropriate environmental parameters, such as cooling/heating rates, pressure, or loading forces. There are many studies that would greatly benefit from fast 3D imaging optimized by using real-time image reconstruction for feedback and control. In material engineering and geomechanics, it is important to understand the mechanisms of failure origination [3]. These processes are very challenging for 3D imaging because a crack may start in different parts of the sample. The authors in [2] conducted experiments on 3D imaging of ultrafast formation of dendrites during the solidification of casting alloys or the growth and coalescence of bubbles in a liquid metal foam. Such metal foams based on aluminum alloys are being investigated as lightweight materials, for example for the construction of electric cars. An important topic in Geosciences is to study fast non-equilibrium pore-scale processes including wetting, dilution, mixing, and reaction phenomena, without significantly sacrificing spatial resolution, for example in fast pore-scale fluid dynamics – an incremental capillary-water movement known as the Haines jumps [4]. In [5] the authors used dynamic in-situ imaging to study the process of methane hydrate formation in porous samples. Besides the fact that the methane hydrate dissociation process is very fast, it also occurs at different sample regions, making representative dynamic 3D even more challenging. A conventional approach for data acquisition in tomographic experiments is based on real-time visualization of 2D projections streamed from the detector. These projections are typically used to align the sample on the rotation stage and adjust the detector exposure time. Further tomographic scanning in fly-scan mode involves saving a series of projections while the sample is continuously rotated. After scanning, the acquired data are transferred from the detector computer to a processing and visualization workstation where the reconstruction procedure and the 3D rendering are performed. Data acquisition/transfer and reconstruction become time-consuming, especially in the case of dynamic tomography experiments. Here, we propose to completely change the approach of doing tomography, see Figure 1. Instead of working with 2D projections coming from the detector, we adopt the streaming approach and work with real-time reconstructions. The streaming approach allows for faster adjustment of acquisition parameters, more convenient alignment, easier selection of the region of interest, saved data reduction, much better control of dynamic experiments, and more. In what follows we will briefly discuss most of the details about the proposed streaming acquisition model and demonstrate how we use it at sector 2-BM of the Advanced Photon Source. More details about the model can be found in [6].
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Synchrotron Radiation News
Synchrotron Radiation News Physics and Astronomy-Nuclear and High Energy Physics
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