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D. Glenn

As seen in: Color Research & Application, Nature, arXiv, Journal of Interventional Radiology (JVIR)
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Articles by D. Glenn

ST-SSMs: Spatial-Temporal Selective State of Space Model for Traffic Forecasting

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By Michael H, D. Glenn
| arXiv
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CCDSReFormer: Traffic Flow Prediction with a Criss-Crossed Dual-Stream Enhanced Rectified Transformer Model

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By Michael H, D. Glenn
| arXiv
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03:00 PM Abstract No. 393 A phase I/II study of direct injection of Bromelain and Acetylcysteine in patients with inoperable mucinous peritoneal tumours

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By D. Glenn, NSW Australia, S. Valle, J. Akhter
| Journal of Interventional Radiology (JVIR) Verified
To view the full text, please login as a subscribed user or purchase a subscription. Click here to view the full text on ScienceDirect. Many patients with mucinous peritoneal tumours achieve long-term recurrence free and overall survival from cytoreductive surgery and intraperitoneal chemotherapy, however recurrence is frequently seen.
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Geometric phase magnetometry using a solid-state spin

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By J. Lee, D. Glenn, K. Arai, C. Belthangady
| Nature Verified
Geometric-phase magnetometry protocol To implement geometric-phase magnetometry, we use a modified version of an experimental protocol (“Berry sequence”) previously applied to a superconducting qubit9. In our realization, the NV spin sensor is placed in a superposition state by a π/2 pulse, where the driving frequency of the π/2 pulse is chosen to be resonant with the NV ms = 0 ↔ ms =  + 1 transition at constant bias field Bbias (≈9.6 mT in our experiment) aligned with the NV axis.
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Micrometer-scale magnetic imaging of geological samples using a quantum diamond microscope

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By D. Glenn, R. Fu, P. Kehayias, D. Le Sage, E. A. Lima, B. P. Weiss, R. L. Walsworth
| Color Research & Application Verified
Remanent magnetization in geological samples may record the past intensity and direction of planetary magnetic fields. Traditionally, this magnetization is analyzed through measurements of the net magnetic moment of bulk millimeter to centimeter sized samples. However, geological samples are often mineralogically and texturally heterogeneous at submillimeter scales, with only a fraction of the ferromagnetic grains carrying the remanent magnetization of interest.
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