Towards a comprehensive description of relative aortic pressure: insights from 4D flow CMR
Alex Pitcher
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Pablo Lamata
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Sebastian B Krittian
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David A Nordslettern
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Malenka M Bissell
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Jane M Francis
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Thomas E Cassar
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Alex J Barker
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Michael Markl
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Stefan Neubauer
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Nic Smith
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Funding work. Funding support is acknowledged from the Eur- opean Community's Seventh Framework Program; the Department of Health via the National Institute for Health Research (NIHR) comprehensive Biomedical Research Centre award to Guy's & St Thomas' NHS Foundation Trust in partnership with King's College London
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Oxford Centre for Clinical Magnetic Resonance Research, Department of Cardiovascular Medicine, University of Oxford
,
Oxford
,
UK
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Background
A complete description of the relative spatiotemporal
pressure gradients which drive blood flow has been a
central goal of hemodynamics research over six decades. We
have previously described a novel computational method
for the in vivo estimation of these relative pressure
gradients in the human cardiovascular system based on 4D
flow Cardiovascular Magnetic Resonance (CMR) datasets
(reference 1). We now describe the application of this
method to allow a comprehensive assessment of the
spatiotemporal distribution of relative pressure in the human
aorta, based on 4D flow CMR datasets, in both healthy
subjects, and in patients with established aortic disease.
We have extended the approach by isolating, and
individually analysing, the three major components of relative
pressure, providing unique insights into the nature and
timing of intra-aortic relative pressure changes.
Methods
Six subjects underwent time-resolved, phase contrast
CMR with 3-directional velocity encoding (4D flow) at 3
Tesla. Three were healthy volunteers and three were
patients with established aortic disease (bicuspid aortic
valve with associated ascending aortic aneurysm, Type A
aortic dissection and Marfan syndrome). Spatiotemporal
pressure maps were computed from the CMR flow fields
using a finite-element implementation of the pressure
Poisson equations. Using this formulation, the individual
components of pressure were separated as time-varying
inertial ("unsteady), spatially-varying inertial (
convective) and viscous component (Figure 1).
Results
Aortic pressure differences are mainly caused by the
unsteady effects (15mmHg at instant of peak
acceleration), followed by the convective and a small viscous
contribution (3.14mmHg and 0.2mmHg respectively at
instant of peak velocity). Visualisation of relative
pressure maps allowed identification of well-localised abrupt
changes in pressure identified in each of the diseased
cases. These regions of abrupt pressure difference were
explained by either differences in aortic geometry, such
as the presence of an aneurysm, a pseudo-coarctation,
or the inlet of a dissection, or by complex flow features,
such as vortical flow, particularly in the case of
convective component of pressure (Figure 2).
Conclusions
We describe the time-resolved relative pressure
distribution, in healthy subjects, and in those with aortic diseases
characterised by aortic dilation, demonstrating that
relative pressure distributions are consistent in the healthy
aorta but differ in disease. The isolation and separate
evaluation of the three components of relative pressure
provides further unique insights into the timings and
contributions of each component to overall pressure
differences, with implications for understanding mechanisms of
aortic disease in populations and in individuals, and with
potential for guiding choice of therapy in future.
Figure 1 Methodology for the computation of the spatiotemporal maps of pressure in the aorta. The top of the illustration represents the data
workflow from a single frame, frame 4, which constitutes the fourth column in the spatiotemporal map, as indicated by the blue arrow. The
horizontal lines in the spatiotemporal map correspond to specific plane locations in the aorta, which are defined at the level of the pulmonary
artery (the two continuous lines), before and after the great vessels of the arch, and the descending in line with the mitral annulus. These planes
divide the aortic anatomy in regions: the ascending aorta (AA1, AA2), the arch and descending aorta (DA1, DA2).
Figure 2 Anatomical inspection of the convective pressure, showing velocity streamlines coloured by pressure, in a healthy volunteer (HV2), a
patient with Marfan syndrome (MFS), a patient with an aortic dissection (AoD), and a patient with bicuspid aortic valve, ascending aortic
dilation, and a pseudo-coarctation (BAV). MFS and BAV both show vortexes characterised by an abrupt drop of pressure, at the beginning of the
proximal descending aorta. AoD shows increased pressure in the aortic root graft, the (dissected) carotid artery, and in the proximal descending
aorta at the outer curvature.
Kings College Hospital NHS Foundation Trust (Lamata,
Krittian, Nordsletten, Smith), the British Heart Foundation
(Pitcher, Bissell), the Oxford NIHR Biomedical Research
Centre (Pitcher, Neubauer), and the Oxfordshire Health
Services Research Funds (Pitcher, Cassar). Stefan
Neubauer and Nic Smith acknowledge support from the BHF
Centres of Research Excellence at Oxford and Kings
College London respectively.
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