The LV-aorta pressure gradient means:
[
\text{LV systolic pressure} - \text{aortic systolic pressure}
]
In obstructive HCM, it is generated because blood cannot leave the LV freely during systole.
Mechanism
- The basal interventricular septum is thickened, making the LV outflow tract narrow.
- As the LV contracts, the mitral valve leaflet is pushed forward toward the septum. This is systolic anterior motion, or SAM.
- The mitral leaflet and septum nearly meet or touch, producing a temporary, severe narrowing of the LVOT.
- The LV must then generate a much higher pressure to force blood through that narrowed opening into the aorta.
- Beyond the obstruction, pressure falls as energy is converted to high-velocity turbulent flow and dissipated.
Therefore, during systole:
[
P_{LV} > P_{aorta}
]
For example, if LV systolic pressure is 180 mm Hg and aortic systolic pressure is 110 mm Hg:
[
\text{LV-aortic gradient} = 180 - 110 = 70\ \text{mm Hg}
]
It is analogous to partially pinching a hose: pressure rises on the side before the pinch, while flow accelerates through the narrowed segment.
This obstruction is dynamic, not a fixed blockage. Reduced LV filling, increased contractility, and reduced afterload make the LV cavity smaller and SAM worse, increasing the gradient. Thus, Valsalva, standing, dehydration, exercise, and catecholamines can increase it. The obstruction is conventionally assessed as an LVOT gradient, with Doppler estimating it as:
[
\Delta P = 4V^2
]
where (V) is peak velocity through the obstructed LVOT. The
ACC explanation of LVOT Doppler gradients notes its dependence on preload, blood pressure, and heart rate.