INTRODUCTION
Comprehensive assessment of ventricular diastolic function is a complex process. Full elucidation generally requires invasive measurements, such as left ventricular (LV) end diastolic pressure, the time constant of isovolumic LV relaxation (τ), the pressure-volume (P-V) relationship of the ventricle at end diastole, and mean left atrial (LA) pressure. Such invasive measurements are inappropriate for routine clinical purposes, and thus diastolic function is generally assessed using Doppler echocardiography, largely through the observation of transmitral and pulmonary venous flow, supplemented by myocardial velocity and color M-mode Doppler information. In order to intelligently use these noninvasive indices to infer actual diastolic function of the heart, however, it is critical that a conceptual framework be in place that reflects the physical and physiological determinants of intracardiac blood flow. In this chapter, we will outline in both basic physical principles and computer simulations the relationship between basic parameters of diastolic function and the intracardiac flow patterns that can be obtained clinically.
PATHOPHYSIOLOGY
Mechanical Properties of Left Ventricular Chamber Diastole
The major function of the heart in diastole is to let the blood column flow from the antechambers (left atrium and pulmonary veins) into the left ventricle, while keeping filling pressures to a minimum. During exercise, this task is compounded by the shortening of time allowed for filling and the increase of volume needed to get into the left ventricle. Of the various chamber-wall properties that affect this process, we will briefly cover three: chamber stiffness, relaxation, and early diastolic suction.
Chamber Stiffness
Chamber stiffness can be defined as the instantaneous change of pressure for a given volume increment, mathematically the first derivative of LV pressure by volume ( dP / dV ). LV pressure is a complex nonlinear function of LV volume, meaning that stiffness changes with diastolic volume. Although the LV P-V relationship was initially considered to be exponential in shape (concave upward), more recent work suggests that it is sigmoidal in shape ( Fig. 5-1 ), with a concave downward portion to the left of the usual rising exponential. This sigmoidal curve can be expressed as:
P = A * e ( V – V d 0 ) K p + + P b + V ≥ V d 0 P = – B * e ( V d 0 – V ) K p – + P b – V < V d 0 ,
Relaxation
Myocardial relaxation occurs because of calcium reuptake at the end of systole, producing a shift downward and rightward, leading to a fall in LV pressure (at a given volume). The rate of pressure decrease during relaxation depends on the velocity of calcium reuptake and on the LV volume: The smaller the volume, the lower the potential for pressure to fall, limited by the end diastolic pressure curve shown in Figure 5-1 . Rate of calcium reuptake is further modified by LV lengthening during relaxation, so true relaxation can be measured only during the isovolumic period. Several equations have been proposed to describe the rate of isovolumic pressure decay, the most general being:
P ( t ) = ( P o – P b ) × e – t / τ + P b ,
P ( t ) = P o × e – t / τ ,
τ ≈ IVRT / ( ln P A V C – ln P MVO ) ,
Importantly, LV relaxation is a never-ending process that critically affects the end diastolic pressure that the patient achieves, particularly during exercise. Consider Figure 5-2A , showing a series of P-V curves representing successive intervals of τ, and Figure 5-2B , the same curves magnified on diastolic pressures. Note that after 6τ, the filling curve is virtually indistinguishable from the end diastolic P-V curve, as relaxation is 99.8% complete. When relaxation rate is normal, the end diastolic filling curve is completely relaxed at normal heart rates (12.5τ, 2C) and almost complete during exercise (5τ, 2D); with delayed relaxation, however, while the EDPV curve is fully relaxed at rest (6.25τ, 2E), it becomes stiff with exercise (3τ, 2F).
The combination of relaxation and the EDPVR results in a dynamic P-V relationship, represented by the round dots in Figure 5-2A . Note that in early diastole, LV pressure continues to fall even though volume is increasing, meaning that the instantaneous stiffness is actually negative, which some consider diastolic suction. Two other definitions of “diastolic suction” are also relevant. Consider ventricular filling from a very low end systolic volume (where the EDPVR is concave downward). If relaxation is very rapid or filling is delayed (by mitral stenosis or experimentally with a mitral occluder ), then LV pressure can fall below atmospheric pressure. Alternatively, suction has been used to refer to the small (1 to 3 mmHg) differences in pressure between the base and the apex, which assist in the low-pressure filling of the ventricle, particularly with exercise, and which will be discussed later.
Determinants of Intracardiac Blood Flow
In the most general sense, the motion of blood inside the heart, as the motion of any fluid, is determined by the Navier-Stokes equations, a complex set of four multidimensional partial differential equations, which must be solved simultaneously at every point in space and moment in time:
∇ ⋅ v = 0
ρ Dv D t = – ∇ P + B + μ ∇ 2 v
To understand how these equations can model the flow within the heart, we first start by replacing the Navier-Stokes equations with the well-known Bernoulli equation, which applies to flow across discrete points such as valves. Here we present it with its inertial and convective terms (we still omit the viscous term, since it is negligible in almost every intracardiac situation):
Δ p = M d v d t + 1 2 ρ Δ ( v 2 ) ,