Basic hydraulic pump work-energy relationship

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SUMMARY

The discussion centers on the hydraulic pump work-energy relationship, specifically in the context of the heart's left ventricle during isovolumetric contraction. It clarifies that during this phase, the ventricle's volume remains constant while pressure increases, despite the wall's stiffness. The participant questions how pressure can rise without volume change, suggesting that even infinitesimal volume changes could facilitate energy transfer to the blood. The conversation also touches on the relationship between pressure, temperature, and density, emphasizing that significant pressure increases yield minimal volume changes in liquids.

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  • Understanding of basic hydraulic principles
  • Familiarity with the cardiac cycle and heart anatomy
  • Knowledge of pressure-volume relationships in fluids
  • Basic concepts of density, temperature, and compressibility
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  • Research the mechanics of isovolumetric contraction in cardiac physiology
  • Study the pressure-volume loop analysis in cardiology
  • Explore the effects of pressure and temperature on fluid density
  • Learn about the compressibility of liquids and solids in engineering contexts
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Students of biology and physics, medical professionals studying cardiac function, and engineers interested in fluid dynamics and hydraulic systems.

Ignis24
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I have a very simple question that's been driving me nuts. It's biology context, but probably all the physics equates to normal positive displacement pumps.

The pressure in and volume of the left ventricle of the heart can be measured experimentally. (For example, https://en.wikipedia.org/wiki/Pressure-volume_loop_analysis_in_cardiology). During a typical contraction, blood stored in the atrium first fills the ventricle while the muscular wall is relaxed. When the ventricle is full enough, the ventricle wall begins to contract. The rising pressure in the ventricle pushes the mitral valve that leads to the atrium closed, meaning there's no backflow out from then on. When the pressure gets high enough, it pushes the aortic valve open, and the ventricle ejects the blood into the aorta.

The phase of contraction after the mitral valve closes but before the aortic valve opens is called isovolumetric contraction. When I first heard this, I assumed that "isovolumetric" has to be a simplification like "infinite conducting wire". I can imagine, from a biological perspective, that the ventricle wall could get stiffer without the ventricle changing its volume. But I have no idea how this increasing stiffness could be translated into rising pressure in the blood inside the ventricle. If the wall does not move, how can it do work on the blood to raise the pressure? How does the blood know how stiff the ventricle wall is if nothing is moving in the system? My guess was, the ventricle is actually shrinking a tiny amount (and blood is not actually perfectly incompressible), which allows for energy transfer to the blood to account for the pressure rise.

My professor swears that I'm confused, and the contraction is truly isovolumetric - not just unmeasurably small. But I still couldn't follow him. Basically, what I'm stuck on is if you block up the outlet of a pump, how does the pressure go up inside?

Thanks...
 
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Changes of density

In general, density can be changed by changing either the pressure or the temperature. Increasing the pressure always increases the density of a material. Increasing the temperature generally decreases the density, but there are notable exceptions to this generalization. For example, the density of water increases between its melting point at 0 °C and 4 °C; similar behavior is observed in silicon at low temperatures.

The effect of pressure and temperature on the densities of liquids and solids is small. The compressibility for a typical liquid or solid is 10−6 bar−1 (1 bar = 0.1 MPa) and a typical thermal expansivity is 10−5 K−1. This roughly translates into needing around ten thousand times atmospheric pressure to reduce the volume of a substance by one percent. (Although the pressures needed may be around a thousand times smaller for sandy soil and some clays.) A one percent expansion of volume typically requires a temperature increase on the order of thousands of degrees Celsius.

source: https://en.wikipedia.org/wiki/Density#Changes_of_density

If nothing goes in and nothing goes out (i.e. mass is constant), then if the density varies, the volume must also vary.

For example, this is the pressure-temperature-density relationship for water (source: http://www.engineeringtoolbox.com/fluid-density-temperature-pressure-d_309.html):

water-density-temperature-pressure_2.png


According to the equation found in the previous link, increasing the pressure of water by 12 000 Pa (90 mmHg) would result in a density increase (or volume decrease) of only 0.00048 %.

I would argue the infinitesimal volume change.
 

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