A siphon works by reducing the pressure at one end of a pipe resulting in the fluid being forced by atmospheric pressure towards the end of the pipe with lesser pressure. Gravity plays play little if any part of this physical phenomena.
The engineering site is correct in this case.
You are right of course, but we could nitpick about the meaning of the words "pull" and "suck"...not very exact terms. Certainly lots of pumps are installed above the water level and there are benefits like in some cases eliminating flooding in rain storms and shorting out the pump. So I would say those pumps are "pulling" or "sucking" in water. The same is true when a pump is below water level. Position of pump relative to water level affects how a pump is primed. But once primed and the pump is running I'd call it a sucking or pulling action. Same as when we suck on a straw. Water can't really be pulled of course, but close enough.
Crane Engineering's definition really chaps my hide by saying atmospheric pressure pushes water...I hate junk science. Gravity causes water to seek its own level, not atmospheric pressure. If the earth lost its atmosphere water would still stay in place, pumps would still work, we wouldn't float off into space. Crane Engineering's web site was probably written by a marketing intern.
neither is responsible solely since siphon has been performed in vacuum successfully without air pressure and also have been done using co2 , more like started by air pressure in tube then gravity plays role
Gravity,
pressure and molecular
cohesion were the focus of work in 2010 by Hughes at the
Queensland University of Technology. He used siphons at air pressure and his conclusion was that: "The flow of water out of the bottom of a siphon depends on the difference in height between the inflow and outflow, and therefore cannot be dependent on atmospheric pressure…"
[28] Hughes did further work on siphons at air pressure in 2011 and concluded that: "The experiments described above demonstrate that ordinary siphons at atmospheric pressure operate through gravity and not atmospheric pressure".
[29]
The father and son researchers, Ramette and Ramette, successfully siphoned
carbon dioxideunder air pressure in 2011 and concluded that molecular cohesion is not required for the operation of a siphon but that: "The basic explanation of siphon action is that, once the tube is filled, the flow is initiated by the greater pull of gravity on the fluid on the longer side compared with that on the short side. This creates a pressure drop throughout the siphon tube, in the same sense that 'sucking' on a straw reduces the pressure along its length all the way to the intake point. The ambient atmospheric pressure at the intake point responds to the reduced pressure by forcing the fluid upwards, sustaining the flow, just as in a steadily sucked straw in a milkshake."
[1]
Again in 2011, Richert and Binder (at the
University of Hawaii) examined the siphon and concluded that molecular cohesion is not required for the operation of a siphon but relies upon gravity and a pressure differential, writing: "As the fluid initially primed on the long leg of the siphon rushes down due to gravity, it leaves behind a partial vacuum that allows pressure on the entrance point of the higher container to push fluid up the leg on that side".
[2]
The research team of Boatwright, Puttick, and Licence, all at the
University of Nottingham, succeeded in running a siphon in
high vacuum, also in 2011. They wrote that: "It is widely believed that the siphon is principally driven by the force of atmospheric pressure. An experiment is described that shows that a siphon can function even under high-vacuum conditions. Molecular cohesion and gravity are shown to be contributing factors in the operation of a siphon; the presence of a positive atmospheric pressure is not required".
[30]
Writing in
Physics Today in 2011, J. Dooley from
Millersville University stated that both a pressure differential within the siphon tube and the
tensile strength of the liquid are required for a siphon to operate.
[31]
A researcher at
Humboldt State University, A. McGuire, examined flow in siphons in 2012. Using the advanced general-purpose multiphysics simulation software package
LS-DYNA he examined pressure initialisation, flow, and pressure propagation within a siphon. He concluded that: "Pressure, gravity and molecular cohesion can all be driving forces in the operation of siphons".
[3]
In 2014, Hughes and Gurung (at the Queensland University of Technology), ran a water siphon under varying air pressures ranging from sea level to 11.9 km (39000 ft) altitude. They noted that: "Flow remained more or less constant during ascension indicating that siphon flow is independent of ambient
barometric pressure". They used
Bernoulli's equation and the
Poiseuille equation to examine pressure differentials and fluid flow within a siphon. Their conclusion was that: "It follows from the above analysis that there must be a direct cohesive connection between water molecules flowing in and out of a siphon. This is true at all atmospheric pressures in which the pressure in the apex of the siphon is above the vapour pressure of water, an exception being ionic liquids".
[32]