Sophie, before I read the link provided, I have gone back over the Siphon thread to try to understand what your problem with the Brixham Experiment is. Which incidentally is far from wasted! The results from the many experiments conducted, some of which I have not included in this forum, produce the results that they were intended to produce. The problem with being a lateral thinker is one tends to processes problems as a whole, and not segmented so that each can be understood.
You say water would move away from the inside of the tube. As water is already compressed by gravity, where is it going to move to? It can't move down the tube because it is linked to other molecules balancing the downward pull equally on the opposite side of the U tube. It can’t flow out because this would require cavitations to form, again to break the cohesive bond. It can’t flow up because of gravity, It can’t collapse the tube because the wall is strong enough to resist the decompression. If molecules move away from the wall, more molecules must replace it because each molecule acts upon its neighbours. Cavitations will inevitably combine to form larger vapour bubbles and this will cause the water columns to fall back to the level at which atmospheric pressure can sustain them @ 10 metre mark, so although the molecules cannot determine which experiment they are in, we must take into account at all times that each molecule is linked to another inside the tube, so deciding the fate or purpose of a single molecule or groups of molecules that are part of a huge volume of molecules in the same experiment is a little difficult to consider to say the least.
I have now read the lengthy paper you linked to and found it to be a report on the progress of science relating to cohesion, adhesion, tension, surface tension and cavitations in water and other various liquids, dealing with ancient science and more modern science approaches to the problems of cavitations in water. Most of which was familiar to myself, and some of which I have included in the two threads, including the spinning tubes, stretched water, etc. Nevertheless, I have not seen this paper before and it does include at least two experiments that I have not heard of before. So thank you for posting the link and for taking the time to look at the experiments.
The terminology I use may not always be in accordance with writing a convincing academic argument and I agree with you on this at least, but if you compare what I have stated to what you have provided in the PDF file we are not far from the mark at all.
Throughout the paper you provided, there is no mention of timescales for cavitations to develop in degassed water, although nucleation is mentioned in relation to impurities in water, I suspect the main seed points are indeed between the water/tube interface. I cannot see another experiment that could show timescales for cavitations other than inside a living plant or tree. The U tube gives us prolonged stability of water under negative pressure and tension allowing us to see cavitations developing through the opaque tubing. There must be clearer tubing produced that could allow us to look more clearly at the forming cavitations.
Deionised water previously boiled will enable the Brixham experiment to easily exceed the 24 metre mark and give us prolonged stability.
I thought the inclusion of particles entering the experiment to cause the nucleation was interesting also. And had not considered this.
The following history event shows how a tiny bubble of gas causes the Huygens experiment, (similar to yours), fails from the paper you provided the link to.
4.1. Pull
A straightforward way to stretch a liquid is to pull directly on it. The pull can be generated by the own weight of the liquid. This is how Huygens made the first experimental observation of negative pressure in 1662, and published his work in 1672 [49]. A tube open at one end is filled with water purged of air, and inverted over a water bath. If the air above the bath is evacuated, water remains suspended in the inverted tube. The pressure at the top of the water column of height h is Psat − ρgh, where ρ is water density, and g the acceleration of gravity. As soon as a bubble of air is injected in the tube, it rises and the water column falls. This experiment was presented to the Royal Society of England, and repeated on water and mercury by several physicists, including the famous Hooke and Boyle,
who reached −0.2 MPa in mercury. The phenomenon was later re-discovered by Donny [23] and Reynolds [47,48]. Details are given by Kell [50]. As Reynolds used a 2.3 m-long tube wetted with water before being filled with mercury, he obtained the most negative pressure for water with this method: −0.3 MPa [48]. Hayward, who thought that the method was invented by Donny [23], re-used it to study different liquids [51]. Another way to pull a liquid is to mechanically increase its volume with a bellow for instance. One can also put the liquid under pressure before warming it up, and eventually releasing the pressure. These techniques have been widely used to make bubble chambers where high energy particles are detected because they trigger cavitation in the metastable liquid (see Ref. [53] for a review); however, volatile liquids with a low surface tension were preferred to water. But the bellow method was used by Hayward to design a water pump with a suction lift of 17 m, corresponding
to a pressure of −0.17 MPa [52]; much higher liquid columns exist in tall trees (see Section 7.1).
Gravity, Learn to live with it, because you can't live without it!