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Prograde satellites of Uranus orbit in the direction Uranus rotates, which is retrograde to the Sun.
All eight planets in the Solar System orbit the Sun in the direction of the Sun's rotation, which is counterclockwise when viewed from above the Sun's north pole. Six of the planets also rotate about their axis in this same direction. The exceptions – the planets with retrograde rotation – are Venus and Uranus. Venus's axial tilt is 177°, which means it is rotating almost exactly in the opposite direction to its orbit. Uranus has an axial tilt of 97.77°, so its axis of rotation is approximately parallel with the plane of the Solar System. The reason for Uranus's unusual axial tilt is not known with certainty, but the usual speculation is that during the formation of the Solar System, an Earth-sized protoplanet collided with Uranus, causing the skewed orientation.
That is only if the moon has originated from the parent planet, I would imagine and gas giants having rocky moons is a non sequitur
originally posted by: ErosA433
a reply to: Hyperboles
Conservation of momentum.
The angular momentum does indeed reference moons which originated along with the planet with prograde orbits. The moons with retrograde and eccentric orbits are probably captured and didn't form with the planet.
originally posted by: Hyperboles
That is only if the moon has originated from the parent planet, I would imagine and gas giants having rocky moons is a non sequitur
originally posted by: ErosA433
a reply to: Hyperboles
Conservation of momentum.
Astronomers think the giants first formed as rocky and icy planets similar to terrestrial planets. However, the size of the cores allowed these planets (particularly Jupiter and Saturn) to grab hydrogen and helium out of the gas cloud from which the sun was condensing, before the sun formed and blew most of the gas away.
According to regulations set by the U.S. Environmental Protection Agency (EPA), the composite liner must have two components: a layer of compacted soil at least two feet thick with a “hydraulic conductivity of no more than 1 X 10-7 centimeters per second. Atop the layer of soil is a flexible membrane liner (FML) at least 30-mil thick.”
“The regulations also require you to manage leachate so that it doesn’t build up on the liner,” says Pat Sullivan, senior vice president and solid waste practice leader for SCS Engineers.
Specifically, EPA regulations require operators to limit leachate buildup on the liner to less than 30 centimeters (just under one foot). To meet the requirement, the leachate management system must be extensive enough to capture the volume of leachate produced by the landfill, which can vary widely.
It seems clear that DeWitt and Graham consider that the multitude of branching worlds are “real” in the ordinary sense of the word. In this sense, their Many Worlds perspective certainly departs from Everett’s intent.
In a 1976 philosophy paper on the interpretation of quantum mechanics, Levy-Leblond offers critical comments on the many worlds interpretation and compared it to his understanding of Everett’s theory.
Now, my criticism here is exactly symmetrical of the one I directed against the orthodox position: the “many worlds” idea again is a left-over of classical conceptions. The coexisting branches here, as the unique surviving one in the Copenhagen point of view, can only be related to “worlds” described by classical physics. The difference is that, instead of interpreting the quantum “plus” as a classical “or”, De Witt et al. interpret it as a classical “and”. To me, the deep meaning of Everett's ideas is not the coexistence of many worlds, but on the contrary, the existence of a single quantum one.The main drawback of the “many-worlds” terminology is that it leads one to ask the question of “what branch we are on”, since it certainly looks as if our consciousness definitely belonged to only one world at a time: But this question only makes sense from a classical point of view, once more. It becomes entirely irrelevant as soon as one commits oneself to a consistent quantum view.
In a letter to Levy-Leblond (Barrett 2011), Everett indicated that he quite agreed with Levy-Leblond’s argument and emphasized that the many worlds terminology was not his. I’m sympathetic with this view.
So isn't it interesting
See the time stamp and distance scale of this photo of the first atomic test?
originally posted by: Hyperboles
Lol Ques:
What role does time play in nuclear and thermonuclear weapons?
2.1.3 Time Scale of the Fission Reaction
The amount of time taken by each link in the chain reaction is determined by the speed of the neutrons and the distance they travel before being captured. The average distance is called the mean free path. In fissile materials at maximum normal densities the mean free path for fission is roughly 13 cm for 1 MeV neutrons (a typical energy for fission neutrons). These neutrons travel at 1.4x10^9 cm/sec, yielding an average time between fission generations of about 10^-8 sec (10 nanoseconds), a unit of time sometimes called a "shake". The mean free path for scattering is only 2.5 cm, so on average a neutron will be scattered 5 times before causing fission. Actual 1 MeV mean free path values are: Density M.F.P. (cm) U-233 18.9 10.9 U-235 18.9 16.5 Pu-239 19.4 12.7 This shows that fission proceeds faster in some isotopes than others. The rate of multiplication can be calculated from the multiplication coefficient k given by: k = f - (lc + le) where f = avg. neutrons generated per fission lc = avg. neutrons lost to capture le = avg. neutrons lost by escaping assembly When k = 1 an assembly is exactly critical and a chain reaction will be self supporting, although it will not increase in rate. When k 1 then it is super-critical and the reaction will continually increase. To make an efficient bomb k must be as high as possible, usually somewhere near 2, when the chain reaction starts.
Many discussions of fission describe the chain reaction as proceeding by discrete generations. Generation zero has 1 neutron, generation one has 2 neutrons, generation two has 4 neutrons, etc. until, say, 2x10^24 atoms have been split - which produces 20 kilotons of energy. The formula for this is: Number of atoms split = 2^(n-1), where n is the generation number. Thus 2x10^24 = 2^(n-1) implies n = (log2 (2x10^24)) + 1 = 81.7 generations. That is, it takes about 82 generations to complete the fission process for a 20 kiloton bomb, if the reaction starts from one neutron. This calculation is a useful simplification, but the fission process does not really proceed by separate steps, each completing before the next begins. It is really a continuous process, the current oldest generation of neutrons starts creating the next generation even while it is still being formed by neutrons from still older generations. An accurate calculation thus requires the use of formulas derived from calculus. We find that both the number of neutrons present in the assembly (and thus the instantaneous rate of the fission reaction), and the number of fissions that have occurred since the reaction began, increase at a rate proportional to e^((k-1)*(t/g)), where e is the natural log base (2.712...), g is the average generation time (time from neutron emission to fission capture), and t is the elapsed time. If k=2, then a single neutron will multiply to 2x10^24 neutrons (and splitting the same number of atoms) in roughly 56 shakes (560 nanoseconds), yielding 20 kilotons of energy. This is one-third less time than the previous approximate calculation. Due to the exponential rate of increase, at any point in the chain reaction 99% of the energy will have been released in the last 4.6 generations. It is a reasonable approximation to think of the first 53 generations as a latency period leading up to the actual explosion, which only takes 3-4 generations. The extremely rapid buildup in the fission rate as the reaction proceeds has some important consequences that should be pointed out.
The longer a neutron takes to cause fission, the less significant it is in contributing to the chain reaction. This is because it becomes quickly outnumbered by the descendants of neutrons that undergo fission capture sooner.Thus faster, more energetic, neutrons contribute disproportionately compared to slower neutrons. This is called "time absorption" since it has the same effect as a neutron absorber with a cross-section inversely proportional to velocity. Similarly, if a neutron leaves the critical mass and is scattered back in, then its contribution is also considerably reduced. In fact since the path of a neutron that leaves the critical assembly, then re-enters is much longer than the average path of neutron that remains within the mass the time absorption in a reflector is very large.