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Only takes 3 or 5, depending on direction. George W. Bush → MIT is 3 or 2. smurrayinchester , 16:16, 5 March 2006 (UTC) Aliens to Vimes There is, according to kate's tool, no path under 10 steps between these articles, however the return path, Vimes to Aliens is only 4 degrees - none of which are date related. Chrisboote
Daniel Streicher Badenhorst (born 6 December 1967), better known as Daantjie Badenhorst and nicknamed Daantjie Dinamiet [1] (Daantjie Dynamite), is a South African quiz show champion, journalist and author.
Note that since the particles in the ideal gas are non-interacting, the probability of finding a particle at a certain distance from another particle is the same as the probability of finding a particle at the same distance from any other point; we shall use the center of the sphere.
Noot vir Noot (Afrikaans for "Note for Note", i.e. music-note for a cash-note) is an Afrikaans language musical quiz show broadcast on SABC 2 on South African television.It was the longest continually running television game show in South Africa and Africa. [2]
In 1907, Edgar Buckingham created the first water retention curve. [2] It was measured and made for six soils varying in texture from sand to clay. The data came from experiments made on soil columns 48 inch tall, where a constant water level maintained about 2 inches above the bottom through periodic addition of water from a side tube.
The moisture content at which it takes 25 drops of the cup to cause the groove to close over a distance of 12.7 millimetres (0.50 in) is defined as the liquid limit. The test is normally run at several moisture contents, and the moisture content which requires 25 blows to close the groove is interpolated from the test results.
A proof of the recursion formula relating the volume of the n-ball and an (n − 2)-ball can be given using the proportionality formula above and integration in cylindrical coordinates. Fix a plane through the center of the ball. Let r denote the distance between a point in the plane and the center of the sphere, and let θ denote the
The density of quartz is around 2.65 g/cm 3 but the dry bulk density of a soil can be less than half that value. Most soils have a dry bulk density between 1.0 and 1.6 g/cm 3 but organic soil and some porous clays may have a dry bulk density well below 1 g/cm 3.