Download Ah Ha By 6000 Degrees

The song "6000 Degrees (AH HA)" by $hyfromdatre is a diss track directed towards a female individual. The lyrics describe the artist's frustration and annoyance with this person who was once a fan but turned into an enemy. The first verse highlights the artist's success with expensive items such as Gucci, which contrasts with the apparent lack of wealth of this person who calls the artist broke. The artist suggests that this person is delusional and seeking attention by creating a fictional conflict. The second verse is more aggressive and graphic, describing the violent actions of this person's baby daddy. The artist also mocks this person's financial struggles and suggests that they cannot afford basic necessities such as tissue. Throughout the song, the artist asserts their dominance over this person and dismisses their attempts to create drama. The song ends with the artist reminding this person that they were once a fan, suggesting that this person's jealousy may be the root of their animosity.

The Earth's core consists mainly of a sphere of liquid iron at temperatures above 4000 degrees and pressures of more than 1.3 million atmospheres. Under these conditions, iron is as liquid as the water in the oceans. It is only at the very centre of the Earth, where pressure and temperature rise even higher, that the liquid iron solidifies. Analysis of earthquake-triggered seismic waves passing through the Earth, tells us the thickness of the solid and liquid cores, and even how the pressure in the Earth increases with depth. However these waves do not provide information on temperature, which has an important influence on the movement of material within the liquid core and the solid mantle above. Indeed the temperature difference between the mantle and the core is the main driver of large-scale thermal movements, which together with the Earth's rotation, act like a dynamo generating the Earth's magnetic field. The temperature profile through the Earth's interior also underpins geophysical models that explain the creation and intense activity of hot-spot volcanoes like the Hawaiian Islands or La Runion.

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To generate an accurate picture of the temperature profile within the Earth's centre, scientists can look at the melting point of iron at different pressures in the laboratory, using a diamond anvil cell to compress speck-sized samples to pressures of several million atmospheres, and powerful laser beams to heat them to 4000 or even 5000 degrees Celsius."In practice, many experimental challenges have to be met," explains Agns Dewaele from CEA, "as the iron sample has to be insulated thermally and also must not be allowed to chemically react with its environment. Even if a sample reaches the extreme temperatures and pressures at the centre of the Earth, it will only do so for a matter of seconds. In this short timeframe it is extremely difficult to determine whether it has started to melt or is still solid."

The scientists determined experimentally the melting point of iron up to 4800 degrees Celsius and 2.2 million atmospheres pressure, and then used an extrapolation method to determine that at 3.3 million atmospheres, the pressure at the border between liquid and solid core, the temperature would be 6000 +/- 500 degrees. This extrapolated value could slightly change if iron undergoes an unknown phase transition between the measured and the extrapolated values.

When the scientists scanned across the area of pressures and temperatures, they observed why Reinhard Boehler, then at the MPI for Chemistry in Mainz (Germany), had in 1993 published values about 1000 degrees lower. Starting at 2400 degrees, recrystallization effects appear on the surface of the iron samples, leading to dynamic changes of the solid iron's crystalline structure. The experiment twenty years ago used an optical technique to determine whether the samples were solid or molten, and it is highly probable that the observation of recrystallization at the surface was interpreted as melting.

Exciting heat transfer phenomena have been discovered with a micron-sized heat transfer element operating in subcooled (20 degrees C) degassed, demineralized water over a wide pressure range (200-6,000psia) at heat fluxes up to 3,500W/cm2. The platinum heat transfer element (diameter 7.5 microns, length 1.14mm) is installed within a one-cm3 stainless steel chamber. Sealed electrical terminals penetrate the chamber to effect direct current heating of the platinum element. Pressure is applied pneumatically. The adiabatic heating rate of the element is 6 degrees C per microsecond at 3,700W/cm2; response is essentially instantaneous for the procedure described herein. The direct current voltage and current are measured from which the power and the resistance (temperature) are determined. The following procedure applies: (1) Pressurize the water-filled stainless steel chamber to 6,000psia. (2) Apply power at 3,000W/cm2. (3) Maintain constant heat flux as pressure is smoothly reduced from 6,000psia to 200psia over a period of 20 seconds. Record voltage, amperage, and pressure at 0.1 second intervals. Heat transfer phenomena thus discovered: (1) Element starting temperature of 370 degrees C at 6,000psia smoothly increased to 380 degrees as pressure was reduced to 3,970psia. (2) At 3,970psia the temperature abruptly stepped upward to 590 degrees C. (3) Temperature smoothly increased to 730 degrees C as pressure was reduced to 3,230psia. (4) In the vicinity of the critical pressure, the temperature turned around and began smoothly decreasing. (5) At 2,350psia, the temperature stepped down from 520 to 350 degrees C. (6) Temperature smoothly decreased to 230 degrees C at 190psia and power was then turned off. Bulk water temperature increased less than 4 degrees C. Controlled gravity (KC-135) tests are planned.

What they ended up seeing that day was a huge milestone for the Space Launch System and a major step toward human exploration of deep space. The motor performed as anticipated for the burn. The inside of the motor, where the propellant had been cooled to 40 degrees Fahrenheit to simulate a cold day at the launch site, reached nearly 6,000 degrees, and the flames leaving the booster melted sand into glass. The test clears the way for qualification of the solid rocket boosters as ready to fly on the first launch of SLS in 2018. 006ab0faaa