Atmosphere temperature history

Shows effects of atmosphere, sample history, purity, etc. Measures sample temperature directly. 

On the basis of runs made with a variety of temperature histories, the following qualitative characteristics were true in a hydrogen atmosphere. 

During pyrolysis, the yield of gases and liquid products may vary from 25 to 70 percent by weight. The yield depends on a number of variables, such as coal type, gas atmosphere, final pyrolysis temperature, time-temperature history, and pressure. A certain operating condition may lead to increased product yield, but achievement of this process condition often is obtained at added expense. 

The Earth is a highly unusual planet because life did evolve on it and it thrived to the extent that the surface and atmosphere of the planet were greatly modified. The Earth is unique in this respect relative to all known astronomical bodies (Taylor, 1999). The Earth s location, composition, and evolutionary history are all significant factors in the planet s success in nurturing life. Critical factors include its temperature, its atmosphere, its oceans, its long-term stability and its "just right" abundance of water and other light element compounds. 

Because of their similar history, the four terrestrial planets have similar layer structures. However, their surfaces and atmospheres show enormous physical and chemical differences. The development of the primeval Earth via the agglomeration of planetesimals was accompanied by a vast temperature increase caused by contributions from three different phenomena ... 

Pyrolysis has a long history in the upgrading of biomass. The dry distillation of hardwood was applied in the early 1990s to produce organic intermediates (methanol and acetic acid), charcoal and fuel gas [3]. Today s processes can be tuned to form char, oil and/or gas, all depending on the temperature and reaction time, from 300 °C and hours, to 400-500 °C and seconds-minutes, to >700 °C and a fraction of a second [3, 19, 23, 24], The process is typically carried out under inert atmosphere. We illustrate the basic chemistry of pyrolysis by focusing on the conversion of the carbohydrate components (Fig. 2.4). The reaction of the lignin will not be covered here but should obviously be considered in a real process. Interested readers could consult the literature, e.g., [25]. Pyrolysis is discussed in more details elsewhere in this book [26],... 

One way scientists have learned about the levels of carbon dioxide in the past is through the analysis of ice cores. An ice core is a tube of ice, usually drilled out of a glacier or ice sheet, that contains bubbles of air trapped inside layers of snow and ice. Each layer of snow and ice represents roughly a year. The deeper the layer, the older the ice sample. From the size and chemical content of each layer, scientists can draw conclusions about the temperatures at that point in history at that spot on the planet. At the same time, the bubbles of air preserved in each layer contain indicators of the amount of atmospheric carbon dioxide present at that time. 

T is temperature, P is pressure, and / is the fugacity of the component. In Equation 3 subscript k refers to each component of the system. In the present discussion the fugacity 42) is employed in preference to the chemical potential 21). Earlier in the history of the petroleum industry, Raoult s 55) and Dalton s laws were applied to equilibrium at pressures considerably above that of the atmosphere. These relationships, which assume perfect gas laws and additive volumes in the gas phase and zero volume for the liquid phase, prove to be of practical utility only at low pressures. Henry s law was found to be a useful approximation only for gases which were of low solubility and at reduced pressures less than unity. 

The properties of rubber depend, often to a considerable extent, on its history before test and the atmospheric conditions under which the test was carried out. That is, the results are affected by the age of the rubber, the conditions such as temperature and humidity under which it was stored, any mechanical deformation before test and temperature and humidity at the time of the test. Hence, to produce consistent results it is essential that these factors are controlled within suitable limits. 

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