Diesel spray mixing limited vaporization with non-ideal and multi-component fuel thermophysical property effects

Internal combustion engines are, and will continue to be, a primary mode of power generation for ground transportation. Challenges exist in meeting fuel consumption regulations and emission standards while upholding performance, as fuel prices rise, and resource depletion and environmental impacts are of increasing concern. Diesel engines are advantageous due to their inherent efficiency advantage over spark ignition engines; however, their NOx and soot emissions can be difficult to control and reduce due to an inherent tradeoff. Diesel combustion is spray and mixing controlled providing an intrinsic link between spray and emissions, motivating detailed, fundamental studies on spray, vaporization, mixing, and combustion characteristics under engine relevant conditions. An optical combustion vessel facility has been developed at Michigan Technological University for these studies, with detailed tests and analysis being conducted. In this combustion vessel facility a preburn procedure for thermodynamic state generation is used, and validated using chemical kinetics modeling both for the MTU vessel, and institutions comprising the Engine Combustion Network international collaborative research initiative. It is shown that minor species produced are representative of modern diesel engines running exhaust gas recirculation and do not impact the autoignition of n-heptane. Diesel spray testing of a high-pressure (2000 bar) multi-hole injector is undertaken including non-vaporizing, vaporizing, and combusting tests, with sprays characterized using Mie back scatter imaging diagnostics. Liquid phase spray parameter trends agree with literature. Fluctuations in liquid length about a quasi-steady value are quantified, along with plume to plume variations. Hypotheses are developed for their causes including fuel pressure fluctuations, nozzle cavitation, internal injector flow and geometry, chamber temperature gradients, and turbulence. These are explored using a mixing limited vaporization model with an equation of state approach for thermopyhysical properties. This model is also applied to single and multi-component surrogates. Results include the development of the combustion research facility and validated thermodynamic state generation procedure. The developed equation of state approach provides application for improving surrogate fuels, both single and multi-component, in terms of diesel spray liquid length, with knowledge of only critical fuel properties. Experimental studies are coupled with modeling incorporating improved thermodynamic non-ideal gas and fuel

Omega-3 fatty acids and the neurovascular responses to mental stress in humans

Hypertension is the most prevalent form of cardiovascular disease (CVD) in the world, and is known to increase the risk for developing other diseases. Recently, the American Heart Association introduced a new classification of blood pressure, prehypertension (PHT). The criteria for PHT include a systolic of 120-139 mmHg and/or a diastolic blood pressure of 80-89 mmHg. It has been observed that individuals with PHT have a higher risk of developing hypertension later in life. Therefore, it is important to understand the mechanisms contributing to PHT in order to possibly prevent hypertension. Omega-3 fatty acids found in fish oils have been suggested as a means of lowering blood pressure. However, little is known on the effects of fish oil in PHT humans. Therefore we conducted two studies. In Study 1 we investigated PHT and normotensive (NT) individuals during a mental stress task. Mental stress is known to contribute to the development of hypertension. In Study 2 PHT and NT subjects were placed in an eight week double-blind placebo controlled study in which subjects consumed 9g/day of either fish oil or placebo (olive oil) in addition to their regular diets. Subjects were tested during a resting baseline (seated and supine), 5 minutes of a mental stress task, and 5 minutes of recovery both pre and post supplementation. We measured arterial pressure (AP), heart rate (HR), muscle sympathetic nerve activity (MSNA), and forearm and calf vascular responses. In Study 1 PHT demonstrated augmented AP and blunted vasodilation during mental stress, but MSNA did not change. In Study 2, fish oil did not directly influence blood pressure, MSNA or vascular responses to mental stress. However, it became clear that fish oil had an effect on some but not all subjects (both PHT and NT). Specifically, subjects who experienced a reduced blood pressure response to fish oil also demonstrated a decrease in MSNA and HR during mental stress. Collectively, the investigations in this dissertation had several novel findings. First, PHT individuals demonstrate an augmented pressor and blunted vascular response to mental stress, a response that may be contributing to the development of hypertension. Second, fish oil does not consistently lower resting blood pressure, but the interindividual responses may be related to MSNA. Third, fish oil attenuated the heart rate and MSNA responses and to mental stress in both PHT and NT. In conclusion, we found that there are both similarities and differences in the way PHT and NT individuals respond to mental stress and fish oil.

Investigations of Cloud Microphysical Response to Mixing Using Digital Holography

Cloud edge mixing plays an important role in the life cycle and development of clouds. Entrainment of subsaturated air affects the cloud at the microscale, altering the number density and size distribution of its droplets. The resulting effect is determined by two timescales: the time required for the mixing event to complete, and the time required for the droplets to adjust to their new environment. If mixing is rapid, evaporation of droplets is uniform and said to be homogeneous in nature. In contrast, slow mixing (compared to the adjustment timescale) results in the droplets adjusting to the transient state of the mixture, producing an inhomogeneous result. Studying this process in real clouds involves the use of airborne optical instruments capable of measuring clouds at the `single particle' level. Single particle resolution allows for direct measurement of the droplet size distribution. This is in contrast to other `bulk' methods (i.e. hot-wire probes, lidar, radar) which measure a higher order moment of the distribution and require assumptions about the distribution shape to compute a size distribution. The sampling strategy of current optical instruments requires them to integrate over a path tens to hundreds of meters to form a single size distribution. This is much larger than typical mixing scales (which can extend down to the order of centimeters), resulting in difficulties resolving mixing signatures. The Holodec is an optical particle instrument that uses digital holography to record discrete, local volumes of droplets. This method allows for statistically significant size distributions to be calculated for centimeter scale volumes, allowing for full resolution at the scales important to the mixing process. The hologram also records the three dimensional position of all particles within the volume, allowing for the spatial structure of the cloud volume to be studied. Both of these features represent a new and unique view into the mixing problem. In this dissertation, holographic data recorded during two different field projects is analyzed to study the mixing structure of cumulus clouds. Using Holodec data, it is shown that mixing at cloud top can produce regions of clear but humid air that can subside down along the edge of the cloud as a narrow shell, or advect down shear as a `humid halo'. This air is then entrained into the cloud at lower levels, producing mixing that appears to be very inhomogeneous. This inhomogeneous-like mixing is shown to be well correlated with regions containing elevated concentrations of large droplets. This is used to argue in favor of the hypothesis that dilution can lead to enhanced droplet growth rates. I also make observations on the microscale spatial structure of observed cloud volumes recorded by the Holodec.