<p>I fokus för denna uppsats står samverkansorganet och kommunalförbundet Region Halland</p><p>eller mer exakt den form av indirekt demokrati som organisationen styrs genom. Studiens</p><p>syfte är att ur ett demokrati och legitimitetsteoretiskt perspektiv undersöka Region Halland</p><p>med fokus på just den indirekta demokratin. Studiens frågeställning är tvådelad och</p><p>undersöker dels hur förankringen av politik inom Region Hallands ram förankras i</p><p>kommunerna och hos medborgarna. Dessutom undersöks vilka demokratipolitiska ambitioner</p><p>som Region Halland har. I uppsatsen används en form av kvalitativ metod nämligen</p><p>samtalsintervjun och intervjuerna genomförs med politiker verksamma i kommunerna och</p><p>Region Halland samt med tjänstemän på Region Halland. Studiens resultat visar att debatten i</p><p>kommunens politiska organ om Region Halland är begränsad och att medborgarna inte heller</p><p>är särdeles involverade i politiska frågor som drivs av Region Halland. Det framkommer även</p><p>att Region Halland inte på egen hand driver demokratipolitiska projekt i någon större</p><p>utsträckning.</p>

I fokus för denna uppsats står samverkansorganet och kommunalförbundet Region Halland eller mer exakt den form av indirekt demokrati som organisationen styrs genom. Studiens syfte är att ur ett demokrati och legitimitetsteoretiskt perspektiv undersöka Region Halland med fokus på just den indirekta demokratin. Studiens frågeställning är tvådelad och undersöker dels hur förankringen av politik inom Region Hallands ram förankras i kommunerna och hos medborgarna. Dessutom undersöks vilka demokratipolitiska ambitioner som Region Halland har. I uppsatsen används en form av kvalitativ metod nämligen samtalsintervjun och intervjuerna genomförs med politiker verksamma i kommunerna och Region Halland samt med tjänstemän på Region Halland. Studiens resultat visar att debatten i kommunens politiska organ om Region Halland är begränsad och att medborgarna inte heller är särdeles involverade i politiska frågor som drivs av Region Halland. Det framkommer även att Region Halland inte på egen hand driver demokratipolitiska projekt i någon större utsträckning.

Gas-expanded liquids (GXLs) are a new and benign class of pressure-tunable liquid solvents which show tremendous promise as the next sustainable processing medium. In order to realize the potential of GXLs fully, it is necessary to elucidate their cybotactic region and gain an understanding of where properties are different in the bulk and micro-scales and how local structure and order affect both reactions and separations. This work explores the cybotactic region of GXLs and probes the existence and implications of those differences. This study is started by exploring the cybotactic region of ambient liquid mixtures. Thermodynamic models based on intermolecular forces are used to predict the solubility of multi-functional solids in a variety of solvent mixtures. While this part does not lend any insight into GXLs directly, it acts as a stepping stone in both understanding the intermolecular forces that govern the cybotactic region and by opening the gateway to studying solid solubility in GXLs. The rest of the study focuses on the differences between bulk and local properties of GXLs. Different probes of polarity in the cybotactic region are compared and the solute dependence of the local structure is explored. Bulk transport properties are measured with different probes in an effort to see if molecular interactions play a role in governing diffusion processes in GXLs.

Abstract ¡§Western areas¡¨is a very Vague concept to indicate a relative position in a particular sector. Since the 1950s'¡Mthis expression has often been shrouded in uncertainty. The earliest division mainly indicated the coastal areas of the country¡Mthe interior and remote areas. Economically speaking¡Monly two major areas¡Mare being referred to¡Mcoastal and interior. Later¡Munder the guiding thought of preparation against war¡Mfirst¡Msecond and third lines were delimited¡]including the big third line and the small third line¡^. For the last few years¡Mthe division into eastern¡Mcentral and werstern areas has also been in usage .Though at different times the aim of division ¡Mall recognized that the level of economic development was completely out of balance. Objectively ¡Mthree economic areas exist¡Geast ¡Mcenter and west. The western areas of the People's Republic of China are vast. Their total area is 5,280,000 square kilometer or 55% of the whole country's territory. The population numbers more than 230 million¡Vabout 23% of the country total population. In economic exploitation the western areas are in comparison with the central or eastern areas¡Mrelatively backward. The western areas¡Malthough their topography is complicated and difficult of acess have with their three¡Vdimensional limate and the perpendicular distribution of flora and fauna which are comparatively concentrated a wide variety of resources. With the rapid development of the economy of our country¡Mdevelopment is bound to start from the eastern seaboard and gradually develop toward the center and the western areas . The exploitation of the latter will strategically become more and more important in China' economy. In the scope of thire contracts and regulations¡Mjoint ventures have the right to conduct reforms of the technology of production ¡Mand increase the variety of designs and colors of the needs of domestic and foreign markets. Inventures may invite foreign businessmen to come to China and send their own personnel abroad business.

In this thesis, a CMOS tunable second-order log-domain filter using pseudo-exponential approximation is proposed. MOSFETs in the circuit are working in the saturation region. This filter has higher frequency response than that of weak inversion CMOS filter. The circuit has been fabricated with 0.35um CMOS technology. It operates with a supply voltage 3V, internal capacitance C is 1pF, the biasing current varies from 2uA~10uA. The cutoff frequency can be turned from 2MHz~37.5MHz. The harmonic distortion is 0.93% and the power consumption is 772uW.

Univ., Diss.--Leiden, 2006. / Zsfassung in niederländ. Sprache.

Thesis (M.A.)--York University, 1997. Graduate Programme in Geography. / Typescript. Includes bibliographical references (leaves 182-185). Also available on the Internet. MODE OF ACCESS via web browser by entering the following URL:http://wwwlib.umi.com/cr/yorku/fullcit?pMQ27340.

published_or_final_version / Surgery / Master / Master of Philosophy

No description available.

The Pima mine, a 39,000 ton per day copper mine, is located 17 miles south of Tucson, Arizona. The mine is in a sequence of Paleozoic and Mesozoic sediments striking east-northeast and dipping southeasterly intruded by Tertiary quartz monzonite porphyry. The Paleozoic Permian(?) dolomites, limestones, and sandstones have been altered to calc-silicate skarn, marble and quartzite. The overlying Mesozoic Triassic(?) clastic sediments have undergone some recrystallization and hydrothermal alteration. The clastic metasediments are divided into three distinct lithologic units: lithic arenite, arkose, and interbedded and overlying black argillite. Three types of hydrothermal alteration in the clastic rocks are propylitic alteration (eqidote, chlorite, and quartz, with or without sericite), quartz-sericite alteration, and potassic alteration (K-feldspar and quartz, with or without sericite and chlorite). The porphyry has undergone potassic alteration. Dominant structures are an east-west post mineral fault in teh western part of the pit, and strong low angle shearing and faulting which truncates the ore body at depth. Two joint sets, one parallel to bedding and the other at right angles to bedding are prominent in the mine. Faulting is in two dominant directions, one striking northwest, dipping northeast and the other striking northeast, dipping northwest. Mineralization is predominantly disseminated pyrite and chalcopyrite, and molybdenite-quartz veinlets. There are less important amounts of magnetite, hematite, sphalerite, galena, tennantite, and bornite. Mineralization is believed to be both structurally and chemically controlled.