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Data publikacji: 6 września 2023

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1

T, Van Dresar Neil, Hasan Mohammad M i United States. National Aeronautics and Space Administration., red. A pressure control analysis of cryogenic storage systems. [Washington, DC]: National Aeronautics and Space Administration, 1991.

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2

George C. Marshall Space Flight Center., red. Performance assessment of low pressure nuclear thermal propulsion. [Marshall Space Flight Center, Ala.]: National Aeronautics and Space Administration, George C. Marshall Space Flight Center, 1993.

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3

Jim, Lozier, i AWWA Research Foundation, red. Natural organic matter fouling of low-pressure membrane systems. Denver, CO: Awwa research Foundation, 2008.

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Jim, Lozier, i AWWA Research Foundation, red. Natural organic matter fouling of low-pressure membrane systems. Denver, CO: Awwa research Foundation, 2008.

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Jim, Lozier, i AWWA Research Foundation, red. Natural organic matter fouling of low-pressure membrane systems. Denver, CO: Awwa research Foundation, 2008.

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6

Winkler, Eric S. Design guidance for shallow trench low pressure pipe systems. Amherst, Mass: Center for Energy Efficiency and Renewable Energy, University of Massachusetts at Amherst, 2001.

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7

Hargett, David L. Technical assessment of low-pressure pipe wastewater injection systems. Cincinnati, OH: U.S. Environmental Protection Agency, Water Engineering Research Laboratory, 1987.

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8

Jim, Lozier, i AWWA Research Foundation, red. Natural organic matter fouling of low-pressure membrane systems. Denver, CO: Awwa research Foundation, 2008.

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9

United States. Environmental Protection Agency. Office of Municipal Pollution Control. Office of Water. i Metcalf & Eddy., red. Heat treatment/low pressure oxidation systems: Design and operational considerations. Washington, D.C: Office of Municipal Pollution Control, Office of Water, U.S. Environmental Protection Agency, 1985.

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10

United States. Environmental Protection Agency. Office of Municipal Pollution Control. Office of Water i Metcalf & Eddy, red. Heat treatment/low pressure oxidation systems: Design and operational considerations. Washington, D.C: Office of Municipal Pollution Control, Office of Water, U.S. Environmental Protection Agency, 1985.

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11

United States. Environmental Protection Agency. Office of Municipal Pollution Control. Office of Water. i Metcalf & Eddy., red. Heat treatment/low pressure oxidation systems: Design and operational considerations. Washington, D.C: Office of Municipal Pollution Control, Office of Water, U.S. Environmental Protection Agency, 1985.

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12

Heating and Ventilating Contractors' Association. Specification for sheet metal ductwork: Low, medium and high pressure/velocity air systems. Penrith: HVCA Publications, 1988.

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13

Specification for sheet metal ductwork: Low, medium and high pressure/velocity air systems. Penrith: HVCA Publications, 1998.

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14

Leeuwen, S. Storm van. A simple and low cost system to measure delay times in pneumatic systems. Amsterdam: National Aerospace Laboratory, 1990.

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15

Starbuck, J. M. Tribological evaluation of dual lubricant condition bearing materials for use in low pressure aerospace fuel pump systems. Portsmouth: University of Portsmouth, 2002.

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16

California Energy Commission. Public Interest Energy Research. Offgases project oil-field flare gas electricity systems: PIER final project report. Sacramento, Calif.]: California Energy Commission, 2008.

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17

Center, Langley Research, red. Summary of a study to determine low-velocity impact damage and residual tension strength for a thick graphite/epoxy motor case. Hampton, Va: National Aeronautics and Space Administration, Langley Research Center, 1990.

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18

NCCER. 32208-08 Low-Pressure Steam Systems TG. Pearson Education, Limited, 2008.

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19

Bentum, Robert Van. Low pressure pipe distribution systems for surface irrigation. 1992.

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20

RSES. Refrigerant Usage Certification Preparation: Type III- Low-Pressure Systems. Elsevier Science & Technology Books, 2008.

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21

The 2006-2011 World Outlook for Non-Aerospace-Type Low-Pressure Hydraulic Fluid Filter Assemblies for Fluid Power Transfer Systems with Less Than 301 P.s.i. Icon Group International, Inc., 2005.

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22

Parker, Philip M. The 2007-2012 World Outlook for Non-Aerospace-Type Low-Pressure Hydraulic Fluid Filter Assemblies for Fluid Power Transfer Systems with Less Than 301 P.s.i. ICON Group International, Inc., 2006.

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23

Dunlop, Storm. 5. Weather systems. Oxford University Press, 2017. http://dx.doi.org/10.1093/actrade/9780199571314.003.0005.

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At temperate latitudes, such as those of the British Isles, the most significant changes in the weather, with major changes in wind strength and direction, as well as rainfall, are associated with the passage of depressions (low-pressure systems), more formally known as extratropical cyclones. ‘Weather systems’ describes the development of depressions, the different features within them (the warm front, the warm sector, the cold front, and the occluded front), and the likely weather produced. It also looks at isolated fronts, the sudden deepening of depressions, thermal and polar lows, atmospheric rivers, and the much quieter weather of high-pressure systems.

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24

Ye, Liu, Jose Porro i Ingmar Nopens, red. Quantification and Modelling of Fugitive Greenhouse Gas Emissions from Urban Water Systems. IWA Publishing, 2022. http://dx.doi.org/10.2166/9781789060461.

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Abstract With increased commitment from the international community to reduce greenhouse gas (GHG) emissions from all sectors in accordance with the Paris Agreement, the water sector has never felt the pressure it is now under to transition to a low-carbon water management model. This requires reducing GHG emissions from grid-energy consumption (Scope 2 emissions), which is straightforward; however, it also requires reducing Scope 1 emissions, which include nitrous oxide and methane emissions, predominantly from wastewater handling and treatment. The pathways and factors leading to biological nitrous oxide and methane formation and emissions from wastewater are highly complex and site-specific. Good emission factors for estimating the Scope 1 emissions are lacking, water utilities have little experience in directly measuring these emissions, and the mathematical modelling of these emissions is challenging. Therefore, this book aims to help the water sector address the Scope 1 emissions by breaking down their pathways and influencing factors, and providing guidance on both the use of emission factors, and performing direct measurements of nitrous oxide and methane emissions from sewers and wastewater treatment plants. The book also dives into the mathematical modelling for predicting these emissions and provides guidance on the use of different mathematical models based upon your conditions, as well as an introduction to alternative modelling methods, including metabolic, data-driven, and AI methods. Finally, the book includes guidance on using the modelling tools for assessing different operating strategies and identifying promising mitigation actions. A must-have book for anyone needing to understand, account for, and reduce water utility Scope 1 emissions. ISBN: 9781789060454 (Paperback) ISBN: 9781789060461 (eBook) ISBN: 9781789060478 (ePub)

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25

Bernal, William, i Alberto Quaglia. Normal physiology of the hepatic system. Oxford University Press, 2016. http://dx.doi.org/10.1093/med/9780199600830.003.0173.

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Hepatic blood inflow is from two sources—high-pressure, well-oxygenated blood from the hepatic artery and low-pressure, partly deoxygenated blood from the portal vein. Hepatic inflow is maintained by variation in flows in these two systems. Although less than a third of total blood flow is delivered via the hepatic artery, it is responsible for the majority of hepatic oxygen supply. The liver can be subdivided into eight functionally independent segments, each with its own vascular inflow, outflow, and biliary drainage. The tri-dimensional hepatic microstructure is complex with geographic heterogeneity of hepatocellular function, and resistance to toxic, ischaemic, and metabolic damage. The liver is central to a wide variety of synthetic, metabolic, and detoxification functions. The overall balance of activity may be altered rapidly in response to systemic inflammatory stimuli.

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26

Candido, Kenneth D., Teresa M. Kusper, Bora Dinc i Nebojsa Nick Knezevic. Epidural Blood Patch. Oxford University Press, 2018. http://dx.doi.org/10.1093/med/9780190271787.003.0036.

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Post-dural-puncture headache (PDPH) is a consequence of neuraxial anesthesia, diagnostic lumbar puncture, intrathecal drug delivery systems, or any other technique involving dural trespass. The spinal headache results from a dural puncture that leads to cerebrospinal fluid (CSF) leakage from the subarachnoid space to the epidural space, culminating in intracranial hypotension and development of a low-pressure headache. A key element of PDPH is an increase in pain severity upon a change in position from supine to upright, which corresponds to a gravity-induced influence on CSF pressure dynamics. Age, sex, and design of the needle used correlate with the risk of headache. Sometimes, the headache resolves spontaneously. At other times, conservative treatment or aggressive measures are required to terminate the pain. An autologous epidural blood patch is an established way preventing or treating PDPH. A careful history must be obtained to identify other causes of headache before the blood patch is attempted.

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27

Jacobsen, Dean, i Olivier Dangles. Living conditions in high altitude waters. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780198736868.003.0003.

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Chapter 3 deals with the abiotic environment in high altitude lakes and streams worldwide. It searches for general patterns in relation to altitude, without overlooking the enormous variability, both temporally as well as at small and large spatial scales. Overall, environmental conditions in high altitude waters may be regarded as harsh. Indeed, certain features such as low temperature, low oxygen pressure, and high ultraviolet radiation (all a direct result of high altitude) as well as transparent and ion-poor waters with low nutrient concentrations are typical of high altitude aquatic systems. However, streams and lakes turbid from inflow of glacial meltwater loaded with glacial mineral flour and peatbogs with deep brown water from a high concentration of coloured dissolved organic matter are equally prominent. So, evidently, environmental conditions in aquatic systems are probably just as variable at high as at low altitudes.

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Dunlop, Storm. 7. Severe and unusual weather events. Oxford University Press, 2017. http://dx.doi.org/10.1093/actrade/9780199571314.003.0007.

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Convective clouds may range from relatively innocuous showers to major supercell systems accompanied by dramatic conditions. ‘Severe and unusual weather events’ explains how convective cells generate in cumulonimbus clouds and how thunderstorms and associated lightning develop. Convective clouds may cluster together resulting in vigorous circulation and heavy precipitation. Even more active and dramatic systems are supercells that create tornadoes. These arise when a deep pool of unstable air is accompanied by a strong increase in wind speed with height, together with directional wind shear. Tropical cyclones are closed, non-frontal, low-pressure systems of high winds arising some 5–10° away from the equator, where the Coriolis acceleration promotes their overall rotation.

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29

Jacobsen, Dean, i Olivier Dangles. The high altitude environment. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780198736868.003.0001.

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Chapter 1 gives a brief overview of the climatic and terrestrial environment in which high altitude waters are embedded. This context is necessary to understand the prevailing environmental conditions in the aquatic systems. The chapter begins by defining high altitude, alpine, and mountain, and provides an overview of the distribution of the world’s main high altitude regions. The overall picture of the climatic setting is drawn, from the inevitable consequences of high altitude (low temperature, low atmospheric pressure, and high solar radiation) to the highly region-specific patterns in precipitation and wind. The various ways that highland regions are formed, their temporal evolution, and climatic changes are treated in a section on the palaeo-environmental perspective. Finally, general patterns in high altitude (alpine) vegetation zones and treelines on different continents are synthesized, as well as major soil-forming processes in the catchments surrounding aquatic systems.

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30

Omstedt, Anders. The Development of Climate Science of the Baltic Sea Region. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.654.

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Dramatic climate changes have occurred in the Baltic Sea region caused by changes in orbital movement in the earth–sun system and the melting of the Fennoscandian Ice Sheet. Added to these longer-term changes, changes have occurred at all timescales, caused mainly by variations in large-scale atmospheric pressure systems due to competition between the meandering midlatitude low-pressure systems and high-pressure systems. Here we follow the development of climate science of the Baltic Sea from when observations began in the 18th century to the early 21st century. The question of why the water level is sinking around the Baltic Sea coasts could not be answered until the ideas of postglacial uplift and the thermal history of the earth were better understood in the 19th century and periodic behavior in climate related time series attracted scientific interest. Herring and sardine fishing successes and failures have led to investigations of fishery and climate change and to the realization that fisheries themselves have strongly negative effects on the marine environment, calling for international assessment efforts. Scientists later introduced the concept of regime shifts when interpreting their data, attributing these to various causes. The increasing amount of anoxic deep water in the Baltic Sea and eutrophication have prompted debate about what is natural and what is anthropogenic, and the scientific outcome of these debates now forms the basis of international management efforts to reduce nutrient leakage from land. The observed increase in atmospheric CO2 and its effects on global warming have focused the climate debate on trends and generated a series of international and regional assessments and research programs that have greatly improved our understanding of climate and environmental changes, bolstering the efforts of earth system science, in which both climate and environmental factors are analyzed together.Major achievements of past centuries have included developing and organizing regular observation and monitoring programs. The free availability of data sets has supported the development of more accurate forcing functions for Baltic Sea models and made it possible to better understand and model the Baltic Sea–North Sea system, including the development of coupled land–sea–atmosphere models. Most indirect and direct observations of the climate find great variability and stochastic behavior, so conclusions based on short time series are problematic, leading to qualifications about periodicity, trends, and regime shifts. Starting in the 1980s, systematic research into climate change has considerably improved our understanding of regional warming and multiple threats to the Baltic Sea. Several aspects of regional climate and environmental changes and how they interact are, however, unknown and merit future research.

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31

Wilson, Shaun. Living Wages and the Welfare State. Policy Press, 2021. http://dx.doi.org/10.1332/policypress/9781447341185.001.0001.

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Living Wages and the Welfare State documents and analyses a key transition now underway in the Anglo-American social model. Although minimum wages are increasing across the world, recent mobilisations for living wages represents a major challenge to the policy consensus of the Anglo-American model in place now for several decades. That consensus promoted adjustments to globalisation and technology by promoting a lean workfare model, maximising dependence on deregulated private labour markets held in place by low minimum wage floors. Growing problems with poor employment quality and low pay, combined with mean and over-policed systems of social protection, have created new pressures on institutions governing the social aspects of employment. Worker activism and a broad net of progressive policymakers have been energised by the broad popular appeal popularity of living wage claims. These reforms have been bolstered by a new political economy of labour markets casting doubt on over-confident claims of inevitable job losses from wage justice for low wage workers. At the same time, major pressure on social protection systems transformed by workfare and mean benefits have forced justice claims into the sphere of low-wage employment. In defending the value of higher and universal minimum wage floors, this book is wary of the limits of minimum wage reforms and explores how the liberal model might be realistically converted into a living wage welfare state. The author argues that living wages represents a realistic and popular platform for beginning a long struggle against rising inequality and disrespect for workers.

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32

Bockenhauer, Detlef, i Robert Kleta. Approach to the patient with salt-wasting tubulopathies. Redaktor Robert Unwin. Oxford University Press, 2018. http://dx.doi.org/10.1093/med/9780199592548.003.0031_update_001.

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Sodium is the main ion of the extracellular compartments, and it is through control of sodium reabsorption that the kidneys maintain volume homoeostasis and systemic blood pressure. The amount of sodium that is first filtered by the glomerulus and then reabsorbed in the tubule is quite staggering: assuming a glomerular filtration rate of 100 mL/min and a serum sodium concentration of 140 mmol/L, an average-sized person filters about 20,000 mmol of sodium per day, equivalent to the amount in 1.2 kg of cooking salt. In the steady state, the amount of sodium excreted is equal to the amount ingested. An average Western diet contains about 8–10 g of salt per day; a low-salt diet may be around 2 g per day. Under physiological conditions, the tubules reabsorb about 99% of filtered sodium. This enormous task is accomplished by a combination of distinct and sequentially oriented sodium or sodium-coupled transport systems along the nephron and the concerted and parallel action of some of these systems within the kidney. These are described, along with the consequences of disorders of the processes. A diagnostic approach to salt-losing states such as Fanconi, Bartter Gitelman and other syndromes, and hypoaldosteronism, is described.

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