By JT Houghton, LG Meira Filho, DJ Griggs and K Maskell (Eds).
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Content material: - Contents, Pages v-viiiChapter 1 - Parameters, Pages 1-8Chapter 2 - Pump Calculations, Pages 9-18Chapter three - Required facts for Specifying Pumps, Pages 19-20Chapter four - Pump kinds, Pages 21-41Chapter five - requisites, Pages 42-44Chapter 6 - Pump Curves, Pages 45-54Chapter 7 - results of Viscosity on Pump functionality, Pages 55-60Chapter eight - Vibration, Pages 61-82Chapter nine - web confident Suction Head (NPSH), Pages 66-73Chapter 10 - Pump Shaft Sealing, Pages 74-82Chapter eleven - Pump Bearings, Pages 83-91Chapter 12 - Metallurgy, Pages 92-99Chapter thirteen - Pump Drivers, Pages 100-113Chapter 14 - Gears, Pages 114-120Chapter 15 - Couplings, Pages 121-127Chapter sixteen - Pump Controls, Pages 128-136Chapter 17 - Instrumentation, Pages 137-139Chapter 18 - Documentation, Pages 140-145Chapter 19 - Inspection and trying out, Pages 142-145Chapter 20 - install and Operation, Pages 146-150Chapter 21 - Troubleshooting, Pages 151-153Appendix 1 - pattern Pump standards, Pages 154-159Appendix 2 - Centrifugal Pump facts Sheet, web page 160Appendix three - inner Combustion Engine info Sheet, web page 161Appendix four - electrical Motor info Sheet, web page 162Appendix five - Centrifugal Pump package deal, web page 163Appendix 6 - greatest doable Suction Lifts at quite a few Altitudes, web page 164Appendix 7 - instructed checklist of owners, Pages 165-174Appendix eight - API-610 Mechanical Seal category Code, web page 175References, web page 176Index, Pages 177-182
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Extra resources for An Introduction to Simple Climate Models used in the IPCC Second Assessment Report (IPCC Technical Paper II - February 1997)
3, the dependence of the CH4 lifetime on CH4 concentration is affected by the concurrent concentrations of NOx, CO and VOCs in the atmosphere, which vary significantly between regions. 3), these emissions were assumed to be constant. This feedback is based on calculations using three-dimensional models, as discussed by Osborn and Wigley (1994). The currently estimated CH4 lifetime is given in Appendix 1. 3) projections of global mean temperature and sea level. If soil absorption was the only removal process, the average lifespan of methane in the atmosphere would be about 150 years.
Although this is not exactly true, the error so introduced is overwhelmed by uncertainties in the link between atmospheric aerosol loading and global mean radiative forcing. 5). 12). In the latter case, total anthropogenic sulphur emissions will increase from 75 TgS in 1990 to 147 TgS in 2100. 2 W m-2), then is held constant. 5 27 Calculating Radiative Forcing From Concentrations Given the concentrations of globally uniform greenhouse gases, the direct radiative forcing can be computed by using simple formulae which provide a close fit to the results of detailed radiative transfer calculations.
3 Uncertainties in Sea Level Projections Uncertainties in the thermal expansion component of global mean sea level change are linked with those of surface temperature change itself, because thermal expansion is computed from the variation of ocean temperature change with depth. 5˚C, the uncertainty in thermal expansion is about a factor of two over the next century. The main uncertainties in deriving the land ice contribution to sea level rise from global mean temperature 30 27 Total Thermal expansion Glaciers/ice caps Greenland Antarctica 25 20 Sea level change (cm) Studies of well-observed glaciers indicate that glaciers in a wetter climate are more sensitive to changes in air temperature than glaciers in dry regions.