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Chapter 1 An Introduction to Environmental Issues

Chapter 1 An Introduction to Environmental Issues

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  • Slide 1
  • Chapter 1 An Introduction to Environmental Issues
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  • Multiple pathways are possible Exposure Routes 1. Inhalation 2. Ingestion 3. Dermal (skin)
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  • Role of Chemical Engineer Examples: (1) formulation of an industrial cleaner; (2) formulation of a paint solvent; (3) Choice of refrigerant for a low-temperature condenser. What information will a chemical engineer need to make informed pollution prevention and risk reduction decisions? Impacts on human exposure (dermal, inhalation and ingestion) Life cycle of a chemical
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  • Formulation of an Industrial Cleaner To lower the aquatic toxicity of the solvent: 1.High Henrys law constant (substance will volatize into the air rather than stay in the water); 2.High biodegradation rate (it will dissipate before exerting adverse health effects); 3.Low fish toxicity parameter (a high value of the concentration lethal to a majority of test organisms or LC_50); 4.Low Bioconcentration Factor, BDF (low tendency for chemicals to partition into the fatty tissue of fish, leading to exposure and adverse health effects upon consumption by humans)
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  • Formulation of a Paint Solvent A chemical will have low risk potential in the air if it has 1.Low toxicity properties (a high Reference Dose [RfD] for inhalation toxicity to humans or a low cancer potency); 2.Low reactivity for smog formation (ground level ozone production).
  • Slide 7
  • Choice of Refrigerant for a Low- Temperature Condenser 1.High atmospheric reaction-rate constant; 2.Low global warming potential; 3.Low ozone depletion potential.
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  • Scope of environmental impacts Raw Materials Extraction Energy Wastes Chemical Processing Wastes Product Manufacturing Wastes Use, Reuse, Disposal Wastes Materials Energy Materials Energy Materials Energy Materials Pollution Control Pollution Control Life- Cycle Stages global warming ozone depletion smog formation acidifi- cation ecological harm Human health and ecosystem damage Midpoints Endpoint
  • Slide 9
  • Global Environmental Issues Global Energy Issues Global Warming Ozone Depletion in the Stratosphere
  • Slide 10
  • Energy Conversion Efficiency Primary energy source (fossil fuel) must be converted to another form (heat or electricity). Examples: automobile (10%) and pump (13%).
  • Slide 11
  • World Energy Statistics From 1960 to 1990, world energy requirements rose from 3.3 to 5.5 gtoe (gigatonnes oil equivalent). Fossil fuels: 85%; renewable sources (hydroelectric, solar and wind power): 8%; nuclear power: 6% (US-20% of electricity demand, Japan-28%, Sweden-50%). Disparity in energy use 65-70% of the energy is used by about 25% of the worlds population. The average citizen in North America consumes almost 15 times the energy consumed by a resident in sub-Saharan Africa. World energy consumption is expected to grow by 75% in the year 2020 compared to 1995.
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  • U.S. Energy Flows, 1997 Annual Energy Review 1997, U.S. DOE, Energy Information Administration, Washington, DC, DOE/EIA-0384(97)
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  • Environmental Effects Associated with Energy Consumption Fossil fuel combustion releases large quantities of (1) carbon dioxide into atmosphere (global warming) and (2) oxides of nitrogen and sulfur oxides (ground-level ozone and acid rain) Hydropower energy generation requires widespread land inundation, habitat destruction, alteration in surface and ground water flow, and decreases the acreage of land available for agricultural use. Nuclear power has environmental problems linked to uranium mining and spent nuclear rod disposal. Use of wood has caused widespread deforestation in localized regions of developing countries. Solar power panels require energy-intensive use of heavy metals and creation of metal wastes.
  • Slide 14
  • Greenhouse Effect The atmosphere allows solar radiation from sun to pass through without significant absorption of energy. Some of the solar radiation reaching the surface of earth is absorbed, heating land and water. Infrared radiation is emitted from the earths surface, but certain gases in the atmosphere absorb this infrared radiation, and redirect a portion back to the surface, thus warming the planet and making life possible. This process is often referred to as greenhouse effect.
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  • Global Warming and Related Impacts Chemical Processing EnergyMaterials Products greenhouse gas emissions CO 2, CH 4, N 2 O climate change; sea level change human mortality or life adjustments Cause and Effect Chain Contribution to global Warming; Phipps, NPPC, http://www.snre.umich.edu/nppc/ Climate Change 1995, Intergovernmental Panel on Climate Change, WMO and UNEP, Cambridge University Press, 1996.
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  • Bad Ozone Tropospheric ozone, created by photochemical reactions involving nitrogen oxides and hydrocarbons at the earths surface, is an important component of smog. A potent oxidant, ozone irritates the breathing passages and can lead to serious lung damage. It is also harmful to crops and trees.
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  • Good Ozone Stratospheric ozone, found in the upper atmosphere, perform a vital and beneficial function for all life on earth by absorbing harmful ultraviolet radiation.
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  • Stratospheric Ozone Layer The stratospheric ozone layer is a region in the atmosphere between 12 and 30 miles (20-50 km) above ground level in which the ozone concentration is elevated compared to all other regions of the atmosphere (10 ppm or 1 out of every 100,000 molecules). Ozone is formed at altitudes between 25 and 35 km in the tropical regions near the equator where solar radiation is consistently strong throughout the year. Because of atmospheric motion, ozone migrates to the polar regions and its highest concentration is found there at about 15 km in altitude.
  • Slide 20
  • Chlorofluorocarbon (CFC) CFCs are highly stable chemical structures composed of carbon, chlorine and fluorine, e.g., CCl3F or CFC-11. CFCs reach the stratosphere due to their chemical properties: high volatility, low water solubility, and persistence (non-reactivity) in the lower atmosphere.
  • Slide 21
  • Destruction of Ozone by CFCs In the stratosphere, the CFCs are photo-dissociated to produce chlorine atoms, which then catalyze the destruction of ozone: Notice that the chlorine is not destroyed in the reaction and can cause the destruction of up to 10000 molecules of ozone before forming HCl by reacting with hydrocarbons. The HCl eventually precipitates from the atmosphere. A similar mechanism also applies to bromine.
  • Slide 22
  • Stratospheric Ozone and Related Impacts Chemical Processing EnergyMaterials Products ozone depleting substances CFCs, HCFCs ozone layer loss increase in uv human mortality or life adjustments ecosystem damage Cause and Effect Chain Toxics Release Inventory Data
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  • Slide 25
  • Air Quality Issues Air pollution sources includes stationary (factories and other manufacturing processes), mobile (transportation and recreational vehicles) and area sources. Pollutants can be classified as primary, e.g., VOC and NOx, and secondary, e.g., smog. Air quality problems are closely associated with combustion processes occurring in the industrial and transportation sectors of the economy.
  • Slide 26
  • Criteria Air Pollutant US Congress in 1970 passed Clean Air Act which charged EPA with identifying those air pollutants which are most deleterious to public health and welfare. EPA identified 6 substances as criteria air pollutants and promulgated primary and secondary standards that make up the National Ambient Air Quality Standards (NAAQS). Primary standards are intended to protect the public health with an adequate margin of safety. Secondary standards are meant to protect public welfare, such as damage to crops, vegetation, and ecosystems or reduction invisibility.
  • Slide 27
  • Slide 28
  • From NOxs, HCs and VOCs to Ground-Level Ozone Ground-level ozone is a component of photochemical smog. The precursor contaminants are NOx and hydrocarbons. NOx along with sunlight cause ozone formation, but the role of hydrocarbons is to accelerate and enhance ozone accumulation.
  • Slide 29
  • Nitrogen Oxides NOxs are formed in high-temperature industrial and transportation combustion processes. In 1997, transportation sources account for 49.2% and non-transportation sources account for 45.4% of the total NOx emission. Short-term exposure (