{ environment and energy guest lecture 2/26/15 marianne nyman
TRANSCRIPT
The surroundings or conditions which a person, animal, or plant lives or operates.
The natural world, as a whole or in a particular geographical area, especially affected by human activity.
Environment
Goal 1:To demonstrate how chemical structures cause the molecular interaction that govern the various transfer and reaction processes.
Goal 2: To illustrate how principles of chemistry, physics, and biology can be used to quantify these processes.
Goal 3: Use Goals 1 and 2 to obtain information about the ecosystem = environment.
Goals
To understand the nature and reactivity of HOCs.
Have to know what they are made of. Atoms Bonds linking them.
Solubility Vapor pressure MW Others
The Makeup of Organic Compounds
Have different personalities: Some volatile. Some insoluble in water. Some have energy value associated with
the compound. Many compounds are carcinogenic and
toxic. Will associate with solid material like
soils and sediments. Problem all over the world.
Hydrophobic Organic Compounds (HOCs)
Phase transfer Air Water Soil/sediment
Equilibrium Abiotic/biotic transformations
Macroscopic scale
QUANTITATE INDIVIDUAL PROCESSES
Modeling Transport Energy Economics
Ecosystem
The system resulting from the integration of all living and non-living factors of the environment. Based on interactions and exchange ofMaterials. Ecosystem is the highest level of ecological interaction, Which is energy-based and this functional unit is capable of energyTransformation, accumulation, and circulation.
COUPLING PROCESSES
Natural (no human activity), terrestial (grassland), aquatic (freshwater andmarine water), and artificial (maneged by humans (cropland))
Cultural
Biological
Physical
Lithosphere
Hydrosphere
Atmosphere
Flora
Fauna
Microbe
Social
Political
Economical Elements of the Environment
Components of population and environment
Physical
Social institution, forms rules, polices, social wellfare
Socila
Derives and utilizes resources
Economic
1. Land changes1. Clearing forests, burning land, changing cropping
plans
2. Construction and excavation1. Dams, diversion of rivers, construction of roads,
urbanization
3. Agricultural practices1. Mechanics of agriculture, use of chemical
fertilizers, pesticides etc.
4. Weather1. Fogs, precipitation
5. Nuclear1. Nuclear energy
Impact on the environment
Indirect = unintentional impact Industrial development for economic
growth Impact noticed after a longer period of time Non-reversible Affects the natural ecosuystem
Impact of man on environment
Toxic Substance
sInsecticid
eGarbage
Land
EffluentIndustrial
WasteChemicals
Water
SmokeCoal
BurningCFC
Air
Impact of human activities on the environment
Biogeochemical cycles
Atmosphere (gas phase)
Biota
Soils Rivers Oceans Volcanoes
ashes,gases
phase
organic
Rocks (weathering and erosion)
Soil and type – very important! Required for plant grouwth Environmental degradation Source of sediment Filter for groundwater Bearing material for roads, pipelines, houses etc.
Formation of soil In-siitu from rocks Dependent on:
Climate (temperature, rain, wind) Type of material (mineral content –clay,silt,sand) Time (length of weathering) Organisms (soil richness)
Contamination of soil HOCs Cadmium Mercury Arsenic Lead
Land Resources
Agriculture Urbanization Development of infrastructure Industry Mining Energy recovery (wind mills)
Impact on human activities on land resources
Water Resources
Pro
tect
s pla
nts
Pro
tect
s w
ater
qual
ity
Prote
cts air
quality
Reduces noise
Protects natureSupports
biodeviersity
Protects human health
Water resources:• Covers over 71% of Earth’s surface• Found everywhere• Important for living org.• Hydrologic cycle• Surface water• Subsurface water• Atmospheric water
Suspended Diameter >1 mm Settles down quickly Can be retained by filtration
Colloidal <0.05 um Very small settling rate Passes through filters due to small size Appears cloudy Gives color to water (blue, green, or red)
Dissolved <0.005 um Does not settle out When neutral = molecules; when charger = ions
Substances in water
Air resources
Atmosphere
Photochemical reaction
(UV)
O3
Photochemical reaction
(UV)
O2 and H2
Ocean (photosynthe
sis and plants)
O2
COs
Emissions
CO2, NH3, H2O
Early organisms started producing OM through photosynthesis.
O2 was liberated Saturated water Filled the atmosphere
O2 had some toxicity to primitive organisms
Other species started to use oxygen for energy through respiration.
N2 evolved from Earth’s interior.
Origin of atmosphere
Capacity to do work Mechanical energy (potential energy) Kinetic energy (motion) Total mechanical energy =
kinetic+potential Other forms of energy
Heat Light Electrical Sound Chemical etc.
Energy
Energy cannot be created or destroyed. It only changes forms from one to another
Conservation of energy
Biogeochemical cycles
Atmosphere (gas phase)
Biota
Soils Rivers Oceans Volcanoes
ashes,gases
phase
organic
Rocks (weathering and erosion)
Renewable energy Water
Hydroelectric energy Obtained from water flow
Wind Has to be higher that 5-10 m/s
Axel of a windmill generates this into energy California – lots of energy produced
Sun Provides continuous source of energy Exceeds demand X-rays, gamma-rays, and UV Small portion of solar radiation is received by Earth Average solar radiation on Earth = 1.2 kW/m2 – ca 0.3 kW/m2 is
refelected back Rest utilized for photosythesis and evaporation
600 x greater than all the rest of the sources combined Tidal
Thermal energy conversion Temp on surface 29-30 C Temp on cold deep sea 5-7 C
Types of energy sources
Non-renewable energy Nuclear
Developed after World War II Substitute for fossil fuel
Gas Methane major constituent Least polluting of all energy sources Lower S content
Coal All over the world Estimated mining 300-850 years Higher S content
Oil
Types of energy sources