Water Cycle and Human Impacts PDF
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Uploaded by BlitheAntimony
L. Francis
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Summary
These lecture notes cover the water cycle and human impacts, including the percentage of available water and the water cycle process. It also explores human impact on water resources, and the importance of maintaining water resources.
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BIOL 123 z Water Cycle and Human impacts by: L. Francis z OBJECTIVES ▪ State the percentage of water available for human use and the source from which it is drawn ▪ Describe the water cycle ▪ Explain...
BIOL 123 z Water Cycle and Human impacts by: L. Francis z OBJECTIVES ▪ State the percentage of water available for human use and the source from which it is drawn ▪ Describe the water cycle ▪ Explain the human impacts on the water cycle z ▪ It is fundamental to life ▪ Covers 75% of the Earth’s surface ▪ 97.5 % of the volume is saltwater of oceans and seas ▪ 2.5% is fresh water ( has a salt content of less than 0.1%) z Fresh Water ▪ Two thirds is bound in the polar ice caps and glaciers ▪ 0.77% → lakes, wetlands , rivers, ground water, biota, soil, atmosphere ▪ Evaporation from oceans combines with precipitation to continually resupply ie hydrologic cycle ▪ Represent ecosystem good and services / capital ▪ Provides drinking water, water for industries and water to irrigate crops z Bodies of Water Provides: ▪ Energy through hydroelectric power ▪ Control flooding by absorbing excess water ▪ Transportation ▪ Recreation ▪ Waste processing ▪ Habitats for aquatic plants and animals z WATER CYCLE / HYDROLOGIC CYCLE ▪ Evaporation ( liquid to gas state) ▪ Transpiration ( loss of water vapor from soil through green plants via leaf pores) ▪ Condensation ( gas state to liquid state) ▪ Precipitation ( rain , sleet, snow, hail) ▪ * green water – water in vapor form ▪ * blue water- liquid water wherever it may occur z z Evaporation ( liquid to gas state} ▪ Weak hydrogen bonds hold water molecules together ( H2O) ▪ Below 32 F (0 C) = low kinetic energy → bond held together = solid form ( ice) ▪ Above freezing but below boiling ( 212 F or 100C) → hydrogen bonds keep breaking and reforming = liquid form ( liquid water ) ▪ Energy absorbed from sunlight or artificial light → increase in kinetic energy → breaking of hydrogen bonds = gas form (water vapour) z Condensation ( gas state to liquid state) ▪ Opposite of evaporation ▪ Droplets formed in the atmosphere =fog and clouds ▪ Droplets formed on cool surfaces of vegetation = dew ▪ Facilitated by aerosols ( microscopic liquid or solid particles from land and water surfaces ), provides sites that attracts water vapor and promotes formation of droplets of moisture z *Purification ▪ Water is separated from the solutes and particles it contains ▪ Occurs naturally in evaporation and condensation Example ▪ water evaporation from the ocean: only the water molecules leave the surface( purified water vapor) , the dissolved salts and other solids remain behind. When condensed again it is purified except for the pollutants and other aersols it may pick up from the air z Transpiration ▪ loss of water vapor from soil through green plants via leaf pores z Precipitation ▪ Warm air encounters lower atmospheric pressure at increasing altitudes = gradually cools as it expands ( adiabatic cooling) ▪ 100% relative humidity + continued cooling = condensation and clouds forming ▪ Condensation intensifies → water droplets become enough to fall ( precipitation) z HUMAN IMPACTS ON THE HYDROLOGIC CYCLE 1. Changes to the surface of the Earth ▪ Loss of vegetation ▪ Taming rivers and wetlands ▪ Building impervious surfaces ( eg roads , buildings etc) ▪ Dams ▪ Moving water to the ocean ( decrease the amounts going to ground water and increases the chances of flood, droughts and erosion) 2. Climate change 3. Atmospheric particles 4. Withdrawal for human use z ▪ BIOL123 Lecturer's Notes ▪ Environmental Science Toward a Sustainable Future by RT Wright and DF Boorse 12 ed