Lecture 12: Hydrologic Cycle Flashcards
-Properties of Water -Water Cycle and Balance -Water on the Land's Surface
What is the chemistry of the water molecule?
- formed by the covalent bonding of two hydrogens to and oxygen
- Bent (104.5º)
- Polar (more negative charge near the oxygen, more positive near the hydrogens)
What are the phases of water?
- Ice
- Liquid Water
- Water Vapour
What transitions between phases absorb energy?
Evaporation, Melting, Sublimation
What transitions between phases release energy?
Condensation (water vapour to liquid water), Freezing, Condensation (water vapour to ice)
Latent heat
The energy absorbed or released by a body or thermodynamic system during a constant-temperature process.
Properties of liquid water
Due to its polarity, it:
- Has a high surface tension
- Is an excellent solvent
Properties of ice
- Lower density than liquid water due to an open crystal lattice
- Floats in liquid water
- Expansion of freezing water can cause physical weathering
Evaporation
Solar energy causes water to evaporate from large bodies of water, moving it into the atmosphere.
Transpiration
The water vapour that is given off by plants.
Condenses
Water vapour condenses into clouds
Precipitation
The water falls back to land or the ocean as precipitation; rain, hail, or snow.
Infiltration
Some of the water infiltrates the ground, where it joins the ground-water reservoir and may eventually be locked up in the lithosphere in the form of the hydrous mineral.
Runoff
Some of the moisture flows back to the sea as surface runoff, while a small amount is captured by the biosphere.
Hydrologic reservoirs
Places in the water cycle where water is stored.
- Nearly all the Earth’s water resides in the oceans
- 75% is locked up as ice at the poles
- Freshwater and surface water bodies comprise less than 3% of the total water on Earth
Residence time
The average amount of time that a water molecule stays in a particular reservoir
Flux
The rate at which water moves between reservoirs
The residence time of Earth’s reservoirs
- Atmosphere: days
- Rivers and lakes: months to years
- Shallow groundwater: decades to centuries
- Oceans: thousands of years
- Antarctic ice: tens of thousands of years
Hydrologic balance
The relationship between flux, reservoir size, and residence times.
-relatively small water reservoirs can have high fluxes because the residence time is short
Overland flow
The initial sheet-like movement of water downhill with gravity.
- Some of the rainfall and meltwater on the landscape begins to flow across the surface once the soil is saturated.
Stream flow
Once the flow of water occurs in an establishmed channel
-Overland flow becomes channelized due to erosion, typicaly over relatively short distances.
Surface runoff
When stream flow and overland flow together they create surface runoff.
What are the two major sources for the flow of water in streams?
- Overland flow contributions
2. Baseflow
Baseflow
The input of groundwater through the bed of a river, contributing to its flow.
River systems
- Streams organize into river systems
- Small streams (tributaries) typically merge downstream