Study Notes For Quiz 2 Flashcards

0
Q

Ecosystem

A

Must include geology since the litho loft supports a variety if species

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1
Q

Ecology

A

Study of living organisms and their links and interactions to each other and the non living environment

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2
Q

How do ecosystems work?

A

Energy flows in and through a system is transformed

Sun > grass > cows > methane

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3
Q

Natural service functions

A

Systems that produce clean water, air, provide nutrients to plants to increase soil fertility

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4
Q

Balance of an ecosystem

A

Need change and disturbance and reaction to that

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5
Q

Types of ecosystems

A

Indigenous, Natural, Human modified, Human Made/Constructed

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6
Q

Keystone Species

A

Individual species with a strong community effect and disproportionate influence to their abundance

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7
Q

Increasing biodiversity

A

Diverse habitat with many potential niches, moderate amount of disturbance, presence of harsh environments, relative constant environmental factors, relatively slow evolution, high midi fixation by life, geology

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8
Q

Decrease Biodiversity

A

Extreme environments in large amounts, extreme or frequent disturbance, fragmented ecosystems, environmental stresses, habitat simplification, exotic or intrusive species that compete with native species, geology that restricts migration of plants/animals

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9
Q

Porosity

A

Space between solid grains of a sample, measured in percent of total volume

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10
Q

Changing porosity

A

Cement, fill with smaller grains, consolidate

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11
Q

Permeability

A

Connectedness of the pores (allows flow through a material) measured in DARCY’S

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12
Q

Primary Openings

A

Naturally occurring porosity

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13
Q

Secondary Openings

A

Something had caused more spaces to occur

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14
Q

Water Table

A

Processes called infiltration causes water table, unsaturated zone, saturated zone, capillary fringe zone

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15
Q

Capillary fringe

A

Not completely saturated, water can move up or down

16
Q

Effluent Stream

A

Intersects water table, recharged by the groundwater, streams get water from water table, perennial streams, discharge water from the water table

17
Q

Influential Stream

A

Recharges the water table, loses water to the water table, usually does not flow year round, intermittent stream or ephemeral stream, low precipitation.

18
Q

Groundwater

A

Fills the spaces between soil particles and fractured rock underground

19
Q

Aquifer

A

Rock with good permeability

20
Q

Aquitard

A

Any geologic material that blocks water flow (impermeable)

21
Q

Spring

A

Where a perched water table hits an aquitard and makes it move laterally, where the water comes out of the side of a hill

22
Q

Perched water Tablr

A

Water table sub sects the subsurface and hits an aquitard, above water table, moves laterally along

23
Q

Artesian Aquifer

A

Confined on top and bottom by aquitard

24
Contour the Water Table
Assume uniform geology unless you have other information, contour as you would surface topography, groundwater flow is at right angles to flow lines
25
Well Yield
Depends on geologic material, topography, climate
26
Cone of depression
When water is pumped faster than it can be replenished in a system a local draw down occurs, can change the regional flow of groundwater
27
Sources of Water Pollution
Can be one time events, continuous, source fed In 2D: plume, concentration highest in centre as water moves away from source In 3D: teardrop shape, accurate in real life, density of pollutant influences whether it will float or sink within the saturated zone
28
Non Point Source
Surface runoff, storm drainage, hydrocarbons, detergents, fertilizers, cause regional ground water pollution
29
Regional Source
Over fertilization, naturally occurring minerals such as selenite, acid mine drainage from water filled shafts, any regional source can be leached
30
Hydraulic gradient
Rise/Run
31
Groundwater Flow
Hydraulic Gradient
32
Apparent groundwater speed
Distance groundwater will travel over some unit of time, assumes homogeneous subsurface, allows mapping if contamination flow, concentration of contamination typically decreases with distance from source
33
Hydraulic conductivity
Movement of groundwater is also a function of materials profanity and permeability
34
Testing Drinking Water
pH, Coliform count, turbidity (sediment in water), taste, total dissolved solids (hardness)
35
Salt water Incursion
Natural Cause: dropping water table allows influx of salt water Man-Made: over pumping of water
36
Subsidence
Sinking or lowering of land surface, may be gradual or very rapid, area may be a few square meters or many square kilometres, multiple causes
37
Causes of Subsidence
Natural: dissolution of limestone (karst), subsurface slat migration, compaction of sediment, caldera formation Man-Made: withdrawal of fluids, mind collapse, broken underground pipelines
38
Karst
Dissolution of primarily limestone by weak carbonic acid Features: sinkholes, solution valleys, caverns, sprigs & disappearing streams Forms: Stalactites & Stalagmites (hang tight from ceiling, be mighty to grow from ground), columns, soda straws, bacon slabs, terraces, tufa deposits.