unit 3 Flashcards

1
Q

top surface litter layer, decomposed leaves and organic matter, normally brown or black, rich in bacteria, fungi, insects and earthworms

A

o horizon

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2
Q

topsoil layer, humus and minerals. roots are in this area, also rich in living organisms, if dark brown or black: rich in nitrogen and organic materials, ***if gray/yellow/red: low in organic material, bad for crops

A

a horizon

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3
Q

subsoil layer, mostly inorganic materials, clay particles, receives material from A horizon through illuviation, may be colored by iron oxides (red), aluminum oxides (yellow), or white due to calcium carbonate, leaching, lots of humus

A

b horizon

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4
Q

weathered parent material, consists of broken fragments of parent rock, caco3 and mgco3 accumulates here forming a hard impenetrable layer

A

c horizon

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5
Q

breaks rocks into smaller pieces (water, machinery, wind, etc)

A

mechanical weathering

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6
Q

change mineral makeup of a rock, chemical reactions between minerals in the rock and the environment

A

chemical weathering

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7
Q

both mechanical/chemical in some ways, but always involves living organisms (ex: lichen secrete acids into rocks that break down its minerals)

A

biological weathering

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8
Q

diameter greater than 0.05 mm, high permeability, poor water capacity, poor nutrient capacity, good aeration, good workability, low porosity (cannot hold water)

A

sand

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9
Q

between 0.002 and 0.05 mm, medium levels of all characteristics

A

silt

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10
Q

less than 0.002 mm, low permeability, good h20 capacity, good nutrient capacity, poor aeration, poor workability, high porosity

A

clay

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11
Q

relatively equal portions of sand, silt, clay (ideal soil for farming)

A

loam

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12
Q

the degree to which soil resists pressure; important when considering how land should be managed

A

soil consistence

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13
Q

mass/volume, expresses how much soil weights per unit volume depending on amount of pore space and density of soil particles

A

bulk density

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14
Q

reduces permeability of soil to water and air, if soil is subjected to pressure, pore spaces can collapse, decreasing pore space

A

compaction

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15
Q

can help determine whether a piece of land should be planted w/ grass, trees, etc., or if it can be used for homes, lots, landfills, septic tanks, etc.

A

slope of the land

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16
Q

presence of gullies, examination of surfaces of soil

A

signs of erosion

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17
Q

character and chem. composition directly impacts soil chemistry and properties (ex: coarse grained parent material=coarse grained texture soil)

A

parent material

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18
Q

content of soil (clay, silt, sand)

A

soil texture

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19
Q

how particles are organized/clumped

A

soil structure

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20
Q

water holding capacity, very porous soil has more spaces, and can hold more water

A

porosity

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21
Q

rate of percolation, related to porosity

A

permebility

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22
Q

ability of air to move through soil

A

aeration

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23
Q

magma cools and solidifies, bulk of crust (ex: granite)

A

igneous rock

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24
Q

sediments “cement” under pressure, weathering forms sediment (ex: contains fossils)

A

sedimentary rock

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25
preexisting rock transformed-heat and pressure
metamorphic rock
26
rocks turn into soil by weathering formation and change in soil over time
soil development
27
- weather is experienced - 0-15 km up in the air - temperature drops as you go up
troposphere
28
cool air on top, warm air on bottom
normal air conditions
29
cold air is heavier, trapping pollutants
temperature inversion
30
- 25% or less cloud cover - light and variable winds (especially below 3mph) - dry soil surface - low elevation areas such as valleys and basins where cool air can sink and collect- inversions will begin sooner, last longer, and be more intense in these areas
conditions that favor temperature inversions
31
- above troposphere - 10-50 km up - increase in temperature (ozone layer!) - contains stratospheric zone
stratosphere
32
main function being to absorb UV rays produced from the sun (shield effect) purple = low 03 green= high 03
the ozone layer
33
- above stratosphere - COLDEST LAYER - 50-80 km up - temperatures fall as you go up
mesosphere
34
- 80-480 km up - as you go up, temperatures rise
thermosphere
35
Found in b/t layers; temps are constant
pauses
36
b/t troposphere and stratosphere (jet stream)
tropopause
37
More direct radiation at equator 🡪 heats up air. Heated air travels north and cools 🡪 descends (density differences). Hadley Cell Creates wind currents.
solar radiation
38
force exerted on a unit of area Movement of air from high (warm air) to low pressure areas (cold air) 🡪 wind. Winds move water and air!
air pressure
39
- coriolis effect (earth's rotation) - objects are deflected - North Hemisphere= right of the equator - South Hemisphere= left of the equator
wind and ocean current direction is affected by...
40
Trade winds relax 🡪 doesn’t move H2O West Pacific 🡪 Warm H2O accumulates in So. America 3-8 yrs. during winter
el nino
41
Decline of upwelling which brings nutrients to surface 🡪 Death/movement of orgs in ocean. - in california, migration/death of orgs due to warmer water, storms in east pacific, lots of rain (hotter water) - in south america, Massive floods, mud slides, Fisheries collapse (little upwelling) 🡪 lack of nutrients, Typhoons, Coral Bleaching (Sensitive to Heat) - in australia, EXTREME drought, dust storms, fires
effects of el nino
42
Opposite of El Niño: Cold air oscillations Usually happen after an El Niño year; water is really cold in east Pacific and needs to be reheated. Unusually cold ocean temps in Eastern Eq. Pacific
effects of la nina
43
climate is largely determined by...
insolation (latitude → angle of insolation & atmosphere)
44
Higher latitudes receive less insolation: cooler, less precipitation (especially at 30 degrees latitude) Equator receives most intense insolation: higher temp, air rises, higher precipitation
45
Mountains– disrupt wind and produce the rain shadow effect Ocean–moderate temperature and add moisture to the air
geography's role
46
Dry air descends down “leeward” side of mtn, warming as it sinks Leads to arid (dry) desert conditions
rain shadows windward--> way wind is coming from leeward--> way wind is going
47
hadley cells
low-latitude overturning circulations that have air rising at the equator and air sinking at roughly 30° latitude. They are responsible for the trade winds in the Tropics and control low-latitude weather patterns
48
Will have many nutrients Takes 100-1000 yrs to form.
fertile soil
49
Measure of spaces per volume of soil 🡪 holds more H2O/air
porosity
50
how fast H2O/air move down in soil.
permeability
51
Prod. a lot of food! Lots of fossil fuels, water, commercial inorganic fertilizers and pesticides used. Makes 1 type of food (monoculture).
high input farming/tillage (but it destroys the soil!!)
52
Reduces irrigation & pesticide use Uses organic fertilizers. Soil conservation techs. Less food
sustainable and low input agriculture
53
Low Input Farm No inorganic fertilizers or chem. pesticides used No GMOs
organi
54
slope converted into broad terraces to retain H2O and soi
terracing (soil conservation techs)
55
# c f plowing and planting in rows across slope of land (slow water and soil runoff)
contour farming
56
Plant a row of 1 type of plant, then plant a row of another type of plant.
strip cropping
57
slows wind down before it hits farm soil.
wind breaks
58
High amounts of NO3, NH4, and PO4. Easily transported, stored, and applied. Do not add humus, release NOx (greenhouse gas) when applied, eutrophication in streams.
inorganic fertilizers
59
1) Animal manure: dung/urine of animals 2) Green manure: plants plowed into soil 3) Compost: semi-broken down org. matter
organic fertilizers
60
Lower fuel emissions of greenhouse gases Less gas used Less transport of pests Less packaging Lower costs of produce Revenues remain local
perks of farmers' markets