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GEO 101

Chapters 21-24

QuestionAnswer
5 factors that lead to soil development parent material, climate, relief, organisms and time
dark brown to black soil color indicates humus (ex. black prairie soils)
red or yellow soil color indicates iron (ex. moist tropical soils)
white flecks or spots in soil indicates calcium
soil texture particle size based on the amounts of silt, sand and clay
soil colloids particles of clay and organic matter
charge of soil colloids negative (they attract positively charged ions which plants need)
how soil colloids retain nutrients? the properties are held by the iron until plants take them up
loam soil that is made up of sand, silt, and a smaller amount of clay
distinct traits of soil horizons color, texture, structure, consistence, and porosity
orientation of soil horizons typically parallel to the ground
what layer of soils are studied? all of them, from surface to bedrock
O organic
A humus/topsoil
the soil horizons O, A, E, B, C, and R
E minerals/eluviated horizon
B colloids/subsoil
C deposits or weathered material/parent material
R unweathered bedrock
vertisols contain a lot of montmorillonite clay. shrinks when it dries and swells when water is added, churning the soil and blurring the lines between the horizons
atmospheric carbon dioxide 410-420 parts per million (ppm)
ways energy flows through an ecosystem the food web, photosynthesis and respiration, net primary production and climate, biomass as an energy source, and the carbon cycle
primary producers plants, use sunlight, water and carbon dioxide to create carbohydrates
consumers all other organisms
primary consumers herbivores
decomposers consume detritus
biomass the accumulated net production from photosynthesis, typical units are average grams/square meter per year
net primary production annual yield of useful energy produced by an ecosystem
lands with most net primary production rainforest of the equatorial zone and freshwater swamps and marshes
lands with least net primary production extreme desert and lakes and streams
oceans with most net primary production algal beds and reefs and estuaries (tidal)
oceans with least net primary production open ocean and continental shelf
human activities that impact the carbon cycle burning fossil fuels, changing land use and using limestone to make concrete
ocean acidification the lowering of the ocean's pH as the ocean absorbs the carbon dioxide released from burning fossil fuels. this harms marine organisms
photosynthesis water + carbon dioxide + light energy = glucose + oxygen
respiration glucose + oxygen = carbon dioxide + water + chemical energy
gross photosynthesis total amount of carbohydrate produced
net photosynthesis amount of carbohydrate remaining after respiration (net photosynthesis = gross photosynthesis - respiration)
light controls seasonal activity through photoperiod or daylight length
wind distorts tree growth
changes in day length impacts a variety of animals
changes in season impacts deciduous vegetation in mid-latitudes (ex. trees that lose their leaves in the fall)
bioclimatic frontier an aera where there is a critical level of climatic stress, exceeding the level to which a species can survive with (ex. distribution of ponderosa pine controlled by rainfall)
geomorphic factor that impacts ecosystems topography
slope steepness the angle that the ground surface makes with respect to the horizontal plane
slope aspect the orientation of a sloping ground with respect to geographic north
relief the difference in elevation divides and valley bottoms
edaphic factors soil conditions such as: texture, structure, humus content, soil horizon development, alkalinity and acidity, salinity, and soil animals
interspecific competition negative interaction between different species
intraspecific competition competition between individuals of the same species
predation one species feeds upon another
parasitism one species gains nutrition from another without the immediate death of the host
herbivory grazing of plants
allelopathy chemical toxins produced by a plant that inhibit the growth of another (ex. knotweed)
climax community the final stable/near equilibrium community in an ecological succession
ecological succession the periodic changes in species composition, structure, and architecture of a given area
pioneer species the species that invade a bare area. these are well adapted to dry soil conditions and are able to withstand temperature extremes
biographic regions same or closely related plants and animals that are typically found together
biodiversity the number of specific in a given area; the variety of life on earth. this is rapidly decreasing
biomes the largest recognizable subdivision of terrestrial ecosystems
types of biomes forest, savanna, grassland, desert, and tundra
what is the greatest storage pool for carbon in the earth system? soil
what is the largest carbon flux in the earth system atmosphere to vegetation
which storage pool is the smallest but has the greatest flux? plants and soils
what causes large fluctuations in animal species populations in boreal forests? low diversity and a highly variable environment
what is an important edaphic factor in differentiating habitat? humus content
what is it called when precipitation exceeds water use in the soil water budget a water surplus
leaching seeping water dissolves soil materials and moves them to deeper soil levels or to the groundwater
what is the ecosystem in which net primary production is the highest? fresh water swamps and marshes
soil composition 25% air, 45% inorganic, 25% water and 5% organic
particle sizes sand, silt and clay
acidic soils can lead to nutrient leaching as acids replace the nutrient bases
four types of soil structure blocky (compact and flat), platy (thin and parallel), prismatic (large and vertical) and granular (small)
soil consistence a combination of soil structure and soil texture
porosity the flow of water through the soil
translocation the movement of dissolved material or small particles by water
eluviation material is removed from a horizon
illuviation material is moved into a horizon
3 soil groups soils with no or poorly developed horizons, soils with large portions of organic matter, and soils with well developed horizons
11 soil orders aridisols, millisols, alfisols, spodosols, ultisols, oxisols, vertisols, histosols, entisols, inceptisols, and andisols
ecological biogeography environmental impact on spatial distributions
historical biogeography how spatial distributions change over time
energy loss in the food web between each level, only 10% of energy is moved with the rest being lost in respiration
pools points where elements remain, can be either short-term or long-term
biogeochemical cycles nitrogen cycle, oxygen cycle, sedimentary cycle and hydrological cycle
global carbon flux carbon exchanged between the atmosphere, oceans, biosphere and lithosphere
flux units gigatons of carbon per year
human activities and carbon dioxide far more carbon dioxide is present than that which can be handled by the carbon cycle
symbiosis positive interactions between species
commensalism one species benefitted and one was unaffected
protocooperation both species benefitted
mutualism one or both species cannot survive alone
primary succession all previous vegetation is removed
secondary succession some remnants of the prior ecosystem remain
old field succession on abandoned farmland
4 key aspects of natural selection variation, inheritance, selection and time
speciation process by which species are differentiated and maintained
allopatric speciation when species undergo genetic drift to adapt to different conditions
major types of forest low latitude, monsoon, subtropical evergreen, midlatitude deciduous, needleleaf, sclerophyll and boreal
vegetation transects the succession of plant formation classes across climatic gradients
Created by: user-1743153
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