Ecology B/C

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quizbowl
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Re: Ecology B/C

Post by quizbowl »

germinator wrote:what would we use a calculator for?
it says it is allowed but i have no idea why
Population growth, carrying capacity, biodiversity, etc.
Make sure to memorize formulas/put them on your sheet - most competitions will not provide them.
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Re: Ecology B/C

Post by germinator »

Thank you
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Re: Ecology B/C

Post by callmesandi »

Okay, so im having some trouble telling the difference between food webs, food chains, and food pyramids? Can you guys help? Thanks, oh, and it wouldnt hurt if you gave a mini lesson with examples.
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Re: Ecology B/C

Post by germinator »

well um
food chain is the simplest
http://image.wistatutor.com/content/env ... chain.jpeg
then food web is like a whole ecosystem
http://chatt.hdsb.ca/~fosterk/FOV1-0009 ... oodweb.gif
and food pyramid is like the energy distribution
and each level you advance up the pyramid you only get 10% of the total energy
http://www.edquest.ca/notesimages/foodpyramid.gif
There ya go
:D
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Re: Ecology B/C

Post by littlea53 »

Formulas? What would be the different formulas for Divison C? (Any help would be Appreciated)
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possible events:ecology, fossils, pentathlon, experimental design
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Re: Ecology B/C

Post by junexia »

What would be the most common cycles to learn? hydrologic, carbon, nitrogen, anything else?
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Re: Ecology B/C

Post by Bubba1960 »

The banana cycle. Sorry, IDK really.
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Re: Ecology B/C

Post by quizbowl »

junexia wrote:What would be the most common cycles to learn? hydrologic, carbon, nitrogen, anything else?
The main biogeochemical ones - hydrologic, carbon and nitrogen. Learn sulfur and phosphate as well. Also, if you have the time, look at potassium - I've seen it on a test before.
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Re: Ecology B/C

Post by quizbowl »

Sorry for the double post, but can someone explain how pingos are formed?
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Re: Ecology B/C

Post by Bubba1960 »

Pingos can only form in a permafrost environment. Evidence of collapsed pingos in an area suggests that there was once permafrost.

Pingos usually grow only a couple centimetres per year, with Ibyuk Pingo growing at a rate of 2 centimetres (0.79 in) a year,[4] and the largest take decades or even centuries to form. The process that creates pingos is believed to be closely related to frost heaving.

Hydrostatic (closed-system) pingos form as a result of hydrostatic pressure on water from permafrost, and commonly form in drained lakes or river channels. Permafrost rises to the drained body's former floor. Pore water is expelled in front of the rising permafrost, and the resulting pressure causes the frozen ground to rise and an ice core to form. The shape and size of a hydrostatic or closed system pingo is often similar to the body of water that it originated from. They can vary from symmetrical conical domes to asymmetric, elongate hills.

Hydraulic (open-system) pingos result from groundwater flowing from an outside source, i.e. subpermafrost or intrapermafrost aquifers. Hydrostatic pressure initializes the formation of the ice core as water is pushed up and subsequently freezes. Open-system pingos have no limitations to the amount of water available unless the aquifers freeze. They often occur at the base of slopes and are commonly known as Greenland type. The groundwater is put under artesian pressure and forces the ground up as it makes an expanding ice core. It is not the artesian pressure itself that forces the ground up, but rather the ice core that is being fed the water from the aquifer. These are often formed in a thin, discontinuous permafrost. These conditions allow an ice core to form, but also provide it with a supply of artesian ground water. These pingos are often oval or oblong shaped. It is still not entirely understood why open system or hydraulic pingos normally occur in unglaciated terrain.[citation needed]

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