M2-3 Flashcards

1
Q

what are the different forms of phos

A

TP
dissolved
particulate
organic (can particulate or dissolved)
inorganic (can be particulate or dissolved)

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2
Q

dominant forms of phos in a lake

A

PO4 3- or FePO4
(freeform)
most P is tied up in org tissues

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3
Q

internal vs external loading of phos into a lake

A

external loading: often sourced from the weathering of rocks, atmos deposits , streams or rivers into a lake
PO4 or org P detritus

internal loading: from lake sediment at the bottom of a lake and in decaying OM. the conditions at the sed-water interface are critical

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4
Q

role of O2 and iron in the phos cycle

A

P is relsease 1000 faster in ANOXIC conditions. in oxic conditions, PO4 is bound to iron.

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5
Q

what is excessove phos linked to

A

cyanobacteria blooms and eutrophication

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6
Q

what % of TP is Solubale reactive phos

A

0.2. note that is is the ofrm of P that plant need to growth

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7
Q

is particulate organic phos or particulate inorganic phos more abundant (give %) and explain why

A

POP (98.5%) as most of it is retained in living organisms

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8
Q

algal mechanisms for phos uptake

A

1) luxury consumption- store P in tissues when very abundant
2) ability to use P at low conc lvl- alter energy budget
3) phosphatase production - some orgs will have enzymes that break the bond between P and org moles in the water, triggered by low P

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9
Q

where are the major zones for P cycling in lakes

A

Sed-water interface
open water in the pelagic zone (uptake and sedimentation)
littoral zone (uptake and plant decomp)

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10
Q

vertical P dist in oligo lakes

A

Low soluble and total phos. O2 follows ortho pattern

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11
Q

vertical P dist in eutroph lakes

A

Low soluble P and total P in epi and meta. Sig increase in the hypo fpr both.
O2 follows clino

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12
Q

human impacts on P cycle and eutroph

A

Cultural eutroph
agricultural input- excess run off of alot of fertilizers (has P)
speeds up the rate- from 1000’s of years to just a few decades

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13
Q

natural eutroph

A

often due to the age of a lake
nautral accumulation of P in a system- often takes 1000s of years

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14
Q

N and productivity

A

N has the ability to limit plant growth- trophic status depends partially on the N content

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15
Q

range of P and N to define lake prod

A

TP:

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16
Q

diff forms of N

A

N2
TN
Dissolved and inorg (NH4+, NO3-, No2-)
in organic compounds

17
Q

N fixation

A

assimilation of N2 in NH4 via nitrogenase enzyme or lightning

occurs in anoxic environ only
may use heterocycts

18
Q

denitrification

A

conversion of inorg N (NO3) into N2

less energy mase when comped to the conversion of Org Carbon to CO2

occur in anoxic

possible solution to dec N in water

19
Q

heterocysts and their function.

A

a strucutire to protect the nitrogenase enzyme from oxygen)

20
Q

nitrification

A

NH4 to NO2 to NO3 and energy

NH4 in water w/ DO, it will have more energy than NO species

done by bActeria, fungi or other autotroph

21
Q

nitrosomonas

A

conver NH4 to NO2

22
Q

nitrobacter

A

convert NO2 to NO3

23
Q

what form of N is easiest to take up

A

NH4 is easiest to tke up from water colomn. from here plant and orgs have metabolic oircesses to convert into useful forms

24
Q

nitrate reductase

A

Nirtate to nitrite. this can be limiting

this is an oxic process

25
Q

nitrites reductase

A

nitrite to Ammonium (NH4) for AA prod
this is an oxic process

26
Q

ammonification

A

org compunds are broken down by bacteria/ fungi and converted to ammonium

occurs in sediments and upper waters

oxic process

27
Q

vert dist of N (eutroph)

A

NO3 start high and dec w/ depth (to 0)
NH4 starts low and inc w/ depth (to mid)
O2 content is a large factor

28
Q

vert dist of N (oligo)

A

NH4 is low all the way down
NO3 is mid low w/ sligh inc w/ depth
O2 content is a large factor