11 Flashcards

1
Q

how does the inorganic carbon, calcium, and carbonate dissolution affect us

A

buffering changes in ocean acidity
climate (ocean as a sink or source for CO2)
solubility of CaCO3 (geology, sediments, biology, calcareous organisms)
is affected by human CO2 emissions (ocean acidification)

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2
Q

what are the species of inorganic carbon found dissolved in the ocean

A

CO2
H2CO3
HCO3-
CO32-

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3
Q

when CO2 dissolves

A

it reacts with water to form carbonicacid H2CO3

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4
Q

what changes pk1 and pk2 for formation of CO32-

A

decrease with T and weaker with S

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5
Q

what is the use of bicarbonate HCO3-

A

acts as a buffer in the ocean

weak acid and base as it is part of two reactions

micture of acid HCO3- and its congugate base CO32- that resist change in pH when acid or base is added

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6
Q

what is the pH of the ocean

A

7.4- 8.2

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7
Q

distribution of carbonic acid forms

A

bc it is a weka acid, its distribution depends on pH and we can use this pH and the two Kas to estimate the distribution at diff pH values

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8
Q

what is the distribution of the bicarbonate forms in the ocean pH

A

dominated by bicarbonate HCO3- (87%) and
second is carbonate CO32- 10%

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9
Q

what species control air sea fluxes

A

CO2 at less than 0.5%

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10
Q

inventory of DOC and POC

A

2%

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11
Q

PIC invintory

A

0.01%

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12
Q

how can we describe the carbon system

A

for a given T,S, P, we can describe it using any of the two systems

DIC
TA
pH
pCO2

we typically measure the first two to get the other two

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13
Q

DIC=

A

[CO2]+[H2CO3]+[HCO3-]+[CO32-]

the first two terms typically equal less than 1%

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14
Q

how is DIC measured

A

acidifying seawater to convert all carbonate and bicarbonate to cO2

bubbling inert gas through solution

measuring gas phase CO2

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15
Q

what is TA

A

total alkalinity

total amount of charges available to buffer strong acids

units- eq/kg

stads for equivalent of a mole of charges

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16
Q

what is TA=

A

[HCO3-]+2[CO32-] account for most of the cabonate alkalinity

+ means species that could remove H+
- are species that could add H+

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17
Q

would a change in pressure or temp change DIC or TA

A

no bc we dont add or remove C or charges

18
Q

would uptake of 100umol/kg of 100 umol/ kg of CO2 from the atmosphere affect DIC or TA

A

dic would inc by 100 and TA wouldnt change

we added C but no charge

19
Q

what effect would formation of 25 umol/kg of CaCO3 have on DIC and TA

A

DIC decreases by 25 and TA decreases by 50 becasue removed CO32- but 2 charges

dissolution of CaCO3 would have the opposite effect

20
Q

what effect would formation of POC have on DIC and TA

A

both change exactly the same depneding on the POM ration if we assume the classic redfield ratio of C:N:P

if one species C then -106 = DIC bc youre forming

TA = 16+1= 17

21
Q

what effect would aerobic respiration/ decomposition of POM have on DIC and TA

A

the opposite effect of formation of POC

DIC would increase and TA would decrease

22
Q

what is the purpose of parallel lines on the DIC/TA graph

A

allows us to find the past CO2 and pH

23
Q

what happens graphically when you form Corg in the DIC/TA graph

A

decrease DIC and slightly increase alkalinity

24
Q

what happens graphically when you have CaCO3 dissolution or formation in the DIC/TA graph

A

dissolution- increases DIC and TA

formation- decrease DIC and TA

25
Q

why is the formation and burial of CaCO3 not a net sink for atm CO2

A

formation of CaCO3 reduces alkalinity more than DIC-

leads to lower pH

shifts larger portion of DIC in surrounding water to CO2

leads to higher pCO2 in water

less room in water for CO2 from air

26
Q

what are the polymorphs of calcium carbonate

A

aragonite

calcite

same chemical composition but diff crystal structures

aragonite is stronger physicially but more chemically vulnerable

27
Q

what causes the formation of one form over the other of the different polymorphs of calcium carbonate

A

depends on the Mg levels in the ocean

high Mg- aragonite seas

28
Q

what happens when Mg subs for Ca

A

high Mg calcite which is less stable and very soluble

29
Q

what kind of reaction is the incorporation of Mg as an impurity in calcite

A

endothermic process

more likely in warmer waters

30
Q

what is the use of formatino of Mg calcite being endothermic

A

using the Mg/Ca ratio in shells of microfossils as a paleothermometer

31
Q

how does CaCO3 enter the oceans

A

through riverine inputs

or

percipitated biogenically - 4x larger
most CaCO3 dissolves following organism death while 25% sinks to sea floor and is buried escaping dissolution

32
Q

abiotic percipitation of CaCO3

A

not a srouce

kinetically unfacourable even in oversaturated solutions

33
Q

where is CaCO3 in the ocean floor found

A

equally distributed in coastal and open ocean regions

34
Q

what is the inorganic carbon pump/ carbonate pump

A

sinking of calcareous hard parts to the deep sea and sediments

35
Q

sinking of CaCO3 versus riverine

A

the sinking by sediment burial is almost equal to the riverine source

leaving the ocean in a steady state with respect to CaCO3

36
Q

what are the most important planktonic calcifers

A

foraminifera

1/2 of PIC exported to sediments from them- they are protozoa

37
Q

layout of foraminifera

A

some benthic- deep ocean, others pelagic

contain skeleton made from calcite

large variation in size, shape, and density

38
Q

what is the second most important organisms for sedimentary PIC

A

coccolithophora- calcite nanofossils

39
Q

coccolithophora as a source of CaCO3

A

deposit CaCO3/ calcite in overlapping plates caleld coccoliths that form their external shell

create and shed the plates continually every hour

40
Q

where are coccolithophora found

A

geographically widespread and form blooms

can be detected by satelite

41
Q

what is another important calicifer

A

pteropods

contain pen shaped internal structure amde of aragonite

42
Q
A