Chapter 2 – The Input of Material to the Ocean Reservoir Flashcards

(76 cards)

1
Q

What are the three major natural sources of material injected into seawater?

A

The continental crust, the oceanic crust, and the atmosphere

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2
Q

What processes mobilize primary material from the continental crust?

A

Low-temperature weathering and high-temperature volcanic activity

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3
Q

What is secondary (pollutant) material mobilized by?

A

Anthropogenic ‘weathering’ processes, often involving high temperatures

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4
Q

What forms does released material take during natural and anthropogenic processes?

A

Particulate, dissolved, and gaseous phases

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5
Q

What are the three principal transport routes for continentally mobilized material to the ocean?

A

River, atmospheric, and glacial transport

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6
Q

Which pathway delivers material most widely across the ocean surface?

A

Atmospheric transport

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7
Q

Which transport pathway is second only to rivers in supplying particulate material to the oceans?

A

Glacial transport

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8
Q

Why is ice transport less important as a source of dissolved material?

A

Because ice has reduced chemical weathering (being frozen)

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9
Q

What are the main oceanic crust processes supplying material to the oceans?

A

Low-temperature weathering and hydrothermal activity at spreading ridges

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10
Q

What is a key hydrothermal contribution to the ocean’s geochemistry?

A

Dominant supply of dissolved manganese

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11
Q

What are the three key questions to evaluate riverine input to the ocean?

A

(1) What is transported by rivers? (2) What happens in estuarine mixing zones? (3) What reaches the open ocean?

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12
Q

What is the dominant chemical signal in river water compared to seawater?

A

River water is dominated by calcium and bicarbonate; seawater by sodium and chloride

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13
Q

What are the main sources of dissolved and particulate materials in rivers?

A

Rock weathering, organic decomposition, atmospheric deposition, and anthropogenic discharges

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14
Q

How is dissolved material in river water operationally defined?

A

Material passing through a 0.2–1 μm filter (includes colloids)

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15
Q

What are colloids and why are they important?

A

Very small particles (<0.2 µm and >1 nm) with high surface area that significantly interact with dissolved species

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16
Q

What are the three end-member types of surface waters in the Gibbs diagram?

A

Precipitation-dominated, rock-dominated, evaporation–crystallization dominated

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17
Q

What cations and anions characterize freshwater and seawater respectively?

A

Ca²⁺ and HCO₃⁻ for freshwater; Na⁺ and Cl⁻ for seawater

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18
Q

What does a high Na/(Na+Ca) and Cl/(Cl+HCO₃) ratio in river water indicate?

A

Precipitation dominance and possible evaporation effects

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19
Q

What types of rocks result in higher weathering products in rivers?

A

Sedimentary rocks (especially carbonates) over crystalline rocks

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20
Q

What environmental factors control river water composition?

A

Lithology, relief, climate, vegetation cover, and pollution

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21
Q

What is the order of weathering intensity among rocks?

A

Evaporites&raquo_space; carbonate rocks&raquo_space; crystalline rocks

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22
Q

What is the primary control on the major ion chemistry of rivers?

A

Rock weathering

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23
Q

How do mean annual runoff and dissolved solids correlate?

A

Higher runoff leads to lower concentration but higher flux of dissolved solids

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24
Q

What are trace elements in river water defined as?

A

Elements with concentrations <1 mg/L (often much lower)

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25
What affects trace metal solubility in river water?
pH, complexation with organic matter, and adsorption to particles
26
Which trace elements are highly mobile (ARD/AUC ratio ≥ 1)?
Chloride, calcium, and molybdenum
27
Which trace elements are poorly mobile in river systems?
Aluminium, lead, and iron
28
What human activities affect trace metal concentrations in rivers?
Mining, agriculture, industry, urban discharges, and atmospheric deposition
29
What are the two main types of atmospheric inputs to the ocean?
Wet deposition (rainfall) and dry deposition (aerosol particles)
30
What is the principal mechanism of atmospheric transport?
Long-range transport via the wind system
31
What type of material is most efficiently transported by the atmosphere?
Fine particles and gases
32
What are the primary sources of atmospheric aerosols?
Sea spray, continental dust, volcanic emissions, biomass burning, fossil fuel combustion
33
How does particle size affect atmospheric transport?
Smaller particles travel farther; large particles settle quickly
34
What is a key natural source of mineral dust?
Arid and semi-arid continental regions
35
What factors influence the chemical composition of dust?
Source region lithology and atmospheric processing during transport
36
What is sea-salt aerosol primarily composed of?
Sodium chloride, with smaller amounts of other seawater-derived ions
37
What processes generate sea-salt aerosol?
Bubble bursting and wave action at the ocean surface
38
What is the significance of non-sea-salt sulfate in marine aerosols?
It indicates sources like volcanic activity or oxidation of marine biogenic gases (e.g., DMS)
39
What is the dominant anthropogenic aerosol component over oceans?
Sulfate derived from fossil fuel combustion
40
What distinguishes marine from continental aerosols?
Marine aerosols are typically coarse and salt-rich; continental aerosols are more variable and often fine-grained
41
What role does rainfall play in atmospheric deposition?
It scavenges both soluble gases and particulate matter from the atmosphere
42
How does pH affect rainfall chemistry?
Low pH (acidic rain) enhances dissolution and transport of trace metals
43
What is the significance of dust inputs for ocean biogeochemistry?
Dust supplies key nutrients (e.g., Fe, P) to surface ocean waters
44
Why is iron input from dust important in some ocean regions?
Because it limits primary production in high-nutrient, low-chlorophyll (HNLC) areas
45
What happens to dust once it reaches the ocean surface?
It can dissolve, sink, or be transformed through biological and chemical processes
46
What is “wet deposition”?
Delivery of material to the ocean via precipitation
47
What is “dry deposition”?
Gravitational settling or impaction of aerosols onto the ocean surface
48
What is the main geological setting for hydrothermal activity?
Mid-ocean ridges and spreading centers
49
What drives hydrothermal circulation at ridge crests?
Heat from underlying magma chambers
50
What happens when seawater penetrates the ocean crust?
It heats up, reacts with basalt, and is returned to the ocean enriched in elements
51
What are the two main types of hydrothermal fluid outputs?
High-temperature vent fluids and low-temperature diffuse flows
52
What is a "black smoker"?
A high-temperature hydrothermal vent emitting metal-rich fluids that precipitate on mixing with seawater
53
What is a key chemical feature of hydrothermal fluids?
Enrichment in metals like Fe, Mn, Zn, Cu, and depletion in Mg and SO₄²⁻
54
Why is Mg absent in hydrothermal fluids?
Because it is removed during water–rock reactions within the crust
55
What mineral forms when hydrothermal Fe oxidizes in seawater?
Iron oxyhydroxides (e.g., Fe(OH)₃)
56
What is the significance of Mn in hydrothermal plumes?
It remains in solution longer, serving as a tracer for vent activity
57
How do hydrothermal inputs affect deep ocean chemistry?
They influence metal budgets and local geochemical cycling
58
What are the primary controls on hydrothermal input composition?
Temperature, rock type, and water–rock reaction extent
59
How does hydrothermal activity act as both source and sink?
It adds some elements (e.g., Mn) and removes others (e.g., Mg, O₂, SO₄²⁻)
60
What is the global significance of hydrothermal vents?
They contribute significantly to the oceanic budget of some trace elements
61
What is the estimated global flux of hydrothermal water?
Around 10¹⁴ kg/year (10⁵ m³/s)
62
What role do microbial communities play at vent sites?
They utilize chemical energy from hydrothermal fluids (chemosynthesis)
63
Why is hydrothermal iron important for surface productivity?
It can be transported via plume dispersion to distant surface waters, aiding primary production
64
What causes rapid precipitation of metals from vent fluids?
Mixing with cold, oxygenated seawater
65
What is the main goal of comparing fluxes in marine geochemistry?
To assess the relative importance of different material sources to the ocean
66
What are the four main pathways supplying material to the ocean?
Fluvial, atmospheric, glacial, and hydrothermal pathways
67
Which pathway delivers the largest flux of dissolved material to the ocean?
Fluvial input
68
Which pathway delivers the largest flux of particulate material?
Atmospheric dust deposition over wide ocean areas
69
How do glacial inputs compare to other pathways?
Significant for particulate input in polar regions but limited globally
70
Why is hydrothermal input often underestimated?
It is difficult to measure and distributed along deep-sea ridges
71
What element is dominantly supplied by hydrothermal activity?
Manganese (Mn)
72
What complicates the calculation of fluxes to the ocean?
Temporal and spatial variability, and limited data for some regions
73
What are the units commonly used to express fluxes?
Grams or moles per year (g/yr or mol/yr)
74
What is a key consideration when comparing dissolved and particulate fluxes?
Many elements cycle between these phases during transport
75
How can atmospheric inputs affect remote ocean regions?
By supplying essential micronutrients like iron (Fe) via dust transport
76
What role do shelf seas play in the global material cycle?
They act as reactive zones processing and transforming inputs from rivers and atmosphere