W2-4 Hydrologic cycle

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Questions and Answers

How does water's role in moderating temperature and controlling climate directly influence global weather patterns?

  • By accelerating the melting of polar ice caps through heat absorption.
  • By uniformly distributing solar radiation across the planet.
  • By increasing the frequency of extreme weather events.
  • By creating a thermal buffer that reduces temperature extremes. (correct)

What aspects of Earth's geological history are most directly shaped by the erosional and depositional actions of water in its various forms?

  • The distribution of fossil fuels in sedimentary basins.
  • The composition of Earth’s early atmosphere.
  • The formation of all mountain ranges and plateaus.
  • The specific patterns of coastal erosion and delta formation. (correct)

How do the unique chemical properties of water contribute to its essential role in supporting life?

  • By creating a magnetic field around living cells.
  • By emitting a unique spectrum of electromagnetic radiation.
  • By directly synthesizing complex organic molecules.
  • By acting as a universal solvent, facilitating biochemical reactions. (correct)

Why is the ocean considered the largest reservoir in the hydrologic cycle, despite its limitations for direct human consumption?

<p>Because it contains the vast majority of Earth's total water volume, over 97%. (A)</p> Signup and view all the answers

What are the primary implications of the polar ice sheets holding the largest reservoir of freshwater on Earth?

<p>The stability of global sea levels and coastal ecosystems. (B)</p> Signup and view all the answers

What critical role does solar energy play in driving the movement of water through the hydrologic cycle?

<p>It powers evaporation and transpiration, lifting water into the atmosphere. (B)</p> Signup and view all the answers

What is the most accurate distinction between 'storm flow' and 'base flow' in the context of stream dynamics after a heavy rainfall?

<p>Storm flow is characterized by a rapid, short-lived increase in stream discharge due to surface runoff; base flow is the sustained contribution from groundwater. (A)</p> Signup and view all the answers

What is the function of a drainage basin (or watershed) within a stream system?

<p>To collect and channel precipitation and runoff into a specific stream or river. (B)</p> Signup and view all the answers

Why is the stream's 'load,' which includes total sediment and dissolved matter, significant for understanding water quality and ecosystem health?

<p>Because it directly affects the stream's ability to support aquatic life through nutrient and pollutant transport. (B)</p> Signup and view all the answers

How do streams and drainage systems play a fundamental role in both the hydrologic cycle and the rock cycle?

<p>By transporting water and sediment, facilitating erosion, deposition, and the cycling of materials. (A)</p> Signup and view all the answers

Why are streams and drainage systems considered constantly evolving in response to changing relief, climate, and vegetation?

<p>Because alteration in climatic conditions and plant cover have a notable influence on hydrological processes and landscape morphology. (B)</p> Signup and view all the answers

How does the process of infiltration contribute to both groundwater recharge and soil moisture content?

<p>By allowing surface water to percolate through the soil, replenishing underground aquifers and sustaining plant life. (D)</p> Signup and view all the answers

What is the primary distinction between ephemeral and perennial streams in terms of their flow characteristics?

<p>Ephemeral streams typically flow only after precipitation events, while perennial streams flow continuously due to consistent base flow. (B)</p> Signup and view all the answers

Consider a landscape where deforestation has significantly reduced vegetation cover. What are the likely consequences for runoff and infiltration rates during a heavy rainfall event?

<p>Increased runoff and decreased infiltration, leading to increased soil erosion. (A)</p> Signup and view all the answers

How does the concept of 'mass balance' apply to the hydrologic cycle on a global scale?

<p>The total mass of water on Earth remains constant over long periods, even though its distribution among different reservoirs may change. (A)</p> Signup and view all the answers

What adjustments occur in a stream as it progresses from its source to its mouth?

<p>Width and depth increase, gradient decreases, flow velocity and discharge increase, turbulence decreases (A)</p> Signup and view all the answers

Which scenario best describes the conditions that lead to the formation of braided stream channels?

<p>A stream overloaded with sediment that it cannot transport, combined with variable discharge and erodible banks, promotes bar formation and channel splitting. (A)</p> Signup and view all the answers

How does the distribution of water velocity differ between the inside and outside of a meander bend, and what is the primary reason for this difference?

<p>Velocity is highest along the outside meanders because the water must travel a greater distance, concentrating the flow along the outer bank. (C)</p> Signup and view all the answers

Which of the following scenarios would primarily control the size and shape of a stream channel?

<p>The balance between the erodibility of the surrounding rock, the steepness of the stream's descent, and the volume of water flowing through the channel. (A)</p> Signup and view all the answers

How do streams minimize resistance to flow, and what observable feature results from this process?

<p>By developing a sinuous, meandering shape that reduces friction against the channel bed and banks, resulting in the formation of meanders. (D)</p> Signup and view all the answers

How do streams adjust their characteristics—such as width, depth, gradient, and flow velocity—as they progress from their source to their mouth?

<p>Streams respond dynamically, with width and depth increasing, gradient decreasing, and flow velocity and discharge increasing. (D)</p> Signup and view all the answers

What is the primary process behind a stream cutting off a meander loop, and what landform typically results from this action?

<p>Progressive erosion and sediment accumulation cause the stream to bypass a channel loop, forming an oxbow lake. (A)</p> Signup and view all the answers

How do the processes of sediment erosion and deposition contribute to the migration of meanders over time?

<p>Sediment accumulates on the inner side of a meander, forming a point bar, while the opposite bank collapses, leading to meander migration. (D)</p> Signup and view all the answers

What role does stream gradient play in determining stream behavior, and how does it typically change from a stream's headwaters to its mouth?

<p>Stream gradient reflects the vertical distance of stream channel descent, generally decreasing downstream, and influencing flow velocity and channel morphology. (A)</p> Signup and view all the answers

How does the size of clasts within a stream typically change from the rocky headwaters to downstream locations, and what primary factor leads to this change?

<p>Clast size decreases downstream due to abrasion and weathering during transport, largely related to the stream's velocity. (D)</p> Signup and view all the answers

What is the primary distinction between the formation of a floodplain and an alluvial fan?

<p>A floodplain is formed by the deposition of fine sediment beyond natural levees during a flood, while an alluvial fan is a fan-shaped deposit at the base of an upland area. (A)</p> Signup and view all the answers

How does the formation of natural levees directly contribute to the development of a floodplain's characteristic features?

<p>By creating higher belts of land adjacent to the channel, leading to differential sediment deposition and varied topography within the floodplain. (C)</p> Signup and view all the answers

Considering the connection between plate tectonics and stream basins, how might a significant tectonic event most likely influence the location and characteristics of a continental divide?

<p>By causing uplift and mountain formation, which can redefine the boundaries of drainage basins and alter the course of major rivers. (A)</p> Signup and view all the answers

How do real-time monitoring systems, combined with river basin geometry data, most effectively enhance flood forecasting capabilities?

<p>By enabling accurate prediction of flood magnitude and timing through integration of current conditions and basin characteristics. (C)</p> Signup and view all the answers

How does the concept of a 'recurrence interval' aid in flood management and infrastructure planning, and what are its limitations?

<p>It offers a probabilistic estimate of the likelihood of floods of a certain magnitude, informing risk assessment and design standards, but does not guarantee future events will follow past patterns. (B)</p> Signup and view all the answers

How might significant alterations to a watershed's land use (e.g., urbanization), affect the stream's discharge and flood dynamics during a major storm event?

<p>Increasing surface runoff due to decreased infiltration, leading to a higher peak discharge and increased flood potential. (A)</p> Signup and view all the answers

What complex feedback mechanisms influence how the temporary storage of water in wetlands affects regional hydrology and ecosystem health?

<p>Wetlands mitigate flood peaks by storing water, recharge groundwater supplies, filter pollutants, and support high biodiversity. (A)</p> Signup and view all the answers

In a region experiencing increased climate variability, what strategies could be implemented to enhance the resilience of floodplain ecosystems while accommodating human development?

<p>Implementing strict zoning regulations to limit development in floodplains and restoring natural wetland areas. (A)</p> Signup and view all the answers

How do lakes, particularly those at high latitudes, influence regional climate patterns and what factors make them vulnerable to climate change?

<p>They moderate temperature extremes, contribute to regional humidity, and are susceptible to changes in ice cover and thermal stratification due to rising temperatures. (D)</p> Signup and view all the answers

How might the reduction in ice cap volume due to climate change affect the dynamics of continental divides and the distribution of freshwater resources?

<p>By diminishing the amount of freshwater stored in ice caps, thereby altering river flow patterns and potentially shifting continental divides. (D)</p> Signup and view all the answers

Which of the following statements accurately describes a significant trade-off associated with the channelization of rivers for flood control?

<p>Channelization, while protecting against flooding in the short term, can damage ecosystems, aggravate pollution, increase the chance of flooding in the long term and may cause subsidence. (B)</p> Signup and view all the answers

Why might historic hydrologic data become invalidated after significant channelization projects?

<p>Channelization fundamentally alters the stream's natural flow regime, making pre-channelization data irrelevant for predicting future hydrological behavior. (A)</p> Signup and view all the answers

Given that groundwater constitutes less than 1% of the liquid water in the hydrosphere, which statement correctly contextualizes the importance of groundwater?

<p>Despite its relatively small volume compared to the entire hydrosphere, groundwater composes a volume 35 times larger than all freshwater lakes and streams. (B)</p> Signup and view all the answers

Assuming that a geological study reveals a high concentration of chlorides, sulfates, and bicarbonates of calcium in local groundwater, what inference can be reliably drawn about the region's geology?

<p>The region's groundwater likely interacts extensively with common rock-forming minerals, from which these elements dissolve. (C)</p> Signup and view all the answers

How does the water table's behavior under hills and valleys influence groundwater availability?

<p>The water table generally mirrors the ground surface, being higher under hills and lower under valleys, affecting groundwater accessibility. (C)</p> Signup and view all the answers

Consider two adjacent geological formations: one with high porosity but low permeability, and another with lower porosity but higher permeability. How would groundwater flow likely differ between the two?

<p>Groundwater would be stored in large quantities in the highly porous formation, but flow would be faster in the highly permeable one. (D)</p> Signup and view all the answers

What factors critically govern groundwater flow rates, and how do these rates relate to the sustainability of water resources?

<p>Groundwater flow rates, which depend on water table gradients, porosity, and permeability, directly impact the replenishment of discharge areas, affecting water resource sustainability. (C)</p> Signup and view all the answers

In the context of groundwater dynamics, what is the most critical distinction between a 'recharge area' and a 'discharge area,' and how does this difference affect water management strategies?

<p>Recharge areas are sites of groundwater replenishment, typically from rainfall or snowmelt, while discharge areas are where groundwater emerges, influencing the sustainability of water resources. (D)</p> Signup and view all the answers

Under what geological conditions would an artesian aquifer most likely develop, and why is it significant for water resource management?

<p>Artesian aquifers occur in confined geological settings with high hydrostatic pressure, causing water to rise freely without pumping, vital for sustainable water access. (D)</p> Signup and view all the answers

Considering the interaction between groundwater and surface topography, how does the distribution of springs typically reflect the influence of subsurface geology and water table dynamics?

<p>Springs primarily occur where the water table intersects the ground surface, often influenced by geological features allowing groundwater to reach the surface naturally. (D)</p> Signup and view all the answers

How does the process of groundwater dissolving limestone or marble contribute to cave formation, and what conditions are necessary for this to occur?

<p>Slow-moving groundwater with the capacity to dissolve limestone or marble creates caves, primarily occurring in voids without direct surface openings. (C)</p> Signup and view all the answers

What crucial assumption underlies the designation of an area as an 'aerated zone,' and what implications does this have for groundwater recharge?

<p>The 'aerated zone' is characterized by pore spaces filled primarily with air, allowing for water infiltration and eventual groundwater recharge. (B)</p> Signup and view all the answers

How does the presence of an aquiclude above and below a confined aquifer influence the aquifer's vulnerability to pollution, and what management strategies are most appropriate in such settings?

<p>Confined aquifers may be particularly vulnerable to pollution if the aquicludes are fractured or if recharge areas are contaminated, necessitating careful monitoring and land use planning. (B)</p> Signup and view all the answers

How does the interconnection between surface water bodies (like streams and lakes) and groundwater reservoirs complicate water resource management, particularly in the context of overuse and contamination?

<p>The interconnection means overuse of either resource can deplete the other, and contamination in one can easily spread, demanding holistic and integrated strategies. (A)</p> Signup and view all the answers

What implications does the modification of river channels have on data integrity, considering the dependence of ecological studies on historical hydrological patterns?

<p>Channel modifications invalidate old data, posing challenges for historical baselines in ecological studies due to altered hydrological patterns. (B)</p> Signup and view all the answers

Considering that karst topography is most developed in moist, tropical regions underlain by limestone, which of the following scenarios would most likely inhibit the formation of extensive karst landscapes?

<p>An arid region with infrequent rainfall and primarily composed of granite. (A)</p> Signup and view all the answers

How do laws and policies related to water quality and quantity most significantly challenge effective groundwater management?

<p>They are often confusing and complicated, leading to difficulties in monitoring and enforcement. (D)</p> Signup and view all the answers

Given that crop irrigation consumes 75% of the total water demand, what far-reaching consequences might arise from a widespread shift to more water-efficient irrigation technologies across various agricultural regions?

<p>A substantial reduction in overall water demand, potentially reallocating water resources to other sectors and ecosystems. (D)</p> Signup and view all the answers

How does the practice of interbasin water transfer most profoundly affect regional political dynamics and water resource management?

<p>It often raises political issues due to the potential environmental and economic impacts on the source and recipient drainage basins. (B)</p> Signup and view all the answers

In what way does excessive groundwater withdrawal pose the most significant long-term risk to environmental sustainability and infrastructure integrity?

<p>By potentially leading to compaction and subsidence, which can damage infrastructure and alter landscapes. (A)</p> Signup and view all the answers

Considering that approximately 1.2 billion people lack access to clean drinking water, mainly in developing countries, which intervention strategy would most effectively address this global crisis in the long term?

<p>Developing sustainable, community-based water management systems that include infrastructure and education. (B)</p> Signup and view all the answers

What critical trade-off is typically encountered when employing chlorination as a method to ensure that North American water sources are free from microorganisms?

<p>The potential formation of harmful disinfection byproducts and alterations in water taste and odor. (A)</p> Signup and view all the answers

What distinctive characteristic makes surface water resources particularly 'highly susceptible to contamination' compared to other water sources?

<p>Their accessibility and direct interaction with various anthropogenic and natural pollutants. (D)</p> Signup and view all the answers

In what way does 'cultural eutrophication' most severely degrade aquatic ecosystems compared to natural eutrophication processes?

<p>It introduces a wider variety of pollutants that are difficult for ecosystems to process, leading to rapid oxygen depletion and biodiversity loss. (A)</p> Signup and view all the answers

Considering the challenges in addressing groundwater contamination, what critical advantage does 'active remediation' offer over 'passive remediation' in cleaning up contaminated sites?

<p>It speeds up the breakdown of contaminants through direct intervention, such as injecting oxygen or other chemicals. (A)</p> Signup and view all the answers

How do cave formations primarily develop?

<p>Due to the precipitation of materials from groundwater. (B)</p> Signup and view all the answers

What geological feature is characteristically described as a large dissolution cavity open to the sky?

<p>A sinkhole. (D)</p> Signup and view all the answers

What unifying characteristic defines regions with exceptionally soluble rocks where sinkholes and caves are so numerous that they create small basins, ridges, and pinnacles?

<p>Karst topography. (B)</p> Signup and view all the answers

Why is a reliable water supply critical for a society's well-being and sustainability?

<p>For human survival, environmental services, industry, and agriculture. (A)</p> Signup and view all the answers

Why is groundwater challenging to monitor effectively?

<p>Groundwater is difficult to monitor. (B)</p> Signup and view all the answers

Flashcards

Hydrologic Cycle

The continuous movement of water on, above, and below the surface of the Earth.

Water's Role in Climate

Water plays a key role in regulating temperature and influencing weather patterns globally.

Ocean Reservoir

The largest water reservoir in the hydrologic cycle, containing over 97.5% of Earth's water.

Polar Ice Sheets

The largest reservoir of fresh water and contains 74% of the Earth's fresh water.

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Groundwater

The largest reservoir of unfrozen fresh water.

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Processes of the Hydrologic Cycle

Movement of water through the cycle via evaporation, condensation, precipitation, transpiration, surface runoff, and infiltration.

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Sheet Flow

Initial phase of water movement downhill during rainfall, spreading across the surface.

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Stream Flow

Concentrated water flow into defined paths; consists of storm flow and base flow.

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Base Flow

The flow in a stream that is not from recent precipitation and is sustained by groundwater discharge.

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Storm Flow

The quick runoff of rainfall or snowmelt into streams.

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Ephemeral Streams

Streams that lack base flow, flowing only after precipitation events.

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Perennial Streams

Streams with continuous base flow, flowing year-round.

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Stream System

A natural system consisting of a channel, drainage basin, and divide.

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Stream Load

The total sediment and dissolved material transported by a stream.

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Drainage Basin

Area of land where precipitation collects and drains into a common outlet, such as a river or bay.

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Stream Channel Controls

The size and shape of a stream channel are influenced by the rock's resistance to erosion, steepness of the slope, and water volume.

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Stream Gradient

The vertical distance a stream channel descends along its course; decreases downstream.

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Factors Controlling Stream Behavior

Average channel width/depth, channel gradient, average water velocity, discharge, and sediment load.

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Stream Adjustments

Stream width and depth increase, gradient decreases, flow velocity and discharge increase, and turbulence decreases.

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Meandering Channels

Streams that assume a sinuous shape with bends due to a low gradient.

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Point Bar

Sediment accumulation on the inner side of a meander.

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Cut Bank

Collapse of the stream bank on the outside of a meander.

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Oxbow Lake

Channel loop that is bypassed then cut off from a stream, forming a lake.

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Braided Channels

Streams unable to transport sediment load, forming bars and interlacing channels.

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Clast Size Downstream

The size of clasts decreases downstream from the rocky headwaters.

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Floodplain

Deposition of fine sediment beyond natural levees during a flood.

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Alluvial Fan

A fan-shaped body of alluvium at the base of an upland area.

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Delta

Triangular-shaped deposit formed when a stream enters the standing water of a sea or lake

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Natural Levees

Created during overbank flooding, when sand and silt are deposited next to the channel

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Continental Divide

The line separating any two major rivers that flow to different oceans.

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Wetlands

Surface water reservoirs that are permanently or intermittently moist, including swamps and marshes

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Flooding

Occurs when stream discharge exceeds the channel's capacity.

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Recurrence Interval

The average time interval between two floods of equal magnitude.

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Channelization

Modifying river channels for flood control, although it has drawbacks.

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Aerated Zone

The area from the ground surface down to the water table, filled with air.

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Saturated Zone

The area below the water table where the regolith is filled with water.

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Water Table

The upper boundary of readily usable groundwater.

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Porosity

The percentage of a rock's total volume that consists of open pore spaces.

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Permeability

A measure of how easily a solid allows fluids to pass through it.

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Aquifer

Rock or regolith with sufficient porosity and permeability to store groundwater.

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Confined Aquifer

An aquifer bounded by impermeable rock layers above and below.

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Aquiclude

Impermeable rock that bounds a confined aquifer.

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Artesian Aquifer

An aquifer with high hydrostatic pressure, resulting in freely flowing water.

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Spring

A flow of groundwater emerging naturally at the ground surface.

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Cone of Depression

A cone-shaped depression in the water table due to water withdrawal exceeding recharge.

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Cave Formations (Groundwater)

Cave formations created by the process of minerals precipitating out of groundwater.

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Sinkhole

A large cavity in the ground formed by the dissolution of soluble rocks, open to the sky.

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Karst Topography

A topography formed in regions of highly soluble rock, characterized by sinkholes, caves, and underground drainage systems.

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Reliable Water Supply

The supply of water that is essential for drinking and sanitation, agriculture, industry, and environmental health.

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Crop Irrigation

The use of water for growing crops, accounting for a large portion of overall water demand.

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Industrial Water Demand

The demand for water from factories and other establishments.

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Domestic Water Use

The water demand from homes for activities such as drinking, cleaning, and sanitation.

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Interbasin Transfer

The transfer of water from one drainage basin to another to address water shortages.

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Groundwater Withdrawal (Excessive)

When excessive removal of groundwater leads to a drop in the water table, resulting in environmental problems.

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Surface Water Contamination

When surface water becomes harmful due to the addition of pollutants.

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Eutrophication

The enrichment of a body of water with nutrients leading to increased plant growth and oxygen depletion.

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Passive Remediation

The process of removing pollutants from contaminated groundwater using natural means.

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Groundwater Contamination

Groundwater that has been made impure by harmful substances.

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Active Remediation

The process of removing pollutants from contaminated groundwater by injecting agents to speed breakdown

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Study Notes

  • The size and shape of a stream channel are controlled by rock erodibility, steepness of descent, and water volume
  • A stream channel's gradient is the vertical distance it descends along its course, decreasing downstream, although not smoothly
  • Stream behavior is controlled by average channel width and depth, channel gradient, average water velocity, discharge, and sediment load
  • Streams experience a continuous interplay among these factors
  • Orderly adjustments occur when following a stream from its source to its mouth include
    • Width and depth increase
    • Gradient decreases
    • Flow velocity and discharge increase
    • Turbulence decreases
  • Straight channels are rare; low gradient streams typically assume a sinuous shape, with each bend forming a meander
  • The shape of a stream minimizes resistance to flow
  • Velocity is lowest along inside meanders and highest along outside meanders
  • Sediment accumulates on the inner side of a meander, forming a point bar
  • Collapse of the stream bank occurs on the outside of a meander, forming a cut bank
  • Meanders tend to migrate, and streams may bypass a channel loop, cutting it off to form an oxbow lake
  • A stream unable to transport its entire sediment load deposits the coarsest and densest sediment, forming a bar that divides and concentrates the flow
  • Braided streams have many interlacing channels and bars, variable discharge, and easily erodible banks
  • The size of clasts a stream can transport is mainly related to velocity
  • Clast size decreases downstream from the rocky headwaters
  • A stream's load consists of bed load, suspended load, and dissolved load

Bed Load

  • Bed load constitutes 5-50% of the total sediment load
  • Bed load moves by rolling, sliding, or saltation

Suspended Load

  • Particles of silt and clay in suspended load provide the muddy character of many streams

Dissolved Load

  • Dissolved load comprises primarily seven ions: bicarbonate, calcium, sulfate, chloride, sodium, magnesium, and potassium
  • Streams form three major depositional landforms
    • Floodplain: deposition of fine sediment beyond natural levees during a flood
    • Alluvial fan: a fan-shaped body of alluvium at the base of an upland area
    • Delta: triangular shaped deposit formed when a stream enters the standing water of a sea or lake
  • Continents are divided into large regions from which major rivers flow to one of the world’s major oceans
    • The line separating any two of these is called a continental divide
  • Continental divides often coincide with crests of mountains
    • There is a close relationship between plate tectonics and the locations of stream basins
  • Water can remain stored in any of several surface water reservoirs
    • Ice caps are the greatest of these
    • Lakes are mainly found in high latitudes, form by glaciation, volcanism, tectonism, streamflow, natural dams, cave collapse, ice dam collapse, permafrost thaw, and coastal processes
    • Wetlands are permanently or intermittently moist, including swamps, marshes and bogs and are highly biologically productive
  • Flooding occurs when a stream’s discharge becomes so great that it exceeds the capacity of the channel
    • Major floods occur infrequently, but can be devastating or catastrophic
    • During a flood, the peak discharge comes well after the rains that produced it
      • After rainfall, surface runoff moves into stream channels, quickly increasing discharge
  • Prediction of floods has become essential
  • The frequency of past floods can be plotted, calculating the average time interval between two floods of equal magnitude
    • This is called the recurrence interval
  • Real-time monitoring during storms in combination with information about the river basin’s geometry helps with forecasting

Flood Prevention and Channelization

  • River channels are often modified for flood control, it is called channelization
  • Channelization has benefits but also drawbacks, including interference with ecosystems and potential pollution aggravation
  • Channelization does not guarantee flood protection, and may even worsen the risk and can lead to subsidence and invalidate historic hydrologic data

Water Under the Ground

  • Less than 1% of the liquid water resides beneath the ground, forming groundwater
  • The volume of groundwater is 35 times larger than all freshwater lakes and streams combined and nearly a third of all glaciers and sea ice
  • Over 50% of groundwater is within 750 m depth of the surface
  • Groundwater contains dissolved elements like chlorides, sulfates, and bicarbonates of calcium, magnesium, sodium, and potassium
  • These elements dissolve from common rock-forming minerals
  • Groundwater composition varies depending on the surrounding rocks
  • From the ground surface down to the water table, the regolith has two zones
    • Aerated zone is filled with air
    • Saturated zone is filled with water
  • The upper surface is water table
  • The water table is the upper limit of readily usable groundwater, following the ground surface shape and higher under hills, lower under valleys
  • Groundwater flows through pore spaces via percolation
  • Flow depends on the porosity and permeability of the rock
    • Porosity is the percentage of the total rock volume consisting of open pore spaces
    • Permeability is how easily fluids pass through a solid
  • Groundwater flows from high to low water table areas due to gravity
  • Replenishment arises when rainfall/snowmelt enters the ground in recharge areas
  • Water travels through the system to discharge areas, where it surfaces in streams, lakes, ponds, or wetlands
  • An aquifer is a rock or regolith body with sufficient porosity and permeability to store and conduct groundwater in significant volumes
    • An aquifer with a water table is unconfined
    • If the rate of groundwater withdrawal exceeds the local groundwater flow rate, a cone of depression may form
    • A confined aquifer is bordered above and below by impermeable rock called aquiclude
    • An artesian aquifer has high hydrostatic pressure and is freely flowing
  • A spring is a flow of groundwater emerging naturally at the surface
  • Slowly moving groundwater can dissolve materials, particularly limestone and marble
  • A cave forms when circulating groundwater dissolves an underground void with no surface opening
  • Water flow enlarges the underground passage along the most favorable path
  • Spectacular cave formations are deposited by precipitation of materials from the groundwater
  • A sinkhole, in contrast to a cave, is a large dissolution cavity open to the sky
  • In regions of exceptionally soluble rock, sinkholes and caves are so numerous that they combine to form a distinct topography of small basins, ridges, and pinnacles called karst
  • Karst is best developed in moist, tropical regions underlain by limestone

Water and Society

  • A reliable water supply is critical for
    • Human survival and health
    • Industry and agriculture
    • Environmental services
  • Water is under threat almost everywhere in the world in terms of quality and quantity
  • Laws and policies are confusing and complicated, and groundwater is difficult to monitor
  • Crop irrigation demands 75% of water
  • Industry demands 20%
  • Domestic use demands 5%
  • Proportions can vary greatly from one region to another
  • Population growth is partly responsible for increasing demand, as are improvements in living standards
  • 29 countries worldwide suffer from water shortages, affecting 450 million people
  • Interbasin transfer of water from one drainage basin to another to meet high water demands raises political issues and can have environmental impacts
  • Excessive groundwater withdrawal can lead to lowering of the water table, drying of springs, compaction and subsidence
  • About 1.2 billion people, mainly in developing countries, do not have access to clean drinking water
  • In North America, water is drawn from relatively clean sources but is still monitored and treated with chlorination to kill microorganisms
  • Surface water's accessibility makes it a useful resource, but also highly susceptible to contamination
  • Contaminants come from
    • Urban, suburban, and agricultural runoff
    • Industrial and landfill effluents
    • Mining, logging, and petroleum discharge
    • Airborne contaminants
    • Thermal pollution
  • A common form of surface water contamination results from excess plant nutrients from fertilizers and detergents
  • This contamination triggers algae growth, and aquatic weeds get out of control, creating an algal bloom
  • The breakdown of algae and weeds causes oxygen depletion, killing other organisms in the water; this is called eutrophication
  • Cultural eutrophication is eutrophication accelerated by the addition of anthropogenic pollutants
  • Groundwater contamination is caused by many of the same pollutants that affect surface water
  • Groundwater contamination is much more difficult to detect, control, and clean up
    • Passive remediation involves relying on natural environmental processes to clean up the site
    • Active remediation involves intervention by injecting oxygen or other chemicals to speed the breakdown of contaminants

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