Groundwater: Forms of Saturated Formation
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Questions and Answers

What is a hydrograph?

A plot of discharge in a stream plotted against time chronologically.

What does an ephemeral stream not have?

  • Groundwater flow
  • Variation in discharge
  • Base flow contribution (correct)
  • Well-defined channel
  • A flood hydrograph represents stream flow due to a storm over a catchment.

    True

    What is the space in which all the pores of soil are filled with water called?

    <p>Saturated zone</p> Signup and view all the answers

    What is the term for the total quantity of surface water that can be expected from a stream at the outlet of its catchment?

    <p>yield</p> Signup and view all the answers

    Match the following stream characteristics with their descriptions:

    <p>Perennial Stream = Always carries some flow throughout the year Intermittent Stream = Limited contribution from groundwater, may dry up during dry season Ephemeral Stream = Does not have any base flow contribution and a well-defined channel</p> Signup and view all the answers

    What are the two categories of runoff based on time delay between precipitation and runoff?

    <p>Storm runoff and base flow</p> Signup and view all the answers

    Surface runoff refers to the flow of water over the land surface only during heavy rainfall.

    <p>False</p> Signup and view all the answers

    The ___ zone is located between the land surface and the water table.

    <p>aeration</p> Signup and view all the answers

    Match the aquifer classification with its description:

    <p>Unconfined aquifer = Free water surface, important for groundwater studies Confined aquifer = Contained between impervious beds, may be leaky if confining beds are not intact Perched water table = Water table retained around impervious material</p> Signup and view all the answers

    Study Notes

    Here are the study notes:

    Groundwater and Saturated Formations

    • Subsurface water is categorized into four forms:
      • AQUIFER: a saturated formation that stores and yields water in sufficient quantity
      • AQUITARD: a partially permeable formation that allows seepage but yields little water
      • AQUICLUDE: an impermeable formation that prevents water flow
      • AQUIFUGE: a formation with low permeability that neither stores nor transmits water

    Subsurface Zones

    • SATURATED ZONE (Groundwater Zone): all pores in the soil are filled with water
    • AERATION ZONE: soil pores are partially saturated with water
    • Three subzones in the Aeration Zone:
      • SOIL WATER ZONE: close to the ground surface, water is lost to the atmosphere through evapotranspiration
      • CAPILLARY FRINGE: water is held by capillary action
      • INTERMEDIATE ZONE: between the Soil Water Zone and Capillary Fringe

    Aquifer Properties

    • IMPORTANT PROPERTIES:
      • Capacity to release water
      • Ability to transmit water flow easily
      • POROSITY
      • SPECIFIC YIELD
      • DARCY'S LAW
      • COEFFICIENT OF PERMEABILITY
      • STRATIFICATION

    Hydrogeologist's Job

    • Identify geologic formations suitable for groundwater development
    • Determine the importance of geologic formations for possible use as an aquifer

    Wells and Drawdown

    • WELLS: forms the most important mode of groundwater extraction from an aquifer
    • CONE OF DEPRESSION: conical shape of the water table due to radial flow into the well
    • DRAWDOWN: drop in water table elevation due to pumping
    • AREA OF INFLUENCE: area extent of the cone of depression
    • RADIUS OF INFLUENCE: radial extent of the cone of depression
    • DRAWDOWN CURVE: develops gradually at a constant rate of pumping
    • UNSTEADY FLOW: phase of drawdown curve formation
    • STEADY FLOW: drawdown surface attains a constant position with respect to time
    • RECUPERATION RECOVERY: gradual accumulation of storage until the original level is reached

    Runoff

    • RUNOFF: draining of flowing off of precipitation from a catchment area through a surface channel
    • OVERLAND FLOW: portion of runoff that refers to the excess precipitation moving over the land surface to reach smaller channels
    • SURFACE RUNOFF: flow in the mode where small channels form larger streams
    • INTERFLOW/THROUGH FLOW/STORM SEEPAGE/QUICK RETURN FLOW: component of runoff that infiltrates, moves laterally, and returns to the surface
    • BASE FLOW: delayed flow that reaches a stream easily as groundwater flow
    • NATURAL FLOW/VIRGIN FLOW: stream flow unaffected by human works of diversion and reservoir structures

    Hydrograph

    • HYDROGRAPH: plot of discharge in a stream plotted against time
    • ANNUAL HYDROGRAPH: shows variation of daily or weekly or 10-daily mean flows over a year
    • MONTHLY HYDROGRAPHS: daily mean flow over a month
    • SEASONAL HYDROGRAPH: variation of discharge during monsoon season or dry season
    • FLOOD HYDROGRAPHS: due to a storm over a catchment area

    Runoff Characteristics of Streams

    • THREE CLASSES OF STREAMS:
      • PERENNIAL STREAM: always carries some flow, even during dry seasons
      • INTERMITTENT STREAM: limited contribution from groundwater, dries up during dry seasons
      • EPHEMERAL STREAM: does not have any base flow contribution
    • YIELD OF STREAM: total quantity of surface water that can be expected in a given period from a stream at the outlet of its catchment

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    Description

    This quiz covers the different forms of subsurface water and saturated formations, including aquifers and their characteristics.

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