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Soil Tech Finals 3
11問 • 2年前
  • Mutated Lemon
  • 通報

    問題一覧

  • 1

    The following are methods used in soil erosion measurement:

    Point measurements, Erosion pins, Paint collars, Bottle tops, Pedestals, Tree mounds and tree roots, Profile meters, Rills and roads, Gullies and streambanks, Catchpits, Runoff plots

  • 2

    This widely-used method consists of driving a pin into the soil so that the top of the pin gives a datum from which changes in the soil surface level can be measured

    Erosion pins

  • 3

    Individual measurements of change in level at a single point will vary widely, but if it is an inexpensive and simple method, and a large number of points can be sampled, then a usable estimate can result.

    Point measurements

  • 4

    When an easily eroded soil is protected from splash erosion by a stone or tree root, isolated pedestals capped by the resistant material are left standing up from the surrounding ground.

    Pedestals

  • 5

    Another simple way to record the original level is to press bottle tops into the soil surface.

    Bottle tops

  • 6

    To measure small changes in surface level along a cross section such as an area with a number of parallel cattle tracks, a profile meter may be suitable.

    Profile meters

  • 7

    In arid or semi-arid climates it is not unusual to find that the surface under trees is raised in a gently sloping dome.

    Tree mounds and tree roots

  • 8

    When the progress of gully erosion is being studied, measurements are needed both of the horizontal spread of the gully and vertical changes within the gully.

    Gullies and streambanks

  • 9

    Measuring the cross-section of all the rills in a sample area or along a sample transect is quick and easy, so the method is suitable for measuring change over short time periods, such as the change caused by a single heavy storm.

    Rills and roads

  • 10

    It is a structure used to measure the overland flow and soil loss thereby under controlled condition. Runoff plots are constructed directly in the field.

    Run-off plots

  • 11

    Surveys of sediment in reservoirs can be used to make quantitative estimates of erosion as discussed in chapter 5, but simple catchpits may be used to demonstrate comparisons

    Catchpits

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    問題一覧

  • 1

    The following are methods used in soil erosion measurement:

    Point measurements, Erosion pins, Paint collars, Bottle tops, Pedestals, Tree mounds and tree roots, Profile meters, Rills and roads, Gullies and streambanks, Catchpits, Runoff plots

  • 2

    This widely-used method consists of driving a pin into the soil so that the top of the pin gives a datum from which changes in the soil surface level can be measured

    Erosion pins

  • 3

    Individual measurements of change in level at a single point will vary widely, but if it is an inexpensive and simple method, and a large number of points can be sampled, then a usable estimate can result.

    Point measurements

  • 4

    When an easily eroded soil is protected from splash erosion by a stone or tree root, isolated pedestals capped by the resistant material are left standing up from the surrounding ground.

    Pedestals

  • 5

    Another simple way to record the original level is to press bottle tops into the soil surface.

    Bottle tops

  • 6

    To measure small changes in surface level along a cross section such as an area with a number of parallel cattle tracks, a profile meter may be suitable.

    Profile meters

  • 7

    In arid or semi-arid climates it is not unusual to find that the surface under trees is raised in a gently sloping dome.

    Tree mounds and tree roots

  • 8

    When the progress of gully erosion is being studied, measurements are needed both of the horizontal spread of the gully and vertical changes within the gully.

    Gullies and streambanks

  • 9

    Measuring the cross-section of all the rills in a sample area or along a sample transect is quick and easy, so the method is suitable for measuring change over short time periods, such as the change caused by a single heavy storm.

    Rills and roads

  • 10

    It is a structure used to measure the overland flow and soil loss thereby under controlled condition. Runoff plots are constructed directly in the field.

    Run-off plots

  • 11

    Surveys of sediment in reservoirs can be used to make quantitative estimates of erosion as discussed in chapter 5, but simple catchpits may be used to demonstrate comparisons

    Catchpits