Quiz 8+9 Flashcards

1
Q

Stream flow responde determined by

A

-spatial and temporal variability in rain
-travel time from watershed area to stream
-travel time from channel entrance to outlet
-slope
-watershed shape
-drainage patterns
-soils and geology

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2
Q

Measurement of stage

A

-height of water surface above arbitrary datum
-manual: staff gauge
-automated: sitting well float

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3
Q

Measurement velocity

A

-distance traveled per unit time
-standard is a six tenths depth

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4
Q

Measurement discharge

A

-rate at which water passes through a given cross section
-destermined using velocity area method

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5
Q

Measurement rating curve

A

-relationship between stage and discharge to each stream.
-uses non linear regression

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6
Q

Rational method

A

-used to predict peak flow rates in small watersheds

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7
Q

Runoff generation

A

-factors affecting
1.precipitation form and intensity
2.storage/soil moisture
3.spatial distribution
4.covergence of flow pathways
5.land use or land disturbance

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8
Q

VSA (variable source area)

A

-most of the storm flow by interflow and saturation Overland flow to stream channel
-infiltration not a limiting factor
-watershed area not a direct index of flow response
-assumes only part of a watershed is making direct contribution to storm flow
Primary contributors
1.interflow
2.saturation excess Overland flow

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9
Q

Vsa vs partial

A

Spatial
1.partial-fixed in area space
2.VSA-expand and contract overtime
Source if water
1.)partial
-INFILTRATION excess Overland flow
2.)VSA
-interflow and saturation excess

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10
Q

Erosion

A

-detachment and transport of unconsolidated material from one place to another

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11
Q

Erosion impacts

A

-nutrient loss
-reduce infiltration
-fills resevoirs
-affects aquatic organisms
-drinking water quality
-carries toxins
-
-

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12
Q

Erosion phases

A

-detachment
Rain drops falling on ground and flowing to dislodge material E=(M)(Vt^2)/2
-transportation
Detached particles moved down hill
-depostion
Particles eventually accumulate somewhere (sedementation)

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13
Q

Sheet erosion

A

-relatively uniform erosion over entire soil surface
-requires Overland flow and is often exacerbated by raindrop impact

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14
Q

Rill erosion

A

-most common form of soil erosion
-occurs when Overland flow breaks up into small channels or microrills

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15
Q

Gully erosion

A

-when depth of a rill is greater than .3m

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16
Q

Surface erosion in forest

A

-high infiltration and interception makes erosion generally not an issue in forest

17
Q

Mass movement commonality

A

-most common in OR, WA, AND CA in coastal and mountain areas

18
Q

Mass movement factors

A

-vegetation, topography, land use, precipitation.

Arid, sparse veg = mudflows/debris

Humid/dense veg = earthflows/soil creep

19
Q

Mass movements slide hazar

A

-slope > 80% except 75% in tyce core area
-headwall configuration
-geology: coast range sandstone with sequences of turbiditbeds

20
Q

Mass movement slides

A

-down slope movement of soil or rock on a surface of rupture
-occur in response to extreme rain events, snowmelt, grading, adding loads to top slope
Two types
1.translational:movement along a roughly planar surface
2.rotational: curved concavely upward

21
Q

Forces promoting failure

A

F = resistance of soil to failure / forces promoting failure
Safety factor
- _< 1 imminent failure
->_1 increasing slope stability

22
Q

Debris flow

A

-form of rapid mass movement in which loose materials flow downslope
-source area: steep gullies

23
Q

Soil creep

A

-very slow (mm/yr)
-caused by sheer force not great enough to cause failure
-evidence is curved trees

24
Q

Erosion measurements

A

-silt fences
-erosion pins
-rainfall simulator

25
Q

USLE

A

-provides an estimate of sheet and rill erosion from rainfall elements on up land areas: principally ag land

26
Q

MUSLE

A

-Adds vegetation management factor to equation which is why it’s used for forestry

Does it work? Not usually

27
Q

WEPP water erosion prediction project

A

Used for small scale watersheds.