Grain Size Flashcards

1
Q
  • A widely used grade scale for expressing particle size
  • A logarithmic and geometric scale with a fix ratio between successive elements
A

Udden-Wentworth Scale

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2
Q

Udden-Wentworth Scale extends from

A

< 1/256 mm to >256 mm

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3
Q

logarithmic scale for sediment size

A

Kumbrein Phi Scale

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4
Q

Increase in abs value negative phi =

A

Increase in mm size

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5
Q
  • Increase in positive phi =
A

decrease in mm size

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6
Q

particles that are settling will pass through a diffracted light, the angle of the diffracted light increases with a decreasing particle size. A detector senses the angular distribution of scattered light energy.

A
  • Laser Diffraction size analyzer
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7
Q

sediments are slowly poured into an electrolyte solution, where sediments will pass through, where changes in the electrical field will produce pulses, translating into the grain size

A
  • Electro-resistant size analysers
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8
Q

Φ < 0.35

A

VW Sorted

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9
Q

0.35 < Φ < 0.5

A

W Sorted

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10
Q

0.5 < Φ < 0.7

A

MW Sorted

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11
Q

0.7 < Φ < 1

A

M Sorted

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12
Q

1 < Φ <2

A

P Sorted

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13
Q

2 < Φ <4

A

VP Sorted

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14
Q

0.4 > Φ

A

EP Sorted

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15
Q
  • based on a constant ratio of two between successive class boundaries together with terms for the classes
  • A Geometric Scale
A

Udden Wentworth Scale

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16
Q

Kumbrein introduced an ?? Measured in ?? uunits

A

Kumbrein; Phi

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17
Q

clast size of conglomerates and breccias can be measured directly with a ?

A

tape measure

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18
Q

With poorly cemented sandstones and unconsolidated sands, ???is the most popular technique

A

sieving

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19
Q
  • Medium silt to small pebble
    • ?? min sieving time
    • ?? gram samples
A

15; 30

20
Q

show the frequency of grains in each size-class and usefully give an immediate impression of the grain-size distribution

A

histogram, smoothed frequency curve

21
Q

shows the percentage frequency of grains coarser than a particular value

A

cumulative frequency curve

22
Q

Most sediments are ??, i.e. one class dominate

A

Unimodal

23
Q

If grain-size distribution is perfectly normal

A

then the median, mean and mode values are the same

24
Q

grain size decreasing away from the source area

A
  • relates to selective sediment transport
  • fluvial and deltaic
  • turbidites in deep-sea basin
  • offshores, wave and current energy decrease
25
Q

a measure of the standard deviation, spread of the grain-size distribution.

A
  • Sorting
26
Q

Several Factors that Determine Sediment Sorting

A

Sediment Source
Grain
Depositional Mechanism

27
Q

A general rule about sorting

A

improves along the sediment transport path

28
Q

a measure of the symmetry of the distribution

A
  • Skewness
29
Q

If the distribution has a ????, i.e. excess coarse material, then the sediment is said to be ????

A

Coarse tail; Negatively Skewed

30
Q

If the distribution has a ????, i.e. excess fine material, then the sediment is said to be ????

A

Fine tail; Positively Skewed

31
Q

If the distribution is symmetrical, then there is ?????.

A

no skew

32
Q

Skewness > 0.30

A

S fine skewed

33
Q

Skewness 0.3>0.1

A

fine skewed

34
Q

Skewness 0.1>–0.10

A

Near-symmetrical

35
Q

Skewness -0.1>–0.30

A

Coarse Skew

36
Q

Skewness >-0.30

A

S Coarse Skew

37
Q

River sands are usually ???? skewed

A

positive

38
Q

Beach sands, for example, tend to have a ??? skew

A

negative

39
Q

n general, sediment becomes more ???? skewed (and finer grained) along its ?????/

A

Negative; Sediment Transport Path

40
Q

????????? becomes more positively skewed and relatively coarse

A

source sediment (lag?

41
Q
  • section diameter of randomly oriented grains are usually smaller than their maximum diameter
  • grains cut marginally in a thin-section plane have smaller apparent diameters
A

Corpuscle Effect

42
Q
  • sharpness or peakedness of a grain-size frequency curve
A

Kurtosis

43
Q
  • Sharp peaked curves
  • better sorting in the central portion of the grain-size distribution
A

Leptokurtic

44
Q
  • flat peaked curves
  • poor sorting in the central portion of the grain-size distribution
A

Playkurtic

45
Q

A method of direct calculation of mean size, std dev, skewness, kurtosis w/o cumulative curve plots

A

Moment Method

46
Q
  • when size distribution of natural sediment, such as dune sand, is plotted on log–log plots and a curve is fitted to these data, the resulting curve actually has the shape of a ??????
A

hyperbola