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
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

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
a measure of the *standard deviation,* spread of the grain-size distribution.
- **Sorting**
26
Several Factors that Determine Sediment Sorting
Sediment Source Grain Depositional Mechanism
27
A general rule about sorting
improves along the sediment transport path
28
a measure of the *symmetry of the distribution*
- **Skewness**
29
If the distribution has a *????,* i.e. *excess coarse material,* then the sediment is said to be *????*
Coarse tail; Negatively Skewed
30
If the distribution has a *????,* i.e. *excess fine material,* then the sediment is said to be *????*
Fine tail; Positively Skewed
31
If the distribution is **symmetrical**, then there is **?????.**
no skew
32
Skewness > 0.30
S fine skewed
33
Skewness 0.3>0.1
fine skewed
34
Skewness 0.1>--0.10
Near-symmetrical
35
Skewness -0.1>--0.30
Coarse Skew
36
Skewness >-0.30
S Coarse Skew
37
*River sands* are usually *????* skewed
positive
38
*Beach sands*, for example, tend to have a *???* skew
negative
39
n general, sediment becomes more *????* skewed (and finer grained) along its *?????/*
Negative; Sediment Transport Path
40
????????? becomes more *positively skewed* and relatively coarse
source sediment (lag?
41
- 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
Corpuscle Effect
42
- sharpness or peakedness of a grain-size frequency curve
Kurtosis
43
- **Sharp peaked** curves - **better sorting** in the **central** portion of the grain-size distribution
Leptokurtic
44
- **flat peaked** curves - **poor sorting** in the **central** portion of the grain-size distribution
Playkurtic
45
A method of direct calculation of mean size, std dev, skewness, kurtosis w/o cumulative curve plots
Moment Method
46
- 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 **??????**
hyperbola