Australian River Assessment System: AusRivAS Physical Assessment Protocol

Melissa Parsons, Martin Thoms and Richard Norris
Cooperative Research Centre for Freshwater Ecology
University of Canberra
Monitoring River Health Initiative Technical Report Number 22
Environment Australia, 2002
ISSN 1447-1280
ISBN 0 642 54888 9


5 Instructions for the Measurement of Each Variable (continued)

Response Variables (continued)

Extent of bars

VARIABLE NAMEExtent of bars
CATEGORYPhysical morphology and bedform
CONTROL OR RESPONSEResponse
OFFICE OR FIELDField
UNITS OF MEASUREMENT% extent of bars
 
INDICATESIncreased bar formation may be associated with increasing sedimentation or reduced instream flows

A bar is a submerged or exposed ridge-like accumulation of sand, gravel or other alluvial material formed in the channel where a decrease in velocity induces deposition (Armantrout, 1998).

At each sampling site, visually estimate the percentage of the streambed area that protrudes to form a bar of any type (Figure 5.20). Also record the dominant sediment particle size of the bars. Streambed area is equivalent to the length of the sampling site and the width of the wetted channel (under baseflow conditions). Bars can be unattached (e.g. islands) or attached to the banks.

Figure 5.20 Examples of bars in a river channel. Figure 5.20 Examples of bars in a river channel. Figure 5.20 Examples of bars in a river channel.

Figure 5.20 Examples of bars in a river channel

Variable derived from the River Habitat Audit Procedure (Anderson, 1993a).


Type of bars

VARIABLE NAMEType of bars
CATEGORYPhysical morphology and bedform
CONTROL OR RESPONSEResponse
OFFICE OR FIELDField
UNITS OF MEASUREMENTChoice of nine categories
 
INDICATESThe types of bars present in a channel are indicative of channel behaviour and channel forming processes

Indicate the presence of one or more of the following bar types along the length of the sampling site:

bars absent bars absent bars formed around obstructions bars formed around obstructions
side/point bars - vegetated side/point bars
VEGETATED
braided channel braided channel
side/point bars unvegetated side/point bars
UNVEGETATED
infilled channel infilled channel
mid-channel island vegetated mid-channel island
VEGETATED
high flow deposits high flow deposits
mid-channel island mid-channel island
UNVEGETATED
 

Variable derived from the River Habitat Audit Procedure (Anderson, 1993a).


Channel shape

VARIABLE NAMEChannel shape
CATEGORYPhysical morphology and bedform
CONTROL OR RESPONSEResponse
OFFICE OR FIELDField
UNITS OF MEASUREMENTChoice of twelve categories
 
INDICATESThe shape of the channel influences many aspects of channel character including discharge, sediment transport and bedform features

At each sampling site, examine the overall shape of the channel as one of the following categories:

categories for overall shape of the channel U shape
Most common natural channel type
categories for overall shape of the channel Box
Commonly encountered with severe gully erosion
categories for overall shape of the channel Flat U shape categories for overall shape of the channel Wide box
categories for overall shape of the channel Deepened U shape
May be naturally incised channels
categories for overall shape of the channel V shaped
categories for overall shape of the channel Widened or infilled categories for overall shape of the channel Trapezoid
Engineered channel shape
categories for overall shape of the channel Two stage
Lowland channel with one bench
categories for overall shape of the channel Concrete V
Engineered channel shape
categories for overall shape of the channel Multi stage

Lowland channel with >1 bench

categories for overall shape of the channel Culvert or pipe

Variable modified from the River Habitat Audit Procedure (Anderson, 1993a).


Bed compaction

VARIABLE NAMEBed compaction
CATEGORYSubstrate
CONTROL OR RESPONSEResponse
OFFICE OR FIELDField
UNITS OF MEASUREMENTChoice of five categories
 
INDICATESPartially determines the erodibility or stability of the bed material.

After examination of the substratum and the bed along the length of the sampling site1, assess the overall character of bed sediment compaction as one of the following categories. The term 'dislodge' refers to the ability to pull individual rocks of different sizes from the streambed with the hands. The term 'overlapping' refers to the relative location of rocks on the streambed (ie. whether they sit on top of each other or next to each other).

Choose the character of bed sediment compaction Tightly packed, armoured
Array of sediment sizes, overlapping, tightly packed and very hard or impossible to dislodge
Choose the character of bed sediment compaction Packed, but not armoured
Array of sediment sizes, overlapping, tightly packed but can be dislodged with moderate effort
Choose the character of bed sediment compaction Moderate compaction
Array of sediment sizes, little overlapping, some packing but can be dislodged with moderate effort
Choose the character of bed sediment compaction Low compaction (1)
Limited range of sediment sizes, little overlapping, some packing and structure but can be dislodged very easily
Choose the character of bed sediment compaction Low compaction (2)
Loose array of fine sediments, no overlapping, no packing and structure and can be dislodged very easily

1 In wadeable streams, the bed can be examined visually along the length of the sampling site. In large rivers, the bed should be examined in relation to the range of sediment sizes present at the sampling site (see substrate composition variable). Generally, beds comprised of gravel, sand and silt sediment sizes are not compacted and are easily moved. Thus, these bed types should be allocated to the low compaction (1) or (2) categories.

Variable derived from the River Habitat Audit Procedure (Anderson, 1993a).


Sediment angularity

VARIABLE NAMESediment angularity
CATEGORYSubstrate
CONTROL OR RESPONSEResponse
OFFICE OR FIELDField
UNITS OF MEASUREMENTChoice of six categories
 
INDICATESIndicates the degree of material reworking.

After visual examination of the substratum and the bed along the length of the sampling site, assess the overall angularity of the cobble, pebble and/or gravel sediment fractions as one of the following categories. Do not include bedrock in the assessment of angularity. Where the cobble, pebble AND gravel fractions are not present at a sampling site (e.g. in lowland rivers), select the 'not present' category.

Choose overall angularity of the cobble, pebble and/or gravel sediment fractions very angular
Choose overall angularity of the cobble, pebble and/or gravel sediment fractions angular
Choose overall angularity of the cobble, pebble and/or gravel sediment fractions sub-angular
Choose overall angularity of the cobble, pebble and/or gravel sediment fractions rounded
Choose overall angularity of the cobble, pebble and/or gravel sediment fractions well-rounded
Choose overall angularity of the cobble, pebble and/or gravel sediment fractions cobble, pebble and gravel fractions not present

Variable derived from the River Habitat Audit Procedure (Anderson, 1993a).