arrow-left

All pages
gitbookPowered by GitBook
1 of 23

Loading...

Loading...

Loading...

Loading...

Loading...

Loading...

Loading...

Loading...

Loading...

Loading...

Loading...

Loading...

Loading...

Loading...

Loading...

Loading...

Loading...

Loading...

Loading...

Loading...

Loading...

Loading...

Loading...

wd

Channel width

sinu

Channel sinuosity

Channel sinuosity is a measure of how much a river or stream channel deviates from a straight line between two points. It is calculated by dividing the length of the channel by the straight-line distance between its endpoints.

For rivers, the conventional classes of sinuosity are:

  • sinu <1.05: almost straight

  • 1.05 ≤ sinu <1.25: winding

  • 1.25 ≤ sinu <1.50: twisty

  • 1.50 ≤ sinu: meandering

erod_fact

Channel erodibility factor

circle-info

A value of erod_fact = 1 indicates that there is no resistance to erosion. A value of erod_fact = 0 is suitable for non-erosive channels.

k

Effective hydraulic conductivity of the channel alluvium

bed_load

Percent of sediment entering the channel that is bed material

clay

Clay content of channel bank and bed

p_conc

Phosphorus concentration in channel bank

slp

Channel slope

The channel slope is calculated by QSWAT+ based on the DEM.

fps

Floodplain slope

len

Channel length

The channel length is calculated by QSWAT+ based on the DEM.

mann

Channel Manning's n

side_slp

Channel side slope

eq_slp

Equilibrium channel slope

carbon

Carbon content of channel bank and bed

cov_fact

Channel cover factor

circle-info

A value of cov_fact = 1 indicates that there is no vegetative cover on the channel. A value of cov_fact = 0 indicates that the channel is completely protected from erosion.

dp

Channel depth

fpn

Floodplain Manning's n

dry_bd

Dry bulk density of the channel

hyd-sed-lte.cha

This file controls the channel hydrology and sediment properties.

Field
Description
Type
Unit
Default
Range

Name of the channel hydrology and sediment record

string

n/a

n/a

n/a

wd

Channel width

real

m

calculated by QSWAT+

dp

Channel depth

real

m

calculated by QSWAT+

slp

Channel slope

real

m/m

calculated by QSWAT+

len

Channel length

real

km

calculated by QSWAT+

mann

Channel Manning's n

real

none

0.05

k

Effective hydraulic conductivity of the channel alluvium

real

mm/h

1.0

erod_fact

Channel erodibility factor

real

none

0.01

cov_fact

Channel cover factor

real

none

0.01

0-1

sinu

Channel sinuosity

real

none

6.0

eq_slp

Equilibrium channel slope

real

m/m

0

d50

Channel median sediment size

real

mm

12.0

clay

Clay content of channel bank and bed

real

%

50.00

0-100

carbon

Carbon content of channel bank and bed

real

%

0

0-100

dry_bd

Dry bulk density of the channel

real

t/m3

0

side_slp

Channel side slope

real

m

0.50

bed_load

Percent of sediment entering the channel that is bed material

real

m

0.50

fps

Floodplain slope

real

m/m

10.0

fpn

Floodplain Manning's n

real

none

n_conc

Nitrogen concentration in channel bank

real

mg/kg

0.10

p_conc

Phosphorus concentration in channel bank

real

mg/kg

0.30

p_bio

Fraction of phosphorus in bank that is bioavailable

real

fraction

0.30

name

p_bio

Fraction of phosphorus in bank that is bioavailable

name (hyd-sed-lte.cha)

Name of the channel hydrology and sediment record

The name of the channel hydrology and sediment record is a primary key referenced by hyd in channel-lte.cha.

n_conc

Nitrogen concentration in channel bank

d50

Channel median sediment size

The table below lists the D50 values of different sediment classes:

Sediment class
Size [µm]
Approximate size

Boulders

> 256,000

> Volley ball

Cobbles

> 64,000

> Tennis ball

Pebbles

> 2,000

> Match Head

Coarse Sand

1,500

Medium Sand

375

Fine Sand

94

Coarse Silt

47

Medium Silt

11.7

Not visible to the human eye

Fine Silt

4.9

Clay

1.95