7. Sources of fine sediment
National-scale sediment source
apportionment for England & Wales Relative
contribution of
agriculture to
annual sediment
load
>50%
<50%
Zhang, Collins et al. (2014) Env. Sci. Pol. 42:16-32
8. Insert image here
Insert image here
WQ0128 Extending the evidence
base on the ecological impacts of
fine sediment and developing a
framework for targeting mitigation
of agricultural sediment losses
23. • Existing evidence base for impacts of fine sediment is
largely correlative
• Failure to elucidate the critical process linkages
between sediment stress and key environmental
parameters/characteristics
Reviews of Biological Impacts
– Key Findings
24. Improved Ecological Evidence
Fish response to sediment stress
– Role of Sediment Oxygen Demand
– New approaches to source apportionment
– Manipulative experiments
26. 0
0.1
0.2
0.3
0.4
0.5
0.6
0.7
0.8
0.9
1
0 50 100 150 200 250
Brown Trout
Atlantic Salmon
Bank Agriculture Road STW
0
0.1
0.2
0.3
0.4
0.5
0.6
0.7
0.8
0.9
1
Brown Trout
Atlantic Salmon
a
b
c
c d
ee e
MortalityMortality
a)
b) A
B
BCC
Sediment mass added (g wet weight)
Both load and
source important
Sear et al. (submitted)
27. • Extended field evidence and
calibration datasets for Sediment
Intrusion and Dissolved Oxygen
(SIDO)-UK spawning habitat model
• Applied new approaches to source
apportionment – tracing sources of
organic matter
• Developed better understanding of
role of Sediment Oxygen Demand
36. Sediment Oxygen Demand
Used SIDO-UK to develop a
better understanding of role
of Sediment Oxygen
Demand
Both agricultural and non-
agricultural sediment has the
potential to impact aquatic
ecology.
More organic sediment
derived from point
sources and damaged road
verges resulted in more
pronounced detrimental
effects.
Sear et al. (2014) Hydrological Processes 28: 86-103
38. Calibration dataset
• 230 sites sampled for macroinvertebrates & deposited
fine sediment
• across a gradient of modelled sediment pressure
• across a gradient of stream types
• free from STW and urban area inputs
• upstream of lakes & reservoirs
• predominantly agricultural catchments
39. Objectives
• Establish relationship between macroinvertebrate
community and fine sediment pressure at an appropriate
management scale
• Develop a diagnostic biotic index
• Independently test new index
40. Macroinvertebrate sampling
At each site:
– macroinvertebrate sample (RIVPACS protocol)
o record physical features of site
o acquire map-based data
41. Fine sediment sampling
At each site:
o remobilisation stilling well
sample surface drape and embedded fine sediment
from erosional and depositional areas
Processed in the lab for:
mass of sediment
organic content
particle size
Duerdoth et al. (2015) Geomorphology 230: 37–50
42. Duerdoth et al. (2015) Geomorphology 230: 37–50
Fine sediment sampling
Reach scale confidence intervals and reproducibility quantified
0
1
2
3
4
5
0 1 2 3 4 5
site mean log10
surface sediment mass (g m-2
) site mean log10
total sediment mass (g m-2
)
surface drape total
samplelog10
surfacesedimentmass(gm-2
)n-volatile
m-2
)
samplelog10
totalsedimentmass(gm-2
)-volatile
m-2
)
a)
b)
95% Confidence
intervals = ±0.237
4
5
0
1
2
3
4
5
0 1 2 3 4 5
4
5
95% Confidence
intervals = ±0.236
95% Confidence
intervals = ±0.235
95% Confidence
intervals = ±0.227
43. Comparison with visual estimates
of bed composition
surface drape: average
mean substratum size phi
sedimentmassg/m
2
-8 -4 0 4 8
10
0
10
1
10
2
10
3
10
4
10
5
total sediment: average
mean substratum size phi
sedimentmassg/m
2
-8 -4 0 4 8
10
0
10
1
10
2
10
3
10
4
10
5
Visual estimates only explain 50-60% of the variation in fine sediment
mass
44. Analytical Approach
Predicted Sediment Load
Predicted Sediment Retention
Measured Retained Sediment
Measured Sediment Quality
Invertebrate community
range of sediment loadings
within river types
45. Analytical Approach
• Association between variation in the macroinvertebrate
community and the fine sediment stressor gradient
having first factored out that portion of the biological
variation correlated with natural background variation
• Empirical basis for a diagnostic biotic index
• Relationship between modelled agricultural fine
sediment inputs, retentiveness of stream reach and
biological condition of the reach quantified
• Link land-use models to WFD water quality status.
47. Invertebrate response to fine sediment stress comprises two
distinct components
ToFSIsp – index of response to organic component of fine
sediment
oFSIsp – index of response to organic component of fine
sediment
The results of these two indices are then combined
CoFSIsp – combined index of fine sediment stress
Index Development
48. Index response (development sites)
54321
6.5
6.0
5.5
5.0
4.5
4.0
log Fine Sediment Mass (g m-2)
cFSIsp
S 0.348063
R-Sq 56.3%
R-Sq(adj) 56.1%
cFSIsp = 6.553 - 0.5467 logSedMass
CoFSIsp
52. Jones et al. (2015) Freshwater Biology
Growns et al. (submitted)
Response variables
Turbidity
Deposited Sediment Mass
Oxygen Penetration
Hyporheic Chemistry
Interaction with Flow
Drift
Community Composition
Index Values
Trait Composition
Hyporheic Invertebrates
CONTROL MODERATE HIGH
53. Before After
e)
Control Moderate High
0
0 . 5
1
1 . 5
2
2 . 5
3
3 . 5
4
4 . 5
5
PSIsp
ASPT
cFSIsp
ToFSIsp
Control Moderate High
0
5
1 0
1 5
2 0
2 5
3 0
3 5
Control Moderate High
0
0 . 5
1
1 . 5
2
2 . 5
3
3 . 5
4
4 . 5
5
Control Moderate High
0
1
2
3
4
5
c) d)
f)
CoFSIsp index performs well
PSI index unstable
55. Outputs
• Quantified changes in macroinvertebrate
community across a gradient of fine sediment
pressure.
– Identify taxa sensitive and tolerant to fine sediment stress
• Developed and tested a new diagnostic biotic index
• Linked diagnostic index to estimates of sediment
pressure
56. New Modelling Framework
daily time step
use of weather data (as opposed to climatic mean)
explicit representation of pathways (tramlines,
compaction, etc)
explicit representation of crops and rotations
drain flow
connectivity and retention:
field boundaries types
particle size distribution and selectivity
57. Conceptual flow pathways in catchments
Preferential flow to
drains
Slow flow to drainsTo groundwater
Plot-scale
runoff
initiation
Field boundary
retention
Landscape
retentionIn-field
retention
MITIGATION
59. • Downscale catchment scale processes to the channel reach
and redd scales
• use of a hydraulic sediment routing model to link network to
reach scales
In-channel sediment routing
Catchment Reach Redd
> 1 km2
100-50 m
< 1 m
Psychic SIDO-UKRouting
61. Use of the modelling toolkit
• catchment-specific
revised sediment targets
• implications for meeting
revised targets of
– mitigation programmes
– climate change
projections for 2020,
2030, 2050, 2080
Mitigation methods for inorganic sediment
Establish cover crops in the autumn
Early harvesting and establishment of crops in the autumn
Cultivate land for crops in spring rather than autumn
Adopt reduced cultivation systems
Cultivate compacted tillage soils
Cultivate and drill across the slope
Leave autumn seedbeds rough
Manage over-winter tramlines
Establish in-field grass buffer strips
Establish riparian buffer strips
Re-site gateways away from high-risk areas
62. Modelling toolkit for managing the
problem
• Ecological status linked to land-use models
to enable managers to explore outcome of
agricultural mitigation options
• Better targeting of mitigation