3.0 Rudsdale Creek Catchment: Riparian Conditions
The Stream Characterization Program evaluated 3.3 km of Rudsdale Creek in 2016. A total of 33 stream survey assessments were completed in the middle of June and July.
During the summer and fall of 2016, the Rideau Valley watershed experienced periods of severe drought. Precipitation levels were measured at less than 40% of the long-term average, as the water supply was unable to meet local demand. The lack of rainfall affected the success and function of farm crops, municipal and private wells, lawns and gardens, navigation and ultimately the health of our lakes, rivers and streams.
Low water conditions were readily observed throughout the watershed, as many of the streams were highly fragmented or completely dry. Aquatic species such as amphibians, fish and macro invertebrates were affected, as suitable habitat may have been limited. Fragmentation of habitat was observed in certain sections along Rudsdale Creek during the drought conditions in 2016.
Rudsdale Creek at Christie Lake Road during the drought in the Fall of 2016
3.1 Rudsdale Creek Overbank Zone
3.1.1 Riparian Buffer Evaluation
The quality of the riparian area increases with the width, complexity and linear extent of its vegetation along a stream or creek. A complex riparian community consists of diverse plant species native to the site, with multiple age-classes providing vertical structural diversity along a watercourse.
Here is a list of watershed benefits from a healthy riparian buffer zone:
- Reduces the amount of pollutants that reach the stream from surface runoff
- Helps reduce and mitigates erosion
- Provides a microclimate that is cooler during the summer months providing cooler water for aquatic organisms
- Provides large wood structure from fallen trees and limbs that form instream cover, create pools, stabilize the streambed, and provide habitat for aquatic organisms
- Provides organic material for stream biota that, among other functions, is the base of the food chain in lower order streams
- Provides habitat for terrestrial insects that drop in the stream and become food for fish and travel corridors for other terrestrial animals
- Dissipates energy during flood events
- Often provides the only refuge areas for fish during out-of-bank flows (behind trees, stumps, and logs)
Figure 11 demonstrates the buffer conditions of the left and right banks separately. Rudsdale Creek had a buffer of greater than 30 meters along 93 percent of the left bank and 89 percent of the right bank.
Figure 11 Riparian Buffer Evaluation along Rudsdale Creek
3.1.2 Riparian Buffer Alterations
Alterations within the riparian buffer were assessed within three distinct shoreline zones (0-5m, 5-15m, 15-30m), and evaluated based on the dominant vegetative community and/or land cover type (Figure 12). The riparian buffer zone along Rudsdale Creek was found to be dominated by scrubland, forest and wetland conditions. There were two areas that had altered riparian zone conditions along the watercourse.
Figure 12 Riparian buffer alterations along Rudsdale Creek
3.1.3 Adjacent Land Use
The RVCA’s Stream Characterization Program identifies six different land uses along Rudsdale Creek (Figure 13). Surrounding land use is considered from the beginning to end of the survey section (100m) and up to 100m on each side of the river. Land use outside of this area is not considered for the surveys but is nonetheless part of the subwatershed and will influence the creek. Scrubland habitat was dominant at 88 percent; wetland habitat was observed in the adjacent lands along Rudsdale Creek at 58 percent of the surveyed sections, 45 percent forest and 15 percent meadow habitat. The remaining land use consisted of industrial/commercial and infrastructure in the form of reduced shoreline buffer areas and road crossings.
Figure 13 Land Use along Rudsdale Creek
3.2 Rudsdale Creek Shoreline Zone
3.2.1 Instream Erosion
Stream erosion is the process by which water erodes and transports sediments, resulting in dynamic flows and diverse habitat conditions. Excessive erosion can result in drastic environmental changes, as habitat conditions, water quality and aquatic life are all negatively affected. Bank stability was assessed as the overall extent of each section with “unstable” shoreline conditions. These conditions are defined by the presence of significant exposed soils/roots, minimal bank vegetation, severe undercutting, slumping or scour and potential failed erosion measures. The majority of Rudsdale Creek had no erosion observed along the surveyed sections with two reaches having low to moderate levels of erosion in the middle to lower reach (Figure 14).
Figure 14 Erosion levels along Rudsdale Creek
3.2.2 Undercut Stream Banks
Stream bank undercuts can provide excellent cover habitat for aquatic life, however excessive levels can be an indication of unstable shoreline conditions. Bank undercut was assessed as the overall extent of each surveyed section with overhanging bank cover present. Figure 15 shows that Rudsdale Creek had no observed undercut banks along the majority of the system, however there were several sections in the middle to lower reaches with low levels of undercut banks.
Figure 15 Undercut stream banks along Rudsdale Creek
3.2.3 Stream Shading
Grasses, shrubs and trees all contribute towards shading a stream. Shade is important in moderating stream temperature, contributing to food supply and helping with nutrient reduction within a stream. Stream cover is assessed as the total coverage area in each section that is shaded by overhanging trees/grasses and tree canopy, at greater than 1m above the water surface. Figure 16 shows low levels of stream shading along the majority of Rudsdale Creek in the upper reaches, which is consistent with wide open water wetland habitat conditions. There were several sections in the lower reaches, where the channel narrows, that had high to moderate levels of stream shading along the creek.
Figure 16 Stream shading along Rudsdale Creek
3.2.4 Instream Wood Structure
Forested shorelines provide essential complex habitat through the perpetual process of shoreline trees falling into the water. This continuous recruitment of trees creates a wood-based physical structure in the littoral zone that is common on natural systems. Insects, fish, amphibians, birds, and other animals have also evolved with this abundance of near shore wood and it is essential to their life cycles. With increased development along many waterways, forested lakeshores have been altered and wood-based physical structure in many waterways has been reduced. It is important to restore this essential habitat to aquatic ecosystems.
- Protects shorelines by providing a barrier from wind and wave erosion
- Reduces sedimentation of the water caused by shoreline slumping due to bank erosion
- Allows detritus to collect and settle on the lake or creek bed providing the substrate structure required for native aquatic vegetation to establish and outcompete invasive species
- Wood complexes are an important food source for invertebrates
- Small fish feed on the abundance of invertebrates that are found around these structures
- Larger fish, waterfowl and shorebirds all benefit from the abundance of invertebrates and small fish feeding around woody structures in the littoral zone
- Cover from predators is essential for many fish and animals to successfully complete their life cycle
- The nooks and crannies of wood complexes offer critters safety from predators while at the same time concentrating prey to make predators more efficient
- Wood provides the structure on which many species must lay or attach their eggs, therefore these complexes provide quality spawning and nesting habitat
- Wood complexes in the littoral zone provide unique edge habitat along the shoreline
- Edge habitats contain more species diversity and higher concentrations of species than the adjoining habitats themselves will have
Figure 17 shows that the majority of Rudsdale Creek had low levels along the majority of the system with one location in the upper reaches having high levels of instream wood structure in the form of branches and trees along the system.
Figure 17 Instream wood structure along Rudsdale Creek
3.2.5 Overhanging Wood Structure
Trees and branches that are less than one meter from the surface of the water are defined as overhanging. Wood structure provides a food source, nutrients and shade which helps to moderate instream water temperatures. Figure 18 shows the system is highly variable with no overhanging branches and trees where the system is wide and is dominated by wetland habitat to an area in the lower reach that has high levels of overhanging wood structure along Rudsdale Creek.
Figure 18 Overhanging wood structure along Rudsdale Creek
3.2.6 Anthropogenic Alterations
Stream alterations are classified based on specific functional criteria associated with the flow conditions, the riparian buffer and potential human influences. Figure 19 shows nine percent of Rudsdale Creek remains “unaltered” with no anthropogenic alterations. Seventy three percent of Rudsdale Creek was classified as natural with minor anthropogenic changes while eighteen percent was considered altered. The alterations along Rudsdale Creek were in the form of buffer/shoreline modifications and road crossings. There were no sections that were classified as being highly altered.
Figure 19 Anthropogenic alterations along Rudsdale Creek
3.3 Rudsdale Creek Instream Aquatic Habitat
3.3.1 Benthic Invertebrates
Freshwater benthic invertebrates are animals without backbones that live on the stream bottom and include crustaceans such as crayfish, molluscs and immature forms of aquatic insects. Benthos represent an extremely diverse group of aquatic animals and exhibit wide ranges of responses to stressors such as organic pollutants, sediments and toxicants, which allows scientists to use them as bioindicators. As part of the Ontario Benthic Biomonitoring Network (OBBN), the RVCA has been collecting benthic invertebrates at the County Road 6 site since 2003. Monitoring data is analyzed for each sample site and the results are presented using the Family Biotic Index, Family Richness and percent Ephemeroptera, Plecoptera and Trichoptera.
Hilsenhoff Family Biotic Index
The Hilsenhoff Family Biotic Index (FBI) is an indicator of organic and nutrient pollution and provides an estimate of water quality conditions for each site using established pollution tolerance values for benthic invertebrates. FBI results for the Rudsdale Creek catchment at the County Road 6 sample location is summarized by year. “Fair” to “Poor” water quality conditions were observed at the Rudsdale Creek sample location (Figure 20) using a grading scheme developed by Conservation Authorities in Ontario for benthic invertebrates.
Figure 20 Hilsenhoff Family Biotic Index at the County Road 6 sample location
Family Richness measures the health of the community through its diversity and increases with increasing habitat diversity suitability and healthy water quality conditions. Family Richness is equivalent to the total number of benthic invertebrate families found within a sample. The County Road 6 location is reported to have “Fair” family richness (Figure 21).
Figure 21 Family Richness on Rudsdale Creek at the County Road 6 sample location
Ephemeroptera (Mayflies), Plecoptera (Stoneflies), and Trichoptera (Caddisflies) are species considered to be very sensitive to poor water quality conditions. High abundance of these organisms is generally an indication of good water quality conditions at a sample location. The community structure is typically dominated by species that are tolerant to poorer water quality conditions at the Rudsdale Creek sample location. As a result, the EPT indicates that the Rudsdale Creek sample location is reported to have “Poor” water quality (Figure 22) during the reporting periods.
Figure 22 EPT on Rudsdale Creek at the County Road 6 sample location
Overall the Rudsdale Creek sample location at County Road 6 aquatic habitat conditions from a benthic invertebrate perspective are considered “Poor” as the samples are dominated with species that are tolerant to high organic pollution levels.
3.3.2 Habitat Complexity
Habitat complexity is a measure of the overall diversity of habitat types and features within a stream. Streams with high habitat complexity support a greater variety of species niches, and therefore contribute to greater diversity. Factors such as substrate, flow conditions (pools, riffles) and cover material (vegetation, wood structure, etc.) all provide crucial habitat to aquatic life. Habitat complexity is assessed based on the presence of boulder, cobble and gravel substrates, as well as the presence of instream woody material.
Low to high habitat complexity was identified for Rudsdale Creek (Figure 23). Regions with increased habitat complexity were observed in the lower reaches of the system within the catchment.
Figure 23 Habitat complexity along Rudsdale Creek
3.3.3 Instream Substrate
Diverse substrate is important for fish and benthic invertebrate habitat because some species have specific substrate requirements and for example will only reproduce on certain types of substrate. The absence of diverse substrate types may limit the overall diversity of species within a stream. Figure 24 shows the overall presence of various substrate types observed along Rudsdale Creek. Substrate conditions were highly diverse along Rudsdale Creek with all substrate types being recorded at various locations along the creek. Figure 25 shows the dominant substrate type observed for each section surveyed along Rudsdale Creek.
Figure 24 Instream substrate along Rudsdale Creek
Figure 25 shows the dominant substrate type along Rudsdale Creek
3.3.4 Instream Morphology
Pools and riffles are important habitat features for aquatic life. Riffles are fast flowing areas characterized by agitation and overturn of the water surface. Riffles thereby play a crucial role in contributing to dissolved oxygen conditions and directly support spawning for some fish species. They are also areas that support high benthic invertebrate populations which are an important food source for many aquatic species. Pools are characterized by minimal flows, with relatively deep water and winter/summer refuge habitat for aquatic species. Runs are moderately shallow, with unagitated surfaces of water and areas where the thalweg (deepest part of the channel) is in the center of the channel. Figure 26 shows that Rudsdale Creek is highly variable; 100 percent of sections recorded runs, 58 percent pools and 21 percent riffles. Figure 27 shows where the riffle habitat areas were observed along Rudsdale Creek.
Figure 26 Instream morphology along Rudsdale Creek
Figure 27 Instream riffle habitat along Rudsdale Creek
3.3.5 Vegetation Type
Instream vegetation provides a variety of functions and is a critical component of the aquatic ecosystem. Aquatic plants promote stream health by:
- Providing direct riparian/instream habitat
- Stabilizing flows reducing shoreline erosion
- Contributing to dissolved oxygen through photosynthesis
- Maintaining temperature conditions through shading
For example emergent plants along the shoreline can provide shoreline protection from wave action and important rearing habitat for species of waterfowl. Submerged plants provide habitat for fish to find shelter from predator fish while they feed. Floating plants such as water lilies shade the water and can keep temperatures cool while reducing algae growth. Submerged and floating plants plants were present in 94 percent of the survey sections, 70 percent of sections contained algae, narrow leaved emergents were observed in 67 percent of sections, 61 percent free floating plants, 15 percent broad leaved emergents and robust emergents were observed in 12 percent of sections surveyed. Figure 28 depicts the plant community structure for Rudsdale Creek. Figure 29 shows the dominant vegetation type observed for each section surveyed along Rudsdale Creek.
Figure 28 Vegetation type along Rudsdale Creek
Figure 29 Dominant vegetation type along Rudsdale Creek
3.3.6 Instream Vegetation Abundance
Instream vegetation is an important factor for a healthy stream ecosystem. Vegetation helps to remove contaminants from the water, contributes oxygen to the stream, and provides habitat for fish and wildlife. Too much vegetation can also be detrimental. Figure 30 demonstrates that Rudsdale Creek reach had normal to common levels of vegetation recorded at 24 and 70 percent of stream surveys. Extensive levels of vegetation were observed in 82 percent of the surveyed sections and were consistent with areas dominated by the invasive aquatic plant known as European frogbit; while six percent of sections had no vegetation.
Figure 30 Instream vegetation abundance along Rudsdale Creek
3.3.7 Invasive Species
Invasive species can have major implications on streams and species diversity. Invasive species are one of the largest threats to ecosystems throughout Ontario and can out compete native species, having negative effects on local wildlife, fish and plant populations. One hundred percent of the sections surveyed along Rudsdale Creek reach had invasive species. The invasive species observed in Rudsdale Creek were European frogbit, Himalayan balsam, purple loosestrife and Manitoba maple. Invasive species abundance (i.e. the number of observed invasive species per section) was assessed to determine the potential range/vector of many of these species (Figure 31).
Figure 31 Invasive species abundance along Rudsdale Creek
A section of Rudsdale Creek with the invasive European Frogbit
3.3.8 Water Chemistry
During the stream characterization survey, a YSI probe is used to collect water chemistry information. Dissolved oxygen (DO), specific conductivity (SPC) and pH are measured at the start and end of each section.
188.8.131.52 Dissolved Oxygen
Dissolved oxygen is a measure of the amount of oxygen dissolved in water. The Canadian Environmental Quality Guidelines of the Canadian Council of Ministers of the Environment (CCME) suggest that for the protection of aquatic life the lowest acceptable dissolved oxygen concentration should be 6 mg/L for warmwater biota and 9.5 mg/L for coldwater biota (CCME, 1999). Figure 32 shows that the dissolved oxygen in Rudsdale Creek supports warmwater and in certain locations coldwater biota along the system. The average dissolved oxygen level observed within Rudsdale Creek was 4.4mg/L which is below the recommended level for warmwater biota. The upper reaches of Rudsdale Creek were within the threshold to support warmwater biota.
Figure 32 Dissolved oxygen ranges along Rudsdale Creek
Conductivity in streams is primarily influenced by the geology of the surrounding environment, but can vary drastically as a function of surface water runoff. Currently there are no CCME guideline standards for stream conductivity; however readings which are outside the normal range observed within the system are often an indication of unmitigated discharge and/or stormwater input. The average conductivity observed within the main stem of Rudsdale Creek was 462.3 µs/cm. Figure 33 shows the conductivity readings for Rudsdale Creek.
Figure 33 Specific conductivity ranges in Rudsdale Creek
Based on the PWQO for pH, a range of 6.5 to 8.5 should be maintained for the protection of aquatic life. Average pH values along Rudsdale Creek averaged 7.37 thereby meeting the provincial standard (Figure 34).
Figure 34 pH ranges along Rudsdale Creek
184.108.40.206 Oxygen Saturation (%)
Oxygen saturation is measured as the ratio of dissolved oxygen relative to the maximum amount of oxygen that will dissolve based on the temperature and atmospheric pressure. Well oxygenated water will stabilize at or above 100% saturation, however the presence of decaying matter/pollutants can drastically reduce these levels. Oxygen input through photosynthesis has the potential to increase saturation above 100% to a maximum of 500%, depending on the productivity level of the environment. In order to represent the relationship between concentration and saturation, the measured values have been summarized into 6 classes:
Dissolved oxygen conditions on Rudsdale Creek varied along the system for both warm and coolwater species (upper reach) (Figure 35). Sections in the lower reaches fell below the guideline to support warmwater biota.
Figure 35 A bivariate assessment of dissolved oxygen concentration (mg/L) and saturation (%) in Rudsdale Creek
220.127.116.11 Specific Conductivity Assessment
Specific conductivity (SPC) is a standardized measure of electrical conductance, collected at or corrected to a water temperature of 25⁰C. SPC is directly related to the concentration of ions in water, and is commonly influenced by the presence of dissolved salts, alkalis, chlorides, sulfides and carbonate compounds. The higher the concentration of these compounds, the higher the conductivity. Common sources of elevated conductivity include storm water, agricultural inputs and commercial/industrial effluents.
In order to summarize the conditions observed, SPC levels were evaluated as either normal, moderately elevated or highly elevated. These categories correspond directly to the degree of variation (i.e. standard deviation) at each site relative to the average across the system.
Normal levels were maintained in the upper reaches of Rudsdale Creek, however there were moderately elevated areas in the middle and lower reaches (Figure 36).
Figure 36 Relative specific conductivity levels along Rudsdale Creek
3.3.9 Thermal Regime
Many factors can influence fluctuations in stream temperature, including springs, tributaries, precipitation runoff, discharge pipes and stream shading from riparian vegetation. Water temperature is used along with the maximum air temperature (using the Stoneman and Jones method) to classify a watercourse as either warm water, cool water or cold water. Figure 37 shows where the thermal sampling sites were located on Rudsdale Creek. Analysis of the data collected indicates that Rudsdale Creek is classified as a cool water system with warm water lower reaches (Figure 38).
Figure 37 Temperature logger locations along Rudsdale Creek
Figure 38 Temperature logger data for the sites on Rudsdale Creek
Each point on the graph represents a temperature that meets the following criteria:
Sampling dates between July 1st and September 7th
Sampling date is preceded by two consecutive days above 24.5 °C, with no rain
Water temperatures are collected at 4pm
Air temperature is recorded as the max temperature for that day
Groundwater discharge areas can influence stream temperature, contribute nutrients, and provide important stream habitat for fish and other biota. During stream surveys, indicators of groundwater discharge are noted when observed. Indicators include: springs/seeps, watercress, iron staining, significant temperature change and rainbow mineral film. Figure 39 shows areas where one or more of the above groundwater indicators were observed during stream surveys and headwater assessments.
Figure 39 Groundwater indicators observed in the Rudsdale Creek catchment
3.3.11 Fish Community
The Rudsdale Creek catchment is classified as a mixed community of warm and cool water recreational and baitfish fishery with 23 species observed in 2016. Figure 40 shows the historical and 2016 fish sampling locations in the catchment.
Figure 40 Fish Community sampling observations for 2016
Table 7 lists the species observed in the watershed historically and during the 2016 sampling effort.
Fish species observed in Rudsdale Creek
RVCA electrosfishing site on Rudsdale Creek
Iowa darter captured during the electrofishing sampling effort
3.3.12 Migratory Obstructions
It is important to know locations of migratory obstructions because these can prevent fish from accessing important spawning and rearing habitat. Migratory obstructions can be natural or manmade, and they can be permanent or seasonal. Figure 41 shows that Rudsdale Creek had no migration barriers at the time of the survey in 2016. However, there were two perched culverts and one debris dam on headwater drainage features within the catchment.
Figure 41 Migratory obstructions in the Rudsdale Creek catchment
3.3.13 Beaver Dam Locations
Overall beaver dams create natural changes in the environment. Some of the benefits include providing habitat for wildlife, flood control, and silt retention. Additional benefits come from bacterial decomposition of woody material used in the dams which removes excess nutrient and toxins. Beaver dams can also result in flooding of agricultural lands and may be potential barriers to fish migration. Six beaver dams were identified along Rudsdale Creek in 2016 (Figure 42).
Figure 42 Beaver Dam type and locations along Rudsdale Creek
Beaver Dam on Rudsdale Creek at the time of the survey in 2016
3.4 Headwater Drainage Feature Assessment
3.4.1 Headwaters Sampling Locations
The RVCA Stream Characterization program assessed Headwater Drainage Features for the Rudsdale Creek catchment in 2017. This protocol measures zero, first and second order headwater drainage features (HDF). It is a rapid assessment method characterizing the amount of water, sediment transport, and storage capacity within headwater drainage features (HDF). RVCA is working with other Conservation Authorities and the Ministry of Natural Resources and Forestry to implement the protocol with the goal of providing standard datasets to support science development and monitoring of headwater drainage features. An HDF is a depression in the land that conveys surface flow. Additionally, this module provides a means of characterizing the connectivity, form and unique features associated with each HDF (OSAP Protocol, 2013). In 2017 the program sampled 32 sites at road crossings in the Rudsdale Creek catchment area (Figure 43).
Figure 43 Location of the headwater sampling sites in the Rudsdale Creek catchment
3.4.2 Headwater Feature Type
The headwater sampling protocol assesses the feature type in order to understand the function of each feature. The evaluation includes the following classifications: defined natural channel, channelized or constrained, multi-thread, no defined feature, tiled, wetland, swale, roadside ditch and pond outlet. By assessing the values associated with the headwater drainage features in the catchment area we can understand the ecosystem services that they provide to the watershed in the form of hydrology, sediment transport, and aquatic and terrestrial functions. The headwater drainage features in the Rudsdale Creek catchment are highly variable they include natural, wetland, channelized, road side ditches and a multi thread feature. Figure 44 shows the feature type of the primary feature at the sampling locations.
Figure 44 Headwater feature types in the Rudsdale Creek catchment
3.4.3 Headwater Feature Flow
The observed flow condition within headwater drainage features can be highly variable depending on timing relative to the spring freshet, recent rainfall, soil moisture, etc. Flow conditions are assessed in the spring and in the summer to determine if features are perennial and flow year round, if they are intermittent and dry up during the summer months or if they are ephemeral systems that do not flow regularly and generally respond to specific rainstorm events or snowmelt. Flow conditions in headwater systems can change from year to year depending on local precipitation patterns. Figure 45 shows the observed flow condition at the sampling locations in the Rudsdale Creek catchment in 2017.
Figure 45 Headwater feature flow conditions in the Rudsdale Creek catchment
A spring photo of the headwater sample site in the Rudsdale Creek catchment located on Gambles Side Road
A summer photo of the headwater sample site in the Rudsdale Creek catchment located on Gambles Side Road
3.4.4 Feature Channel Modifications
Channel modifications were assessed at each headwater drainage feature sampling location. Modifications include channelization, dredging, hardening and realignments. The Rudsdale Creek catchment area had a majority of features with no channel modifications observed, five sites as having been historically dredged/channelized and one location had mixed modifications. Figure 46 shows the channel modifications observed at the sampling locations for Rudsdale Creek.
Figure 46 Headwater feature channel modifications in the Rudsdale Creek catchment
3.4.5 Headwater Feature Vegetation
Headwater feature vegetation evaluates the type of vegetation that is found within the drainage feature. The type of vegetated within the channel influences the aquatic and terrestrial ecosystem values that the feature provides. For some types of headwater features the vegetation within the feature plays a very important role in flow and sediment movement and provides wildlife habitat. The following classifications are evaluated no vegetation, lawn, wetland, meadow, scrubland and forest. Figure 47 depicts the dominant vegetation observed at the sampled headwater sites in the Rudsdale Creek catchment.
Figure 47 Headwater feature vegetation types in the Rudsdale Creek catchment
3.4.6 Headwater Feature Riparian Vegetation
Headwater riparian vegetation evaluates the type of vegetation that is found along the adjacent lands of a headwater drainage feature. The type of vegetation within the riparian corridor influences the aquatic and terrestrial ecosystem values that the feature provides to the watershed. Figure 48 depicts the type of riparian vegetation observed at the sampled headwater sites in the Rudsdale Creek catchment.
Figure 48 Headwater feature riparian vegetation types in the Rudsdale Creek catchment
3.4.7 Headwater Feature Sediment Deposition
Assessing the amount of recent sediment deposited in a channel provides an index of the degree to which the feature could be transporting sediment to downstream reaches (OSAP, 2013). Evidence of excessive sediment deposition might indicate the requirement to follow up with more detailed targeted assessments upstream of the site location to identify potential best management practices to be implemented. Sediment deposition ranged from none to substantial for the headwater sites sampled in the Rudsdale Creek catchment area. Figure 49 depicts the degree of sediment deposition observed at the sampled headwater sites in the Rudsdale Creek catchment. Sediment deposition conditions ranged from no sediment deposition to substantial.
Figure 49 Headwater feature sediment deposition in the Rudsdale Creek catchment
3.4.8 Headwater Feature Upstream Roughness
Feature roughness will provide a measure of the amount of materials within the bankfull channel that could slow down the velocity of water flowing within the headwater feature (OSAP, 2013). Materials on the channel bottom that provide roughness include vegetation, woody Structure and boulders/cobble substrates. Roughness can provide benefits in mitigating downstream erosion on the headwater drainage feature and the receiving watercourse by reducing velocities. Roughness also provides important habitat conditions for aquatic organisms. Figure 50 shows the feature roughness conditions at the sampling locations in the Rudsdale Creek catchment were highly variable ranging from minimal to extreme.
Figure 50 Headwater feature roughness in the Rudsdale Creek catchment