Sediment Budget Research

Data on the Jack River

Collecting integrated sampler at Jack River following the 2009-2010 wet season. (Photo: John

Overview: An Empirically-based Sediment Budget for the Normanby Basin

Why was this research necessary?

Located at the northern end of the Great Barrier Reef, the Normanby Basin plays a major role in determining the health of the ecosystems in Princess Charlotte Bay, part of the GBR "lagoon".

Sediment downloadUntil this study very few attempts had been made to measure the sediments being deposited in the Bay. Scientists and policy makers only had models and a scattering of data samples on which to base their understanding of how the Basin actually works.

On-ground research and an improved model were necessary in order to make better decisions about land management, rehabilitation, conservation, and new development. This research has delivered a new model, supported by multiple lines of empirical evidence.

(see Main Report 1.1: Normanby Basin in Context for more info)

Who funded this research?

Main funding was provided by the Australian Government, through the Caring for Our Country programme, under the Reef Rescue Plan.

What were the core research questions?

The research addresses the following questions:

  1. What is the proportional contribution of suspended sediment from eastern Cape York rivers to the GBR lagoon compared with the rest of the GBR catchments?
  2. To what extent are the contemporary sediment loads from this area elevated above pre-European levels?
  3. Which sub-catchments or stream segments are disproportionately contributing to the total sediment load?
  4. Of the current key sediment sources, which ones are elevated as a result of land-use intensification, and can anything be done to practically reduce the supply of sediment from these sources?

(see Main Report 1.2 Core Research Questions: Key Objectives and Approach for more info)

How did the research answer the core questions?

1. Our data confirm that the Normanby Catchment is a major contributor of sediment to the Great Barrier Reef Lagoon. Our data are in general agreement with previous predictions of the sediment loads flowing from the upper catchment.

Importantly, however, our research shows that these loads come from entirely different sources than was previously thought. The new model will help land managers make much more effective decisions than in the past.

In addition, we have identified a coastal/floodplain source that is in the order of 4 times greater than the upper catchment derived sources. This finding highlights the urgent need for further research now that the upper catchment is better understood.

2. It is still not easy to determine the extent to which the catchment sediment loads are elevated above ‚Äúpre-European‚ÄĚ levels. What we can say is that the previous models, which predicted a 5-fold increase in sediment loads, are not accurate. Using air photos and stratigraphic evidence, our work does show a catchment-wide acceleration of gully erosion within the last 100 years or so, and this can be tied to the introduction of cattle into the catchment.

3. Sediment load flowing into the Bay can be roughly identified as coming from the upper catchment or the lower catchment. The amount of sediment originating in the lower catchment is about 4 times larger than what originates in the upper catchment.

In the upper catchment, alluvial and colluvial gully erosion are major sources of sediment. We have mapped these areas across the catchment, and have identified several large concentrations, specifically on the Granite Normanby River, near the East and West Normanby River confluence, and the Laura River immediately upstream of Crocodile Gap. These areas could be targeted to reduce sediment yields through passive and active gully rehabilitation measures.

4. Alluvial gully erosion has accelerated since European settlement, through overgrazing cattle and soil disturbance on the sodic floodplain soils of river frontages. Some of these areas could be targeted with management actions to reduce sediment yields through passive and active gully rehabilitation measures.

Roads and fencelines are often associated with erosion processes. Although they are individually small, localised effects, their cumulative impact is significant. There is plenty of room for improvement in their design and implementation.

(see Main Report 1.4 Summary Response to Research Questions for more info)

What are the main recommendations coming from the research?

We put forward 12 main recommendations, each of which is achievable. Together, they contribute to building a better future for the Normanby basin and the people who call it home.

1.5.01    Empirical data must provide the foundation to the models
1.5.02    RUSLE-based models merit special scrutiny
1.5.03    Invest in gully rehabilitation/restoration research and works
1.5.04    Clarify the mechanisms and extent of land use impacts
1.5.05    Focus on erosion and sedimentation dynamics in the lower catchment
1.5.06    Acquire additional flood plume geochemical tracing
1.5.07    Undertake direct measurement of sedimentation on surrounding reefs
1.5.08    Develop a better understanding of land use drivers of bank erosion in small alluvial channels
1.5.09    Develop a PCB sediment sink mass balance
1.5.10    Analyse gauge flow and sediment bypass around Kalpowar
1.5.11    Establish and improve the collection of hydrological data, especially time-series
1.5.12    Additional key recommendations with implications beyond the Normanby

(see Main Report 1.5 Conclusions and Recommendations for more info)