Eurobodalla
Indicator: Land Degradation
Results for this indicator are also available for [an error occurred while processing this directive]
What the results tell us for Eurobodalla
For the 2004-08 reporting period, existing salinity hazards are limited to two small areas with no increase in extents anticipated. Drought was experienced throughout the Shire for much of the period with some relief towards the end of the reporting period. Landuse in the Shire remained largely compatible with its capability class. Since the last reporting period there has been no noteworthy data released on erosion, acidic or sulphate soils.
Sustainability of landuse
See also: Landuse
Landuse within the Eurobodalla Shire tended to be suitable land capability class (refer Figure 1 and Table 1). Approximately 2% of land in use is vulnerable to erosion because of unsuitable practices.
Figure 1. Landuse within Eurobodalla Shire
Source: NSW Department of Lands 2008
Some 9% of land within the Shire is classed as suitable for grazing of which 90% of this land is used in this manner. The remaining land is considered at high risk of erosion if cleared and is recommended to be revegetated (Department of Lands).
Around 9% of the Shire is under cropping of which 83% of this land was not suitable for reasons of either climatic conditions or future soil degradation (CSIRO 2003).
About 6% of the Shire is used for rural residential, the majority of which was not suitable for cultivation. (Eurobodalla Shire Council - State of Environment Report (2004)).
| Landuse | Land Capability Class | |||||||
|---|---|---|---|---|---|---|---|---|
| Lands suitable for regular cultivation | Lands suitable for grazing—occasional cultivation | Lands suitable for grazing—no cultivation | Other lands | |||||
| I | II | III | IV | V | VI | VII | VIII | |
| Cropping | 530 | 2,052 | 245 | 277 | 19 | 22 | ||
| Estimated grazing | 2,559 | 15,449 | 1,005 | 7,197 | 2,212 | 1,089 | ||
| Horticulture | 372 | 82 | 1 | |||||
| Rural residential | 61 | 2,944 | 15 | 1,563 | 368 | 22 | ||
| Totals (ha) | 3,522 | 20,526 | 1,265 | 9,038 | 2,599 | 1,133 | ||
Note: the areas in Table 1 relate to the 12 percent of agricultural land within the Shire.
Types of land degradation
Erosion
Soil erosion data was restricted to surveys carried out between 1985 and 1992 (refer Figure 1 and Tables 2 and 3). Note: data made available for Figure 1 contains errors and has not rendered erosion correctly for the entire Shire. The surveys revealed 19 km of gully erosion and 145 km streambank erosion (refer Table 2). Minor to severe sheet erosion was present throughout the Shire (refer Table 3).
Gully erosion was predominately classed as minor to moderate with gullies less than 3.0m deep (Table 2), most of which was caused soon after the original native vegetation was removed. Gully lengths have since stabilised however accelerated erosion continues as is revealed by the high sediment loads to streams (Hughes and Prosser 2003). In New South Wales (NSW) the estimated overall accelerated erosion rate is 10–50 times the natural rates (Edwards and Zierholz 2001).
Figure 2. Degree of erosion within the Eurobodalla Shire
Source: NSW Department of Lands 2008
| Erosion type | Depth | Kilometres |
|---|---|---|
| Erosion of farm tracks | Some linear features on south coast depict eroded tracks caused by intensive animal activity. | 1 |
| Extreme gully erosion | greater than 6m deep | 7 |
| 3 to 6m deep | 4 | |
| 1.5 to 3m deep | 1 | |
| less than 1.5m deep | 0.06 | |
| Extreme gully erosion total | 12 | |
| Severe gully erosion | 3 to 6m deep | 0.4 |
| 1.5 to 3m deep | 0.5 | |
| Severe gully erosion total | 0.9 | |
| Moderate gully erosion | 1.5 to 3m deep | 0.4 |
| less than 1.5m deep | 4 | |
| Moderate gully erosion total | 4 | |
| Minor gully erosion | less than 1.5m deep | 2 |
| Streambank erosion | greater than 6m deep | 0.9 |
| 3 to 6m deep | 7 | |
| 1.5 to 3m deep | 7 | |
| less than 1.5m deep | 130 | |
| Streambank erosion total | 145 |
| Major erosion type | Degree / type | Hectares |
|---|---|---|
| Mass movement | rock debris avalanche | 14 |
| soil debris avalanche | 11 | |
| Rill erosion | extreme rill erosion | 14 |
| severe rill erosion | 17 | |
| moderate rill erosion | 5 | |
| minor rill erosion | 23 | |
| Sheet erosion | extreme sheet erosion | 509 |
| severe sheet erosion | 410 | |
| moderate sheet erosion | 18,078 | |
| minor sheet erosion | 75,652 | |
| Wind Erosion | extreme wind erosion | 95 |
| severe wind erosion | 44 | |
| moderate wind erosion | 33 | |
| minor wind erosion | 41 |
Salinity
Soil salinity is relatively limited in the Eurobodalla Shire. There are only two known sites - a ~5km2 area near Garlandtown and a smaller site (<2km2) near Turlinjah. Forecasts to the year 2050 do not indicate soil salinity extending beyond the current extents (refer Figure 2 and 3).
Figure 3. Extent of salinity (2000)
Source: Australian National Resource Atlas 2001
Figure 4. Forecast extent of salinity (2050)
Source: Australian National Resource Atlas 2001
Acid soils
Soil acidity can have an impact through reducing crop yields, and affecting perennial pastures, ground water quality and inturn increasing soil erosion and salinity (Upjohn et al., 2005). In rural Australia, soil acidity is usually associated with nutrient depletion or fertiliser use by agriculture.
In Eurobodalla Shire, soil classed as strongly acid covered approximately 84% of the district. Distribution was throughout the Shire with some interruption to the north-east. A further 8% of the Shire is classed as slightly acidic (DLWC 2002a and b).
Figure 5. Soil acidity in Eurobodalla Shire
Source: NSW Department of Primary Industries 2008
Causes of land degradation
Land degradation can be caused directly by human activities, such as land clearing, over use of fertiliser and changing water tables. Indirect influences, can include flooding of overgrazed or over cultivated land with little ground cover and erosion by wind and water. Drought breaking rain may also cause erosion and can make up about 90% of the total soil loss in an area in a 20–30 year cycle (DPI 2005).
Drought and vegetation condition
According to a recent study by the Bureau of Meteorology (BoM) and the Commonwealth Scientific and Industrial Research Organisation (CSIRO) (BoM, CSIRO 2008) the frequency and extent of exceptionally hot years and exceptionally dry years in NSW are likely to increase in the future. The mean projections indicate that:
- by 2010-2040, exceptionally hot years are likely to affect about 60% of the region, and occur every 1.6 years on average;
- by 2010-2040, no change is likely in the frequency or areal extent of exceptionally low rainfall years;
- by 2030, exceptionally low soil moisture years are likely to affect about 7% of the region and occur about once every 14 years on average.
As of September 2008 the Department of Primary Industry has classed 71.6% of NSW as ‘In drought’. Eurobodalla Shire is considered ‘marginal’ (refer Figure 6).
Figure 6. Drought declared areas (as of September 2008)
Source: NSW Department of Primary Industries 2008
South Coast Rural Land Protection Board rated the Eurobodalla Shire to be in drought for much of the reporting period, however, for the last reporting year condition appear to have generally improved (refer Table 4)(DPI 2008). Figure 6 illustrates the impact of the drought on pasture growth for the area (NAMS 2008). Pasture growth reached 0% during the 2007 summer but made a steady recovery with the break in drought conditions late in the same year.
| Months | Seasonal Conditions |
|---|---|
| September 2004 | Drought |
| December 2004 | Drought |
| March 2005 | Marginal |
| June 2005 | 50% satisfactory, 50% marginal |
| September 2005 | 30% satisfactory, 70% marginal |
| December 2005 | Satisfactory |
| March 2006 | Marginal |
| June 2006 | Drought |
| September 2006 | Drought |
| December 2006 | Drought |
| March 2007 | Marginal |
| June 2007 | Satisfactory |
| September 2007 | Satisfactory |
| December 2007 | Marginal |
| March 2008 | Satisfactory |
| June 2008 | Marginal |
Figure 7. Pasture growth in the Eurobodalla Shire for the period 2004 to 2008
What is being done to improve land condition?
Over the reporting period Eurobodalla Shire Council has undertaken a wide range of estuary and riverine projects. Many of these projects are aimed at addressing land degradation issues, particularly where they are impacting on areas of high biodiversity value or water quality. Estuary Management Plans are used to prioritise these projects. Details of some projects can be retrieved from Annual State of the Environment Reports
Eurobodalla Shire Council also actively supports Eurobodalla Landcare. To alleviate or reverse land degradation, Eurobodalla Landcare has undertaken the following projects:
- Extension of Capacity Planning Project to on-ground
- Deua River Habitat Linkage Restoration and Erosion
- Repairing a wildlife corridor and vulnerable vegetation
- Riparian Revegetation and Riverbank Stabilisation in Moruya District
- Kyla Park Rehabilitation Project
- Travelling Environmental Education Stall
About the data
For the current reporting period there has been a lack of new soil data due to the relatively long intervals between studies. Given the relevancy of the information in the 2000-2004 report, some sections have been retained for this report. Where material has been used from the Supplementary Report reference has been given to the report and original source.
References
Australian National Resource Atlas Mapmaker facility http://www.anra.gov.au/mapmaker/mapservlet?app=anra
AWR - Australian Water Resources
Australian Water Resources (2000) National Land and Water Audit. www.nlwra.gov.au/
Australian Water Resources (2005) Land Salinity Maps. www.nlwra.gov.au/
Australian National Resource Atlas Mapmaker facility http://www.anra.gov.au/mapmaker/mapservlet?app=anra
BoM and CSIRO – see Bureau of Meteorology and the Commonwealth Scientific and Industrial Research Organisation
Bureau of Meteorology and the Commonwealth Scientific and Industrial Research Organisation (2008) An Assessment of the Impact of Climate Change on the Nature and Frequency of Exceptional Climatic Event.
Commonwealth of Australia (2005) National Action Plan for Salinity and Water Quality and Natural Heritage Trust Regional Programs Report 2003–04, Departments of the Environment and Heritage and Agriculture, Fisheries and Forestry, viewed 18 April 2005, http://www.nrm.gov.au/publications/regional-report/03-04/.
Eurobodalla Shire Council Annual Report 2006/2007,http://www.esc.nsw.gov.au/plans/documents/archive/ARIndex.html
CRCCH—see Cooperative Research Centre for Catchment Hydrology
Department of Infrastructure, Planning and Natural Resources, NSW (2004a) 2003/04 Combined NSW Catchment Management Authorities Annual Report, Volume 1: CMA Activities and Achievements, Department of Infrastructure, Planning and Natural Resources, Sydney.
Department of Infrastructure, Planning and Natural Resources, NSW (2005) Meeting the Challenge: NSW Salinity Strategy Premier's Annual Report 2003–04. NSW Department of Infrastructure, Planning and Natural Resources, viewed 12 May 2006, http://www.dlwc.nsw.gov.au/salinity/pdf/2003_2004_salinity_annual_report.pdf
Department of Land and Water Conservation (NSW) (1999) Groundwater Quality Protection Policy, Department of land and Water Conservation, Sydney, on line at http://www.dnr.nsw.gov.au/water/pdf/nsw_state_groundwater_quality_policy.pdf.
Department of Land and Water Conservation, NSW (2000) Taking on the Challenge: The NSW Salinity Strategy, Department of Infrastructure, Planning and Natural Resources, viewed 4 May 2006, http://www.dlwc.nsw.gov.au/salinity/government/govt-docs.htm.
Department of Land and Water Conservation, NSW (2002) Soil Acidification Hazard Mapping, produced for the 2003 NSW State of the Environment Report, Department of Land and Water Conservation, Parramatta.
Department of Lands NSW (2008) Soil Landscape Mapping Program – Soil and Landscape Qualities and Limitations http://www.naturalresources.nsw.gov.au/care/soil/ssu/quals4.htm
Department of Primary Industries, NSW (2005) Soil Management Following Drought, Agnote DPI 355, Third Edition, Department of Primary Industries, viewed 18 April 2006, http://www.agric.nsw.gov.au/reader/pasture-crops-recovery/dpi355.htm.
Department of Primary Industries, NSW (2006) Drought maps—areas of NSW suffering drought conditions, Department of Primary Industries, viewed 8 May 2006, http://www.agric.nsw.gov.au/reader/drt-area?picQuant=100.
Department of Primary Industries, NSW (2008) Drought maps and drought assistance eligibility status of RLPBs http://www.dpi.nsw.gov.au/agriculture/emergency/drought/situation/drought-maps
Department of Primary Industries, NSW (2008) Drought maps and drought assistance eligibility status of RLPBs http://www.dpi.nsw.gov.au/agriculture/emergency/drought/situation/drought-maps
DIPNR—see Department of Infrastructure, Planning and Natural Resources, NSW
DLWC—see Department of Land and Water Conservation, NSW
DPI—see Department of Primary Industries, NSW
Edwards, K and Zierholz, C (2001) Soil Formation and Erosion Rates, in PEV Charman and BW Murphy (eds) Soils: Their Properties and Management, 2nd Edition, pp 39–58, Oxford University Press, Oxford, cited in Lu, H, Prosser, IP, Monn, CJ, Gallant, JC, Priestley, G and Stevenson, JG (2003) Predicting sheetwash and rill erosion over the Australian continent, Australian Journal of Soil Research Vol. 41, 1037–1062, viewed 3 May 2006, http://palaeoworks.anu.edu.au/pubs/AustJSS03.pdf.
Hughes, AO and Prosser, IP (2003) Gully and Riverbank Erosion Mapping for the Murray-Darling Basin, Technical Report 3/03, March 2003, CSIRO Land and Water, Canberra, viewed 26 April 2006, http://www.clw.csiro.au/publications/technical2003/tr3-03.pdf.
Upjohn, B., Fenton, G. and Conyers, M. (2005) Soil Acidity and Liming Agfact AC.19 3rd Edition. NSW Department of Primary Industries, viewed 17 July 2006, http://www.agric.nsw.gov.au/reader/soil-acid/2991-soil-acidity-and-liming-.pdf
