Goulburn Mulwaree

Indicator: Land Degradation

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What the results tell us for Goulburn Mulwaree

For the 2004-08 reporting period, existing salinity hazards are limited to one area with little increase in extent expected for the short-term. Drought was experienced throughout the Council area for much of the period with some relief towards the end of the reporting period. Landuse in the Council area 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 Goulburn Mulwaree tended to be suitable for the 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 Goulburn Mulwaree Council area

Figure 1. Landuse within Goulburn-Mulwaree Council areaKey for Figure 1. Landuse within Goulburn-Mulwaree Council area

Source: NSW Department of Lands 2008

Some 55% of land within the Council area is classed as suitable for grazing of which 96% 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 Water and Energy).

About 0.1% of the Council area is under cropping, of which none is suitable for its soil type for reasons of either climatic conditions or future soil degradation (CSIRO 2003).

All rural residential landuse is suitable to the location (Goulburn Mulwaree Council - State of Environment Report (2004)).

Table 1. Area (ha) of landuse types within each land capability class in Goulburn Mulwaree Council area
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
Cropping 0.1 9 4 13
Estimated grazing 584 895 97,688 49,592 20,757 7,348 317
Horticulture 110 4 0.1
Mixed farming 0.1 1 0.5 0.2
Rural residential 144 170 56
Totals (hectares) 584 1,005 97,846 49,767 20,826 7,348 317

 

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). The surveys revealed 950km of gully erosion and 260km streambank erosion (refer Table 2). Minor to severe sheet erosion was present throughout the Council area (refer Table 3).

Gully erosion was predominately classed as minor to moderate with gullies less than 3m 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. In New South Wales (NSW), the estimated overall accelerated erosion rate are 10–50 times the natural rates (Edwards and Zierholz, 2001).

Figure 2. Degree of erosion within Goulburn Mulwaree Council area

Figure 2. Degree of erosion within Goulburn Mulwaree Council areaKey for Figure 2. Degree of erosion within Goulburn Mulwaree Council area

Source: NSW Department of Lands 2008

Table 2. Gully and streambank erosion in Goulburn Mulwaree Council area (prior to the current reporting period)
Erosion type Depth Kilometres
Extreme gully erosion 3 to 6m deep 33
1.5 to 3m deep 56
less than 1.5m deep 26
Extreme gully erosion total 115
Severe gully erosion 3 to 6m deep 17
1.5 to 3m deep 119
less than 1.5m deep 72
Severe gully erosion total 208
Moderate gully erosion 3 to 6m deep 2
1.5 to 3m deep 84
less than 1.5m deep 192
Moderate gully erosion total 278
Minor gully erosion 3 to 6m deep 2
1.5 to 3m deep 42
less than 1.5m deep 308
Minor gully erosion total 352
Streambank erosion 3 to 6m deep 15
1.5 to 3m deep 66
less than 1.5m deep 177
Streambank erosion total 258

 

Table 3. Types of erosion (excluding gully erosion) in Goulburn Mulwaree Council area (prior to the current reporting period)
Major erosion type Degree / type Hectares
Mass movement rock debris avalanche 67
Rill erosion extreme rill erosion 1,012
severe rill erosion 620
moderate rill erosion 201
minor rill erosion 30
Sheet erosion extreme sheet erosion 990
severe sheet erosion 17,959
moderate sheet erosion 49,664
minor sheet erosion 119,096

 

Salinity

Soil salinity is relatively limited in the Goulburn Mulwaree Council area with only one small (~16km2) region approximately 15km west of Goulburn city (refer Figure 3 and 4). The extent of soil salinity is forecast to remain relatively steady with only a <10km2 increase in the vicinity of the affected area.

Figure 3. Extent of salinity (2000)

Figure 3. Extent of salinity (2000) Figure 4. Forecast extent of salinity (2050)

Source: Australian National Resource Atlas 2001

 

Figure 4. Forecast extent of salinity (2050)

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 to nutrient depletion or fertiliser use by agriculture.

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 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’. This includes most of Goulburn Mulwaree Council area (refer Figure 5).

Figure 5. Drought declared areas (as of September 2008)

Figure 5. Drought declared areas (as of September 2008)

Source: NSW Department of Primary Industries 2008

Goulburn Rural Land Protection Board rated the Goulburn Mulwaree Council area to be in drought for much of the reporting period, however, for the last reporting year condition appears 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.

Table 4. Drought conditions for the Goulburn Mulwaree Council area, July 2004—June 2008
Months Seasonal Conditions
September 2004 Drought
December 2004 Satisfactory
March 2005 Satisfactory
June 2005 Drought
September 2005 Marginal
December 2005 Satisfactory
March 2006 Satisfactory
June 2006 Drought
September 2006 Drought
December 2006 Drought
March 2007 Drought
June 2007 Drought
September 2007 Drought
December 2007 Drought
March 2008 Drought
June 2008 Drought

 

Figure 6. Pasture growth in the Goulburn Mulwaree Council area for the period 2004 to 2008

Figure 6. Pasture growth in the Goulburn Mulwaree Council area for the period 2004 to 2008

 

What is being done to improve land condition?

Goulburn Mulwaree Council actively supports Goulburn City Landcare. To alleviate or reverse land degradation and increase awareness Goulburn City Landcare has undertaken activities to improve the river corridors on the Wollondilly, weed elimination, and community river environment awareness programs.

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 2000/04 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

Australian Water Resources (2000) National Land and Water Audit. www.nlwra.gov.au/

Australian Water Resources (2005) Land Salinity Maps. www.nlwra.gov.au/

AWR - see Australian Water Resources

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/.

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 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

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.

Goulburn Mulwaree Council ^Annual Report 2006/2007 `http://www.goulburn.nsw.gov.au/council/1124/5596.html

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

 

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